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Sample records for balsas river valley

  1. FLUCTUACIONES ECONÓMICAS PREHISPÁNICAS EN LA CUENCA DEL RÍO BALSAS, MÉXICO (Prehispanic Economic Fluctuations in the Balsas River Basin, Mexico

    Directory of Open Access Journals (Sweden)

    Pascual Izquierdo-Egea

    2014-07-01

    Full Text Available Aplicando el método de valoración contextual al análisis del registro funerario de la cuenca del río Balsas, México, podemos aislar las fluctuaciones económicas y los cambios sociales prehispánicos codificados en la composición de los ajuares mortuorios. Entre los relevantes resultados obtenidos, destaca que el colapso de las antiguas civilizaciones mesoamericanas —Teotihuacan, Monte Albán o la maya clásica— aparezca perfectamente reflejado en las ofrendas de los entierros del periodo Clásico Tardío. ENGLISH: By applying the contextual valuation method to the analysis of the mortuary record in the Balsas River basin, Mexico, we can isolate the prehispanic economic fluctuations and social changes encoded in the composition of grave goods. Among the relevant results obtained, highlights that the collapse of ancient Mesoamerican civilizations (Teotihuacan, Monte Alban and the Maya Classic appears perfectly reflected in the offerings of Late Classic burials.

  2. Mississippi River Valley alluvial aquifer

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This data set represents the extent of the Mississippi River Valley alluvial aquifer in the states of Missouri, Kentucky, Tennessee, Arkansas, Mississippi, and...

  3. Valley evolution by meandering rivers

    Science.gov (United States)

    Limaye, Ajay Brian Sanjay

    Fluvial systems form landscapes and sedimentary deposits with a rich hierarchy of structures that extend from grain- to valley scale. Large-scale pattern formation in fluvial systems is commonly attributed to forcing by external factors, including climate change, tectonic uplift, and sea-level change. Yet over geologic timescales, rivers may also develop large-scale erosional and depositional patterns that do not bear on environmental history. This dissertation uses a combination of numerical modeling and topographic analysis to identify and quantify patterns in river valleys that form as a consequence of river meandering alone, under constant external forcing. Chapter 2 identifies a numerical artifact in existing, grid-based models that represent the co-evolution of river channel migration and bank strength over geologic timescales. A new, vector-based technique for bank-material tracking is shown to improve predictions for the evolution of meander belts, floodplains, sedimentary deposits formed by aggrading channels, and bedrock river valleys, particularly when spatial contrasts in bank strength are strong. Chapters 3 and 4 apply this numerical technique to establishing valley topography formed by a vertically incising, meandering river subject to constant external forcing---which should serve as the null hypothesis for valley evolution. In Chapter 3, this scenario is shown to explain a variety of common bedrock river valley types and smaller-scale features within them---including entrenched channels, long-wavelength, arcuate scars in valley walls, and bedrock-cored river terraces. Chapter 4 describes the age and geometric statistics of river terraces formed by meandering with constant external forcing, and compares them to terraces in natural river valleys. The frequency of intrinsic terrace formation by meandering is shown to reflect a characteristic relief-generation timescale, and terrace length is identified as a key criterion for distinguishing these

  4. A balsa violin

    Science.gov (United States)

    Waltham, Chris

    2009-01-01

    Almost half a century ago John Schelleng determined the scaling rules that show how violins can be made from nontraditional materials. These principles suggest that balsa wood may be a possible, if unlikely, construction material. To test this idea, a balsa violin was constructed and found to be playable. Its vibrational behavior is shown to be in agreement with Schelleng's scaling rules. The instrument was not difficult to build, and its construction can be repeated by anyone of moderate skill with a chisel and sandpaper and access to an audio frequency analysis program. The reward is a tactile appreciation for the vibrational behavior of materials and the physics of musical instruments that is difficult to gain otherwise.

  5. 27 CFR 9.57 - Green Valley of Russian River Valley.

    Science.gov (United States)

    2010-04-01

    ... 27 Alcohol, Tobacco Products and Firearms 1 2010-04-01 2010-04-01 false Green Valley of Russian... Areas § 9.57 Green Valley of Russian River Valley. (a) Name. The name of the viticultural area described in this section is “Green Valley of Russian River Valley”. For purposes of part 4 of this...

  6. 27 CFR 9.66 - Russian River Valley.

    Science.gov (United States)

    2010-04-01

    ... 27 Alcohol, Tobacco Products and Firearms 1 2010-04-01 2010-04-01 false Russian River Valley. 9.66... Russian River Valley. (a) Name. The name of the viticultural area described in this section is “Russian River Valley.” (b) Approved maps. The appropriate maps for determining the boundaries of the...

  7. Fire Management Plan Rappahannock River Valley National Wildlife Refuge 2009

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This plan for Rappahannock River Valley National Wildlife Refuge will provide guidance on a wide range of fire management activities including preparedness,...

  8. Rappahannock River Valley National Wildlife Refuge [Land Status Map

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This map was produced by the Division of Realty to depict landownership at Rappahannock River Valley National Wildlife Refuge. It was generated from rectified...

  9. Biological Profile for Rappahannock River Valley National Wildlife Refuge 2002

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The objectives of the Rappahannock River Valley National Wildlife Refuge are: to preserve and enhance the refuge's lands and water in a manner that will conserve...

  10. Fire Management Plan Rappahannock River Valley National Wildlife Refuge 2009

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This plan for the Rappahannock River Valley National Wildlife Refuge will provide guidance on a wide range of fire management activities including preparedness,...

  11. Skillful seasonal prediction of Yangtze river valley summer rainfall

    Science.gov (United States)

    Li, Chaofan; Scaife, Adam A.; Lu, Riyu; Arribas, Alberto; Brookshaw, Anca; Comer, Ruth E.; Li, Jianglong; MacLachlan, Craig; Wu, Peili

    2016-09-01

    China suffers from frequent summer floods and droughts, but seasonal forecast skill of corresponding summer rainfall remains a key challenge. In this study, we demonstrate useful levels of prediction skill over the Yangtze river valley for summer rainfall and river flows using a new high resolution forecast system. Further analysis of the sources of predictability suggests that the predictability of Yangtze river valley summer rainfall corresponds to skillful prediction of rainfall in the deep tropics and around the Maritime Continent. The associated dynamical signals favor increased poleward water vapor transport from South China and hence Yangtze river valley summer rainfall and river flow. The predictability and useful level of skill demonstrated by this study imply huge potential for flooding and drought related disaster mitigation and economic benefits for the region based on early warning of extreme climate events.

  12. Groundwater quality in the Santa Clara River Valley, California

    Science.gov (United States)

    Burton, Carmen A.; Landon, Matthew K.; Belitz, Kenneth

    2011-01-01

    The Santa Clara River Valley (SCRV) study unit is located in Los Angeles and Ventura Counties, California, and is bounded by the Santa Monica, San Gabriel, Topatopa, and Santa Ynez Mountains, and the Pacific Ocean. The 460-square-mile study unit includes eight groundwater basins: Ojai Valley, Upper Ojai Valley, Ventura River Valley, Santa Clara River Valley, Pleasant Valley, Arroyo Santa Rosa Valley, Las Posas Valley, and Simi Valley (California Department of Water Resources, 2003; Montrella and Belitz, 2009). The SCRV study unit has hot, dry summers and cool, moist winters. Average annual rainfall ranges from 12 to 28 inches. The study unit is drained by the Ventura and Santa Clara Rivers, and Calleguas Creek. The primary aquifer system in the Ventura River Valley, Ojai Valley, Upper Ojai Valley, and Simi Valley basins is largely unconfined alluvium. The primary aquifer system in the remaining groundwater basins mainly consists of unconfined sands and gravels in the upper portion and partially confined marine and nonmarine deposits in the lower portion. The primary aquifer system in the SCRV study unit is defined as those parts of the aquifers corresponding to the perforated intervals of wells listed in the California Department of Public Health (CDPH) database. Public-supply wells typically are completed in the primary aquifer system to depths of 200 to 1,100 feet below land surface (bls). The wells contain solid casing reaching from the land surface to a depth of about 60-700 feet, and are perforated below the solid casing to allow water into the well. Water quality in the primary aquifer system may differ from the water in the shallower and deeper parts of the aquifer. Land use in the study unit is approximately 40 percent (%) natural (primarily shrubs, grassland, and wetlands), 37% agricultural, and 23% urban. The primary crops are citrus, avocados, alfalfa, pasture, strawberries, and dry beans. The largest urban areas in the study unit are the cities of

  13. Contrasts of Atmospheric Circulation and Associated Tropical Convection between Huaihe River Valley and Yangtze River Valley Mei-yu Flooding

    Institute of Scientific and Technical Information of China (English)

    HONG Jieli; LIU Yimin

    2012-01-01

    The significant differences of atmospheric circulation between flooding in the Huaihe and Yangtze River valleys during early mei-yu (i.e.,the East Asian rainy season in June) and the related tropical convection were investigated.During the both flooding cases,although the geopotential height anomalies always exhibit equivalent barotropic structures in middle to high latitudes at middle and upper troposphere,the phase of the Rossby wave train is different over Eurasian continent.During flooding in the Huaihe River valley,only one single blocking anticyclone is located over Baikal Lake.In contrast,during flooding in the Yangtze River valley,there are two blocking anticyclones.One is over the Ural Mountains and the other is over Northeast Asia.In the lower troposphere a positive geopotential height anomaly is located at the western ridge of subtropical anticyclone over Western Pacific (SAWP) in both flooding cases,but the location of the height anomaly is much farther north and west during the Huaihe River mei-yu flooding.Furthermore,abnormal rainfall in the Huaihe River valley and the regions north of it in China is closely linked with the latent heating anomaly over the Arabian Sea and Indian peninsula.However,the rainfall in the Yangtze River valley and the regions to its south in China is strongly related to the convection over the western tropical Pacific.Numerical experiments demonstrated that the enhanced latent heating over the Arabian Sea and Indian peninsula causes water vapor convergence in the region south of Tibetan Plateau and in the Huaihe River valley extending to Japan Sea with enhanced precipitation; and vapor divergence over the Yangtze River valley and the regions to its south with deficient precipitation.While the weakened convection in the tropical West Pacific results in moisture converging over the Yangtze River and the region to its south,along with abundant rainfall.

  14. Rivers and valleys of Pennsylvania, revisited

    Science.gov (United States)

    Morisawa, Marie

    1989-09-01

    The 1889 paper by William Morris Davis on the "Rivers and Valleys of Pennsylvania" is a landmark in the history of geomorphology. It was in this manuscript that he set forth what came to be known as the Davisian system of landscape. It is important to understand that Davis' interpretation of landforms was restricted by the geologic paradigms of his day. Uniformitarianism was strongly entrenched and Darwin's theory of evolution had become popularly accepted. The concept of the landmass Appalachia and then current theories on mountain building affected the approach that Davis took in hypothesizing the origin and development of the Folded Appalachian drainage. All of these geologic precepts influenced the formulation and explanation of his theories. In his exposition he adapted, synthesized and embellished on ideas he derived from fellow geologists such as Gilbert, Dutton, Powell, and McGee. A number of the concepts he proposed in the 1889 paper quickly became the bases for geomorphic studies by others: the cycles of river erosion and landscape evolution and the peneplain (here called base level erosion). The cycle of erosion became the model for subsequent geomorphic analyses, and peneplain hunting became a popular sport for geomorphologists. Davis' hypothesis of the origin and development of Pennsylvanian drainage stimulated subsequent discussion and further hypotheses by others. In fact, many of the later theories were refinements and/or elaborations of ideas mentioned in this paper of Davis. He proposed the origin of the drainage as consequent streams, then antecedence, superposition, headward extension of divides by piracy, erosion along lines of weaknesses (faults, easily erodible beds) through resistant ridges and normal fluvial erosion. Thus, the hypotheses of regional superposition (Johnson), extended consequents (Ruedemann), consequents and local superposition (Meyerhoff and Olmstead), the utilization of structural weaknesses in development of transverse

  15. Systematization of river valleys in different morphostructural areas

    Science.gov (United States)

    Opekunova, Marina

    2014-05-01

    The aim of our research was to identify the features of development of river valleys within the south of Eastern Siberia. One of the objectives to achieve this aim was the typing of river valleys, which was based on the principle of the location of a river valley or its part within different morphostructural areas, determining the morphology and individual (general or specific) development features that make it possible to specify the pattern of development of river valleys at different topological levels. Within the study area the following major morphostructures are distinguished: Altai-Sayan and Baikal mountain-folded regions, the Baikal rift zone, and the Siberian platform, within which morphostructures of the lower order are identified. Thus, a large variability in types of interaction and interpenetration of different areas provides for the development of various types of river valleys, depending on their location in the morphostructural areas. This approach was the basis for the typing of river valleys, i.e. idenifying their typological characteristics, depending on their location within a particular morphostructural area, geological and geomorphological conditions, and the history of development. The basic principles for the typing of river valleys are: 1) their location with respect to morphostructural areas, and 2) a set of characteristics of valleys of different morphostructural areas. Based on the above mentioned approach, and using GIS (MapInfo software), a map of river valleys typing was compiled, which included the database of the hydrographic network with space-time characteristics, tabulated for each streamflow. The procedure for determining the types of river valleys within each morphostructure was as follows. Boundaries of morphostructures of different orders were identified according to cartographic and literature data and allocated in the GIS space (MapInfo software). In the database, each distinguished morphostructure has the following

  16. Landscape pattern change in the upper valley of Min River

    Institute of Scientific and Technical Information of China (English)

    ZHAO Yong-hua; HE Xing-yuan; HU Yuan-man; CHANG Yu

    2005-01-01

    The upper valley of Min River (102° 59′ -104° 14′ E, 31° 26′ - 33° 16′ N), which is consisted of the counties Wenchuan, Maoxian, Lixian, Heishui, and Songpan, refers to the part up to Dujiangyan City, and locates on the transition zone from the Tibetan Plateau to the Sichuan Basin. It is one of the most important forest areas in China, especially in Sichuan Province. Over past two decades, the landscape changed remarkably in the region. The 3S techniques (Remote Sensing (RS), Geographic Information System (GIS) and Global Position System (GPS)) were used to classify the images and analyze the landscape change. The remotely sensed data of Landsat TM 1986 and Landsat ETM+ 2000 were used to analyze the landscape change of the region. The landscape were classified into 10 types of cropland, forest, shrub land, economic forest, grassland, build up land, river, lake, swamp, and unused land. The results showed that: 1) the woodland and grassland were dominating landscape types in the upper valley of Min River, which is more than 91% of the study area; 2) the alteration of the landscape was mainly happened among forest, shrub land, grassland, economic forest, cropland, and build up land, where forest decreased from 51.17% to 47.56%; 3) the landscape fragmentation in the upper valley of Min River was aggravated from 1986 to 2000.

  17. Balsa Tower Walls Brave "Big Buster"

    Science.gov (United States)

    Granlund, George

    2008-01-01

    Like many technology teachers, the author, a technology education teacher at Arthur Hill High School in Saginaw, Michigan, tries to stretch his budget by "milking" each student activity for maximum benefit. In the technology department, they use balsa wood towers to teach the basics of structural engineering. To get the most from their materials,…

  18. Arsenic hydrogeochemistry in an irrigated river valley - A reevaluation

    Science.gov (United States)

    Nimick, D.A.

    1998-01-01

    Arsenic concentrations in ground water of the lower Madison River valley, Montana, are high (16 to 176 ??g/L). Previous studies hypothesized that arsenic-rich river water, applied as irrigation, was evapoconcentrated during recharge and contaminated the thin alluvial aquifer. Based on additional data collection and a reevaluation of the hydrology and geochemistry of the valley, the high arsenic concentrations in ground water are caused by a unique combination of natural hydrologic and geochemical factors, and irrigation appears to play a secondary role. The high arsenic concentrations in ground water have several causes: direct aquifer recharge by Madison River water having arsenic concentrations as high as 100 ??g/L, leaching of arsenic from Tertiary volcano-clastic sediment, and release of sorbed arsenic where redox conditions in ground water are reduced. The findings are consistent with related studies that demonstrate that arsenic is sorbed by irrigated soils in the valley. Although evaporation of applied irrigation water does not significantly increase arsenic concentrations in ground water, irrigation with arsenic-rich water raises other environmental concerns.

  19. Composition and structure of balsa (Ochroma pyramidale) wood

    OpenAIRE

    Borrega, Marc; Ahvenainen, Patrik; Serimaa, Ritva; Gibson, Lorna

    2014-01-01

    Balsa, with its low density and relatively high mechanical properties, is frequently used as the core in structural sandwich panels, in applications ranging from wind turbine blades to racing yachts. Here, both the cellular and cell wall structure of balsa are described, to enable multi-scale modeling and an improved understanding of its mechanical properties. The cellular structure consists of fibers (66–76 %), rays (20–25 %) and vessels (3–9 %). The density of balsa ranges from roughly 60 t...

  20. Evolution of valley-fill terraces in the Alaknanda Valley, NW Himalaya: Its implication on river response studies

    Science.gov (United States)

    Devrani, Rahul; Singh, Vimal

    2014-12-01

    The present study attempts to understand the importance of place and local factors in the process of valley filling in an active mountain belt. The accumulation of sediments in a valley stretch depends upon the relationship between sediment carried from upstream by the main river entering into the stretch (qi), locally derived sediments (i.e., from local streams (qt), hillslopes (qh), and glacial and periglacial processes (qg)), and sediment exiting that stretch (qo); these are in turn governed by other processes like tectonic activity, intensity of precipitation, and lithology. As an example a valley stretch in the NW Himalaya is chosen in the Alaknanda River, one of the two uppermost tributaries of the Ganga River. This stretch is called as Pipalkoti Valley after the name of the main town; it is located close to the Main Central Thrust (MCT) and falls in the zone of orographic precipitation. Detailed geomorphic mapping reveals four surfaces and two terraces. Three debris-flow surfaces suggest their deposition by local mass flows and stream flows with very small contributions from the Alaknanda River. Terrace T2 occurs as a strath in some parts and is made up of fluvial and lacustrine sediments in others. The presence of lacustrine sediments suggests local damming of the river. Thick fluvial sediment is deposited in stretches of the rivers where it becomes wide due to the joining of a tributary. Synsedimentary deformation has been noted indicating that tectonic activity has affected sedimentation. The results suggest that local processes played a dominant role in the accumulation of sediments in this valley stretch. A model is proposed showing the role of glacial activity, high intensity meteorological events, river width, active faults and landslide damming in the origin of valley-fill deposits of the Pipalkoti Valley. It is concluded that before correlating valley-fill deposits along the lengths of the Himalayan valleys, it is important to evaluate the role of

  1. Control of medfly by SIT in the Nereva river valley

    Energy Technology Data Exchange (ETDEWEB)

    Bjelis, Mario, E-mail: mario.bjelis@zzb.h [Institut for Plant Protection in Agriculture and Foresty of Republic of Croatia, Zagreb, Zvonimirova (Croatia); Ljubetic, Visnja [Ministry of Agriculture, Forestry and Watter Managment of Republic of Croatia, Zagreb (Croatia); Novosel, Nevenka [State Office for Nuclear Safety, Zagreb (Croatia)

    2006-07-01

    A feasibility study of medfly suppression by means of sterile males released program in the Neretva Vallley, Croatia, is presented. The increase of medfly infestation is considered, as almost all cultures of the region represent host plants for the insect. Environmental friendly methods such well developed SIT technique associated with other organic methods are mentioned as an option of no disruption of the present natural balance. Area study and strategy planning is briefly presented. Population dynamics of Ceratitis capitata in the different parts of the delta Neretva valley, during period 2002 - 2004 Year is reported. Medfly capture on selected locations with different host availability in Neretva river is studied. (MAC)

  2. Emergy Analysis of Sustainability of Eco-economic System in Sichuan’s Baisha River Valley

    Institute of Scientific and Technical Information of China (English)

    2012-01-01

    Using emergy analysis method,I conduct quantitative analysis of social,economic and natural systems in Sichuan’s Baisha River valley during the period 2002-2006,through the establishment of indicators.I compare the emergy of Baisha River valley,with that of Xinjiang’s Manas River valley and Sichuan Province,and evaluate the sustainable development conditions in Baisha River valley,in order to provide corresponding reference for the development and utilization of Baisha River valley in the future.The results show that from the perspective of emergy input of economic system,Baisha River valley is a typical ecological and economic zone with rich resources to be developed;in terms of the development of natural conditions and utilization of ecological resources,the resource utilization intensity of Baisha River valley is weak and the environmental loading ratio there is low,thus the level of emergy yield needs to be improved;the system of Baisha River valley has enormous capacity for sustainable development and good potential for development.

  3. AMS exposure dating: evolution of river valley profiles across Himalayas during late Quaternary-Holocene

    International Nuclear Information System (INIS)

    River valley profile is one geomorphic feature, which contain relict landforms inherited from past periods with changing intensities of tectonic and climatic parameters. This aspect has been a subject of current research interest, using exposure dating technique. The results of some recent studies from major river valleys across Himalayas are being discussed

  4. D GIS for Flood Modelling in River Valleys

    Science.gov (United States)

    Tymkow, P.; Karpina, M.; Borkowski, A.

    2016-06-01

    The objective of this study is implementation of system architecture for collecting and analysing data as well as visualizing results for hydrodynamic modelling of flood flows in river valleys using remote sensing methods, tree-dimensional geometry of spatial objects and GPU multithread processing. The proposed solution includes: spatial data acquisition segment, data processing and transformation, mathematical modelling of flow phenomena and results visualization. Data acquisition segment was based on aerial laser scanning supplemented by images in visible range. Vector data creation was based on automatic and semiautomatic algorithms of DTM and 3D spatial features modelling. Algorithms for buildings and vegetation geometry modelling were proposed or adopted from literature. The implementation of the framework was designed as modular software using open specifications and partially reusing open source projects. The database structure for gathering and sharing vector data, including flood modelling results, was created using PostgreSQL. For the internal structure of feature classes of spatial objects in a database, the CityGML standard was used. For the hydrodynamic modelling the solutions of Navier-Stokes equations in two-dimensional version was implemented. Visualization of geospatial data and flow model results was transferred to the client side application. This gave the independence from server hardware platform. A real-world case in Poland, which is a part of Widawa River valley near Wroclaw city, was selected to demonstrate the applicability of proposed system.

  5. Pool fire upon a balsa-filled shock absorber

    International Nuclear Information System (INIS)

    When performing a safety assessment of a transport flask with balsa-filled shock absorbers it is important to know how the shock absorbers, which may have the outer skin punctured by an impact, will perform in a fire. A 30 minute pool test, which satisfied all the requirements of a thermal test under the IAEA regulations, was carried out upon a small, balsa-filled shock absorber. The outer steel shell was partly cut away exposing the wood to the fire and the air. The balsa wood prevented 90% of the heat from the fire from being transferred through the shock absorber, even though the balsa was only 133 mm thick. The maximum heat flux through to the inside of the shock absorber due to the burning of the balsa wood was relatively low, 2.8 kW/m2, and occurred 2 to 3 hours after the end of the pool fire. (author)

  6. Oscillation characteristics of summer precipitation in the Huaihe River valley and relevant climate background

    Institute of Scientific and Technical Information of China (English)

    2010-01-01

    Based on the summer precipitation data from the Huaihe River valley and the middle and lower reaches of the Yangtze River from 1922 to 2007,we analyzed the interannual and interdecadal oscillation and probability distribution characteristics of summer precipitation in the Huaihe River valley during the same period,using the wavelet transform and generalized extreme distribution methods.Whereby,we studied the climate background of East Asia Summer Monsoon (EASM),Sea Surface Temperature (SST),East Asia telecorrelation circulation,and their relationship with the interannual and interdecadal oscillation of summer precipitation in the Huaihe River valley.We further compared the difference of interdecadal oscillation of summer precipitation and the relevant climate background between the Huaihe River valley and the middle and lower reaches of the Yangtze River.The results show that:1) The intensity change of quasi-biennial oscillation (QBO) of summer precipitation in the Huaihe River valley is consistent with that of interdecadal oscillation.The summer precipitation in the Huaihe River valley has been more than normal since the end of the 1990s,and the QBO is very significant.Meanwhile,the probability of occurrence of extreme heavy rainfall increased obviously.2) The interdecadal oscillation of summer precipitation in the Huaihe River valley has a close relationship with the Pacific Decadal Oscillation (PDO) and interdecadal oscillation of EASM.When PDO is in the cold phase and EASM weakens,the summer precipitation will be greater than normal.3) QBO of summer precipitation in the Huaihe River valley is mainly controlled by that of EASM,and it has a relationship with a circulation pattern of "positive-negative-positive" from the high to the low latitudes in East Asia.4) There is interdecadal phase difference in summer precipitation between the Huaihe River valley and the middle and the lower reaches of the Yangtze River,which is mainly related to the intensity and

  7. Agricultural water and energy use in the Senegal River Valley

    Science.gov (United States)

    Masiyandima, M. C.; Sow, A.

    2015-12-01

    Assessment of the productivity of irrigation water is important measuring the performance of irrigation schemes especially in water scarce areas. Equally important for performance is the energy cost of providing water for irrigation. Sahel irrigation schemes are dependent on pumping water from rivers into a network of gravity operated channels. In the Senegal River valley in Senegal the cost of pumping water and for irrigation has been estimated to be 20-25% of total rice production costs. Irrigation schemes in the valley are characterized by low water productivity. We analysed rice production, irrigation water use and energy use for supplying irrigation water at Pont Gendarme, Ndiawar and Ngallenka MCA irrigation schemes in the Senegal River valley. For the 2013 rainfall season the mean yield ranged between 6 and 8t ha-1. Dry season yield ranged between 1.7 and 6.8t ha-1. Energy use for irrigation in the Ndiawar irrigation scheme was 8kg MJ-1 and 6.4kg MJ-1 in the 2013 and 2014 rainfall seasons respectively. In 2014 (rainfall season) energy productivity of irrigation water was 8.5, 8.0 and 16.4 kg MJ-1 at Ngallenka MCA, Ndiawar and Pont Gendarme respectively. Dry season (2014) energy productivity at Ndiawar and Pont Gendarme was 3.4 and 11.2kg MJ-1 respectively. Productivity of irrigation water was similar for all schemes (0.37kg m-3 at Pont Gendarme, 0.42kg m-3 at Ngallenka MCA, and 0.41kg m-3 Ndiawar). Energy use for the supply of irrigation water in the rainfall season ranged from 403 to 1,002MJ ha-1. Dry season irrigation energy use was 589MJ ha-1 Pont Gendarme and 331MJ ha-1 at Ndiawar. Reducing water use in these schemes through better water management will result in lower production costs and increased margins for the farmers. The observations from 2013 - 2014 highlight the importance of using both water and energy productivity to assess performance of irrigation schemes.

  8. Debris flow occurrence and sediment persistence, Upper Colorado River Valley, CO

    Science.gov (United States)

    Grimsley, Kyle J; Rathburn, Sara L.; Friedman, Jonathan M.; Mangano, Joseph F.

    2016-01-01

    Debris flow magnitudes and frequencies are compared across the Upper Colorado River valley to assess influences on debris flow occurrence and to evaluate valley geometry effects on sediment persistence. Dendrochronology, field mapping, and aerial photographic analysis are used to evaluate whether a 19th century earthen, water-conveyance ditch has altered the regime of debris flow occurrence in the Colorado River headwaters. Identifying any shifts in disturbance processes or changes in magnitudes and frequencies of occurrence is fundamental to establishing the historical range of variability (HRV) at the site. We found no substantial difference in frequency of debris flows cataloged at eleven sites of deposition between the east (8) and west (11) sides of the Colorado River valley over the last century, but four of the five largest debris flows originated on the west side of the valley in association with the earthen ditch, while the fifth is on a steep hillslope of hydrothermally altered rock on the east side. These results suggest that the ditch has altered the regime of debris flow activity in the Colorado River headwaters as compared to HRV by increasing the frequency of debris flows large enough to reach the Colorado River valley. Valley confinement is a dominant control on response to debris flows, influencing volumes of aggradation and persistence of debris flow deposits. Large, frequent debris flows, exceeding HRV, create persistent effects due to valley geometry and geomorphic setting conducive to sediment storage that are easily delineated by valley confinement ratios which are useful to land managers.

  9. Debris Flow Occurrence and Sediment Persistence, Upper Colorado River Valley, CO.

    Science.gov (United States)

    Grimsley, K J; Rathburn, S L; Friedman, J M; Mangano, J F

    2016-07-01

    Debris flow magnitudes and frequencies are compared across the Upper Colorado River valley to assess influences on debris flow occurrence and to evaluate valley geometry effects on sediment persistence. Dendrochronology, field mapping, and aerial photographic analysis are used to evaluate whether a 19th century earthen, water-conveyance ditch has altered the regime of debris flow occurrence in the Colorado River headwaters. Identifying any shifts in disturbance processes or changes in magnitudes and frequencies of occurrence is fundamental to establishing the historical range of variability (HRV) at the site. We found no substantial difference in frequency of debris flows cataloged at eleven sites of deposition between the east (8) and west (11) sides of the Colorado River valley over the last century, but four of the five largest debris flows originated on the west side of the valley in association with the earthen ditch, while the fifth is on a steep hillslope of hydrothermally altered rock on the east side. These results suggest that the ditch has altered the regime of debris flow activity in the Colorado River headwaters as compared to HRV by increasing the frequency of debris flows large enough to reach the Colorado River valley. Valley confinement is a dominant control on response to debris flows, influencing volumes of aggradation and persistence of debris flow deposits. Large, frequent debris flows, exceeding HRV, create persistent effects due to valley geometry and geomorphic setting conducive to sediment storage that are easily delineated by valley confinement ratios which are useful to land managers.

  10. Potential Vorticity Structure and Inversion of the Cyclogenesis Over the Yangtze River and Huaihe River Valleys

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    In this paper, the potential vorticity structure and inversion of the cyclogenesis over the Yangtze River and Huaihc River valleys during 21-23 June 2003 are investigated with a potential vorticity (PV) framework.The cyclogenesis is manifested by a lower-tropospheric PV anomaly over the Yangtze River and Huaihe River valleys at early stages mainly due to latent heat release, which greatly affects the evolution of the associated lower-tropospheric geopotential height and wind fields as demonstrated by piecewise PV inversion. At later stages, an upper-tropospheric PV anomaly develops, resulting in the growth of ridges over the cyclone in both the upstream and downstream, which provide a favorable background field for the low-level cyclone development. But the effect of a surface thermal anomaly always impedes the development of the cyclone to different extents during this cyclogenesis. It is further demonstrated that the position and the strength of the PV anomaly are closely related to the low-level cyclone development, and the lower-tropospheric PV anomaly seems to constitute the most significant feature, for instance, contributing about 60% to the low-level jet (LLJ).

  11. A Natural Heritage Inventory of the Rappahannock River Valley National Wildlife Refuge Potential Acquisition Area

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report documents the results of a project undertaken through this cooperative agreement to inventory the Rappahannock River Valley National Wildlife Refuge...

  12. Contaminant exposure and reproductive health of sandhill cranes in the Central Platte River Valley, Nebraska

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The central Platte River Valley provides crucial staging habitat for the endangered whooping crane (Grus americana) and the mid-continent population of sandhill...

  13. Mississippi River Valley Alluvial Aquifer, Alabama, Arkansas, Illinois, Kentucky, Louisiana, Mississippi, Tennessee; 2006-2008

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Outcrop and subcrop extent of the Mississippi River Valley Alluvial Aquifer in Alabama, Arkansas, Illinois, Kentucky, Louisiana, Mississippi, and Tennessee.

  14. Evapotranspiration by woody phreatophytes in the Humboldt River Valley near Winnemucca, Nevada

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report presents the results of cooperative studies ofevapotranspiration by phreatophytes in the Winnemucca reachof the Humboldt River valley. Water that is...

  15. Regional economic analysis of current and proposed management alternatives for Rappahannock River Valley National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The purpose of this study was to assess the regional economic implications associated with draft CCP management strategies for Rappahannock River Valley NWR. This...

  16. Fisheries and Aquatic Resources Managment Plan Rappahannock River Valley National Wildlife Refuge 2007

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — In June of 2007 there was an electro-fishing survey done within a small lake at the Laurel Grove Tract of the Rappahannock River Valley National Wildlife Refuge....

  17. Estimated Thickness of Quaternary Sediment in the Wood River Valley aquifer system, South-Central Idaho

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This dataset is the estimated thickness of Quaternary sediment of the Wood River Valley aquifer system. This isopach map was constructed by subtracting the...

  18. Sport Fishing Management Plan Rappahannock River Valley National Wildlife Refuge 2009

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The Rappahannock River Valley National Wildlife Refuge was first opened for recreational fishing in 2003. Wilna Pond was the only site suitable for this activity at...

  19. Community survey results for Rappahannock River Valley National Wildlife Refuge : Completion report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report provides a summary of results for the survey of residents of communities adjacent to Rappahannock River Valley NWR conducted from the spring through the...

  20. Landform-Sediment Assemblages Units of the Upper Mississippi River Valley

    Data.gov (United States)

    Iowa State University GIS Support and Research Facility — Wisconsinan and Holocene Landform-Sediment Assemblages of the Upper Mississippi River Valley. Knowledge of the spatial distribution of natural and cultural...

  1. State of the Refuge Habitat Report: Rappahannock River Valley National Wildlife Refuge 2011

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This plan outlines management strategies for every tract at the Rappahannock River Valley National Wildlife Refuge for 2011. This includes action priorities for...

  2. Aquifer Boundary of the Wood River Valley Aquifer System, South-Central Idaho

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This dataset contains the boundary of the Wood River Valley aquifer system as modified and expanded from that defined by Skinner and others (2007): It has been...

  3. Artificial flood support on Senegal river : a challenge to protect natural resources in the valley

    OpenAIRE

    Bader, Jean-Claude; Albergel, Jean

    2015-01-01

    Formed on the upper basin by the annual monsoon, the flood of Senegal River inundates a vast floodplain on its lower course, called "the valley". This one, several hundred kilometres long, can be regarded as an inland delta. This annual flooding, which offers ecosystem services and promotes traditional activities, must be maintained despite the presence on the Bafing of the Manantali reservoir dam, which controls since 1987 half of the river flows through the valley. In addition to its other ...

  4. RESEARCH OF FLORISTIC AND PHYTOCOENOTICAL DIVERSITY IN THE FORESTS OF SEVERTSKIY DONETS RIVER VALLEY

    Directory of Open Access Journals (Sweden)

    Yarotskaia М. А.

    2013-04-01

    Full Text Available We highlighted and analyzed the main reasearch stages and research trends of floristicand phytocoenotic diversity of forests in Severskiy Donets river valley from XIX up to now.We determined some three historical periods and characterized three lines of research: floristic, geobotanic and phytosociological. The urgent tasks of further studies of the flora and vegetation of forest valley of Severskiy Donets river were suggested with special attention to their dynamics and human health.

  5. Importance of Flood Severity Estimation for Flood Plain Management in a River Valley

    OpenAIRE

    Saqib Ehsan; Walter Marx; Silke Wieprecht

    2013-01-01

    Climate changes strongly affect the occurrence of floods. Extreme flooding can occur due to dam failure but sometimes high outflows that exceed the downstream safe channel capacity can also cause significant flooding. This paper emphasizes the importance of flood severity estimation in a river valley for long-term flood plain management. For hydraulic analysis, about 329 km long, the Jhelum river valley downstream of Mangla dam in Pakistan has been considered. The project reach has been model...

  6. [Ethnic dimension to migration in the Senegal river valley].

    Science.gov (United States)

    Traore, S

    1993-08-01

    Studies of the factors determining migratory patterns in the Senegal River Valley usually stress the importance of economic factors related to colonial domination. But when cultural factors and the social relations governing them are examined in a comparative study of ethnic groups, distinct population subgroups may be revealed to have differential migratory patterns. The Soninka and the Poular, two groups highly affected by migration, were chosen for an analysis of the impact of specific historical experiences on migratory behavior. A historical analysis of colonial archives and anthropological and historical monographs and the 1982-83 "Survey of Migration in the Valley of the Senegal River" provided data. The survey indicated that Soninka and Poular migratory patterns differed from each other, but that both differed from the migratory patterns of all other ethnic groups in the region. Soninka migration is international and oriented primarily toward Europe. It has recently become more intense than that of the poular. The determinants of migration in the two groups appear related more to the structure of households than to lack of educational and health facilities or even of food at the village level. Pastoral life and its associated beliefs and religious ideology appear to have been the principal determinants of precolonial movement among the Poular, while Soninka migration responded more to competition over control of manpower. Itinerant commercial activity was coupled with use of slave labor to ensure food production. But the suppression of slavery and crises of subsistence aggravated by colonial policy provoked ever more distant migration, which found a focus in the French demand for labor after World War II. Migration as an alternative does not appear to have been as significant for the Poular until more recently, when subsistence agriculture and the sale of animals were no longer sufficient to cover monetary needs. Male migration among the Soninka is a

  7. Using hydraulic heads, geochemistry and 3H to understand river bank infiltration; an example from the Ovens Valley, southeast Australia

    Science.gov (United States)

    Yu, Matthew; Cartwright, Ian

    2014-05-01

    Defining the relationship between the river and its river bank is important in constraining baseflow to a river and enhancing our ability in protecting water resources and riparian ecology. Hydraulic heads, geochemistry and 3H were measured in river banks along the Ovens River, southeast Australia. The Ovens River is characterised by the transition from a single channel river residing within a mountain valley to a multi-channel meandering river on broad alluvial plains in the lower catchment. The 3H concentrations of most near-river groundwater (less than 10 m from river channel) and bank water (10 - 30 m from the river channel) in the valley range between 1.93 and 2.52 TU. They are similar to those of the river, which are between 2.37 and 2.24 TU. These groundwater also have a Na/Cl ratio of 2.7 - 4.7 and are close to the river Na/Cl ratios. These similarities suggest that most river banks in the valley are recharged by the river. The hydraulic heads and EC values indicate that some of these river banks are recharged throughout the year, while others are only recharged during high flow events. Some near-river groundwater and bank water in the valley have a much lower 3H concentration, ranging from 0.97 to 1.27 TU. They also have a lower Na/Cl ratio of 1.6 - 3.1. These differences imply that some of the river banks in the valley are rarely recharged by the river. The lack of infiltration is supported by the constant head gradient toward the river and the constant EC values in these river banks. The river banks with bank infiltration are located in the first few hundred kilometres in the valley and in the middle catchment where the valley is broaden. In the first few hundred kilometres in the valley, it has a relatively flat landscape and does not allow a high regional water table to form. The river thus is always above the water table and recharges the river banks and the valley aquifers. In the broader valley, the relatively low lateral hydraulic gradient is

  8. Forest types of the "Argentino River Valley" Natural Reserve

    Directory of Open Access Journals (Sweden)

    Bagnato S

    2008-09-01

    Full Text Available Forest classification is a fundamental target for understanding forest stand dynamics and for sustainable management strategy applications. In this paper the methodological approach of forest types, already used in other Italians region, was applied for the classification of the RNO "Argentino River Valley" (southern Apennine, Italy. This study has been organized in 4 steps: 1 bibliographic analysis and collection of the acquired knowledge; 2 preliminary verification of forest types in the field; 3 description of the different units; 4 final validation of typological units. Using this approach we have characterized 9 categories and 12 forest types units. The description of each units has been filed as cards, where information of different nature is summarized and related to the organization of the typological units, to its location, to the description of the qualitative indicators (disturbances, cohort, mortality, natural dynamic tendencies, SDT, CWD etc. and quantitative indicators (dbh, average height, current annual increment, etc., to the functioning and the current management. For a better understanding of types functioning, "sylvology models" based on the "Spatial Pattern of Relative Collective Interaction" (PSICR and on the principal characteristics influencing and characterizing forest stand dynamics (availability of resources, type and frequency of disturbances, stand development, etc. have been singled out and proposed. The "forest types map" and other maps useful for the management of forest resources have been obtained. Moreover, data collected did allow to formulate several hypotheses on sustainable management.

  9. Holocene river dynamics in Northland, New Zealand: The influence of valley floor confinement on floodplain development

    Science.gov (United States)

    Richardson, J. M.; Fuller, I. C.; Holt, K. A.; Litchfield, N. J.; Macklin, M. G.

    2013-11-01

    Valley floor mapping, sedimentology, and 14C-dating have been used to reconstruct the fluvial history at eight floodplain sites spread throughout Northland, a region removed from the main areas of tectonic and volcanic activity in New Zealand. We present a probability-based record of Holocene river behaviour for Northland using 14C-dated Holocene fluvial deposits and compare this with independent palaeoclimate proxy records from the North Island. Holocene floodplain evolution and fluvial behaviour have been conditioned by the degree of valley-floor confinement. In the most and least confined valley settings, Holocene floodplain evolution has involved the development of a single floodplain surface. At partly confined sites, the river terrace and floodplain geomorphology are more complex. Region-wide progressive floodplain alluviation through the mid to late Holocene and a period of increased river activity between 3500 and 2800 cal. YBP in response to climatically driven increases in sediment supply was followed by a period of valley floor incision and terrace formation beginning after 1900 cal. YBP. In partly confined valley settings, this was followed by the aggradation of a lower Holocene floodplain surface, with rapid rates of vertical accretion in response to post-settlement catchment disturbance. The results of this study indicate that valley floor confinement has played a major role in controlling Northland Holocene river floodplain development, producing a continuum of floodplain and river terrace landforms in response to climatically and anthropogenically driven variations in sediment flux.

  10. Lithologic Heterogeneity and Variable Valley Width in the Buffalo River Watershed, AR

    Science.gov (United States)

    Shepherd, S. L.; Keen-Zebert, A.

    2014-12-01

    Lithologic heterogeneity across catchments is thought to be a key control on the style of incision, whether dominated by vertical or lateral processes, but little field evidence is available to support the claims. Map and field observations from the Buffalo National River (BNR) indicate that valley width is related to variation in lithology along the length of the river. The BNR is a gravel-mantled, ingrown meandering, bedrock river that incises through a sequence of Pennsylvanian, Mississippian, and Ordovician carbonate and clastic sedimentary rocks. Using GIS, valley width was measured at 250 m intervals along the entire length of the river through two sequences of limestone and sandstone reaches that represent the dominant lithologies of the catchment. Preliminary results show measurable and statistically significant differences in valley width between limestone and sandstone reaches. Where limestone strata is exposed at river level the mean width is ~ 360 m and is highly variable with a standard deviation of 227 m. The mean width in sandstone strata is ~240 m with a standard deviation of 88 m. At each transition from limestone to sandstone there is a greater than 20% decrease in valley width downstream, with no visible change in channel width at map scales. It is possible the atypical pattern in valley width in the BNR is due to variation in lithologic resistance. These results support the assumption that lithologic heterogeneity exerts control on stream valley evolution.

  11. Long term effects of climate on human adaptation in the middle Gila River Valley, Arizona, America

    NARCIS (Netherlands)

    Zhu, T.; Ertsen, M.W.; Van der Giesen, N.C.

    2015-01-01

    The Hohokam, an irrigation-based society in the American South West, used the river valleys of the Salt and Gila Rivers between 500 and 1500 AD to grow their crops. Such irrigated crops are linking human agency, water sources and the general natural environment. In order to grow crops, water availab

  12. Geological and Geothermal Investigation of the Lower Wind River Valley, Southwestern Washington Cascade Range

    Energy Technology Data Exchange (ETDEWEB)

    Berri, Dulcy A.; Korosec, Michael A.

    1983-01-01

    The Wind River Valley, on the west slope of the Cascade Range, is a northwest-trending drainage that joins the Columbia River near Carson, Washington. The region has been heavily dissected by fluvial and glacial erosion. Ridges have sharp crests and deep subsidiary valleys typical of a mature topography, with a total relief of as much as 900 m. The region is vegetated by fir and hemlock, as well as dense, brushy ground-cover and undergrowth. The lower 8 km of the valley is privately owned and moderately populated. The upper reaches lies within the Gifford Pinchot National Forest, and include several campgrounds and day parks, the Carson National Fish Hatchery, and the Wind River Ranger Station and Wind River Nursery of the US Forest Service. Logging activity is light due to the rugged terrain, and consequently, most valley slopes are not accessible by vehicle. The realization that a potential for significant geothermal resources exists in the Wind River area was brought about by earlier exploration activities. Geologic mapping and interpretation was needed to facilitate further exploration of the resource by providing a knowledge of possible geologic controls on the geothermal system. This report presents the detailed geology of the lower Wind River valley with emphasis on those factors that bear significantly on development of a geothermal resource.

  13. Geological and geothermal investigation of the lower Wind River valley, southwestern Washington Cascade Range

    Energy Technology Data Exchange (ETDEWEB)

    Berri, D.A.; Korosec, M.A.

    1983-01-01

    The detailed geology of the lower Wind River valley is presented with emphasis on those factors that bear significantly on development of a geothermal resource. The lower Wind River drainage consists primarily of the Ohanapecosh Formation, an Oligocene unit that is recognized across the entire southern Washington Cascade Range. The formation is at least 300 m thick in the Wind River valley area. It consists largely of volcaniclastic sediments, with minor massive pyroclastic flows, volcanic breccias and lava flows. Low grade zeolite facies metamorphism during the Miocene led to formation of hydrothermal minerals in Ohanapecosh strata. Metamorphism probably occurred at less than 180{sup 0}C.

  14. Evaluation of reforestation in the Lower Mississippi River Alluvial Valley

    Science.gov (United States)

    King, S.L.; Keeland, B.D.

    1999-01-01

    Only about 2.8 million ha of an estimated original 10 million ha of bottomland hardwood forests still exist in the Lower Mississippi River Alluvial Valley (LMAV) of the United States. The U.S. Fish and Wildlife Service, the U.S. Forest Service, and state agencies initiated reforestation efforts in the late 1980s to improve wildlife habitat. We surveyed restorationists responsible for reforestation in the LMAV to determine the magnitude of past and future efforts and to identify major limiting factors. Over the past 10 years, 77,698 ha have been reforested by the agencies represented in our survey and an additional 89,009 ha are targeted in the next 5 years. Oaks are the most commonly planted species and bare-root seedlings are the most commonly used planting stock. Problems with seedling availability may increase the diversity of plantings in the future. Reforestation in the LMAV is based upon principles of landscape ecology; however, local problems such as herbivory, drought, and flooding often limit success. Broad-scale hydrologic restoration is needed to fully restore the structural and functional attributes of these systems, but because of drastic and widespread hydrologic alterations and socioeconomic constraints, this goal is generally not realistic. Local hydrologic restoration and creation of specific habitat features needed by some wildlife and fish species warrant attention. More extensive analyses of plantings are needed to evaluate functional success. The Wetland Reserve Program is a positive development, but policies that provide additional financial incentives to landowners for reforestation efforts should be seriously considered.

  15. Numerical Simulation of the 1999 Yangtze River Valley Heavy Rainfall Including Sensitivety Experiments with Different SSTA

    Institute of Scientific and Technical Information of China (English)

    郭裕福; 王嘉; 赵彦

    2004-01-01

    With the IAP/LASG GOALS model,the heavy rainfall of the summer of 1999 in the Yangtze River valley is simulated with observational sea surface temperature (SST).Comparing the simulations of 1999 with the corresponding ones of 1998 and the sensitivity experiments with different sea surface temperature anomalies (SSTA) at different ocean regions,the relationships between the floods in the Yangtze River valley and the SSTA in the Pacific and Indian Oceans are studied.The results show that the positive SSTAin the tropical Indian Ocean are a major contributor to the heavy rainfall and may be a very important index to predict the heavy rainfall over the Yangtze River valley in the summer.The simulations also show that the relationships between the SSTA in the tropical eastern Pacific and the heavy rainfall in the Yangtze River valley are very complicated,and the heavy rainfall in the Yangtze River valley can occur in both a decaying and an intensifying El Ninio event and also in a La Nina event.However,the different SSTA of different periods in the above three cases play different parts.

  16. Using a novel flood prediction model and GIS automation to measure the valley and channel morphology of large river networks

    Science.gov (United States)

    Traditional methods for measuring river valley and channel morphology require intensive ground-based surveys which are often expensive, time consuming, and logistically difficult to implement. The number of surveys required to assess the hydrogeomorphic structure of large river n...

  17. Aeolian Processes and Landforms in River Valleys of Central Russian Plain in MIS 2

    Science.gov (United States)

    Matlakhova, Ekaterina

    2015-04-01

    Late Pleistocene terraces in river valleys of Central Russian Plain were subject to aeolian reworking after the alluvial sedimentation had finished. Severe natural conditions of LGM (cold and dry climate, scarce vegetation) contributed activation of aeolian processes. Ground water lowering because of deep pre-LGM incision of rivers made deep aeolian reworking possible at low hypsometric levels of valley bottom. We studied lithological structure of terraces in river valleys of Central Russian Plain. The key sites were located in Seim (the middle Dnieper catchment) and Khoper (the middle Don catchment) river valleys. Field data was combined with quartz grains morphoscopy technique (study of texture of sediment particles using scanning electron microscope). Wide participation of aeolian sediments in terrace deposits was detected. During this study a new technique of the distinguishing of short-term aeolian reworking of alluvial deposits using quartz grains morphoscopy technique was developed. The main problem of interpretation the results of quartz grains morphoscopy is that aeolian signals are sometimes not clear due to short duration of wind action over alluvial sands. However, detailed studies of the quartz grains surfaces under scanning electron microscope helped to solve this problem. We used scanning electron microscope JEOL JSM-661 LV and worked with magnification from ×160 to ×400 for whole grains and up to ×1800 for some parts of grains. Deep aeolian reworking of Late Pleistocene terrace alluvium in river valleys of Central Russian Plain during LGM led to the formation of aeolian covers on the terrace surfaces. Also there are many relict dunes on Late Pleistocene river terrace surfaces. Sometimes the development of aeolian processes could led to more significant changes in the shape of the valley and formation of aeolian aprons. The thickness of aeolian covers can reach 3-5 m or more. Due to this reason morphology and topography of river terraces could

  18. Formation mechanism and development pattern of aeolian sand landform in Yarlung Zangbo River valley

    Institute of Scientific and Technical Information of China (English)

    李森; 董光荣; 申建友; 杨萍; 刘贤万; 王跃; 靳鹤龄; 王强

    1999-01-01

    Aeolian sand landforms in the Yarlung Zangbo River valley can be divided into 4 classes and 21 types. The river valley has favourable environment conditions for the development of aeolian sand landforms. Simulation of MM4 mid-scale climate model showed that the near-surface flow field and wind vector field during the winter half year in the fiver valley are generally favourable for the aeolian sand deposition and as a whole they also affect the distribution zones and sites of aeolian sand landforms. Sand dunes and sand dune groups in the fiver valley developed mainly in three ways, namely windward retarding deposition, leeward back flow deposition and bend circumfluence deposition. Through alternating positive-reverse processes of sand dune formation under wind actions and sand dune vanishing under water actions, sand dunes developed from primary zone through main-body zone then to vanishing zone where climbing dunes and falling dunes are declining and are even disappearing.

  19. COMPLEX LANDSLIDE IN THE RJEČINA RIVER VALLEY

    OpenAIRE

    1999-01-01

    This paper presents the first phase investigation results of the complex landslide situated on north-eastern slope of the Rječina valley, between Valići damm and the village of Pašac. The valley slopes were formed in Paleogene flysch and Quaternary formations. The limestone rocks are present on the top sites, forming the scarps there. The complex landslide formation has been preconditioned by the geological structure and morphogenesis of the Rječina valley. This is the type of complex retrogr...

  20. Recycling of Pleistocene valley fills dominates 125 ka of sediment flux, upper Indus River

    Science.gov (United States)

    Munack, Henry; Blöthe, Jan Henrik; Fülöp, Réka-Hajnalka; Codilean, Alexandru T.; Fink, David; Korup, Oliver

    2016-04-01

    Rivers draining the semiarid Transhimalayan Ranges along the western Tibetan Plateau margin underwent alternating phases of massive valley infill and incision in Pleistocene times. The imprints of these cut-and-fill cycles on long-term sediment fluxes have remained largely elusive. We investigate the timing and geomorphic consequences of headward incision of the Zanskar River, which taps the vast More Plains valley fill that currently impedes drainage of the endorheic high-altitude basins of Tso Kar and Tso Moriri. In situ 10Be exposure dating and topographic analyses indicate that a phase of valley infill gave way to net dissection of the >250-m thick sedimentary stacks ˜125 ka ago, i.e. during the last interglacial (MIS 5e). Rivers eroded >14.7 km3 of sediment from the Zanskar headwaters since then, fashioning specific sediment yields that surpass 10Be-derived denudation rates from neighbouring catchments by factors of two to ten. We conclude that recycling of Pleistocene valley fills has provided Transhimalayan headwater rivers with more sediment than bedrock denudation, at least since the beginning of the last glacial cycle. This protracted liberation of sediment stored in thick valley fills could bias rate estimates of current sediment loads and long-term bedrock denudation.

  1. Geomorphological record of transformations of upland river valley bottoms at variable rate of gully erosion (case study: Wieprz River valley in Roztocze)

    Science.gov (United States)

    Kociuba, Waldemar

    2014-06-01

    In the upland geosystems of the moderate climate zone, any change in the conditions of functioning of a catchment causes a response of the system involving variable dynamics of fluvial processes (Gregory, Walling 1973; Schumm 1977, 1981; Kostrzewski, Szpikowski 2003; Świeca, Kociuba 2007). In the conditions of low anthropopressure, the direction and intensity of the processes modelling the valley bottom are determined by environmental factors, i.e. the geology and lithology of sediments, and land relief, and climate-driven factors, i.e. precipitation and groundwater supply determining water and sediment discharge rate (Froehlich 1982; Kostrzewski et al. 1994; Krzemień 1999; Dearing, Jones 2003, Meybeck et al. 2003; Kociuba et al. 2003; Świeca, Kociuba 2007; Rodzik et al. 2008). In the conditions of strong anthropopressure, the processes of transformation of the valley bottom can be largely accelerated due to disturbances in the stability of the catchment’s environmental conditions. Their geomorphological ef fects are manifested in changes in the channel shape (in the plan and cross profile), and in the modelling of the zone outside the channel, as a result of both flood and delluvial sediment deposition, particularly in the mouth zones of dry valleys and erosional dissections (Bork 1989; Rodzik et al. 2008; Brown 2009). Transformations of valley landforms resulting from changes in natural conditions and anthropopressure on the valley system can be traced based on the example of the meridional part of the Roztocze section of the Wieprz River valley (Fig. 1) - a typical medium-sized upland river of the moderate climate zone (Rodzik et al. 2008). The modern relief of the alluvial plain of the Roztocze fragment of the Wieprz River valley results from complex morphogenetic processes (Kociuba, Brzezińska-Wójcik 2002; Kociuba, Superson 2004). The primary morphostructural features developed with the contribution of tectonic movements in the Neogene and Early

  2. Types of river valleys as a criterion for estimation of the territory geodiversity

    Science.gov (United States)

    Opekunova, Marina; Vyrkin, Vladimir

    2015-04-01

    The Oka plateau occupies an intermediate position between large morphostructures of Southern Siberia. It is a unique object, where the features of relief development of the contiguous areas were reflected. The structure of the plateau also includes the Ilchir-Kitoi depression, located in the southeast, and the Oka depression, which lies in the north-west. The river network is characterized by deeply incised valleys, the relief of which bears traces of glacial activity, manifestations of Cenozoic volcanism, and active neotectonic movements. These factors also determine a wide variability in distribution of the types of river valleys: from the valleys with the hilly-moraine topography to the broad-floodplain sections of valleys with an instrativ floodplain-terrace complex and incised type of channel when the river crosses basalt fields. Thus, the antecedent Oka river valley of ancient formation was actively affected by volcanism and glaciation in Late Cenozoic. Lava flows enabled the formation of the incised and adapted types of channels within the south-western part of the Oka depression. Large areas of distribution of basalts on the left-bank part of the Oka river basin, occupying mainly the watershed positions, contributed to the formation of a certain type of longitudinal profiles of channels, characterized by a shallow form in the upper reaches (in the field of basalts development) and by a steep form in the middle and lower sections of the valleys. The distribution of fluvioglacial landforms and moraine ridges descending into the Oka valley along the tributaries (Sentsa, Gargan and others), and the presence of facies transitions from fluvioglacial and glacial to alluvial deposits determine the specific type of river valleys, developed under the conditions of the glacial relief formation. Due to the uplift of the Kropotkin range, the river erosion within the plateau is relatively slowed down in comparison with the surrounding mountains, which is reflected in the

  3. Revegetation of Reconstructed Reaches of the Provo River, Heber Valley, Utah

    OpenAIRE

    Rice, John A.

    2006-01-01

    Prior to the 1950s, the middle Provo River in Utah offered outstanding fish and wildlife habitat. This was due in part to the Provo River freely meandering through the Heber Valley. These bends in the river provided deep holes for fish and a dense streamside forest for many species of birds. This productive habitat was altered in the 1940s and 1950s when the river was dammed, channelized, and forced between dikes (figure 1). These dikes were constructed by the USDI Bureau of Reclamation (USBR...

  4. Quaternary Geochronology, Paleontology, and Archaeology of the Upper San Pedro River Valley, Sonora, Mexico

    Science.gov (United States)

    Gaines, E. P.

    2013-12-01

    This poster presents the results of multi-disciplinary investigations of the preservation and extent of Quaternary fossil-bearing strata in the San Pedro River Valley in Sonora, Mexico. Geologic deposits in the portions of the San Pedro Valley in southern Arizona contain one of the best late Cenozoic fossil records known in North America and the best record of early humans and extinct mammals on the continent. The basin in the U.S. is one of the type locations for the Blancan Land Mammal Age. Hemiphilian and Irvingtonian fossils are common. Rancholabrean remains are widespread. Strata in the valley adjacent to the international border with Mexico have yielded the densest concentration of archaeological mammoth-kill sites known in the western hemisphere. Despite more than 60 years of research in the U.S., however, and the fact that over one third of the San Pedro River lies south of the international boundary, little has been known about the late Cenozoic geology of the valley in Mexico. The study reported here utilized extensive field survey, archaeological documentation, paleontological excavations, stratigraphic mapping and alluvial geochronology to determine the nature and extent of Quaternary fossil-bearing deposits in the portions of the San Pedro Valley in Sonora, Mexico. The results demonstrate that the Plio-Pleistocene fossil -bearing formations known from the valley in Arizona extend into the uppermost reaches of the valley in Mexico. Several new fossil sites were discovered that yielded the remains of Camelids, Equus, Mammuthus, and other Proboscidean species. Late Pleistocene archaeological remains were found on the surface of the surrounding uplands. AMS radiocarbon dating demonstrates the widespread preservation of middle- to late- Holocene deposits. However, the late Pleistocene deposits that contain the archaeological mammoth-kill sites in Arizona are absent in the valley in Mexico, and are now known to be restricted to relatively small portions of

  5. Holocene climatic events recorded in palaeoflood slackwater deposits along the middle Yiluohe River valley, middle Yellow River basin, China

    Science.gov (United States)

    Zhao, Xueru; Huang, Chun Chang; Pang, Jiangli; Zha, Xiaochun; Guo, Yongqiang; Hu, Guiming

    2016-06-01

    Palaeohydrological investigations were carried out in the middle reaches of the Yiluohe River, a major tributary in the lower-middle Yellow River basin. Typical palaeoflood slackwater deposits (SWDs) were identified in the Holocene pedostratigraphy on the cliffy river banks. Analytical results, including magnetic susceptibility and grain-size distribution data, indicated that these SWDs were deposited from the suspended sediment load in flood water. These SWDs are different from eolian loess, soils and aeolian sands in the riverbank profile. They recorded several episodes of extraordinary palaeoflood events. In the Longmenxia reaches of the Yihe River valley, these flood events were dated at 3100-3000 a, 1800-1700 a, 770-610 a, and 420-340 a using the optically stimulated luminescence method in combination with the pedostratigraphic correlations. In the Longhutan reaches of the Luohe River valley, the palaeoflood events were dated at 1975-1466 a, i.e., from the Han to Wei dynasties (AD 25-534), during which the capital city on the river banks was flooded many times, as recorded in the literature. These extraordinary flood events are well correlated chronologically with the known Holocene climatic events that occurred in the Northern Hemisphere. Thus, the monsoonal climate was highly variable with both floods and droughts occurring frequently during these episodes. These results are important for understanding the response of river systems in eastern Asia to global changes.

  6. SLOPE LITHOLOGIC PROPERTY, SOIL MOISTURE CONDITION AND REVEGETATION IN DRY-HOT VALLEY OF JINSHA RIVER

    Institute of Scientific and Technical Information of China (English)

    XIONG Dong-hong; ZHOU Hong-yi; YANG Zhong; ZHANG Xin-bao

    2005-01-01

    The dry-hot valley of the Jinsha River is one of the typical eco-fragile areas in Southwest China, as well as a focus ofrevegetation study in the upper and middle reaches of the Changjiang River. Due to its extremely dry and hot climate, severely degraded vegetation and the intense soil and water loss, there are extreme difficulties in vegetation restoration in this area and no great breakthrough has ever been achieved on studies of revegetation over the last several decades. Through over ten years' research conducted in the typical areas-the Yuanmou dry-hot valley, the authors found that the lithologic property is one of the crucial factors determining soil moisture conditions and vegetation types in the dry-hot valley, and the rainfall infiltration capability is also one of the key factors affecting the tree growth. Then the revegetation zoning based on different slopes was conducted and revegetation patterns for different zones were proposed.

  7. Paper birch: Sentinels of climate change in the Niobrara River Valley, Nebraska

    Science.gov (United States)

    Stroh, Esther D.

    2011-01-01

    The Niobrara River Valley in the northern Great Plains supports scattered stands of paper birch (Betula papyrifera Marsh), a species more typical of boreal forests. These birch stands are considered to be relictual populations that have persisted since the end of the Wisconsin glaciation. Localized summer microclimates have likely facilitated the persistence of birch populations in a region otherwise unsuitable for the species. Dieback of canopy-sized birch has been observed throughout the valley in recent years, although no onset dates are documented. Changes in spring weather patterns may be causing rootlet injury so that trees die in spite of the still-cool summer microclimates. Current weather patterns, combined with little evidence of recruitment of young birch and great geographic distances from potential immigrant sources, make the future persistence of birch in the Niobrara River Valley stands uncertain.

  8. Moisture transport source/sink structure of the Meiyu rain belt along the Yangtze River valley

    Institute of Scientific and Technical Information of China (English)

    XU Xiangde; CHEN Lianshou; WANG Xiurong; MIAO Qiuju; TAO Shiyan

    2004-01-01

    Based on the analyses of the moisture transport structure in the whole layer of the troposphere along the Yangtze River valley during drought/flood years using the NCEP reanalysis data, this paper reveals that there exists a key region with a "Large Triangle" shape of transporting moisture for the Tibetan Plateau to Meiyu Belt and its "source/sink" structure; discloses that the interannual variation of the whole budget of inflow and outflow of moisture through the boundaries of a "Large Triangle" key region has the in-phase characteristic. Then a moisture transport structure over the skirt of the plateau and a conceptual model on the "transfer post" of moisture transport in the area of the South China Sea-Tibetan Plateau-Yangtze River valley in summer are put forward in this paper; the anti-phase feature of whole layer moisture transport flow patterns of Yangtze River valley during drought/flooding years is exhibited using the computational scheme of whole layer moisture transport correlation vector fields; a comprehensive dynamic model and its physical diagram of the tele- connection source/sink structure of the moisture transport of the Meiyu rain belt have been made. It shows that the moisture transfer effect over the skirt of the plateau from the ocean (Indian Ocean, South China Sea and west North Pacific) led to a moisture confluence belt in the Yangtze River valley and the teleconnection moisture transport source/sink structure over the "Large Triangle" shape area in flooding years.

  9. Hydrogeologic framework of the Wood River Valley aquifer system, south-central Idaho

    Science.gov (United States)

    Bartolino, James R.; Adkins, Candice B.

    2012-01-01

    The Wood River Valley contains most of the population of Blaine County and the cities of Sun Valley, Ketchum, Hailey, and Bellevue. This mountain valley is underlain by the alluvial Wood River Valley aquifer system, which consists primarily of a single unconfined aquifer that underlies the entire valley, an underlying confined aquifer that is present only in the southernmost valley, and the confining unit that separates them. The entire population of the area depends on groundwater for domestic supply, either from domestic or municipal-supply wells, and rapid population growth since the 1970s has caused concern about the long-term sustainability of the groundwater resource. As part of an ongoing U.S. Geological Survey effort to characterize the groundwater resources of the Wood River Valley, this report describes the hydrogeologic framework of the Wood River Valley aquifer system. Although most of the Wood River Valley aquifer system is composed of Quaternary-age sediments and basalts of the Wood River Valley and its tributaries, older igneous, sedimentary, or metamorphic rocks that underlie these Quaternary deposits also are used for water supply. It is unclear to what extent these rocks are hydraulically connected to the main part of Wood River Valley aquifer system and thus whether they constitute separate aquifers. Paleozoic sedimentary rocks in and near the study area that produce water to wells and springs are the Phi Kappa and Trail Creek Formations (Ordovician and Silurian), the Milligen Formation (Devonian), and the Sun Valley Group including the Wood River Formation (Pennsylvanian-Permian) and the Dollarhide Formation (Permian). These sedimentary rocks are intruded by granitic rocks of the Late Cretaceous Idaho batholith. Eocene Challis Volcanic Group rocks overlie all of the older rocks (except where removed by erosion). Miocene Idavada Volcanics are found in the southern part of the study area. Most of these rocks have been folded, faulted, and

  10. Hydrogeology of the western part of the Salt River Valley area, Maricopa County, Arizona

    Science.gov (United States)

    Brown, James G.; Pool, D.R.

    1989-01-01

    The Salt River Valley is a major population and agricultural center of more than 3,000 mi2 in central Arizona (fig. 1). The western part of the Salt River Valley area (area of this report) covers about 1,500 mi2. The Phoenix metropolitan area with a population of more than 1.6 million in 1985 (Valley National Bank, 1987) is located within the valley. The watersheds of the Salt, Verde, and Agua Fria Rivers provide the valley with a reliable but limited surface-water supply that must be augmented with ground water even in years of plentiful rainfall. Large-scale ground-water withdrawals began in the Salt River Valley in the early part of the 20th century; between 1915 and 1983, the total estimated ground-water pumpage was 81 million acre-ft (U.S. Geological Survey, 1984). Because of the low average annual rainfall and high potential evapotranspiration, the principal sources of ground-water recharge are urban runoff, excess irrigation, canal seepage and surface-water flows during years of higher-than-normal rainfall. Withdrawals greatly exceed recharge and, in some area, ground-water levels have declines as much as 350 ft (Laney and other, 1978; Ross, 1978). In the study area, ground-water declines of more than 300 ft have occurred in Deer Valley and from Luke Air Force Base north to Beardsley. As a result, a large depression of the water table has developed west of Luke Air Force Base (fig. 2). Ground-water use has decreased in recent years because precipitation and surface-water supplies have been greater than normal. Increased precipitation also caused large quantities of runoff to be released into the normally dry Salt and Gila River channels. From February 1978 to June 1980, streamflow losses of at least 90,000 acre-ft occurred between Jointhead Dam near the east boundary of the study area and Gillespie Dam several miles southwest of the west edge of the study area (Mann and Rhone, 1983). Consequently, ground-water declines in a large part of the basin have

  11. Irrigation runoff insecticide pollution of rivers in the Imperial Valley, California (USA)

    International Nuclear Information System (INIS)

    The Alamo and New Rivers located in the Imperial Valley, California receive large volumes of irrigation runoff and discharge into the ecologically sensitive Salton Sea. Between 1993 and 2002 we conducted a series of studies to assess water quality using three aquatic species: a cladoceran (Ceriodaphnia dubia), a mysid (Neomysis mercedis), and a larval fish (Pimephales promelas). Although no mortality was observed with the P. promelas, high-level toxicity to the invertebrate species was documented in samples from both rivers during many months of each year. Toxicity identifications and chemical analyses identified the organophosphorus insecticides (OP), chlorpyrifos and diazinon, as the cause of C. dubia toxicity. The extent of the C. dubia mortality was highly correlated with quantities of these OPs applied in the river watersheds. C. dubia mortality occurred during more months of our 2001/2002 study than in the 1990s investigations. During 2001/2002, the extensive C. dubia mortality observed in New River samples was caused by OP insecticide pollution that originated from Mexico. Mortality to N. mercedis in New River samples was likely caused by contaminants other than OP insecticides. Our studies document OP insecticide-caused pollution of the Alamo River over a 10-year period and provide the necessary information for remediation efforts. - Capsule: Organophosphorous insecticides in runoff water from the USA and Mexico have impacted rivers in the Imperial Valley, California

  12. Irrigation runoff insecticide pollution of rivers in the Imperial Valley, California (USA)

    Energy Technology Data Exchange (ETDEWEB)

    Vlaming, V. de [Aquatic Toxicology Laboratory, VM: APC, 1321 Haring Hall, University of California, Davis, CA 95616 (United States)]. E-mail: vldevlaming@ucdavis.edu; DiGiorgio, C. [Department of Water Resources, P.O. Box 942836, Sacramento, CA 94236 (United States); Fong, S. [Aquatic Toxicology Laboratory, VM: APC, 1321 Haring Hall, University of California, Davis, CA 95616 (United States); Deanovic, L.A. [Aquatic Toxicology Laboratory, VM: APC, 1321 Haring Hall, University of California, Davis, CA 95616 (United States); Paz Carpio-Obeso, M. de la [Colorado River Basin Region Water Quality Control Board, 73-720 Fred Waring Drive, Suite 100, Palm Desert, CA 92260 (United States); Miller, J.L. [AQUA-Science, 17 Arboretum Drive, Davis, CA 95616 (United States); Miller, M.J. [AQUA-Science, 17 Arboretum Drive, Davis, CA 95616 (United States); Richard, N.J. [Division of Water Quality, State Water Resources Control Board, 1001 I Street, Sacramento, CA 95814 (United States)

    2004-11-01

    The Alamo and New Rivers located in the Imperial Valley, California receive large volumes of irrigation runoff and discharge into the ecologically sensitive Salton Sea. Between 1993 and 2002 we conducted a series of studies to assess water quality using three aquatic species: a cladoceran (Ceriodaphnia dubia), a mysid (Neomysis mercedis), and a larval fish (Pimephales promelas). Although no mortality was observed with the P. promelas, high-level toxicity to the invertebrate species was documented in samples from both rivers during many months of each year. Toxicity identifications and chemical analyses identified the organophosphorus insecticides (OP), chlorpyrifos and diazinon, as the cause of C. dubia toxicity. The extent of the C. dubia mortality was highly correlated with quantities of these OPs applied in the river watersheds. C. dubia mortality occurred during more months of our 2001/2002 study than in the 1990s investigations. During 2001/2002, the extensive C. dubia mortality observed in New River samples was caused by OP insecticide pollution that originated from Mexico. Mortality to N. mercedis in New River samples was likely caused by contaminants other than OP insecticides. Our studies document OP insecticide-caused pollution of the Alamo River over a 10-year period and provide the necessary information for remediation efforts. - Capsule: Organophosphorous insecticides in runoff water from the USA and Mexico have impacted rivers in the Imperial Valley, California.

  13. Umpqua River Oregon Garden Valley PhotoMosaic 1939

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The Umpqua River drains 12,103 square kilometers (4,673 square miles) in southwest Oregon before flowing into the Pacific Ocean at Winchester Bay near the city of...

  14. Umpqua River Oregon Garden Valley PhotoMosaic 1967

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The Umpqua River drains 12,103 square kilometers (4,673 square miles) in southwest Oregon before flowing into the Pacific Ocean at Winchester Bay near the city of...

  15. The Brahmaputra River: a stratigraphic analysis of Holocene avulsion and fluvial valley reoccupation history

    Science.gov (United States)

    Hartzog, T. R.; Goodbred, S. L.

    2011-12-01

    The Brahmaputra River, one of the world's largest braided streams, is a major component of commerce, agriculture, and transportation in India and Bangladesh. Hence any significant change in course, morphology, or behavior would be likely to influence the regional culture and economy that relies on this major river system. The history of such changes is recorded in the stratigraphy deposited by the Brahmaputra River during the Holocene. Here we present stratigraphic analysis of sediment samples from the boring of 41 tube wells over a 120 km transect in the upper Bengal Basin of northern Bangladesh. The transect crosses both the modern fluvial valley and an abandoned fluvial valley about 60 km downstream of a major avulsion node. Although the modern Brahmaputra does not transport gravel, gravel strata are common below 20 m with fluvial sand deposits dominating most of the stratigraphy. Furthermore, the stratigraphy preserves very few floodplain mud strata below the modern floodplain mud cap. These preliminary findings will be assessed to determine their importance in defining past channel migration, avulsion frequency, and the reoccupation of abandoned fluvial valleys. Understanding the avulsion and valley reoccupation history of the Brahmaputra River is important to assess the risk involved with developing agriculture, business, and infrastructure on the banks of modern and abandoned channels. Based on the correlation of stratigraphy and digital surface elevation data, we hypothesize that the towns of Jamalpur and Sherpur in northern Bangladesh were once major ports on the Brahmaputra River even though they now lie on the banks of small underfit stream channels. If Jamalpur and Sherpur represent the outer extent of the Brahmaputra River braid-belt before the last major avulsion, these cities and any communities developed in the abandoned braid-belt assume a high risk of devastation if the next major avulsion reoccupies this fluvial valley. It is important to

  16. Composition Patterns of Waterbirds from La Vieja River, Geographic Valley of Cauca River, Colombia

    Directory of Open Access Journals (Sweden)

    Laura Milena Ramírez-Urrea

    2014-02-01

    Full Text Available We compiled and analyzed data gathered from observations during the period 2001-2013 in three sectors along La Vieja river, located in the Cauca river valley, Colombia. We describe spatial and temporal aspects of such dataset, focusing in indentify patterns of species’ composition and abundance. We recorded 28 waterbird species in 33 transects, being 22 species observed in more than 50 % of these transects. The species richness among transects did not shows significant differences. However, two cluster analyses, considering both presence/absence and abundance data, showed that there is spatial structure in the species composition along the river. In contrast, although observations were conducted during more than ten years there is no evidence of temporal changes in species composition. Still, some species showed increase ordecrease trends in their frequency. We present a new record for one species (Chloroceryle aenea for the region. Despite that the landscape surrounding La Vieja river have faced a high anthropogenic impact, the river still presents a significant diversity of waterbirds, which could add value to the conservation plans in the zone. PATRONES DE LA COMPOSICIÓN DE AVES ACUÁTICAS EN ELRÍO LA VIEJA, VALLE GEOGRÁFICO DEL RÍO CAUCA, COLOMBIARESUMENCompilamos y analizamos los datos de observaciones realizadas entre los años 2001 y 2013 en tres sectores a lo largo del cauce del río La Vieja, ubicado en el valle geográfico del río Cauca, Colombia. Describimos los datos espacial y temporalmente, enfocándonos en identificar patrones de composición y abundancia de especies. Registramos 28 especies de aves acuáticas en 33 transectos, siendo 22 especies observadas en más del 50 % de los transectos. Las diferencias en el número de especies por transecto no fueron significativas entre los tres sectores del río. Sin embargo, dos análisis de agrupamiento, considerando tanto los datos de presencia/ausencia como de

  17. Salinity in the Colorado River in the Grand Valley, western Colorado, 1994-95

    Science.gov (United States)

    Butler, David L.; von Guerard, Paul B.

    1996-01-01

    Salinity, or the dissolved-solids concentration, is the measure of salts such as sodium chloride, calcium bicarbonate, and calcium sulfate that are dissolved in water. About one-half of the salinity in the Colorado River Basin is from natural sources (U.S. Department of the Interior, 1995), such as thermal springs in the Glenwood-Dotsero area, located about 90 miles upstream from Grand Junction (fig. 1). Effects of human activities, such as irrigation, reservoir evaporation, and transbasin diversions, have increased the levels of salinity in the Colorado River. High salinity can affect industrial and municipal water users by causing increased water-treatment costs, increased deterioration of plumbing and appliances, increased soap needs, and undesirable taste of drinking water. High salinity also can cause lower crop yields by reducing water and nutrient uptake by plants and can increase agricultural production costs because of higher leaching and drainage requirements. Agricultural losses might occur when salinity reaches about 700?850 milligrams per liter (U.S Department of the Interior, 1994). Figure 1. Irrigated area in the Grand Valley and locations of sampling sites for the 1994?95 salinity study of the Colorado River. The Colorado River is the major source of irrigation water to the Grand Valley (fig. 1) and also is one source of water for the Clifton Water District, which supplies domestic water to part of the eastern Grand Valley. During spring and early summer in 1994, the Colorado River in the Grand Valley had lower than average streamflow. There was concern by water users about the effect of this low streamflow on salinity in the river. In 1994, the U.S. Geological Survey (USGS), in cooperation with the Colorado River Water Conservation District, began a study to evaluate salinity in the Colorado River. This fact sheet describes results of that study. The specific objectives of the fact sheet are to (1) compare salinity in the Colorado River among

  18. Teleconnection between the Indian summer monsoon onset and the Meiyu over the Yangtze River Valley

    Institute of Scientific and Technical Information of China (English)

    LIU YunYun; DING YiHui

    2008-01-01

    Based on the Indian and Chinese precipitation data and the NCEP-NCAR reanalysis circulation data,the relationship between the Indian summer monsoon (ISM) onset and the Meiyu over the Yangtze River Valley has been discussed by the methods of correlation analysis and composite analysis. The results show that the date of ISM onset over Kerala in the southwestern coast of the Indian Peninsula is about two weeks earlier than the beginning of the Meiyu over the Yangtze River Valley. After the outbreak of ISM,the teleconnection mode sets up from the western coast of India via the Bay of Bengal (BOB) to the Yangtze River Valley and southern Japan. It is different both in time and space from the teleconnection mode which is from the northwest of India via the Tibetan Plateau to northern China. The former mode is defined as the "south" teleconnection of the Asian summer monsoon,forming in the period of ISM onset; while the latter mode is called the "north" teleconnection,mainly occurring in the Asian monsoon culminant period. During the process of the "south" teleconnection's formation,the Asian monsoon circulation has experienced a series of important changes: ISM onset,the northward movement of the south Asia high (SAH),the onset vortex occurrence,the eastward extension of the stronger tropical westerly belt,and the northeastward jump of the western Pacific subtropical high(WPSH),etc. Consequently,since ISM sets up over Kerala,the whole Asian continent is covered by the upper SAH after about two weeks,while in the mid- and lower troposphere,a strong wind belt forms from the Arabian Sea via the southern India,BOB and the South China Sea (SCS),then along the western flank of WPSH,to the Yangtze River Valley and southern Japan. With the northward moving of the subtropical jet streams,the upper westerly jet stream and the low level jet have been coupled vertically over east Asia,while the Yangtze River Valley happens to locate in the ascending motion area between the upper jet

  19. 27 CFR 9.111 - Kanawha River Valley.

    Science.gov (United States)

    2010-04-01

    ....111 Section 9.111 Alcohol, Tobacco Products and Firearms ALCOHOL AND TOBACCO TAX AND TRADE BUREAU...) Addison, Ohio—W. Va., dated 1960; (2) Gallipolis, Ohio—W. Va., dated 1958; (3) Apple Grove, Ohio—W. Va... Ohio River (across the Gallipolis and Apple Grove quadrangles) southwesterly to the point at which...

  20. MODFLOW-USG model of groundwater flow in the Wood River Valley aquifer system in Blaine County, Idaho

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — A three-dimensional numerical groundwater flow model (MODFLOW-USG) was developed for the Wood River Valley (WRV) aquifer system, south-central Idaho, to evaluate...

  1. Boundary of the Eagle River Watershed Valley-Fill Aquifer, Eagle County, North-Central Colorado, 2006-2007

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This vector data set delineates the approximate boundary of the Eagle River watershed valley-fill aquifer (ERWVFA). This data set was developed by a cooperative...

  2. Report on counts of migrating raptors along the Mississippi River Valley conducted during the fall of 1992

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Counts of migrating raptors were conducted along the Mississippi River Valley during the fall of 1992 for 211.3 hours (34 days) at Effigy Mounds National Monument....

  3. The Importance of Lower Mississippi River Alluvial Valley Reforestation and Wetland Restoration Sites to Wintering Migratory Birds; Annual Report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Major efforts have been initiated in the Lower Mississippi River Alluvial Valley (LMA V. Fig. I) from within both the U.S. Departments of Interior and Agriculture...

  4. Recycling of Pleistocene valley fills dominates 135 ka of sediment flux, upper Indus River

    Science.gov (United States)

    Munack, H.; Blöthe, J. H.; Fülöp, R. H.; Codilean, A. T.; Fink, D.; Korup, O.

    2016-10-01

    Rivers draining the semiarid Transhimalayan Ranges at the western Tibetan Plateau margin underwent alternating phases of massive valley infill and incision in Pleistocene times. The effects of these cut-and-fill cycles on millennial sediment fluxes have remained largely elusive. We investigate the timing and geomorphic consequences of headward incision of the Zanskar River, a tributary to the Indus, which taps the >250-m thick More Plains valley fill that currently plugs the endorheic high-altitude basins of Tso Kar and Tso Moriri. In situ 10Be exposure dating and topographic analyses show that a phase of valley infill gave way to net dissection and the NW Himalaya's first directly dated stream capture in late Marine Isotope Stage (MIS) 6, ∼135 ka ago. Headwaters of the Indus are currently capturing headwaters of the Sutlej, and rivers have eroded >14.7 km3 of sediment from the Zanskar headwaters since, mobilising an equivalent of ∼8% of the Indus' contemporary sediment storage volume from only 0.3% of its catchment area. The resulting specific sediment yields are among the rarely available rates averaged over the 105-yr timescale, and surpass 10Be-derived denudation rates from neighbouring catchments three- to tenfold. We conclude that recycling of Pleistocene valley fills has fed Transhimalayan headwaters with more sediment than liberated by catchment denudation, at least since the last glacial cycle began. This protracted release of sediment from thick Pleistocene valley fills might bias estimates of current sediment loads and long-term catchment denudation.

  5. Groundwater Dynamics in Part of the Sava River Valley

    Directory of Open Access Journals (Sweden)

    Dragutin Dolanjski

    1999-03-01

    Full Text Available The main research object was to determine the dynamics of groundwater in the area Oborovo. Major hydrological indicators (precipitation, Sava water level, groundwater level in hydro-pedological and hydro-geological piezometers were analyzed per monthly decades during a fiveyear period. Relation of the analyzed hidrological indicators was determined using the method of cross-correlation analysis. A slight increasing trend was determined for precipitation and middle water of the Sava during the trial period. Marked differences in groundwater dynamics were also recorded. The highest monthly and annual fluctuations of groundwater level were recorded in the immediate vicinity of the Sava. Going away from the river, the fluctuation got much less expressed. Direct influence of the Sava water level upon groundwater dynamics was determined within a narrow belt next to the river. The prevailing direction of the groundwater course is from the elevated peripheral parts of the Sava basin toward the Sava River. The Sava and the other surface watercourses, Zelina, Črnec and the Lonja-Strug Canal, have no considerable influence on the genesis and dynamics of groundwater in the area under study.

  6. Foraging Ecology of Fall-Migrating Shorebirds in the Illinois River Valley

    OpenAIRE

    Smith, Randolph V.; Joshua D Stafford; Yetter, Aaron P.; Michelle M Horath; Christopher S Hine; Hoover, Jeffery P.

    2012-01-01

    Populations of many shorebird species appear to be declining in North America, and food resources at stopover habitats may limit migratory bird populations. We investigated body condition of, and foraging habitat and diet selection by 4 species of shorebirds in the central Illinois River valley during fall migrations 2007 and 2008 (Killdeer [Charadrius vociferus], Least Sandpiper [Calidris minutilla], Pectoral Sandpiper [Calidris melanotos], and Lesser Yellowlegs [Tringa flavipes]). All speci...

  7. Soil Stratigraphy from Three Pleistocene Archaeological Sites of the Middle Ter River Valley, Catalonia, Spain

    OpenAIRE

    Sayantani NEOGI

    2010-01-01

    This dissertation summarizes the stratigraphic description of three Pleistocene archaeological sites inthe middle Ter river valley. A long history of archaeological research in this region suggests thepossibility of developing contextual studies. This work is basically an investigation of two soilformation processes from the deep soil horizons of the Mediterranean region: clay illuviation andcarbonatation. This approach has been developed by soil micromorphology, a technique well suitedfor th...

  8. Coupled flow and salinity transport modelling in semi-arid environments: The Shashe River Valley, Botswana

    Science.gov (United States)

    Bauer, Peter; Held, Rudolf J.; Zimmermann, Stephanie; Linn, Flenner; Kinzelbach, Wolfgang

    2006-01-01

    Numerical groundwater modelling is used as the base for sound aquifer system analysis and water resources assessment. In many cases, particularly in semi-arid and arid regions, groundwater flow is intricately linked to salinity transport. A case in point is the Shashe River Valley in Botswana. A freshwater aquifer located around an ephemeral stream is depleted by the combined effect of transpiration and pumping. Quantitative system analysis reveals that the amount of water taken by transpiration is far more than the quantities pumped for water supply. Furthermore, the salinity distribution in and around Shashe River Valley as well as its temporal dynamics can be satisfactorily reproduced if the transpiration is modelled as a function of groundwater salinity. The location and dynamics of the saltwater-freshwater interface are highly sensitive to the parameterization of evaporative and transpirative salt enrichment. An existing numerical code for coupled flow/transport simulations (SEAWAT) was adapted to this situation. Model results were checked against a large set of field data including water levels, water chemistry, isotope data and ground and airborne geophysical data. The resulting groundwater model was able to reproduce the long-term development of the freshwater lens located in Shashe River Valley as well as the decline in piezometric heads observed over the last decade. Furthermore, the old age of the saline water surrounding the central freshwater lens could be explained.

  9. SIR2012-5282 Surficial Geology: Hydrogeology of the Susquehanna River valley-fill aquifer system and adjacent areas in eastern Broome and southeastern Chenango Counties, New York

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The hydrogeology of the valley-fill aquifer system along a 32-mile reach of the Susquehanna River valley and adjacent areas was evaluated in eastern Broome and...

  10. BALSA: integrated secondary analysis for whole-genome and whole-exome sequencing, accelerated by GPU

    Directory of Open Access Journals (Sweden)

    Ruibang Luo

    2014-06-01

    Full Text Available This paper reports an integrated solution, called BALSA, for the secondary analysis of next generation sequencing data; it exploits the computational power of GPU and an intricate memory management to give a fast and accurate analysis. From raw reads to variants (including SNPs and Indels, BALSA, using just a single computing node with a commodity GPU board, takes 5.5 h to process 50-fold whole genome sequencing (∼750 million 100 bp paired-end reads, or just 25 min for 210-fold whole exome sequencing. BALSA’s speed is rooted at its parallel algorithms to effectively exploit a GPU to speed up processes like alignment, realignment and statistical testing. BALSA incorporates a 16-genotype model to support the calling of SNPs and Indels and achieves competitive variant calling accuracy and sensitivity when compared to the ensemble of six popular variant callers. BALSA also supports efficient identification of somatic SNVs and CNVs; experiments showed that BALSA recovers all the previously validated somatic SNVs and CNVs, and it is more sensitive for somatic Indel detection. BALSA outputs variants in VCF format. A pileup-like SNAPSHOT format, while maintaining the same fidelity as BAM in variant calling, enables efficient storage and indexing, and facilitates the App development of downstream analyses. BALSA is available at: http://sourceforge.net/p/balsa.

  11. Natural Regeneration after Long-Term Bracken Fern Control with Balsa (Ochroma pyramidale in the Neotropics

    Directory of Open Access Journals (Sweden)

    Samuel I. Levy-Tacher

    2015-06-01

    Full Text Available In many parts of the Neotropics, deforested areas are often colonized by the highly competitive invasive bracken fern (Pteridium aquilinum, which inhabits naturally regenerated forests and successional forests on abandoned farmland. Within the tropical forest region of Chiapas in southern Mexico, we implemented an experiment in 2005 to out-compete bracken fern infestation and reduce or eliminate live bracken rhizomes using several treatments: Direct sowing of balsa seeds (Ochroma pyramidale; Malvaceae, a traditional Lacandon treatment of scattering balsa seeds, transplanting balsa seedlings, and a control treatment (without balsa. For each treatment, we applied three different bracken weeding frequencies: No weeding, biweekly weeding, and monthly weeding. In this study, we present data gathered four years after establishing the experiment regarding: Bracken fern rhizome biomass, balsa density, basal area, height, density, species richness of naturally regenerating vegetation for all treatments, and bracken weeding frequencies. We also evaluated the importance of balsa and its regenerative attributes in controlling bracken fern by correlating it with remaining belowground live rhizome biomass. Living rhizome biomass was completely eradicated in all treatments with biweekly and monthly weeding. Density and species richness of a naturally regenerated species were negatively correlated with bracken fern rhizome biomass, and the density of this species was highest in areas with no rhizome biomass. Although balsa tree stands are effective short-term solutions for controlling rhizome biomass, the success of natural regeneration following balsa establishment can be critical to long-term elimination of bracken fern.

  12. Digital elevation model based geomorphological mapping in the lower River Boyne valley, Ireland

    Science.gov (United States)

    Foster, Gez; Turner, Jonathan; Gallagher, Colman; Lewis, Helen

    2010-05-01

    Interpretation of digital elevation models (DEMs) is rapidly becoming a valuable extension to field-based geomorphic mapping. High-resolution LiDAR data (Light Detection and Ranging; point spacing 1m, vertical accuracy 0.1m) is ideally-suited for mapping areas of complex and subtle geomorphology, such as fluvial landscapes. This poster outlines how LiDAR data are being used to map and characterise the postglacial fluvial terraces of the lower Boyne valley, Co. Meath, Ireland. Comprehensive mapping, together with longitudinal profiles, demonstrate that the valley contains a suite, or ‘staircase', of six main fluvial terraces, spanning an altitude range of ca. 20m. These terraces represent a chronosequence of ‘palaeo' floodplains, with the highest (T1) being the oldest level, and the lowest (T6) the youngest. The evolution of the valley has thus involved progressive erosion, punctuated by episodes of vertical stability or re-filling. Classified maps of the river terrace sequence indicate that terrace T1 is closely associated with glacial landforms, while T2 exhibits multiple channels with large bar-forms, and could mark a braided river system that conveyed huge water and sediment loads during deglaciation ca. 20-17 ka BP. The ‘modern' floodplain (T6) is ubiquitous, and preliminary field studies have dated two of its palaeochannels to >1,000 cal. BP. The LiDAR based model of geomorphic evolution in the lower Boyne valley is being used to underpin field-based geomorphological and sediment studies, focusing on the acquisition of OSL and radiocarbon dates to secure the timing of river terrace formation and to assess the relationships between fluvial development and environmental change since the Late Glacial period.

  13. Hydrogeology and ground-water/surface water interactions in the Des Moines River valley, southwestern Minnesota, 1997-2001

    Science.gov (United States)

    Cowdery, Timothy K.

    2005-01-01

    Increased water demand in and around Windom led the U.S. Geological Survey, in cooperation with the Minnesota Department of Natural Resources, local water suppliers, and Cottonwood County, to study the hydrology of aquifers in the Des Moines River Valley near Windom. The study area is the watershed of a 30-kilometer (19-mile) reach of the Des Moines River upstream from Windom.

  14. A Study of Earlier Neolithic Tombs in the Yellow River Valley%黄河流域前期新石器时代墓葬的研究

    Institute of Scientific and Technical Information of China (English)

    白云翔; 张建锋

    2001-01-01

    Archaeologists have found some 800 early Neolithic burials dating to before 5000 BC in the Yellow River valley, which belong to the Dadiwan, Peiligang, Houli, and Beixin cultures. These burials shared remarkable similarities, since they situated in the same social developmental stage with similar cultural tradition, geographical environment, and subsistent economy. Although some similarities also shared by the burials of the Yellow River valley and those of the Yangzi River valley, the differences between the two regions were obvious.

  15. Watermills – a Forgotten River Valley Heritage – selected examples from the Silesian voivodeship, Poland

    Directory of Open Access Journals (Sweden)

    Fajer Maria

    2014-06-01

    Full Text Available This study is an attempt to describe the current condition of the watermills situated in the river valleys of the Silesian voivodeship. Changes in the number and distribution of mills from the late 18th century until the 20th century have been presented (as exemplified by the Liswarta River basin in the northern part of the voivodeship. Watermills have been discussed both as industrial monuments that document the history of the milling industry and as tourist attractions. Currently, working mills that serve the local population in rural areas are a rarity, and working watermills are unique sites that should be protected as industrial monuments that constitute an important part of our cultural heritage. They are among those industrial monuments that are particularly vulnerable to destruction. Such mills increasingly attract the interest of industrial tourism promoters. Activities aimed at promoting watermills as cultural heritage sites and leading to their protection and preservation as part of the river valley landscape have also been discussed. In the Silesian voivodeship, there are many watermills that deserve attention; some of these are listed in the register of monuments maintained by the National Heritage Board of Poland. Unfortunately, most disused mills are falling into disrepair and are slowly disappearing; only a few have been preserved in good condition. Many of these have long histories and they are also situated in areas attractive for tourists. There is no doubt that watermills should be preserved. Their inclusion in open-air museums is not the only solution – any form of protection in situ by putting them to different uses is also valuable. Changing the function of a mill to serve as a hotel, restaurant, cultural centre, etc. makes it possible to maintain these sites as parts of river valley landscapes.

  16. Snake River Sockeye Salmon Sawtooth Valley Project Conservation and Rebuilding Program : Supplemental Fnal Environmental Assessment.

    Energy Technology Data Exchange (ETDEWEB)

    United States. Bonneville Power Administration.

    1995-03-01

    This document announces Bonneville Power Administration`s (BPA) proposal to fund three separate but interrelated actions which are integral components of the overall Sawtooth Valley Project to conserve and rebuild the Snake River Sockeye salmon run in the Sawtooth Valley of south-central Idaho. The three actions are as follows: (1) removing a rough fish barrier dam on Pettit Lake Creek and constructing a weir and trapping facilities to monitor future sockeye salmon adult and smolt migration into and out of Pettit Lake; (2) artificially fertilizing Readfish Lake to enhance the food supply for Snake River sockeye salmon juveniles released into the lake; and (3) trapping kokanee fry and adults to monitor the fry population and to reduce the population of kokanee in Redfish Lake. BPA has prepared a supplemental EA (included) which builds on an EA compled in 1994 on the Sawtooth Valley Project. Based on the analysis in this Supplemental EA, BPA has determined that the proposed actions are not major Federal actions significantly affecting the quality of the human environment. Therefore an Environmental Impact Statement is not required.

  17. Centipede (Chilopoda richness and diversity in the Bug River valley (Eastern Poland

    Directory of Open Access Journals (Sweden)

    Malgorzata Lesniewska

    2015-06-01

    Full Text Available The main aim of the survey was to describe the diversity and richness of Chilopoda in the selected area of the Bug River valley. The study sites were located in two regions differing in the shape of the valley, the presence of thermophilous habitats and the size of riparian forests. Pitfall traps were used as a sampling method. As a result, 444 specimens belonging to 12 centipede species of two orders – Geophilomorpha (four species and Lithobiomorpha (eight species were caught. Lithobius (Monotarsobius curtipes C.L.Koch, 1847, Pachymerium ferrugineum (C.L.Koch, 1835, Lamyctes (Lamyctes emarginatus (Newport, 1844 and Lithobius (Monotarsobius dudichi Loksa, 1947 were the most common and the most numerous species. Of particular note is L. dudichi found in Poland for the first time and previously known based on a single specimen. Two to 10 Chilopoda species were found in each habitat under investigation. The greatest species richness was found in thermophilous thickets (10 species, sandy grasslands (eight, xerothermic grasslands (eight and mesic meadows (six. The fewest number of species (two was found in rushes at oxbows and in wet meadows. We found differences in the species composition and the number of Chilopoda between the lower (102 specimens, six species and the middle (324 specimens, 11 species section of the river valley. Our results confirm the need to protect xerothermic habitats, unique almost throughout entire Central Europe, which due to their distribution and their small area covered are fairly easily subject to the process of destruction.

  18. Tectonic controls on the morphodynamics of the Brahmaputra River system in the upper Assam valley, India

    Science.gov (United States)

    Lahiri, Siddhartha K.; Sinha, Rajiv

    2012-10-01

    The Brahmaputra is one of the largest tropical rivers of the world and is located in an area of high structural instability as evidenced from the presence of a large number of earthquakes in the Himalayan catchment through which it flows. Syntectonic evidence of changes in the morphodynamics is difficult to identify for the large rivers. Nevertheless, we note that the Brahmaputra River has become astonishingly large in planform in a historical timescale. Reconstruction of planform changes over a period of 90 years in the upper reaches of the Assam valley shows that the 240-km-long channel belt is widening all along its course in the region. From the average width of 9.74 km in 1915, the channel belt has widened to the average width of 14.03 km in 2005 (44% widening), and in certain reaches the average widening is as high as 250%. However, the bank line shift is not symmetric along both banks. Further, the planform characteristics of the Brahmaputra River reveal significant spatial and temporal variability from upstream to downstream reaches, and we attribute this variability to tectonogeomorphic zonation of the river based on subsurface configuration and channel slope. Further, the tributaries joining the northern and southern banks of the Brahmaputra differ remarkably in terms of river dynamics, and this is attributed to the differences in tectonic regimes of the Himalaya in the north and the Naga Patkai hills in the south.

  19. Is history of rivers important in restoration projects? The example of human impact on a lowland river valley (the Obra River, Poland)

    Science.gov (United States)

    Słowik, Marcin

    2015-12-01

    Palaeoenvironmental and palaeohydrological reconstructions can provide important guidance for river restoration projects. This paper reconstructs the trajectory of river pattern changes of a lowland river (the Obra River, western Poland) as a basis to inform realistic restoration activities. The history of river changes is reconstructed for the last 12,700 radiocarbon years BP. The sequence and timing of change differ from widely recognized, conventional assessments of transitions from braided to meandering planforms in the Polish Lowlands. Traces of a laterally migrating anabranching system were found in the middle Obra valley. In its lower course, a transition from a braided to meandering planform took place later than in other rivers of the Polish Lowlands. Sediment delivery from parts of the catchment situated downstream of lakes in the river course could have been the main reason for maintenance of the braided pattern. Restoration scenarios that take into account the trajectory of river planform changes are hypothesized in relation to variations of sediment supply and degree of anthropogenic impact.

  20. Grain-size cycles in Salawusu River valley since 150 ka BP

    Institute of Scientific and Technical Information of China (English)

    2001-01-01

    The palaeo-mobile dune sands and fluvio-lacustrine facies with palaeosols in Milanggouwan stratigraphic section of the Salawusu River valley situated at the southeast of the Mu Us Desert experienced abundant remarkable alternative changes of coarse and fine rhythms in grainsize since 150 ka BP, and the grain-size parameters - Mz, σ, Sk, Kg and SC/I also respond to the situation of multi-fluctuational alternations between peak and valley values. Simultaneity the grainsize eigenvalues - Ф5, Ф16, P25, Ф50, Ф75, Ф84 and Ф95 are respondingly manifested as greatly cadent jumpiness. Hereby, the Milanggouwan section can be divided into 27 grain-size coarse and fine sedimentary cycles, which can be regarded as a real and integreted record of climate-geological process of desert vicissitude resulted from the alternative evolvement of the ancient winter and summer monsoons of East Asia since 150 ka BP.

  1. A study of temperature's spatial distribution in Neuquen River valley through satellite imaging

    Directory of Open Access Journals (Sweden)

    Marisa Gloria Cogliati

    2010-01-01

    Full Text Available This paper looks into the spatial distribution of brightness and surface temperature through the use of LAND SAT7 ETM+ and NO AA-AVHRR satellite imagery in the cultivated valley of the Neuquén river. Studying the spatial distribution of temperatures in an area with a somewhat complex terrain requires the use of a great density of meteorological measurements. It is often impossible to obtain the right density of the argometeorological network due to the high installation and maintenance costs. Remote sensors provide a large flow of information in various resolutions, at considerably lower costs. Determining the valley's warm and cold zones would allow for more efficient irrigation and frost-protection methods, and it would provide tools to improve the area's productive planning.

  2. Groundwater-flow model for the Wood River Valley aquifer system, south-central Idaho

    Science.gov (United States)

    Fisher, Jason C.; Bartolino, James R.; Wylie, Allan H.; Sukow, Jennifer; McVay, Michael

    2016-06-27

    A three-dimensional numerical model of groundwater flow was developed for the Wood River Valley (WRV) aquifer system, Idaho, to evaluate groundwater and surface-water availability at the regional scale. This mountain valley is located in Blaine County and has a drainage area of about 2,300 square kilometers (888 square miles). The model described in this report can serve as a tool for water-rights administration and water-resource management and planning. The model was completed with support from the Idaho Department of Water Resources, and is part of an ongoing U.S. Geological Survey effort to characterize the groundwater resources of the WRV. A highly reproducible approach was taken for constructing the WRV groundwater-flow model. The collection of datasets, source code, and processing instructions used to construct and analyze the model was distributed as an R statistical-computing and graphics package.

  3. Seismic local site effects characterization in the Andarax River Valley (SE Spain) from ambient seismic noise

    Science.gov (United States)

    Carmona, Enrique; García-Jerez, Antonio; Luzón, Francisco; Sánchez-Martos, Francisco; Sánchez-Sesma, Francisco J.; Piña, José

    2014-05-01

    This work is focused on the characterization of seismic local effects in the Low Andarax River Valley (SE Spain). The Low Andarax River valley is located in an active seismic region, with the higher seismic hazard values in Spain. The landform is composed mainly by sedimentary materials which increase its seismic hazard due to the amplification of the seismic inputs and spectral resonances. We study seismic local effects in the Low Andarax River by analyzing the Horizontal-to-Vertical Spectral Ratio (HVSR) of ambient noise records. The noise data were recorded during two field campaigns in 2012 and 2013. There have been a total of 374 noise measurements with 15 and 30 minutes duration. The acquisition was performed with a Digital Broadband Seismometer Guralp CMG-6TD. The distance between measurements was about 200 meters, covering an area around 40 km2. There have been 6 significant peak frequencies between 0.3 Hz and 5 Hz. It was possible to find interesting areas with similar spectral peaks that coincide with zones with similar microgravimetric anomalies at the alluvial valley. It is also observed a decrease in the frequency peaks from West to East suggesting increased sediment layer. We also compute the soil models at those sites where geotechnical information is available, assuming that the seismic noise is diffuse. We invert the HVSR for these places using horizontally layered models and in the imaginary part the Green functions at the source. It is observed that the S wave velocity inverted models are consistent with the known geotechnical information obtained from drilled boreholes. We identify the elastodynamic properties of the limestone-dolomite materials with a formation of phyllites and quartzite that form the basement of the depression, and those properties of the Miocene and Pliocene detrital deposits (marls, sandy silts, sands and conglomerates) that fill the valley. These results together with the observed resonant frequencies along the Andarax

  4. Examining the spatial and temporal variation of groundwater inflows to a valley-to-floodplain river using 222Rn, geochemistry and river discharge: the Ovens River, southeast Australia

    Directory of Open Access Journals (Sweden)

    M. C. L. Yu

    2013-04-01

    Full Text Available Radon (222Rn and major ion geochemistry were used to define and quantify the catchment-scale river-aquifer interactions along the Ovens River in the southeast Murray-Darling Basin, Victoria, Australia, between September 2009 and October 2011. The Ovens River is characterized by the transition from a single channel river residing within a mountain valley in the upper catchment to a multi-channel meandering river on flat alluvial plains in the lower catchment. Overall, the river is dominated by gaining reaches, receiving groundwater from both alluvial and basement aquifers. The distribution of gaining and losing reaches is governed by catchment morphology and lithology. In the upper catchment, rapid groundwater recharge through sediments that have high hydraulic conductivities in a narrow valley produces higher baseflow to the river during wet (high flow periods as a result of hydraulic loading. In the lower catchment, the open and flat alluvial plains, lower rainfall and finer-gained sediments reduce the magnitude and variability of hydraulic gradient between the aquifer and the river, producing lower and constant groundwater inflow. With a small difference between the water table and the river height, small changes in river height or in groundwater level can result fluctuating gaining and losing behaviour along the river. The middle catchment represents a transition in river-aquifer interactions from upper to lower catchment. High baseflow in some parts of the middle and lower catchments is caused by groundwater flow over basement highs. Mass balance calculations based on 222Rn activities indicate that groundwater inflow is 4–22% of total flow with higher baseflow occurring in high flow periods. Uncertainties in gas exchange coefficient and 222Rn activities of groundwater alter the calculated groundwater inflow to 3–35%. Ignoring hyporheic exchange appears not to have a significant impact on the total groundwater estimates. In comparison to

  5. The Ohio River Valley CO2 Storage Project AEP Mountaineer Plan, West Virginia

    Energy Technology Data Exchange (ETDEWEB)

    Neeraj Gupta

    2009-01-07

    This report includes an evaluation of deep rock formations with the objective of providing practical maps, data, and some of the issues considered for carbon dioxide (CO{sub 2}) storage projects in the Ohio River Valley. Injection and storage of CO{sub 2} into deep rock formations represents a feasible option for reducing greenhouse gas emissions from coal-burning power plants concentrated along the Ohio River Valley area. This study is sponsored by the U.S. Department of Energy (DOE) National Energy Technology Laboratory (NETL), American Electric Power (AEP), BP, Ohio Coal Development Office, Schlumberger, and Battelle along with its Pacific Northwest Division. An extensive program of drilling, sampling, and testing of a deep well combined with a seismic survey was used to characterize the local and regional geologic features at AEP's 1300-megawatt (MW) Mountaineer Power Plant. Site characterization information has been used as part of a systematic design feasibility assessment for a first-of-a-kind integrated capture and storage facility at an existing coal-fired power plant in the Ohio River Valley region--an area with a large concentration of power plants and other emission sources. Subsurface characterization data have been used for reservoir simulations and to support the review of the issues relating to injection, monitoring, strategy, risk assessment, and regulatory permitting. The high-sulfur coal samples from the region have been tested in a capture test facility to evaluate and optimize basic design for a small-scale capture system and eventually to prepare a detailed design for a capture, local transport, and injection facility. The Ohio River Valley CO{sub 2} Storage Project was conducted in phases with the ultimate objectives of demonstrating both the technical aspects of CO{sub 2} storage and the testing, logistical, regulatory, and outreach issues related to conducting such a project at a large point source under realistic constraints. The site

  6. Stream seepage and groundwater levels, Wood River Valley, south-central Idaho, 2012-13

    Science.gov (United States)

    Bartolino, James R.

    2014-01-01

    Stream discharge and water levels in wells were measured at multiple sites in the Wood River Valley, south-central Idaho, in August 2012, October 2012, and March 2013, as a component of data collection for a groundwater-flow model of the Wood River Valley aquifer system. This model is a cooperative and collaborative effort between the U.S. Geological Survey and the Idaho Department of Water Resources. Stream-discharge measurements for determination of seepage were made during several days on three occasions: August 27–28, 2012, October 22–24, 2012, and March 27–28, 2013. Discharge measurements were made at 49 sites in August and October, and 51 sites in March, on the Big Wood River, Silver Creek, their tributaries, and nearby canals. The Big Wood River generally gains flow between the Big Wood River near Ketchum streamgage (13135500) and the Big Wood River at Hailey streamgage (13139510), and loses flow between the Hailey streamgage and the Big Wood River at Stanton Crossing near Bellevue streamgage (13140800). Shorter reaches within these segments may differ in the direction or magnitude of seepage or may be indeterminate because of measurement uncertainty. Additional reaches were measured on Silver Creek, the North Fork Big Wood River, Warm Springs Creek, Trail Creek, and the East Fork Big Wood River. Discharge measurements also were made on the Hiawatha, Cove, District 45, Glendale, and Bypass Canals, and smaller tributaries to the Big Wood River and Silver Creek. Water levels in 93 wells completed in the Wood River Valley aquifer system were measured during October 22–24, 2012; these wells are part of a network established by the U.S. Geological Survey in 2006. Maps of the October 2012 water-table altitude in the unconfined aquifer and the potentiometric-surface altitude of the confined aquifer have similar topology to those on maps of October 2006 conditions. Between October 2006 and October 2012, water-table altitude in the unconfined aquifer rose by

  7. A MACRO-SCALE SEMI-DISTRIBUTED HYDROLOGICAL MODEL AND APPLICATION TO THE DATONG RIVER VALLEY

    Institute of Scientific and Technical Information of China (English)

    YANG Zhi-feng; LIU Lu-liu; SHEN Zhen-yao; GORDON G. Huang

    2005-01-01

    A daily distributed hydrological model was developed using routine hydro-meteorological data on the basis of the raster DEM and land cover data.Then the model was used to model daily runoff of the Datong River Valley located in the upper catchment of the Yellow River Basin.The runoff comprises surface flow, subsurface flow and ground water flow.Evapotranspiration comprises canopy evaporation, snow sublimation and soil evapotranspiration.The infiltration to the soil was estimated with improved Green-Ampt model, and the potential evapotranspiration is estimated with Morton CRAE method, which only needs the routine meteorological data.Simulation results and the comparison with semi-distributed SLURP hydrological model show that the structure of the model presented herein is reasonable.

  8. Late Quaternary tectonic landforms and fluvial aggradation in the Saryu River valley: Central Kumaun Himalaya

    Science.gov (United States)

    Kothyari, Girish Ch.; Luirei, Khayingshing

    2016-09-01

    The present study has been carried out with special emphasis on the aggradational landforms to explain the spatial and temporal variability in phases of aggradation/incision in response to tectonic activity during the late Quaternary in the Saryu River valley in central Kumaun Himalaya. The valley has preserved cut-and-fill terraces with thick alluvial cover, debris flow terraces, and bedrock strath terraces that provide signatures of tectonic activity and climate. Morphostratigraphy of the terraces reveals that the oldest landforms preserved south of the Main Central Thrust, the fluvial modified debris flow terraces, were developed between 30 and 45 ka. The major phase of valley fill is dated between 14 and 22 ka. The youngest phase of aggradation is dated at early and mid-Holocene (9-3 ka). Following this, several phases of accelerated incision/erosion owing to an increase in uplift rate occurred, as evident from the strath terraces. Seven major phases of bedrock incision/uplift have been estimated during 44 ka (3.34 mm/year), 35 ka (1.84 mm/year), 15 ka (0.91 mm/year), 14 ka (0.83 mm/year), 9 ka (1.75 mm/year), 7 ka (5.38 mm/year), and around 3 ka (4.4 mm/year) from the strath terraces near major thrusts. We postulate that between 9 and 3 ka the terrain witnessed relatively enhanced surface uplift (2-5 mm/year).

  9. Sedimentary cycles of trace elements in Salawusu River Valley since 150 ka BP

    Institute of Scientific and Technical Information of China (English)

    2002-01-01

    The paper makes some analyses on 11 trace elements in the Milanggouwan stratigraphical section in the Salawusu River valley, which is regarded as a prototype geology-palaeoclimate record since 150 ka BP. The results show that the content and variation of trace elements has experienced remarkably regular changes in the pace with coarse and fine sedimentary cycles of palaeo-aeolian sands to its overlying fluvio-lacustrine facies or/and palaeosols. The trace elements with chemical properties of relatively active (V, Sr, Cu, Ni, As) and relatively stable (P, Pb, Rb, Mn, Nb, Zr) are a manifestation of the corresponding 27 changeable cycles between peak and valley values, appearing a multi-fluctuational process line of relative gathering and migration since then. The low numerical value distribution of these two types of trace elements in the aeolian sand facies represents erosion and accumulation under wind force during the cold-dry climate. Whereas their enrichments in both fluvio-lacustrine facies and palaeosols are related to the valley's special low-lying physiognomic position between the Ordos Plateau and the Loess Plateau under the warm and humid climate conditions. The above relatively migrated and gathered change of the trace elements is the result of 27 climatic cycles of cold-dry and warm-humid, which is probably caused by repeated alternations of winter monsoon and summer monsoon in the Mu Us Sandy Land influenced by the climate vicissitudes in northern hemisphere during glacial and interglacial periods since 150 ka BP.

  10. Water quality and processes affecting dissolved oxygen concentrations in the Blackwater River, Canaan Valley, West Virginia

    Science.gov (United States)

    Waldron, M.C.; Wiley, J.B.

    1996-01-01

    The water quality and environmental processes affecting dissolved oxygen were determined for the Blackwater River in Canaan Valley, West Virginia. Canaan Valley is oval-shaped (14 miles by 5 miles) and is located in the Allegheny Mountains at an average elevation of 3,200 feet above sea level. Tourism, population, and real estate development have increased in the past two decades. Most streams in Canaan Valley are a dilute calcium magnesium bicarbonate-type water. Streamwater typicaly was soft and low in alkalinity and dissolved solids. Maximum values for specific conductance, hardness, alkalinity, and dissolved solids occurred during low-flow periods when streamflow was at or near baseflow. Dissolved oxygen concentrations are most sensitive to processes affecting the rate of reaeration. The reaeration is affected by solubility (atmospheric pressure, water temperature, humidity, and cloud cover) and processes that determine stream turbulence (stream depth, width, velocity, and roughness). In the headwaters, photosynthetic dissolved oxygen production by benthic algae can result in supersaturated dissolved oxygen concentrations. In beaver pools, dissolved oxygen consumption from sediment oxygen demand and carbonaceous biochemical oxygen demand can result in dissolved oxygen deficits.

  11. GIS-based terrain analysis of linear infrastructure corridors in the Mackenzie River Valley, NWT

    International Nuclear Information System (INIS)

    The impact of global warming on permafrost terrain was discussed with particular reference to the structural stability and performance reliability of the proposed pipelines and roads in the Mackenzie River Valley in the Northwest Territories. Engineers, regulators and decision makers responsible for the development of these networks must have access to information about current and future terrain conditions, both local and regional. The Geological Survey of Canada is developing an ArcGIS resident, multi-component terrain analysis methodology for evaluating permafrost terrain in terms of the probable geothermal and geomorphological responses to climate warming. A GIS-integrated finite-element transient ground thermal model (T-ONE) can predict local-regional permafrost conditions and future responses of permafrost to climate warming. The influences of surface and channel hydrology on local erosion potentials can be determined by analyzing the topographic and topologic characteristics of the terrain. A weights of evidence-based landscape-process model, currently under development, will consider multiple terrain factors for mapping terrain that is susceptible to slope failure, subsidence or erosion. This terrain analysis methodology is currently being applied to a 2 km buffer spanning the proposed Mackenzie Gas Pipeline right-of-way, and along winter and all-weather road networks in the Mackenzie River Valley. Initial ground thermal modeling has identified thermally sensitive terrain for which permafrost will either completely disappear or warm significantly to near isothermal conditions within the next 25 to 55 years

  12. Influence of hydrologic modifications on Fraxinus pennsylvanica in the Mississippi River Alluvial Valley, USA

    Science.gov (United States)

    Gee, Hugo K.W.; King, Sammy L.; Keim, Richard F.

    2015-01-01

    We used tree-ring analysis to examine radial growth response of a common, moderately flood-tolerant species (Fraxinus pennsylvanica Marshall) to hydrologic and climatic variability for > 40 years before and after hydrologic modifications affecting two forest stands in the Mississippi River Alluvial Valley (USA): a stand without levees below dams and a stand within a ring levee. At the stand without levees below dams, spring flood stages decreased and overall growth increased after dam construction, which we attribute to a reduction in flood stress. At the stand within a ring levee, growth responded to the elimination of overbank flooding by shifting from being positively correlated with river stage to not being correlated with river stage. In general, growth in swales was positively correlated with river stage and Palmer Drought Severity Index (an index of soil moisture) for longer periods than flats. Growth decreased after levee construction, but swales were less impacted than flats likely because of differences in elevation and soils provide higher soil moisture. Results of this study indicate that broad-scale hydrologic processes differ in their effects on the flood regime, and the effects on growth of moderately flood-tolerant species such as F. pennsylvanica can be mediated by local-scale factors such as topographic position, which affects soil moisture.

  13. Groundwater hydrogeochemistry of mayor ions in the Radovna River valley (NW Slovenia)

    Science.gov (United States)

    Torkar, Anja; Brenčič, Mihael; Vreča, Polona

    2013-04-01

    Chemical analysis of major elements was used to investigate the characteristics of various springs and surface water in the Radovna River valley. The valley is situated in the north-western part of Slovenia. It is 17-kilometre long Alpine river flowing between karstic plateaus of Pokljuka and Mežakla confluenting with Sava Dolinka River. Wider area of the valley is built up by Triassic limestone and dolomite. Quaternary alluvial and glacial sediments occur in the bottom of the valley and on the slopes of the plateaus. Water was sampled monthly from May 2005 till March 2007 at 10 locations along the valley. Locations are divided into: 5 springs, 3 surface water locations, 1 small lake and 1 artesian borehole. On site conductivity, pH and water temperature was measured and samples for chemical analyses were collected. Groundwater, spring water and surface water are related to carbonate rocks; therefore the pH of the samples is in range between 7.1 and 8.4. In most cases pH of river water is higher than that of groundwater and spring water. Conductivity of the water varied in the interval between 188 μS/cm and 374 μS/cm. Results of chemical analyses show that concentration of Ca2+ exceeds that of Mg2+ in all of the samples and Ca/Mg ratio varies between 2.6 and 16.8. The concentration of Na+ is lower than Mg2+, but always higher than that of K+. Predominant anion is the HCO3- and varies between 100 mg/l and 211 mg/l. Concentration of anions Cl-, NO3- and SO42- are low and range from 0.1 mg/l to 7.47 mg/l and between 0.62 mg/l and 12 mg/l for Cl- and SO42-, respectively. NO3- is in almost all of the samples below 1 mg/l. Water data shows that waters are alkaline and the dominant facies is Ca-Mg-HCO3-. Ion concentrations fluctuate seasonally and are related to changes in discharge. In winter and early spring, when the discharge is low, the ion concentrations are higher and in late spring and summer during snowmelt, when the discharge is higher, the ion concentration

  14. Susceptibility assessment of debris flows using the analytic hierarchy process method-A case study in Subao river valley, China

    Institute of Scientific and Technical Information of China (English)

    Xingzhang Chen; Hui Chen; Yong You; Jinfeng Liu

    2015-01-01

    Many debris flows have occurred in the areas surrounding the epicenter of the Wenchuan earthquake. Susceptibility assessment of debris flows in this area is especially important for disaster prevention and mitigation. This paper studies one of the worst hit areas, the Subao river valley, and the susceptibility assessment of debris flows is performed based on field surveys and remote sensing interpretation. By investigating the formation conditions of debris flows in the valley, the following assessment factors are selected: mixture density of landslides and rock avalanches, distance to the seismogenic fault, stratum lithology, ground roughness, and hillside angle. The weights of the assessment factors are determined by the analytic hierarchy process (AHP) method. Each of the assessment factors is further divided into five grades. Then, the assessment model is built using the multifactor superposition method to assess the debris flow susceptibility. Based on the assessment results, the Subao river valley is divided into three areas: high susceptibility areas, medium susceptibility areas, and low susceptibility areas. The high susceptibility areas are concentrated in the middle of the valley, accounting for 17.6%of the valley area. The medium susceptibility areas are in the middle and lower reaches, most of which are located on both sides of the high susceptibility areas and account for 45.3% of the valley area. The remainders are clas-sified as low susceptibility areas. The results of the model are in accordance with the actual debris flow events that occurred after the earthquake in the valley, confirming that the proposed model is capable of assessing the debris flow susceptibility. The results can also provide guidance for reconstruction planning and debris flow prevention in the Subao river valley.

  15. Late Pleistocene valley fills source sediment flux of Tibetan Plateau margin rivers, Zanskar, India

    Science.gov (United States)

    Blöthe, J. H.; Munack, H.; Korup, O.; Fulop, R. H.; Codilean, A.; Fink, D.

    2015-12-01

    The Indus and its tributaries, one of Asia's largest river systems, drain the NW Himalaya and the Transhimalayan ranges that border the western Tibetan Plateau margin. From the internally drained low-relief areas of the Tibetan Plateau, local relief increases towards the Western Himalayan Syntaxis, where it exceeds 7 km. Simultaneously, average denudation rates rise from as little as 10 mm ka-1 at the Tibetan Plateau margin to rates of >1000 mm ka-1 close to the western Himalayan Syntaxis. In this rugged bedrock landscape, river valleys frequently alternate between deeply incised gorges and broad alluviated reaches. Vast fill terrace staircases of up to 400 m height above current river levels, and intercalated lake sediments point to repeated phases of incision and aggradation within the region. Despite a broad interest in a better understanding of mechanisms that modulate plateau erosion, age constraints on the generation of these impressive features remain sparse, though indicate mainly Pleistocene formation ages. Here we present new data from the More Plains section, a vast sedimentary fill, located in the headwaters of the Zanskar River, the largest tributary to the upper Indus. The vast sedimentary successions of the More Plains originally belonged to a former endorheic basin that has been tapped by the Zanskar River, today revealing a sedimentary exposures of >250 m thickness. We combine morphometric analysis and field based observations with 10Be surface exposure dating and basin-wide denudation rates to constrain the late Quaternary history of this setting. Analysis of a 10Be depth profile on top of the More Plains section indicate a surface exposure age of ~125 +/- 15 ka, which is supported by ages from nearby amalgamated surface samples. Grounding on a morphometric approach, we estimate that ~1.65-1.95 km3 were removed from this section by fluvial erosion since aggradation ceased, requiring a specific sediment yield of 85-100 t km-2 yr-1 averaged over the

  16. Morphology and filling of incised submarine valleys on the continental shelf near the mouth of the Fly River, Gulf of Papua

    Science.gov (United States)

    Crockett, J. S.; Nittrouer, C. A.; Ogston, A. S.; Naar, D. F.; Donahue, B. T.

    2008-03-01

    Much historical perspective about terrestrial and marine processes can be obtained from examination of fluvial valleys formed during lower sea level on surfaces that are now continental shelves. The continental shelf near the mouth of the Fly River (Gulf of Papua) has three incised valleys, which were not extensively modified or filled during the Holocene Transgression. Multibeam mapping of the valleys documents their morphology; seismic profiling reveals stratigraphy of sediment fill; and coring within and near the valleys suggests mechanisms of filling. Kiwai Valley is deep (20-50 m relief), narrow (˜1 km wide), steep-sided and meandering, due to river flows that caused its excavation through competent sedimentary deposits. Purutu Valley is shallow (10-20 m relief) and broad (>2 km wide). Umuda Valley is widest (˜14 km) and has multiple channels with variable incision depths, suggesting more extensive fluvial activity than the other two valleys. Valley filling has occurred in several ways, reflecting valley morphology and location relative to the present river mouth. Kiwai and Umuda valleys reveal three stages of infill: (1) hemipelagic sedimentation at distal sites, (2) gravity-driven flows spreading down the valley, and (3) subsequent clinoform progradation that completely fills the valley. Purutu Valley fill is dominated by clinoform progradation. Clinoform progradation in Umuda Valley is driven by intense sediment reworking on the surrounding topset regions, and its large width allows progradation from the sides as well as down its axis. Most shelf valleys around the world were filled long ago, and available techniques have severe limitations for documenting the details of morphology and the mechanisms of filling. The shelf valleys described in this paper provide a unique perspective to terrestrial and marine processes before, during, and after the Holocene Transgression.

  17. Fertilisation of the Southern Atlantic: Ephemeral River Valleys as a replenishing source of nutrient-enriched mineral aerosols

    Science.gov (United States)

    Dansie, Andrew; Wiggs, Giles; Thomas, David

    2016-04-01

    Oceanic dust deposition provides biologically important iron and macronutrients (Phosphorus (P) and Nitrogen-based (N) compounds) that contribute to phytoplankton growth, marine productivity and oceanic atmospheric CO2 uptake. Research on dust emission sources to date has largely focused on the northern hemisphere and on ephemeral lakes and pans. Our work considers the ephemeral river valleys of the west coast of Namibia as an important yet overlooked source of ocean-fertilizing dust. Dust plumes are frequently emitted from the river valleys by strong easterly winds during the Southern Hemisphere winter, when the upwelling of the Benguela Current is at its weakest. We present field data from dust emission source areas along the main river channels near the coastal termini of the Huab, Kuiseb and Tsauchab river valleys. Collected data include erodible surface sediment, wind-blown flux, and associated meteorological data. Extensive surface sediment sampling was also undertaken throughout the combined 34,250 km2 extent of each river valley catchment with samples collected from within the main river channels, the main branches of each river system, selected tributaries, and into the upper watersheds. Geochemical data show valley sediment and wind-blown flux material have high concentrations of bioavailable Fe, P and N, exceeding that measured at the major dry lake basin dust sources in southern Africa. The contribution of fertilising deposition material is enhanced by both the spatial proximity of the source areas to the ocean and enrichment of source material by ephemeral fluvial accumulation and desiccation. Results show that geographical factors within each watershed play a key role in the nutrient composition of the emitting fluvial deposits in the river valleys. Analysis explores potential relationships between land use, geology, climate and precipitation in the upper watersheds and their influence on bioavailability of Fe, P and N compounds in wind

  18. Mountains, glaciers, and mines—The geological story of the Blue River valley, Colorado, and its surrounding mountains

    Science.gov (United States)

    Kellogg, Karl; Bryant, Bruce; Shroba, Ralph R.

    2016-01-01

    This report describes, in a nontechnical style, the geologic history and mining activity in the Blue River region of Colorado, which includes all of Summit County. The geologic story begins with the formation of ancient basement rocks, as old as about 1700 million years, and continues with the deposition of sedimentary rocks on a vast erosional surface beginning in the Cambrian Period (about 530 million years ago). This deposition was interrupted by uplift of the Ancestral Rocky Mountains during the late Paleozoic Era (about 300 million years ago). The present Rocky Mountains began to rise at the close of the Mesozoic Era (about 65 million years ago). A few tens of millions years ago, rifting began to form the Blue River valley; a major fault along the east side of the Gore Range dropped the east side down, forming the present valley. The valley once was filled by sediments and volcanic rocks that are now largely eroded. During the last few hundred-thousand years, at least two periods of glaciation sculpted the mountains bordering the valley and glaciers extended down the Blue River valley as far south as present Dillon Reservoir. Discovery of deposits of gold, silver, copper, and zinc in the late 1800s, particularly in the Breckenridge region, brought an influx of early settlers. The world-class molybdenum deposit at Climax, mined since the First World War, reopened in 2012 after a period of closure.

  19. Mountains, glaciers, and mines—The geological story of the Blue River valley, Colorado, and its surrounding mountains

    Science.gov (United States)

    Kellogg, Karl; Bryant, Bruce; Shroba, Ralph R.

    2016-02-10

    This report describes, in a nontechnical style, the geologic history and mining activity in the Blue River region of Colorado, which includes all of Summit County. The geologic story begins with the formation of ancient basement rocks, as old as about 1700 million years, and continues with the deposition of sedimentary rocks on a vast erosional surface beginning in the Cambrian Period (about 530 million years ago). This deposition was interrupted by uplift of the Ancestral Rocky Mountains during the late Paleozoic Era (about 300 million years ago). The present Rocky Mountains began to rise at the close of the Mesozoic Era (about 65 million years ago). A few tens of millions years ago, rifting began to form the Blue River valley; a major fault along the east side of the Gore Range dropped the east side down, forming the present valley. The valley once was filled by sediments and volcanic rocks that are now largely eroded. During the last few hundred-thousand years, at least two periods of glaciation sculpted the mountains bordering the valley and glaciers extended down the Blue River valley as far south as present Dillon Reservoir. Discovery of deposits of gold, silver, copper, and zinc in the late 1800s, particularly in the Breckenridge region, brought an influx of early settlers. The world-class molybdenum deposit at Climax, mined since the First World War, reopened in 2012 after a period of closure.

  20. Interactions of Growth-faulting with Incised Valleys and Channels on the Late Miocene to Recent Mississippi River Delta, LA

    Science.gov (United States)

    Armstrong, C. P.; Mohrig, D.; Steel, R. J.

    2011-12-01

    The interaction between incised valleys and growth-fault related subsidence is poorly understood in the Late Miocene to Recent Mississippi River Delta. Previous work has found little evidence that growth-faults are able to affect the course or geometry of small ( 1km in width and 25m in depth) has not been previously evaluated in this area. We use a 1400 km2 3D seismic volume located under Breton Sound, LA, integrated with a selection of well logs to document the effect of growth-faults on 12 valleys and 14 channels present within the upper 1.5 kilometers of the seismic volume. In contrast to the majority of smaller distributary channels found within the survey, valleys appear to be steered along or away from growth-faults. This observation suggests that faults are able to affect the course of valleys to a greater extent than small channels. We suggest that this is because valleys are long lived features which do not avulse before being influenced by shorter time scale faulting events. This study contributes to our understanding of the dynamics of growth-faults and valleys in the subsurface and has important long term societal implications for populations living near large rivers in areas with active growth-faulting.

  1. Late quaternary morphotectonic evolution of upper Indus valley profile: a cosmogenic radionuclide study of river polished surfaces

    International Nuclear Information System (INIS)

    We have studied cosmogenic exposure ages in a set of five samples from the river polished surfaces (1-46 m above present river level) of the Indus river (Ladakh), at maximum discharge yield during August. These ages not only provide an opportunity to unravel the complex morphotectonic history of the upper Indus valley, but also yield estimates of river incision rates during down-cutting of bedrocks. The three lower surfaces, 21 m, 6 m and 1 m above the river level have monotonically decreasing cosmic ray exposure ages of 22, 15 and 3 ka BP, suggesting that the river has been cutting the bedrocks initially (22-15 ka) at high rate of 2 mm yr which reduced to 0.3-0.4 mm yr-1 since 15 ka BP. The latter is at par with the reported values of exhumation rate for the Ladakh region. The present data together with similar data from the Indus valley west of Skardu, reported earlier, give a better understanding of the so far poorly understood interplay of regional exhumation, incision rate and the role of climate in the morphotectonic evolution of the upper Indus valley. (author)

  2. Snake River sockeye salmon Sawtooth Valley project: 1992 Juvenile and Adult Trapping Program

    International Nuclear Information System (INIS)

    Sockeye salmon (Oncorhynchus nerka) runs in the Snake River Basin have severely declined. Redfish Lake near Stanley, Idaho is the only lake in the drainage known to still support a run. In 1989, two adults were observed returning to this lake and in 1990, none returned. In the summer of 1991, only four adults returned. If no action is taken, the Snake River sockeye salmon will probably cease to exist. On November 20, 1991, the National Marine Fisheries Service (NMFS) declared the Snake River sockeye salmon ''endangered'' (effective December 20, 1991), pursuant to the Endangered Species Act (ESA) of 1973. In 1991, in response to a request from the Idaho Department of Fish and Game and the Shoshone-Bannock Tribes, the Bonneville Power Administration (BPA) funded efforts to conserve and begin rebuilding the Snake River sockeye salmon run. The initial efforts were focused on Redfish Lake in the Sawtooth Valley of southcentral Idaho. The 1991 measures involved: trapping some of the juvenile outmigrants (O. nerka) from Redfish Lake and rearing them in the Eagle Fish Health Facility (Idaho Department of Fish and Game) near Boise, Idaho; Upgrading of the Eagle Facility where the outmigrants are being reared; and trapping adult Snake River sockeye salmon returning to Redfish Lake and holding and spawning them at the Sawtooth Hatchery near Stanley, Idaho. This Environmental Assessment (EA) evaluates the potential environmental effects of the proposed actions for 1992. It has been prepared to meet the requirements of the National Environmental Policy Act (NEPA) of 1969 and section 7 of the ESA of 1973

  3. Crown Jewel of the Fleet: Design, Construction, and Use of the Seagoing Balsa of the Pre-Columbian Andean Coast

    OpenAIRE

    Emanuel, Jeffrey Paul

    2012-01-01

    The seaworthiness of the balsa sailing raft, and the seafaring aptitude of those who built and sailed it, has been the subject of critically biased, often conflicting accounts over the nearly five centuries since contact. This paper objectively marshals historical evidence to recover the preColumbian design and construction of this ‘Crown Jewel’ of the coastal Andean fleet. Sailing balsas were constructed of balsa tree (ochroma spp.) trunks lashed together with henequen, covered with one or m...

  4. Practical aspects of registration the transformation of a river valley by beavers using terrestrial laser scanning

    Science.gov (United States)

    Tyszkowski, Sebastian; Błaszkiewicz, Mirosław; Brykała, Dariusz; Gierszewski, Piotr; Kaczmarek, Halina; Kordowski, Jarosław; Słowiński, Michał

    2016-04-01

    Activity of beavers (Castor fiber) often significantly affects the environment in which they life. The most commonly observed effect of their being in environment is construction of beaver dams and formation a pond upstream. However, in case of a sudden break of a dam and beaver pond drainage, the valley below the dam may also undergo remodelling. The nature and magnitude of these changes depends on the quantity of water and its energy as well as on the geological structure of the valley. The effects of such events can be riverbank erosion, and the deposition of the displaced of erosion products in the form of sandbars or fans. The material can also be accumulated in local depressions or delivered to water bodies. Such events may occur multiple times in the same area. To assess their impact on the environment it is important to quantify the displaced material. The study of such transformations was performed within a small valley of the river of Struga Czechowska (Tuchola Pinewood Forest, Poland). The valley is mainly cut in sands and gravels. Its steep banks are overgrown with bushes and trees. The assessment of changes in morphology were based on the event of the beaver pond drainage of 2015. The study uses the measurements from the terrestrial laser scanning (scanner Riegl VZ-4000). The measurements were performed before and after the event. Each of the two models obtained for comparison was made up of more than 20 measurement stations. Point clouds were joined by Multi-Station Adjustment without placing in the terrain any objects of reference. During measurements attention was paid to the changes in morphology of both riverbed and valley surrounding. The paper presents the example of the recorded changes as well as the measurement procedure. Moreover, the aspects of fieldwork and issues related to post-processing, such as merging, filtering of point clouds and detection of changes, are also presented. This study is a contribution to the Virtual Institute of

  5. Spatiotemporal Co-existence of Two Mycobacterium ulcerans Clonal Complexes in the Offin River Valley of Ghana

    Science.gov (United States)

    Aboagye, Samuel; Kerber, Sarah; Danso, Emelia; Asante-Poku, Adwoa; Asare, Prince; Parkhill, Julian; Harris, Simon R.; Pluschke, Gerd; Yeboah-Manu, Dorothy; Röltgen, Katharina

    2016-01-01

    In recent years, comparative genome sequence analysis of African Mycobacterium ulcerans strains isolated from Buruli ulcer (BU) lesion specimen has revealed a very limited genetic diversity of closely related isolates and a striking association between genotype and geographical origin of the patients. Here, we compared whole genome sequences of five M. ulcerans strains isolated in 2004 or 2013 from BU lesions of four residents of the Offin river valley with 48 strains isolated between 2002 and 2005 from BU lesions of individuals residing in the Densu river valley of Ghana. While all M. ulcerans isolates from the Densu river valley belonged to the same clonal complex, members of two distinct clonal complexes were found in the Offin river valley over space and time. The Offin strains were closely related to genotypes from either the Densu region or from the Asante Akim North district of Ghana. These results point towards an occasional involvement of a mobile reservoir in the transmission of M. ulcerans, enabling the spread of bacteria across different regions. PMID:27434064

  6. Potentiometric-surface altitude of the confined aquifer, Wood River Valley aquifer system, south-central Idaho, October 2012.

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Water levels in 93 wells completed in the Wood River Valley aquifer system were measured during October 22–24, 2012; these wells are part of a network established...

  7. Spatiotemporal Co-existence of Two Mycobacterium ulcerans Clonal Complexes in the Offin River Valley of Ghana.

    Directory of Open Access Journals (Sweden)

    Araceli Lamelas

    2016-07-01

    Full Text Available In recent years, comparative genome sequence analysis of African Mycobacterium ulcerans strains isolated from Buruli ulcer (BU lesion specimen has revealed a very limited genetic diversity of closely related isolates and a striking association between genotype and geographical origin of the patients. Here, we compared whole genome sequences of five M. ulcerans strains isolated in 2004 or 2013 from BU lesions of four residents of the Offin river valley with 48 strains isolated between 2002 and 2005 from BU lesions of individuals residing in the Densu river valley of Ghana. While all M. ulcerans isolates from the Densu river valley belonged to the same clonal complex, members of two distinct clonal complexes were found in the Offin river valley over space and time. The Offin strains were closely related to genotypes from either the Densu region or from the Asante Akim North district of Ghana. These results point towards an occasional involvement of a mobile reservoir in the transmission of M. ulcerans, enabling the spread of bacteria across different regions.

  8. Water-table altitude of the unconfined aquifer, Wood River Valley aquifer system, south-central Idaho, October 2012.

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Water levels in 93 wells completed in the Wood River Valley aquifer system were measured during October 22–24, 2012; these wells are part of a network established...

  9. Summary of investigations on chemical compounds found in fish tissue taken from Wasilla Lake in the Matanuska Valley and Delta Clearwater River and Lake in the Tanana Valley, 1977

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report is a summary of investigations on chemical compounds found in fish tissue take from Wasilla Lake in the Matansuka Valley and Delta Clearwater River and...

  10. A physically-based statistical forecast model for the middle-lower reaches of the Yangtze River Valley summer rainfall

    Institute of Scientific and Technical Information of China (English)

    FAN Ke; WANG HuiJun; CHOI YoungJean

    2008-01-01

    A new approach to forecast the middle-lower reaches of the Yangtze River Valley summer rainfall in June-August (JJA) is proposed in this paper. The year-to-year increment of the middle-lower reaches of the Yangtze River Valley is forecasted and hence the summer precipitation could be predicted. In this paper, DY is defined as the difference of a variable between the current year and the preceding year (year-to-year increment). YR denotes the seasonal mean precipitation rate of the middle-lower reaches of the Yangtze River Valley summer rainfall. After analyzing the atmospheric circulation anomalies in winter and spring that were associated with the DY of YR, six key predictors for the DY of YR have been identified. Then the forecast model for the DY of YR is established by using the multi-linear regression method. The predictors for the DY of YR are Antarctic Oscillation, the meridional wind shear between 850hPa and 200hPa over the Indo-Australian region, and so on. The prediction model shows a high skill for the hindcast during 1997-2006, with the average relative root mean square error is at 18%. The model can even reproduce the upward and downward trends of YR during 1984-1998 and 1998-2006. Considering that the current operational forecast models of the summer precipitation over the China region have the average forecast scores at 60%-70% and that the prediction skill for the middle-lower reaches of Yangtze River Valley summer precipitation remains quite limited up to now, thus this new approach to predict the year-to-year increment of the summer precipitation over the Yangtze River Valley (and hence the summer precipitation itself) has the potential to significantly increase the operational forecast skill of the summer precipitation.

  11. Harmonious Economic Development Model in the Niyang River Valley under Environmental Constraints

    Institute of Scientific and Technical Information of China (English)

    2012-01-01

    We select gross national happiness(GNH),per capita GDP,the number of tourists received in rural areas,waste gas emission and other indicators that are closely related to harmonious economic development.Using the indicator data,we establish the multiple linear regression model that is in line with the harmonious economic development model in the Niyang River valley,and conduct empirical analysis.According to the analysis results,the following recommendations are put forward:adhering to laying equal stress on protection and development;improving the quality of the population;protecting environment and curbing environmental pollution;speeding up the construction of ecological environment relying on technology;increasing investment in poverty alleviation to eradicate poverty;extensively mobilizing the public to participate in ecological and environmental protection;coordinating the relationship between the ecological environment and economic development.

  12. Invisible geomorphosites. A case study in the Rhone River valley (Switzerland)

    Science.gov (United States)

    Clivaz, Mélanie; Reynard, Emmanuel

    2016-04-01

    During the last two decades, numerous inventories of geosites have been carried out at various scales. As all kinds of inventory, they aim at documenting the state of the geological heritage, which is the basis for management strategies (geoconservation, geoeducation, geotourism, etc.). In very humanized regions, where the original geomorphology has been highly modified by human infrastructures, agriculture, urban sprawling, and various modifications of the landforms, it is interesting to inventory not only the landforms visible today but also former landforms that have been destroyed or hidden by human activities. To address the issue of the inventory of invisible geomorphosites, two approaches have been tested in the Rhone River valley, in Switzerland. For centuries the river was flowing quite freely on the floodplain and alternated - both in time and space - braided and meandering sectors. Tributaries fed by glaciers and snow-melting as well as torrential systems were building alluvial fans at their confluence with the Rhone River, and more or less extensive wetlands were isolated by these alluvial fans and the braided sectors of the main river. Floods were frequent and temporary lakes were formed during the snow-melting season and during intensive rainfall events, especially in autumn. Even sand dunes were visible in several places due to the remobilisation of fine fluvial deposits by wind processes. During the second half of the 19th century, the Rhone River and the majority of its tributaries was channelized, the sand dunes were completely destroyed - partly for filling the depressions -, and most wetlands were drained during the first half of the 20th century and replaced by intensive agricultural crops. The first study consisted to inventory the geomorphosites of the research area. Not only the visible landforms but also the landforms that had completely disappeared were evaluated using the assessment method of Reynard et al. (2015). A total of 28

  13. Geo-referenced social accounting with application to integrated watershed planning in the Hudson River Valley

    Science.gov (United States)

    Nowosielski, Audra Ann

    Changing economic activity and patterns of human habitation have long been a cause of concern for the ecological health of the Hudson River and its tributaries. Today, economic development in the Hudson River Valley is often characterized as a battle between proponents of economy-wide growth and citizen groups concerned about the cumulative impact of incremental development on the watershed. Current development trends in the Hudson River Valley are driving the conversion of rural, agricultural and forestland to urban or industrial uses. This thesis is part of a larger study of the economic changes that lead to land use and environmental changes. It focuses specifically on the economic drivers of development in Dutchess County, an area of the lower watershed on the east bank of the Hudson, midway between New York City and the state capital of Albany. The objective was to engage the Dutchess County planning community in developing a planning model, the economic portion of which characterizes the economy with a Social Accounting Matrix (SAM) referenced to a Geographical Information System (GIS). The model was used to assess economic impacts of locally relevant development scenarios including a new IBM semiconductor plant, agro-tourism, and commuting behavior. These scenarios each discuss economic changes that have land use consequences. For example, a new IBM plant will likely instigate new residential development, agro-tourism offers a way to keep land in agricultural use, and the study of commuting behavior leads to insights on how residential growth may depend on commuting patterns, as well as information on the effects of second home communities. The final model will help stakeholders to visualize not only how economic shocks will change their communities, but also how these changes may lead to land use and cumulative environmental impact. Stakeholders will be able to visualize the trade-off between new economic growth and the possible loss of environmental

  14. Anomalous Midsummer Rainfall in Yangtze River-Huaihe River Valleys and Its Association with the East Asia Westerly Jet

    Institute of Scientific and Technical Information of China (English)

    XUAN Shouli; ZHANG Qingyun; SUN Shuqing

    2011-01-01

    In this study, the interannual and interdecadal relationship between midsummer Yangtze River-Huaihe River valley (YHRV) rainfall and the position of the East Asia westerly jet (EAWJ) were investigated. The midsummer YHRV rainfall was found to significantly increase after the 1980s. Moreover, the location of the EAWJ was found abnormally south of the climatic mean during 1980-2008 (ID2) compared to 1951-1979 (ID1). During ID2, associated with the southward movement of the EAWJ, an anomalous upper-level convergence occurred over middle-high latitudes (35°-55°N) and divergence occurred over lower latitudes (~30°N)of East Asia. Correspondingly, anomalous descending and ascending motion was observed in middle-high and lower latitudes along 90°-130°E, respectively, favoring more precipitation over YHRV. On an interannual time scale, the EAWJ and YHRV rainfall exhibited similar relationships during the two periods. When the EAWJ was centered abnormally southward, rainfall over YHRV tended to increase. However, EAWJrelated circulations were significantly different during the two periods. During ID1, the circulation of the southward-moving EAWJ exhibited alternating positive-negative-positive distributions from low to middlehigh latitudes along the East Asian coast; the most significant anomaly appeared west of the Okhotsk Sea.However, during ID2 the EAWJ was more closely correlated with the tropical and subtropical circulations.Significant differences between ID1 and ID2 were also recorded sea surface temperatures (SSTs). During ID1, the EAWJ was influenced by the extratropical SST over the northern Pacific; however, the EAWJ was more significantly affected by the SST of the tropical western Pacific during ID2.

  15. Impacts of mine subsidence on the strata and hydrology of river valleys/management guidelines for undermining cliffs gorges and river systems

    Energy Technology Data Exchange (ETDEWEB)

    Arthur Waddington

    2002-06-01

    Prior to commencement of this project, there had been considerable concern about the impacts of mining on creeks and rivers in the Hunter Valley, water storage reservoirs in the Southern Coalfield, escarpments and cliffs in the Southern and Western Coalfields and the Cataract River Gorge, at Tower Colliery. Numerous longwall extractions have already been completed and many more longwalls are planned beneath creeks, river valleys, gorges and clifflines in the NSW Coalfields. Indeed, the topography makes it virtually impossible to avoid such features. All of the current coal mining operations in the Southern Coalfield, and most of those that are planned in future, are taking place in areas of steep topography and are likely to have some impact on creeks, river valleys, gorges, clifflines and associated infrastructure. The research work was undertaken by a multi-disciplinary team included surveys and monitoring of ground movements, geological investigations and hydrological studies, rock classification and testing and in situ stress measurements; numerical modelling and development of numerically based predictive methods; design and construction of a physical scaled model that can be used to illustrate the underlying mechanisms of strata movements for a range of different mining scenarios. This report includes a literature review and comprehensive discussion on the findings that have arisen from the empirical studies, the numerical modelling work and the physical modelling facility. The research work has provided new insights into the mechanisms involved as creeks, river valleys, gorges and clifflines are undermined and has resulted in new methods for the prediction and assessment of subsidence impacts. The final output from the research project will be a management information handbook, to assist coal mining companies that are planning to mine in areas of steep topography.

  16. Large flood on a mountain river subjected to restoration: effects on aquatic habitats, channel morphology and valley infrastructure

    Science.gov (United States)

    Hajdukiewicz, Hanna; Wyżga, Bartłomiej; Mikuś, Paweł; Zawiejska, Joanna; Radecki-Pawlik, Artur

    2016-04-01

    The Biała River, Polish Carpathians, was considerably modified by channelization and channel incision in the twentieth century. To restore the Biała, establishing an erodible corridor was proposed in two river sections located in its mountain and foothill course. In these sections, longer, unmanaged channel reaches alternate with short, channelized reaches; and channel narrowing and incision increases in the downstream direction. In June 2010 an 80-year flood occurred on the river; and this study aims at determining its effects on physical habitat conditions for river biota, channel morphology, and valley-floor infrastructure. Surveys of 10 pairs of closely located, unmanaged and channelized cross sections, performed in 2009 and in the late summer 2010, allowed us to assess the flood-induced changes to physical habitat conditions. A comparison of channel planforms determined before (2009) and after (2012) the flood provided information on the degree of channel widening as well as changes in the width of particular elements of the river's active zone in eight stretches of the Biała. The impact of the flood on valley-floor infrastructure was confronted with the degree of river widening in unmanaged and channelized river reaches. Before the flood, unmanaged cross sections were typified by finer bed material and greater lateral variability in depth-averaged and near-bed flow velocity than channelized cross sections. The flood tended to equalize habitat conditions in both types of river cross sections, obliterating differences (in particular physical habitat parameters) between channelized and unmanaged channel reaches. River widening mostly reflected an increase in the area of channel bars, whereas the widening of low-flow channels was less pronounced. A comparison of channel planform from 2009 and 2012 indicated that intense channel incision typical of downstream sections limited river widening by the flood. Active channel width increased by half in the unmanaged

  17. Demographics and movements of least terns and piping plovers in the Central Platte River Valley, Nebraska

    Science.gov (United States)

    Roche, Erin A.; Sherfy, Mark H.; Ring, Megan M.; Shaffer, Terry L.; Anteau, Michael J.; Stucker, Jennifer H.

    2016-08-09

    The Central Platte River Valley provides breeding habitat for a variety of migratory birds, including federally endangered interior least terns (Sternula antillarum; least tern) and threatened piping plovers (Charadrius melodus). Since 2009, researchers have collected demographic data on both species that span their lifecycle (that is, from egg laying through survival of adults). Demographic data were used to estimate vital rates (for example, nest survival, chick survival, and so on) for both species and assess how these vital rates were related to type and age of nesting habitat. Nest survival of both species was unrelated to the age of the site a nest was initiated on. Piping plover chick survival to fledging age was not related to the age of the site it was hatched at, however, the probability of a least tern chick surviving to fledging was higher at older sites. In general there were fewer piping plover nests than least tern nests found at sites created through either the physical construction of a new site or new vegetation management regimes, during 2009–14.Mean daily least tern nest survival was 0.9742 (95-percent confidence interval [CI]: 0.9692–0.9783) and cumulative nest survival was 0.59 (95-percent CI: 0.53–0.65). Mean daily least tern chick survival was 0.9602 (95-percent CI: 0.9515–0.9673) and cumulative survival to fledging was 0.54 (95-percent CI = 0.48–0.61). Annual apparent survival rates were estimated at 0.42 (95-percent CI = 0.22–0.64) for adult least terns nesting in the Central Platte River Valley and an apparent survival rate of 0.14 (95-pecent CI = 0.04–0.41) for juvenile least terns. The number of least tern nests present at sites created during 2009–14 was associated with the age of the site; more least tern nests were associated with older sites. During 2009–14, there were four (less than 1 percent of all chicks marked) least tern chicks hatched from the Central Platte River Valley that were subsequently captured on

  18. Demographics and movements of least terns and piping plovers in the Central Platte River Valley, Nebraska

    Science.gov (United States)

    Roche, Erin A.; Sherfy, Mark H.; Ring, Megan M.; Shaffer, Terry L.; Anteau, Michael J.; Stucker, Jennifer H.

    2016-08-09

    The Central Platte River Valley provides breeding habitat for a variety of migratory birds, including federally endangered interior least terns (Sternula antillarum; least tern) and threatened piping plovers (Charadrius melodus). Since 2009, researchers have collected demographic data on both species that span their lifecycle (that is, from egg laying through survival of adults). Demographic data were used to estimate vital rates (for example, nest survival, chick survival, and so on) for both species and assess how these vital rates were related to type and age of nesting habitat. Nest survival of both species was unrelated to the age of the site a nest was initiated on. Piping plover chick survival to fledging age was not related to the age of the site it was hatched at, however, the probability of a least tern chick surviving to fledging was higher at older sites. In general there were fewer piping plover nests than least tern nests found at sites created through either the physical construction of a new site or new vegetation management regimes, during 2009–14.Mean daily least tern nest survival was 0.9742 (95-percent confidence interval [CI]: 0.9692–0.9783) and cumulative nest survival was 0.59 (95-percent CI: 0.53–0.65). Mean daily least tern chick survival was 0.9602 (95-percent CI: 0.9515–0.9673) and cumulative survival to fledging was 0.54 (95-percent CI = 0.48–0.61). Annual apparent survival rates were estimated at 0.42 (95-percent CI = 0.22–0.64) for adult least terns nesting in the Central Platte River Valley and an apparent survival rate of 0.14 (95-pecent CI = 0.04–0.41) for juvenile least terns. The number of least tern nests present at sites created during 2009–14 was associated with the age of the site; more least tern nests were associated with older sites. During 2009–14, there were four (less than 1 percent of all chicks marked) least tern chicks hatched from the Central Platte River Valley that were subsequently captured on

  19. Ground-water level contours for the unconfined aquifer in the Wood River Valley, south-central Idaho, representing partial-development conditions.

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The entire population of the Wood River Valley depends on ground water for domestic supply, either from domestic or municipal-supply wells, rapid population growth...

  20. Estimated Altitude of the Consolidated Rock Surface Underlying Quaternary Sediments of the Wood River Valley aquifer system, South-Central Idaho

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This dataset is the estimated altitude of the consolidated rock surface underlying Quaternary sediment of the Wood River Valley aquifer system. This surface is...

  1. Probability of Elevated Nitrate Concentrations in Groundwater in the Eagle River Watershed Valley-Fill Aquifer, Eagle County, North-Central Colorado, 2006-2007

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This raster data set delineates the predicted probability of elevated nitrate concentrations in groundwater in the Eagle River watershed valley-fill aquifer, Eagle...

  2. Difference between the 2006 and partial-development ground-water conditions for the unconfined aquifer in the Wood River Valley, south-central Idaho.

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The entire population of the Wood River Valley depends on ground water for domestic supply, either from domestic or municipal-supply wells, rapid population growth...

  3. Estimated Altitude of the Top of the Uppermost Unit of Fine-Grained Sediment within the Wood River Valley aquifer system, South-Central Idaho

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This dataset is the estimated altitude of the top of the uppermost fine-grained sediment within the Wood River Valley aquifer system. This map was compiled by...

  4. Ground-water level contours for the confined aquifer in the Wood River Valley, south-central Idaho, representing the partial-development conditions.

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The entire population of the Wood River Valley depends on ground water for domestic supply, either from domestic or municipal-supply wells, rapid population growth...

  5. Ground-water level contours for the confined aquifer in the Wood River Valley, south-central Idaho, representing conditions during October 2006.

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The entire population of the Wood River Valley depends on ground water for domestic supply, either from domestic or municipal-supply wells, rapid population growth...

  6. The preservation status of the lichen biota in the designed Special Area of Conservation NATURA 2000 „Middle Łyna River Valley – Smolajny”

    Directory of Open Access Journals (Sweden)

    Dariusz Kubiak

    2014-06-01

    Full Text Available The paper presents the list of 159 taxa, including 151 lichens and 8 saprotrophic or parasitic (lichenicolous fungi, recorded in the designed Special Area of Conservation NATURA 2000 „Middle Łyna River Valley – Smolajny” (the Forest Division of Wichrowo. The analysed area (2953 ha covers mostly forest communities, with natural character, associated with the valley of the Łyna river (hillside lime-oak-hornbeam forests, streamside alder-ash forest, riparian black alder forest.

  7. Experience of the chronological correlation of the Holocene sea coastal landforms in the Tuloma River valley and the Kola Bay

    Directory of Open Access Journals (Sweden)

    Tolstobrov D. S.

    2016-03-01

    Full Text Available The paper is a continuation of studies of the Earth's crust neotectonic movements within the north-western part of the Kola region. New radiocarbon data of the lake bottom sediments in the Tuloma River valley allowed to modify diagram of the relative uplift lines of the Earth surface in the north-western part of the Kola region and to compare them with previously constructed epeirogenic spectra of coastal landforms for the study area. The dynamics and nature of the area uplift have been established and the dating of the ancient shorelines within the Tuloma River valley and the Kola Bay of the Barents Sea during the Holocene has been carried out

  8. Clustering Analysis on the Climatic Conditions in Hundreds of Kilometers of Celery Belts in Hulu River Valley

    Institute of Scientific and Technical Information of China (English)

    Jun; SUN; Cunlu; SU; Guangyang; WE; Xufeng; QI

    2013-01-01

    By using climate data in national stations in Xiji County,Ningxia during 1981 and 2020,a regression analysis was carried out on weather data in crop growth season in three automatic weather stations in Hulu River Valley. The results showed that celery belts of Hulu River Valley was divided into two groups: early-maturing region of south Xinglong-Xiaohe where is warm and rainy,serotinous region of north Jiqiang-Xinying where is warm and cold and rainless. Four subregions: Xinlong,Xiaohe,Jiqiang,Xinying. Each sub-region was divided into five regions according to climate layer and observation in growth season: temperature accumulating planting period,low temperature seedling period,suitable temperature for external leaf growth stage,high-temperature for celery mulching-sanded plantation in different sowing periods, water and fertilizer,insect prevention,time to market sales.

  9. Characterization of Amazon fibers of the peach palm, balsa, and babassu by XDR, TGA and NMR

    International Nuclear Information System (INIS)

    The aim of this work was to present the results by testing X-ray diffraction (XRD), thermogravimetric analysis (TG), nuclear magnetic resonance (NMR) and determining the moisture content of the peach palm, balsa and babassu fibers for assessing the feasibility of composite materials. The fibers of peach palm, balsa and babassu showed characteristic chemical structure of lignocellulosic material, and good thermal stability up to 220 deg C. The fiber with the highest crystallinity index (Ic) is the peach palm (72%) and the less crystalline is the babassu (37%), while the balsa fibers have Ic equal to 64%. The results have shown that these fibers can be used in the manufacture of composite materials. (author)

  10. Principal Disease and Insect Pests of Jatropha curcas L. in the Lower Valley of the Senegal River

    OpenAIRE

    Terren, M.; Mignon, J.; Declerck, C.; Jijakli, H.; Savery, S.; Jacquet de Haveskercke, P.; Winandy, S.; Mergeai, G.

    2012-01-01

    Jatropha curcas L. seed oil is proven to be toxic to many microorganisms, insects and animals. Despite its toxicity, Jatropha is not pest and disease resistant. The following major pests and diseases affecting Jatropha in the lower valley of the Senegal river have been identified: the leaf miner Stomphastis thraustica (Meyrick, 1908) (Lepidoptera, Gracillariidae), the leaf and stem miner Pempelia morosalis (Saalmuller, 1880) (Lepidoptera, Pyralidae) and the shield-backed bug Calidea panaethio...

  11. Bovid ecomorphology and hominin paleoenvironments of the Shungura Formation, lower Omo River Valley, Ethiopia.

    Science.gov (United States)

    Plummer, Thomas W; Ferraro, Joseph V; Louys, Julien; Hertel, Fritz; Alemseged, Zeresenay; Bobe, René; Bishop, L C

    2015-11-01

    The Shungura Formation in the lower Omo River Valley, southern Ethiopia, has yielded an important paleontological and archeological record from the Pliocene and Pleistocene of eastern Africa. Fossils are common throughout the sequence and provide evidence of paleoenvironments and environmental change through time. This study developed discriminant function ecomorphology models that linked astragalus morphology to broadly defined habitat categories (open, light cover, heavy cover, forest, and wetlands) using modern bovids of known ecology. These models used seven variables suitable for use on fragmentary fossils and had overall classification success rates of >82%. Four hundred and one fossils were analyzed from Shungura Formation members B through G (3.4-1.9 million years ago). Analysis by member documented the full range of ecomorph categories, demonstrating that a wide range of habitats existed along the axis of the paleo-Omo River. Heavy cover ecomorphs, reflecting habitats such as woodland and heavy bushland, were the most common in the fossil sample. The trend of increasing open cover habitats from Members C through F suggested by other paleoenvironmental proxies was documented by the increase in open habitat ecomorphs during this interval. However, finer grained analysis demonstrated considerable variability in ecomorph frequencies over time, suggesting that substantial short-term variability is masked when grouping samples by member. The hominin genera Australopithecus, Homo, and Paranthropus are associated with a range of ecomorphs, indicating that all three genera were living in temporally variable and heterogeneous landscapes. Australopithecus finds were predominantly associated with lower frequencies of open habitat ecomorphs, and high frequencies of heavy cover ecomorphs, perhaps indicating a more woodland focus for this genus. PMID:26208956

  12. Radon and remedial action in Spokane River Valley residences: an interim report

    International Nuclear Information System (INIS)

    Fifty-six percent of 46 residences monitored in the Spokane River Valley in eastern Washington/northern Idaho have indoor radon concentrations above the National Council for Radiation Protection (NCRP) guidelines of 8 pCi/1. Indoor levels were over 20 pCi/1 in eight homes, and ranged up to 132 pCi/1 in one house. Radon concentrations declined by factors of 4 to 38 during summer months. Measurements of soil emanation rates, domestic water supply concentrations, and building material flux rates indicate that diffusion of radon does not significantly contribute to the high concentrations observed. Rather, radon entry is dominated by pressure-driven bulk soil gas transport, aggravated by the local subsurface soil composition and structure. A variety of radon control strategies are being evaluated in 14 of these homes. Sub-surface ventilation by depressurization and overpressurization, basement overpressurization, and crawlspace ventilation are capable of successfully reducing radon levels below 5 pCi/1 in these homes. House ventilation is appropriate in buildings with low-moderate concentrations, while sealing of cracks has been relatively ineffective

  13. Diet of the grass lizard Microlophus thoracicus icae in the Ica river valley, Peru

    Directory of Open Access Journals (Sweden)

    José Pérez Z.

    2015-10-01

    Full Text Available The diet of grass lizard, Microlophus thoracicus icae, was evaluated in three localities of the Ica River Valley, Peru. The dietary pattern was characterized by high consumption of vegetable material, mainly Prosopis spp. leaves, and invertebrates as ants and insect larvae. No significant relationships were found between body size, number of prey eaten or volume consumed. The juvenile, male and female M. t. icae not showed significant differences regarding number of ants or insect larvae consumed, neither on the proportion consumed of plant material. However, total volume of plant material was different between males and females, compared to juveniles. Multivariate analysis showed no evident difference in the diets of juveniles, males and females. Trophic niche amplitude for M. t. icae was Bij = 6.97. The consumption of plant material and invertebrates is important for both juvenile and adult iguanas, therefore; no clear age difference in diet was observed in the individuals studied. This species would present great diet plasticity (omnivory influenced by the local variation of food resources. Possible consequences of a varied diet may include particular characteristics of its parasites, foraging strategies and efficiency, thermoregulation, morphology, among others.

  14. Characteristics of Two General Circulation Patterns During Floods over the Changjiang-Huaihe River Valley

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    Characteristics of the atmospheric general circulation during the catastrophic floods over the Changjiang-Huaihe River Valley (CHRV) are investigated. There are two precipitation patterns over China in the CHRV flood years: the CHRV flood-whole country-wet (P1) pattern and the CHRV flood-south (north) side-dry (P2) pattern. The circulation analysis results show that there are obvious differences between the NH 500-hPa geopotential height fields of P1 and P2 precipitation patterns. The establishment of East Asia-Atlantic (EAA) correlation chain (the South China Sea (SCS) high-the Meiyu trough-the Okhotsk Sea high over East Asia) is a critical condition for excessive summer precipitation over the CHRV, while the European blocking high plays an important role in determining the precipitation pattern over China in the CHRV flood years. Besides, the relation between the EAA correlation chain and the sea surface temperature anomaly (SSTA) in the North Pacific is also studied.

  15. Laser-controlled land grading for farmland drainage in the Red River Valley: an economic evaluation

    International Nuclear Information System (INIS)

    A study was conducted in the Red River Valley to evaluate the benefits of laser land grading for drainage. Graded fields were compared with ungraded fields to measure changes in crop yields due to better drainage on the graded fields. Cut-and-fill areas were studied in graded fields to evaluate the effect of grading on nutrient levels and crop uniformity. Potential cut-and-fill areas on an ungraded field were also studied for yield uniformity and nutrient levels and compared with the graded field. Crop maturity and yield were more uniform on graded fields (0.05 level of significance) than on ungraded fields. Aerial photographs indicated graded fields had more uniform drainage and, consequently, more uniform crop maturity at harvest. A method is presented for determining the economic feasibility of land grading based upon the percentage of land lost to drown out, the value of the crop, and the cost of grading. The economic analysis indicates that land grading on the areas studied resulted in an 8-year payback and a positive investment return for a longer period of time. (author)

  16. Late Quaternary paleoenvironmental records from the Chatanika River valley near Fairbanks (Alaska)

    Science.gov (United States)

    Schirrmeister, Lutz; Meyer, Hanno; Andreev, Andrei; Wetterich, Sebastian; Kienast, Frank; Bobrov, Anatoly; Fuchs, Margret; Sierralta, Melanie; Herzschuh, Ulrike

    2016-09-01

    Perennially-frozen deposits are considered as excellent paleoenvironmental archives similar to lacustrine, deep marine, and glacier records because of the long-term and good preservation of fossil records under stable permafrost conditions. A permafrost tunnel in the Vault Creek Valley (Chatanika River Valley, near Fairbanks) exposes a sequence of frozen deposits and ground ice that provides a comprehensive set of proxies to reconstruct the late Quaternary environmental history of Interior Alaska. The multi-proxy approach includes different dating techniques (radiocarbon-accelerator mass spectrometry [AMS 14C], optically stimulated luminescence [OSL], thorium/uranium radioisotope disequilibria [230Th/U]), as well as methods of sedimentology, paleoecology, hydrochemistry, and stable isotope geochemistry of ground ice. The studied sequence consists of 36-m-thick late Quaternary deposits above schistose bedrock. Main portions of the sequence accumulated during the early and middle Wisconsin periods. The lowermost unit A consists of about 9-m-thick ice-bonded fluvial gravels with sand and peat lenses. A late Sangamon (MIS 5a) age of unit A is assumed. Spruce forest with birch, larch, and some shrubby alder dominated the vegetation. High presence of Sphagnum spores and Cyperaceae pollen points to mires in the Vault Creek Valley. The overlying unit B consists of 10-m-thick alternating fluvial gravels, loess-like silt, and sand layers, penetrated by small ice wedges. OSL dates support a stadial early Wisconsin (MIS 4) age of unit B. Pollen and plant macrofossil data point to spruce forests with some birch interspersed with wetlands around the site. The following unit C is composed of 15-m-thick ice-rich loess-like and organic-rich silt with fossil bones and large ice wedges. Unit C formed during the interstadial mid-Wisconsin (MIS 3) and stadial late Wisconsin (MIS 2) as indicated by radiocarbon ages. Post-depositional slope processes significantly deformed both, ground

  17. Updated glacial chronology of the South Fork Hoh River valley, Olympic Peninsula, Washington through detailed stratigraphy and OSL dating

    Science.gov (United States)

    Wyshnytzky, C.; Rittenour, T. M.; Thackray, G. D.

    2012-12-01

    The Olympic Peninsula lies within a maritime climatic zone under the direct influence of westerly atmospheric flow and Pacific Ocean sea surface temperature variations (i.e. ENSO and PDO). During the last glaciation, large valley glaciers extended radially from the Mt. Olympus area and carved deep valleys, which preserve glacial diamicton, outwash, and lacustrine sediment emplaced during ice advance and retreat. Previous work by Thackray (1996) mapped glacial deposits through several key drainages in the western Olympic Mountains and used exposures along the South Fork Hoh River to reconstruct MIS 2 glaciation and determine the relative extent of the LGM ice margin in the region. Findings suggest that the extent of mountain glaciers in the western Olympics were much reduced during MIS 2 in comparison to MIS 3/4, with glacier mass balance primarily controlled by moisture delivery. Here we discuss new data constraining the style and timing of deglaciation in the South Fork Hoh River valley of the western Olympic Mountains, Washington, USA. Previous research in the South Fork Hoh River used radiocarbon ages, geomorphic mapping, and general stratigraphic relationships to establish a chronostratigraphic framework (Thackray, 1996). To further that understanding and provide new insight on the style and timing of MIS 2 glaciation, we examine the sedimentology and stratigraphic architecture of glacial landforms, which contain invaluable information about glacial processes and style. Optically stimulated luminescence (OSL) dating, commonly regarded as problematic in glacial sediments, constrains the ages of proximal glacial outwash and glaciolacustrine deposits that were traditionally difficult to date due to the lack of organic matter for radiocarbon dating. OSL ages are internally coherent and stratigraphically consistent with previous radiocarbon ages. Results from this research in the South Fork Hoh River valley and associated work in the Queets River valley, the next

  18. Relationship between precipitation and the infiltration depth over the middle and lower reaches of the Yellow River and Yangtze-Huaihe River Valley

    Institute of Scientific and Technical Information of China (English)

    Zhixin Hao; Jingyun Zheng; Quansheng Ge; Xifeng Guo

    2008-01-01

    The purpose of the paper iS to extract and make the best use of rainfall information contained in the Chinese historical archives of Qing Dynasty,and reconstruct the precipitation series during 1736-1911.The study followed the Yu-Fen-Cun(rainfall infiltration depth)observation method in Qing Dynasty,to conduct soil infiltration experiment under the natural rainfall conditions during 2004-2006.The related parameters,such as precipitation,intensity,initial soil moisture content and infiltration depth have been measured at 10 stations (east of 105°E,30°-40°N)with representative climatic conditions and soil physical texture in the middle and lower reaches of the Yellow River and Yangtze-Huaihe River Valley.The statistical results indicate that precipitation is the primary influencing factor to infiltration depth and is positively correlated with the infiltration depth.Additionally,the effects of every factor On infiltration depth are significantly difierent between the middle and lower reaches of the Yellow River and Yangtze-Huaihe River Valley.Finally,the relationship equations of precipitation and infiltration depth are established for each site,most of which can pass over 60%of the variance explanations and provide quantitative models to reconstruct the precipitation series using Yu-Fen-Curt records in Qing Dynasty.

  19. Ground ice and hydrothermal ground motions on aufeis plots of river valleys

    Directory of Open Access Journals (Sweden)

    V. R. Alekseev

    2015-01-01

    of river valleys are the most «hot» points of the permafrost zone. A comprehensive study of them requires organization of several reference aufeis test areas located in different natural-climatic and geocryological zones. In addition to the natural-historical and methodological aspects, the future research program should include consideration of problems related to interaction between engineering structures and aufeis events and aufeis ice-ground complexes. 

  20. The present and the Archaic River Valley morphology and groundwater condition in the Plaosan Temple complex Central Java-Indonesia

    Directory of Open Access Journals (Sweden)

    Eko Haryono

    2013-07-01

    Full Text Available The Plaosan Temple which was built during the eighth and tenth century AD is one of four temple complexes in the Prambanan area, Central Java-Indonesia. On going excavation in the temple complex discloses the occurrence of canals along the outer fences. The canals are eight meters wide and four meters deep. This article aims at reconstructing archaic river course and groundwater condition due to the construction of the canals. Aerial photo interpretation, excavation, ground water level measurement and valley morphology measurement reveal an anomaly of the nearest river in the temple complex. The river had seemingly been bypassed south-eastward to its tributary just before entering Plaosan Temple complex. Groundwater level dropped and its flow direction changed from nearly southward to south-eastward direction. These phenomena indicate that the canals were groundwater-discharged canals.

  1. Management of invasive plant species in the valley of the River Ślepiotka in Katowice – the example of the REURIS project

    OpenAIRE

    Frelich Małgorzata; Bzdęga Katarzyna

    2014-01-01

    In recent years, programmes aimed at improving environmental conditions in river valleys within urban spaces have been initiated in many of the European Community countries. An example is the project “Revitalization of Urban River Spaces – REURIS” which was implemented in 2009-2012. Its main aim was to revitalize a part of the valley of the River Ślepiotka in Katowice. One of the tasks of the project was a comprehensive treatment to combat invasive plant species occurring in this area, carrie...

  2. The oasis expansion and eco-environment change over the last 50 years in Manas River Valley, Xinjiang

    Institute of Scientific and Technical Information of China (English)

    CHENG; Weiming; ZHOU; Chenghu; LIU; Haijiang; ZHANG; Yang; JIANG; Yan; ZHANG; Yichi; YAO; Yonghui

    2006-01-01

    The oasis expansion and economic development of the Manas River Valley is one of the most successful examples in Xinjiang. In this paper, the oasis spatial distribution pattern and dynamic change were examined using imageries of Landsat MSS, TM and ETM, land use and topographic maps in six different periods (such as 1949, 1962, 1976, 1989, 1999 and 2001) over the last 50 years in the valley. The oasis expansion process could be divided into two stages according to the annual rate of oasis area increase, the fast oasization stage (from 1949 to 1976) when the oasis area expanded from 156.385 km2 in 1949 to 3,639.491 km2 in 1976 because of rapidly increased population and quickly enlarged farmland area; and the urbanization stage (from 1976 to 2001) when the expansion ratio of farmland slowed down, and the urbanization process quickened, the total oasis area reached 5042.440 km2 in 2001. With the continuous expansion of oasis and farmland, a large quantity of river water was drawn into irrigation ditch and plain lakes, so only a small quantity of river water could flow into lakes, as a result, the Manas Lake dried up, salization and basification problems happened in the low-lying oasis region. The natural swamp around the lake was shrunk greatly and biodiversity decreased significantly. The driving force analysis reveals that human activities, such as reclamation and population growth, played a major role in the oasis expansion and ecological deterioration in the Manas River Valley. So further efforts should be made to improve the efficiency of water resource utility and adjust layout of the regional agricultural and animal husbandry to keep the sustainable development of oasis economic belt of the northern slope of Tianshan Mts.

  3. Topographic growth around the Orange River valley, southern Africa: A Cenozoic record of crustal deformation and climatic change

    Science.gov (United States)

    Dauteuil, Olivier; Bessin, Paul; Guillocheau, François

    2015-03-01

    We reconstruct the history of topographic growth in southern Africa on both sides of the Orange River valley from an integrated analysis of erosion surfaces, crustal deformation and climate change. First, we propose an inventory of erosion surfaces observed in the study area and classify them according to their most likely formative process, i.e. chemical weathering or mechanical erosion. Among the various land units observed we define a new class of landform: the pedivalley, which corresponds to a wide valley with a flat erosional floor. In the Orange River valley, we mapped three low-relief erosion surfaces, each bevelling a variety of lithologies. The oldest and most elevated is (1) a stripped etchplain evolving laterally into (2) a stepped pediplain bearing residual inselbergs; (3) a younger pediplain later formed in response to a more recent event of crustal deformation. These are all Cenozoic landforms: the etchplain is associated with a late Palaeocene to middle Eocene weathering event, and the two pediplains are older than the middle Miocene alluvial terraces of the Orange River. Landscape evolution was first driven by slow uplift (10 m/Ma), followed by a second interval of uplift involving a cumulative magnitude of at least 200 m. This event shaped the transition between the two pediplains and modified the drainage pattern. A final phase of uplift (magnitude: 60 m) occurred after the Middle Miocene and drove the incision of the lower terraces of the Orange River. Climate exerted a major control over the denudation process, and involved very humid conditions responsible for lateritic weathering, followed by more arid conditions, which promoted the formation of pedivalleys. Collectively, these produce pediplains.

  4. Hydrodynamic and isotopic characterization of a site contaminated by chlorinated solvents: Chienti River Valley, Central Italy

    International Nuclear Information System (INIS)

    Highlights: ► The fate of chlorinated solvents in groundwater in an alluvial aquifer has been investigated. ► Heterogeneity of the aquifer sediments causes vertical components of groundwater flow. ► Multilevel data shows the VOC’s stratification in the aquifer. ► Concentration and δ13C and δ37Cl data showed that dilution controls the VOC’s distribution. ► Biodegradation has been confirmed by isotope data only in low permeability layers. - Abstract: Contaminant sources have been attributed to shoe manufacturers in an alluvial aquifer located along 26 km2 in the Chienti River Valley, Central Italy. During the 1980s and 1990s, the main chlorinated compound used in the study area was 1,1,1-Trichloroethane (1,1,1-TCA), which was substituted by Perchloroethene (PCE) in the last 15 years. A hydrogeological conceptual model has been developed for the alluvial aquifer taking into account the presence of low permeability lenses, forming a multilayer semi-confined aquifer. Hydrodynamic tests (pumping and flowmeter heat-pulse tests) coupled with standard and multilevel hydrochemical and isotopic samplings were performed. Flowmeter tests showed the existence of vertical flow between aquifer levels having different permeability. Physical–chemical parameter logs agreed with the existence of a multilayer aquifer. Concentration data collected in 21 wells located downgradient of the different sources revealed VOC (Volatile Organic Compound) levels lower than 100 μg/L in the upper part of the valley and levels reaching about 200 μg/L in the near shore areas. PCE is the main compound present in the aquifer. No evidence of the presence of TCA was found in the upper areas of the Chienti Valley, but in the areas near the shore, TCA and its degradation products are predominant. Data collected at multilevels located at two sites (upper and near shore areas) to refine the results obtained in the regional survey show a stratification of the VOC concentrations; values of

  5. Influence of Organic Agriculture on the Net Greenhouse Effect in the Red River Valley, Minnesota

    Science.gov (United States)

    Phillips, R. L.

    2004-12-01

    Fluxes for the suite of biologically-produced greenhouse gases (CH4, N2O and CO2) are strongly influenced by agriculture, yet the influence of organic agriculture on all three gases, which comprise the net greenhouse effect (GHE), is not clear in the context of large-scale agricultural production. Greenhouse gas mitigation potential will depend upon the net balance for all three gases [GHE balance (CO2 equiv.)= CO2 flux+ 23CH4flux + 296N2Oflux]. On-farm, field-scale experiments were performed to test the hypothesis that the net GHE at the soil-atmosphere interface is reduced under organic wheat production, compared with conventional, and that effects vary inter-seasonally. Trace gas fluxes were measured at the soil-atmosphere interface for organic and conventional wheat farms in the Red River Valley, Minnesota, one of the most productive agricultural regions in the US. We utilized 40-60 ha field pairs planted with hard red spring wheat (Triticum aestivum L.). Treatment pairs were located 6km apart and consisted of fields continuously cropped for wheat/soybean/sugar beet production for over 20 yr. Ten random, permanent points were generated for each 8.1 ha sub-plot nested inside each field. Each field pair was similar with respect to crop, climate, cultivation history, tillage, rotation, soil texture, pH, macronutrients, bulk density, and water holding capacity. Differences between treatments for the last five years were soil amendments (compost or urea) and herbicide/fungicide application versus mechanical weed control. We collected gas fluxes at each of the 41 points from April (wheat emergence) until the end of July (maturity) to determine the hourly and seasonally integrated net GHE for each management practice, given similar soil/plant/climatic conditions. Moreover, we analyzed inter-seasonal variability to determine the relationship between wheat phenology and flux under field conditions for soil temperature and moisture (water-filled pore space). The net GHE

  6. Foraging ecology of fall-migrating shorebirds in the Illinois River valley.

    Directory of Open Access Journals (Sweden)

    Randolph V Smith

    Full Text Available Populations of many shorebird species appear to be declining in North America, and food resources at stopover habitats may limit migratory bird populations. We investigated body condition of, and foraging habitat and diet selection by 4 species of shorebirds in the central Illinois River valley during fall migrations 2007 and 2008 (Killdeer [Charadrius vociferus], Least Sandpiper [Calidris minutilla], Pectoral Sandpiper [Calidris melanotos], and Lesser Yellowlegs [Tringa flavipes]. All species except Killdeer were in good to excellent condition, based on size-corrected body mass and fat scores. Shorebird diets were dominated by invertebrate taxa from Orders Diptera and Coleoptera. Additionally, Isopoda, Hemiptera, Hirudinea, Nematoda, and Cyprinodontiformes contribution to diets varied by shorebird species and year. We evaluated diet and foraging habitat selection by comparing aggregate percent dry mass of food items in shorebird diets and core samples from foraging substrates. Invertebrate abundances at shorebird collection sites and random sites were generally similar, indicating that birds did not select foraging patches within wetlands based on invertebrate abundance. Conversely, we found considerable evidence for selection of some diet items within particular foraging sites, and consistent avoidance of Oligochaeta. We suspect the diet selectivity we observed was a function of overall invertebrate biomass (51.2 ± 4.4 [SE] kg/ha; dry mass at our study sites, which was greater than estimates reported in most other food selection studies. Diet selectivity in shorebirds may follow tenants of optimal foraging theory; that is, at low food abundances shorebirds forage opportunistically, with the likelihood of selectivity increasing as food availability increases. Nonetheless, relationships between the abundance, availability, and consumption of Oligochaetes for and by waterbirds should be the focus of future research, because estimates of foraging

  7. Molecular epidemiology of Vibrio cholerae associated with flood in Brahamputra River valley, Assam, India.

    Science.gov (United States)

    Bhuyan, Soubhagya K; Vairale, Mohan G; Arya, Neha; Yadav, Priti; Veer, Vijay; Singh, Lokendra; Yadava, Pramod K; Kumar, Pramod

    2016-06-01

    Cholera is often caused when drinking water is contaminated through environmental sources. In recent years, the drastic cholera epidemics in Odisha (2007) and Haiti (2010) were associated with natural disasters (flood and Earthquake). Almost every year the state of Assam India witnesses flood in Brahamputra River valley during reversal of wind system (monsoon). This is often followed by outbreak of diarrheal diseases including cholera. Beside the incidence of cholera outbreaks, there is lack of experimental evidence for prevalence of the bacterium in aquatic environment and its association with cholera during/after flood in the state. A molecular surveillance during 2012-14 was carried out to study prevalence, strain differentiation, and clonality of Vibrio cholerae in inland aquatic reservoirs flooded by Brahamputra River in Assam. Water samples were collected, filtered, enriched in alkaline peptone water followed by selective culturing on thiosulfate bile salt sucrose agar. Environmental isolates were identified as V. cholerae, based on biochemical assays followed by sero-grouping and detailed molecular characterization. The incidence of the presence of the bacterium in potable water sources was higher after flood. Except one O1 isolate, all of the strains were broadly grouped under non-O1/non-O139 whereas some of them did have cholera toxin (CT). Surprisingly, we have noticed Haitian ctxB in two non-O1/non-O139 strains. MLST analyses based on pyrH, recA and rpoA genes revealed clonality in the environmental strains. The isolates showed varying degree of antimicrobial resistance including tetracycline and ciprofloxacin. The strains harbored the genetic elements SXT constins and integrons responsible for multidrug resistance. Genetic characterization is useful as phenotypic characters alone have proven to be unsatisfactory for strain discrimination. An assurance to safe drinking water, sanitation and monitoring of the aquatic reservoirs is of utmost importance for

  8. Molecular epidemiology of Vibrio cholerae associated with flood in Brahamputra River valley, Assam, India.

    Science.gov (United States)

    Bhuyan, Soubhagya K; Vairale, Mohan G; Arya, Neha; Yadav, Priti; Veer, Vijay; Singh, Lokendra; Yadava, Pramod K; Kumar, Pramod

    2016-06-01

    Cholera is often caused when drinking water is contaminated through environmental sources. In recent years, the drastic cholera epidemics in Odisha (2007) and Haiti (2010) were associated with natural disasters (flood and Earthquake). Almost every year the state of Assam India witnesses flood in Brahamputra River valley during reversal of wind system (monsoon). This is often followed by outbreak of diarrheal diseases including cholera. Beside the incidence of cholera outbreaks, there is lack of experimental evidence for prevalence of the bacterium in aquatic environment and its association with cholera during/after flood in the state. A molecular surveillance during 2012-14 was carried out to study prevalence, strain differentiation, and clonality of Vibrio cholerae in inland aquatic reservoirs flooded by Brahamputra River in Assam. Water samples were collected, filtered, enriched in alkaline peptone water followed by selective culturing on thiosulfate bile salt sucrose agar. Environmental isolates were identified as V. cholerae, based on biochemical assays followed by sero-grouping and detailed molecular characterization. The incidence of the presence of the bacterium in potable water sources was higher after flood. Except one O1 isolate, all of the strains were broadly grouped under non-O1/non-O139 whereas some of them did have cholera toxin (CT). Surprisingly, we have noticed Haitian ctxB in two non-O1/non-O139 strains. MLST analyses based on pyrH, recA and rpoA genes revealed clonality in the environmental strains. The isolates showed varying degree of antimicrobial resistance including tetracycline and ciprofloxacin. The strains harbored the genetic elements SXT constins and integrons responsible for multidrug resistance. Genetic characterization is useful as phenotypic characters alone have proven to be unsatisfactory for strain discrimination. An assurance to safe drinking water, sanitation and monitoring of the aquatic reservoirs is of utmost importance for

  9. Facies and facies association of the siliciclastic Brak River and carbonate Gemsbok formations in the Lower Ugab River valley, Namibia, W. Africa

    Science.gov (United States)

    Paciullo, F. V. P.; Ribeiro, A.; Trouw, R. A. J.; Passchier, C. W.

    2007-03-01

    The Neoproterozoic Zerrissene Turbidite Complex of central-western Namibia comprises five turbiditic units. From the base to the top they are the Zebrapüts Formation (greywacke and pelite), Brandberg West Formation (marble and pelite), Brak River Formation (greywacke and pelite with dropstones), Gemsbok River Formation (marble and pelite) and Amis River Formation (greywacke and pelites with rare carbonates and quartz-wacke). In the Lower Ugab River valley, five siliciclastic facies were recognised in the Brak River Formation. These are massive and laminated sandstones, classical turbidites (thick- and thin-bedded), mudrock, rare conglomerate and breccia. For the carbonate Gemsbok River Formation four facies were identified including massive non-graded and graded calcarenite, fine grained evenly bedded blue marble and calcareous mudrock. Most of these facies are also present in the other siliciclastic units of the Zerrissene Turbidite Complex as observed in other areas. The vertical facies association of the siliciclastic Brak River Formation is interpreted as representing sheet sand lobe to lobe-fringe palaeoenvironment with the abandonment of siliciclastic deposition at the top of the succession. The vertical facies association of the carbonate Gemsbok Formation is interpreted as the slope apron succession overlain by periplatform facies, suggesting a carbonate slope sedimentation of a prograding depositional shelf margin. If the siliciclastic-carbonate paired succession would represent a lowstand relative sea-level and highstand relative sea-level, respectively, the entire turbidite succession of the Zerrissene Turbidite Complex can be interpreted as three depositional sequences including two paired siliciclastic-carbonate units (Zebrapüts-Brandberg West formations; Brak River-Gemsbok formations) and an incomplete succession without carbonate at the top (Amis River Formation).

  10. Siphateles (Gila) sp. and Catostomus sp. from the Pleistocene OIS-6 Lake Gale, Panamint Valley, Owens River system, California

    Science.gov (United States)

    Jayko, A. S.; Forester, R. M.; Smith, G. R.

    2014-12-01

    Panamint Valley lies within the Owens River system which linked southeastern Sierra Nevada basins between Mono Lake and Death Valley during glacial-pluvial times. Previous work indicates that late Pleistocene glacial-pluvial Lake Gale, Panamint Valley was an open system during OIS-6, a closed ground water supported shallow lake during OIS-4, and the terminal lake basin for the Owens River system during OIS-2. We here report the first occurrence of fossil fish from the Plio-Pleistocene Panamint basin. Fish remains are present in late Pleistocene OIS-6 nearshore deposits associated with a highstand that was spillway limited at Wingate Wash. The deposits contain small minnow-sized remains from both Siphateles or Gila sp. (chubs) and Catostomus sp. (suckers) from at least four locations widely dispersed in the basin. Siphateles or Gila sp. and Catostomus are indigenous to the Pleistocene and modern Owens River system, in particular to the historic Owens Lake area. Cyprinodon (pupfish) and Rhinichthys (dace) are known from the modern Amargosa River and from Plio-Pleistocene deposits in Death Valley to the east. The late Pleistocene OIS-6 to OIS-2 lacustrine and paleohydrologic record in Panamint basin is interpreted from ostracod assemblages, relative abundance of Artemia sp. pellets, shallow water indicators including tufa fragments, ruppia sp. fragments and the relative abundance of charophyte gyrogonites obtained from archived core, as well as faunal assemblages from paleoshoreline and nearshore deposits. The OIS-4 groundwater supported shallow saline lake had sufficiently low ratios of alkalinity to calcium (alk/Ca) to support the occurrence of exotic Elphidium sp. (?) foraminfera which are not observed in either OIS-2 or OIS-6 lacustrine deposits. The arrival of Owens River surface water into Panamint Basin during OIS-2 is recorded by the first appearance of the ostracod Limnocythere sappaensis at ~27 m depth in an ~100 m archived core (Smith and Pratt, 1957) which

  11. Lithology, hydrologic characteristics, and water quality of the Arkansas River Valley alluvial aquifer in the vicinity of Van Buren, Arkansas

    Science.gov (United States)

    Kresse, Timothy M.; Westerman, Drew A.; Hart, Rheannon M.

    2015-01-01

    A study to assess the potential of the Arkansas River Valley alluvial aquifer in the vicinity of Van Buren, Arkansas, as a viable source of public-supply water was conducted by the U.S. Geological Survey in cooperation with the Little Rock, District, U.S. Army Corps of Engineers. An important study component was to identify possible changes in hydrologic conditions following installation of James W. Trimble Lock and Dam 13 (December 1969) on the Arkansas River near the study area. Data were gathered for the study in regard to the lithology, hydrologic characteristics, and water quality of the aquifer. Lithologic information was obtained from drillers’ logs of wells drilled from 1957 through 1959. Water-quality samples were collected from 10 irrigation wells and analyzed for inorganic constituents and pesticides. To evaluate the potential viability of the alluvial aquifer in the Van Buren area, these data were compared to similar stratigraphic, lithologic, and groundwater-quality data from the Arkansas River Valley alluvial aquifer at Dardanelle, Ark., where the aquifer provides a proven, productive, sole-source of public-supply water.

  12. A new green anole lizard of the "Dactyloa" clade (Squamata: Dactyloidae) from the Magdalena river valley of Colombia .

    Science.gov (United States)

    Velasco, Julián A; Hurtado-Gómez, Juan Pablo

    2014-01-01

    We describe a new species of Anolis from the Magdalena river valley in Colombia. The new species is morphologically similar to Anolis ibanezi and A. chocorum, but differs in body and dewlap color, and head scalation. We performed an exploratory multivariate analysis based on 15 morphological characteristics of the new species and A chocorum and found that differences between both species are mainly associated with head dimensions. A phylogenetic analysis based on morphological characters suggests that the new species is nested within the "Dactyloa" clade of Anolis. Finally, we discuss phylogenetic relationships and biogeographical affinities based in its distribution.  PMID:24872178

  13. Groundwater resources of the Wood River Valley, Idaho--A groundwater-flow model for resource management

    Science.gov (United States)

    Bartolino, James; Vincent, Sean

    2013-01-01

    The U.S. Geological Survey (USGS), in collaboration with the Idaho Department of Water Resources (IDWR), will use the current understanding of the Wood River Valley aquifer system to construct a MODFLOW numerical groundwater-flow model to simulate potential anthropogenic and climatic effects on groundwater and surface-water resources. This model will serve as a tool for water rights administration and water-resource management and planning. The study will be conducted over a 3-year period from late 2012 until model and report completion in 2015.

  14. Mercury Loads in the South River and Simulation of Mercury Total Maximum Daily Loads (TMDLs) for the South River, South Fork Shenandoah River, and Shenandoah River: Shenandoah Valley, Virginia

    Science.gov (United States)

    Eggleston, Jack

    2009-01-01

    Due to elevated levels of methylmercury in fish, three streams in the Shenandoah Valley of Virginia have been placed on the State's 303d list of contaminated waters. These streams, the South River, the South Fork Shenandoah River, and parts of the Shenandoah River, are downstream from the city of Waynesboro, where mercury waste was discharged from 1929-1950 at an industrial site. To evaluate mercury contamination in fish, this total maximum daily load (TMDL) study was performed in a cooperative effort between the U.S. Geological Survey, the Virginia Department of Environmental Quality, and the U.S. Environmental Protection Agency. The investigation focused on the South River watershed, a headwater of the South Fork Shenandoah River, and extrapolated findings to the other affected downstream rivers. A numerical model of the watershed, based on Hydrological Simulation Program-FORTRAN (HSPF) software, was developed to simulate flows of water, sediment, and total mercury. Results from the investigation and numerical model indicate that contaminated flood-plain soils along the riverbank are the largest source of mercury to the river. Mercury associated with sediment accounts for 96 percent of the annual downstream mercury load (181 of 189 kilograms per year) at the mouth of the South River. Atmospherically deposited mercury contributes a smaller load (less than 1 percent) as do point sources, including current discharge from the historic industrial source area. In order to determine how reductions of mercury loading to the stream could reduce methylmercury concentrations in fish tissue below the U.S. Environmental Protection Agency criterion of 0.3 milligrams per kilogram, multiple scenarios were simulated. Bioaccumulation of mercury was expressed with a site-specific exponential relation between aqueous total mercury and methylmercury in smallmouth bass, the indicator fish species. Simulations indicate that if mercury loading were to decrease by 98.9 percent from 189

  15. Idea, Goal and Framework in Xiangjiang River Valley Governance%湘江流域治理:思路、目标与框架

    Institute of Scientific and Technical Information of China (English)

    汤长安

    2011-01-01

    The paper analyzes chief problems existing in Xiangjiang river valley governance, .puts forward a general idea and stage goals, and then constitutes comprehensive control framework to achieve water improvement, ecological restoration , flood protection, drought combat and shipping development in Xiangjiang river valley, provides scientific reference for comprehensive control, reinstate and planning for Xiangjiang river valley.%通过分析湘江流域生态环境治理存在的主要问题,提出湘江流域综合治理的总体思路、阶段性目标,进而构建了湘江流域实现水质改善、生态恢复、防洪抗旱、航运开发的综合治理框架,为湘江流域生态治理、恢复和规划提供科学参考。

  16. Geotechnical Investigations on Sediments from Alluvial Fans in the Upper Sava River Valley, NW Slovenia

    Science.gov (United States)

    Petkovšek, A.; Maček, M.; Mikoš, M.

    2009-04-01

    In order to estimate whether any alluvial (torrential) fan should be rather classified as a debris cone (mainly formed by debris flows; at least occasionally threatened by debris flows) we performed a combined field and laboratory investigation on selected alluvial fans in the Upper Sava River valley between Rateče (border to Italy) and Jesenice in NW Slovenia. This work was done as a part of three year targeted research project "Debris flow risk assessment in Slovenia". This region was chosen due to its high potential for debris flow generation. In the distal or/and in the proximal part of each of the selected alluvial fans (Trebiža, Suhelj, Presušnik, Koroška Bela, Javorniški Rovt), one or two sedimentological trenches reaching over 5 m in depth were excavated. For each trench we assured qualitative geological (sedimentological) inventory and description of lithological structure, and in some trenches we tried to assess age of the sediments. From selected layers in different depths in the majority of trenches sediment samples have been taken for further geotechnical laboratory investigations. The main aim of the study was to assess transport properties of sediment material to flow in the form of a debris flow. We compared elaborated values of the main geotechnical parameters (grain size distribution, USCS classification, natural water content, Atterberg limits, plasticity index, density, dry density, shear strength as a function of sample water content) of these sediment samples with known corresponding values for samples taken in the past from other active landslides (Macesnik, Slano Blato) and debris flows (Stože, Strug) in Slovenia. The comparison of the samples' shear strengths as a function of sample water content has shown that samples from selected alluvial fans don't contain enough fines and are less sensitive to water content as the samples taken from the Stože debris flow, that was in November 2000 with the magnitude of over 1 million m3 the

  17. Tree growth and recruitment in a leveed floodplain forest in the Mississippi River Alluvial Valley, USA

    Science.gov (United States)

    Gee, Hugo K.W.; King, Sammy L.; Keim, Richard F.

    2014-01-01

    Flooding is a defining disturbance in floodplain forests affecting seed germination, seedling establishment, and tree growth. Globally, flood control, including artificial levees, dams, and channelization has altered flood regimes in floodplains. However, a paucity of data are available in regards to the long-term effects of levees on stand establishment and tree growth in floodplain forests. In this study, we used dendrochronological techniques to reconstruct tree recruitment and tree growth over a 90-year period at three stands within a ring levee in the Mississippi River Alluvial Valley (MAV) and to evaluate whether recruitment patterns and tree growth changed following levee construction. We hypothesized that: (1) sugarberry is increasing in dominance and overcup oak (Quercus lyrata) is becoming less dominant since the levee, and that changes in hydrology are playing a greater role than canopy disturbance in these changes in species dominance; and (2) that overcup oak growth has declined following construction of the levee and cessation of overbank flooding whereas that of sugarberry has increased. Recruitment patterns shifted from flood-tolerant overcup oak to flood-intolerant sugarberry (Celtis laevigata) after levee construction. None of the 122 sugarberry trees cored in this study established prior to the levee, but it was the most common species established after the levee. The mechanisms behind the compositional change are unknown, however, the cosmopolitan distribution of overcup oak during the pre-levee period and sugarberry during the post-levee period, the lack of sugarberry establishment in the pre-levee period, and the confinement of overcup oak regeneration to the lowest areas in each stand after harvest in the post-levee period indicate that species-specific responses to flooding and light availability are forcing recruitment patterns. Overcup oak growth was also affected by levee construction, but in contrast to our hypothesis, growth actually

  18. Geographic information science: Contribution to understanding salt and sodium affected soils in the Senegal River Valley

    Science.gov (United States)

    Ndiaye, Ramatoulaye

    The Senegal River valley and delta (SRVD) are affected by long term climate variability. Indicators of these climatic shifts include a rainfall deficit, warmer temperatures, sea level rise, floods, and drought. These shifts have led to environmental degradation, water deficits, and profound effects on human life and activities in the area. Geographic Information Science (GIScience), including satellite-based remote sensing methods offer several advantages over conventional ground-based methods used to map and monitor salt-affected soil (SAS) features. This study was designed to assess the accuracy of information on soil salinization extracted from Landsat satellite imagery. Would available imagery and GIScience data analysis enable an ability to discriminate natural soil salinization from soil sodication and provide an ability to characterize the SAS trend and pattern over 30 years? A set of Landsat MSS (June 1973 and September 1979), Landsat TM (November 1987, April 1994 and November 1999) and ETM+ (May 2001 and March 2003) images have been used to map and monitor salt impacted soil distribution. Supervised classification, unsupervised classification and post-classification change detection methods were used. Supervised classifications of May 2001 and March 2003 images were made in conjunction field data characterizing soil surface chemical characteristics that included exchange sodium percentage (ESP), cation exchange capacity (CEC) and the electrical conductivity (EC). With this supervised information extraction method, the distribution of three different types of SAS (saline, saline-sodic, and sodic) was mapped with an accuracy of 91.07% for 2001 image and 73.21% for 2003 image. Change detection results confirmed a decreasing trend in non-saline and saline soil and an increase in saline-sodic and sodic soil. All seven Landsat images were subjected to the unsupervised classification method which resulted in maps that separate SAS according to their degree of

  19. Effect of irrigation management on soil salinization in Manas River Valley,Xinjiang,China

    Institute of Scientific and Technical Information of China (English)

    2008-01-01

    The irrigated area of Manas River Valley in Northwest China is an example of the successful reclamation of massive land affected by shallow ground water levels and salinization.To determine the effect of irrigation management practices on soil salinization,soil profiles representing various soil types were sampled.The historical records on the characteristics of irrigation management practices,groundwater level and soil salts accumulation in this region at four key periods,namely:flood irrigation without drainage;flood irrigation with drainage but of low efficiency;irrigation in combination with lined irrigation canals and exploitation of groundwater;and irrigation with the application of water-saving irrigation techniques,were analyzed emphatically.In addition,the salinization status of cultivated land in 2010 and 2020 was also predicted by using analogism according to the relationship between soil salinization and irrigation practices.The results revealed that the application of the traditional irrigation methods,such as flood irrigation and ridge irrigation,resulted in a rapid rising of groundwater level and salts accumulation in soil surface layers.However,with the way of well irrigation and well drainage,the groundwater level and the desalinization in soil layers apparently lowered,leading to a substantial increase of crop yield.Currently,the application of drip irrigation under mulch decreased the salts concentration in soil layers and increased the crop yield.With the continuous application of drip irrigation,the average soil desalinization efficiency in soil layers may increase.It is predicted that the percentage of salinized land would be reduced to 35%-40% when irrigation water is utilized reasonably in 2010.With the high efficient utilization of irrigation water after 2020,the salinized land would remain below 30%.It is concluded that with the improvement of irrigation management,an obvious desalinization would appear in the soil surface layers and the

  20. Regional economic analysis of current and proposed management alternatives for Rappahannock River Valley National Wildlife Refuge

    Science.gov (United States)

    Koontz, Lynne; Sexton, Natalie; Donovan, Ryan

    2009-01-01

    The National Wildlife Refuge System Improvement Act of 1997 requires all units of the National Wildlife Refuge System to be managed under a Comprehensive Conservation Plan. The Comprehensive Conservation Plan must describe the desired future conditions of a refuge and provide long-range guidance and management direction to achieve refuge purposes. The Rappahannock River Valley National Wildlife Refuge (refuge) is in the process of developing a range of management goals, objectives, and strategies for the Comprehensive Conservation Plan. The Comprehensive Conservation Plan for the refuge must contain an analysis of expected effects associated with current and proposed refuge management strategies. The purpose of this study was to assess the regional economic implications associated with draft Comprehensive Conservation Plan management strategies. Special interest groups and local residents often criticize a change in refuge management, especially if there is a perceived negative impact to the local economy. Having objective data on economic impacts may show that these fears are overstated. Quite often, the extent of economic benefits a refuge provides to a local community is not fully recognized, yet at the same time the effects of negative changes is overstated. Spending associated with refuge recreational activities, such as wildlife viewing and hunting, can generate considerable tourist activity for surrounding communities. Additionally, refuge personnel typically spend considerable amounts of money purchasing supplies in local stores, repairing equipment and purchasing fuel at the local service stations, and reside and spend their salaries in the local community. For refuge Comprehensive Conservation Plan planning, a regional economic assessment provides a means of estimating how current management (no action alternative) and proposed management activities (alternatives) could affect the local economy. This type of analysis provides two critical pieces of

  1. Ampliación de la distribución y presencia de una colonia reproductiva de la guacamaya verde (Ara militaris en el alto Balsas de Guerrero, México Range expansion and reproductive colony of the Military Macaw (Ara militaris in the upper Balsas basin, Guerrero, México

    Directory of Open Access Journals (Sweden)

    Víctor H. Jiménez-Arcos

    2012-09-01

    Full Text Available Se registra una población y colonia reproductora de guacamaya verde (Ara militaris en el alto Balsas de Guerrero. La colonia se ubica en el bosque tropical seco de la localidad de Papalutla, al margen del río Atoyac, en el extremo noreste del estado. A lo largo de 4 años de conteos (n= 20, se registró una abundancia de 22.7 ± 2.8 individuos. Este registro confirma que la guacamaya verde aún se reproduce en Guerrero y amplía en aproximadamente 100 km hacia el extremo noreste del estado su distribución conocida.We report a new population of green macaw (Ara militaris to the Mexican state of Guerrero. The colony is located besides the Atoyac River, in the dry tropical forest of Papalutla, in the far northeast corner of the state. Along 4 years of counts (n= 20, an abundance of 22.7 ± 2.8 individuals has been registered. This report is relevant because it is the first record of a resident colony of green macaw in the upper Balsas basin, extending its known distribution range to the northwestern limit of Guerrero.

  2. Hydrogeology of the Susquehanna River valley-fill aquifer system in the Endicott-Vestal area of southwestern Broome County, New York

    Science.gov (United States)

    Randall, Allan D.; Kappel, William M.

    2015-07-29

    The village of Endicott, New York, and the adjacent town of Vestal have historically used groundwater from the Susquehanna River valley-fill aquifer system for municipal water supply, but parts of some aquifers in this urban area suffer from legacy contamination from varied sources. Endicott would like to identify sites distant from known contamination where productive aquifers could supply municipal wells with water that would not require intensive treatment. The distribution or geometry of aquifers within the Susquehanna River valley fill in western Endicott and northwestern Vestal are delineated in this report largely on the basis of abundant borehole data that have been compiled in a table of well records.

  3. Holocene ethnobotanical and paleoecological record of human impact on vegetation in the Little Tennessee River Valley, Tennessee

    Science.gov (United States)

    Delcourt, Paul A.; Delcourt, Hazel R.; Cridlebaugh, Patricia A.; Chapman, Jefferson

    1986-05-01

    Human occupation and utilization of plant resources have affected vegetation in the lower Little Tennessee River Valley of East Tennessee for 10,000 yr. Changes in Indian cultures and land use are documented by radiocarbon chronologies, lithic artifacts, ceramics, settlement patterns, and ethnobotanical remains from 25 stratified archaeological sites within the Holocene alluvial terrace. The ethnobotanical record consists of 31,500 fragments (13.7 kg) of wood charcoal identified to species and 7.7 kg of carbonized fruits, seeds, nutshells, and cultigens from 956 features. Pollen and plant macrofossils from small ponds both in the uplands and on lower stream terraces record local vegetational changes through the last 1500 to 3000 yr. Human impact increased after cultigens, including squash and gourd, were introduced ca. 4000 yr B.P. during the Archaic cultural period. Forest clearance and cultivation disturbed vegetation on both the floodplain and lower terraces after 2800 yr B.P., during the Woodland period. Permanent Indian settlements and maize and bean agriculture extended to higher terraces 1.5 km from the floodplain by the Mississippian period (1000 to 300 yr B.P.). After 300 yr B.P., extensive land clearance and cultivation by Historic Overhill Cherokee and Euro-Americans spread into the uplands beyond the river valley.

  4. Status and understanding of groundwater quality in the Santa Clara River Valley, 2007-California GAMA Priority Basin Project

    Science.gov (United States)

    Burton, Carmen A.; Montrella, Joseph; Landon, Matthew K.; Belitz, Kenneth

    2011-01-01

    Groundwater quality in the approximately 460-square-mile Santa Clara River Valley study unit was investigated from April through June 2007 as part of the Priority Basin Project of the Groundwater Ambient Monitoring and Assessment (GAMA) Program. The GAMA Priority Basin Project is conducted by the U.S. Geological Survey (USGS) in collaboration with the California State Water Resources Control Board and the Lawrence Livermore National Laboratory. The Santa Clara River Valley study unit contains eight groundwater basins located in Ventura and Los Angeles Counties and is within the Transverse and Selected Peninsular Ranges hydrogeologic province. The Santa Clara River Valley study unit was designed to provide a spatially unbiased assessment of the quality of untreated (raw) groundwater in the primary aquifer system. The assessment is based on water-quality and ancillary data collected in 2007 by the USGS from 42 wells on a spatially distributed grid, and on water-quality data from the California Department of Public Health (CDPH) database. The primary aquifer system was defined as that part of the aquifer system corresponding to the perforation intervals of wells listed in the CDPH database for the Santa Clara River Valley study unit. The quality of groundwater in the primary aquifer system may differ from that in shallow or deep water-bearing zones; for example, shallow groundwater may be more vulnerable to surficial contamination. Eleven additional wells were sampled by the USGS to improve understanding of factors affecting water quality.The status assessment of the quality of the groundwater used data from samples analyzed for anthropogenic constituents, such as volatile organic compounds (VOCs) and pesticides, as well as naturally occurring inorganic constituents, such as major ions and trace elements. The status assessment is intended to characterize the quality of untreated groundwater resources in the primary aquifers of the Santa Clara River Valley study unit

  5. Temporal changes of meadow and peatbog vegetation in the landscape of a small-scale river valley in Central Roztocze

    Directory of Open Access Journals (Sweden)

    Bożenna Czarnecka

    2015-07-01

    Full Text Available The Szum is a right-side tributary of the Tanew River crossing the southern escarpment zone of the Central Roztocze region (SE Poland. Downstream of the strict river break in a section between the 10th and 12th km of the river course in the Szum valley, meadow and peatbog complexes have developed, associated with semi-hydrogenic and marshy soils. In an area of approx. 13 ha of the most valuable non-forest habitats, a variety of plant communities have been identified, including habitats of the Natura 2000 network and habitats that are protected under the Regulation of the Minister of the Environment (2001. These are, for instance, meadow associations Lysimachio vulgaris-Filipenduletum, Lythro-Filipenduletum, Filipendulo ulmariae-Menthetum longifoliae, Angelico-Cirsietum oleracei, and Cirsietum rivularis. The moss–sedge and sphagnum bog communities comprise noteworthy associations Caricetum limosae, Rhynchosporetum albae, Caricetum lasiocarpae, Caricetum paniceo-lepidocarpae, Caricetum davallianae, and Sphagnetum magellanici. These communities are composed of ca. 160 vascular plant species and 40 moss and liverwort species. In 1999–2014, the greatest changes occurred within macroforb meadows, i.e. small Angelico-Cirsietum oleracei and Cirsietum rivularis patches have been transformed into Lysimachio vulgaris-Filipenduletum, while some patches of the latter association have been transformed into a Caricetum acutiformis rush. Several patches of bog-spring associations Caricetum paniceo-lepidocarpae and Carici canescentis-Agrostietum caninae have been irretrievably destroyed. Sphagnetum magellanici appears to be the least stable community among the preserved peatbogs. The changes of meadow and peatbog vegetation observed for the last 15 years are a consequence of natural processes that take place in the river valley and to a large extent human activity connected with the so-called small-scale water retention as well as the presence of a beaver

  6. Probabilistic fatigue life of balsa cored sandwich composites subjected to transverse shear

    DEFF Research Database (Denmark)

    Dimitrov, Nikolay Krasimirov; Berggreen, Christian

    2015-01-01

    model are obtaining characteristic S–Ncurves corresponding to a given survival probability, and calibrating partial safety factorsfor material fatigue. The latter is demonstrated by a calibration performed using reliability analysis with the first-order reliability method. The measured variance in balsa...... shearproperties, for both static strength and fatigue failure, is higher than the variance normallyobserved in the properties for fiber-reinforced polymer composite laminates. This could be attributed to the fact that end-grain balsa wood is the product of a naturally occurringgrowth process, which cannot...... be controlled to the same extent as an industrial manufacturing processes. The large variance in the probabilistic model for fatigue life is reflected in the corresponding calibrated partial safety factors, which are higher thanthe factors usually associated with synthetic materials such as fiber...

  7. THE OHIO RIVER VALLEY CO2 STORAGE PROJECT - PRELIMINARY ASSESSMENT OF DEEP SALINE RESERVOIRS AND COAL SEAMS

    Energy Technology Data Exchange (ETDEWEB)

    Michael J. Mudd; Howard Johnson; Charles Christopher; T.S. Ramakrishnan, Ph.D.

    2003-08-01

    This report describes the geologic setting for the Deep Saline Reservoirs and Coal Seams in the Ohio River Valley CO{sub 2} Storage Project area. The object of the current project is to site and design a CO{sub 2} injection facility. A location near New Haven, WV, has been selected for the project. To assess geologic storage reservoirs at the site, regional and site-specific geology were reviewed. Geologic reports, deep well logs, hydraulic tests, and geologic maps were reviewed for the area. Only one well within 25 miles of the site penetrates the deeper sedimentary rocks, so there is a large amount of uncertainty regarding the deep geology at the site. New Haven is located along the Ohio River on the border of West Virginia and Ohio. Topography in the area is flat in the river valley but rugged away from the Ohio River floodplain. The Ohio River Valley incises 50-100 ft into bedrock in the area. The area of interest lies within the Appalachian Plateau, on the western edge of the Appalachian Mountain chain. Within the Appalachian Basin, sedimentary rocks are 3,000 to 20,000 ft deep and slope toward the southeast. The rock formations consist of alternating layers of shale, limestone, dolomite, and sandstone overlying dense metamorphic continental shield rocks. The Rome Trough is the major structural feature in the area, and there may be some faults associated with the trough in the Ohio-West Virginia Hinge Zone. The area has a low earthquake hazard with few historical earthquakes. Target injection reservoirs include the basal sandstone/Lower Maryville and the Rose Run Sandstone. The basal sandstone is an informal name for sandstones that overlie metamorphic shield rock. Regional geology indicates that the unit is at a depth of approximately 9,100 ft below the surface at the project site and associated with the Maryville Formation. Overall thickness appears to be 50-100 ft. The Rose Run Sandstone is another potential reservoir. The unit is located approximately 1

  8. Natural Regeneration after Long-Term Bracken Fern Control with Balsa (Ochroma pyramidale) in the Neotropics

    OpenAIRE

    Samuel I. Levy-Tacher; Ivar Vleut; Francisco Román-Dañobeytia; James Aronson

    2015-01-01

    In many parts of the Neotropics, deforested areas are often colonized by the highly competitive invasive bracken fern (Pteridium aquilinum), which inhabits naturally regenerated forests and successional forests on abandoned farmland. Within the tropical forest region of Chiapas in southern Mexico, we implemented an experiment in 2005 to out-compete bracken fern infestation and reduce or eliminate live bracken rhizomes using several treatments: Direct sowing of balsa seeds (Ochroma pyramidale...

  9. Ampelographic evaluation of wild grapevine characters VitisVinifera G. ssp Sylvestris in Vlora’s river valley

    Directory of Open Access Journals (Sweden)

    BARDHOSH FERRAJ

    2014-06-01

    Full Text Available The wild grapevine (Vitisvitifera G. ssp Sylvestris has been growing spontaneously for thousands of years in Vlora’s river valley. It has been growing in the forests and the villages located along this river, starting from the low hills and ending with villages, located at approximately 600 - 700 m above the sea level such as Mesaplik, Brataj, Tërbaç, Vranisht, Kuç, Sevaster, ect. Observing the flower’s characteristics we concluded that 13% of the flowers are hermaphrodites, 41% of the individuals have a functioning male flower and 46 % of the individuals have a functional female flower. The leaf has different dimensions starting from small to medium, it has 5 lobes, a pentagon form and a smaller petiole than the length of the grown leaf. Above the main venations there are no signs of anthocyanin pigmentation. The average length of the blade above the venation N2 is 10.1\\ 9.6=1.05. The grains contain 2-4 seeds with an average length of 4.85 mm and an average width of 4.5mm, the ratio length\\width of the seed is 4.5\\4.85 = 0.92. The pulp of the grain contains 44.5% must, 21% sugar and 13.1% acidity in total. In the forests and the villages of Vlora’s river valley, the wild grapevine is usually accompanied with other plants like, A.unedo L., C.siliquastrum L., C. mas L., E. arboreaL., I.aquifolium L., Q.cerris L., P.alba L., Q.frainetto Ten., P.spina-christi M., O. vulgare L., W. pear, J. oxycedrus L., W.plum, Blackberries, W. rose, etc, and some herbaceous plants that typically grow in this area such as: M.camomila, strawberry, trefoil, rosemary , lavender, B. perennis L., ect.

  10. Late Pleistocene-Holocene earthquake-induced slumps and soft-sediment deformation structures in the Acequion River valley, Central Precordillera, Argentina

    Directory of Open Access Journals (Sweden)

    Perucca Laura P

    2014-07-01

    Full Text Available Evidence of earthquake-induced liquefaction features in the Acequión river valley, central western Argentina, is analysed. Well-preserved soft-sediment deformation structures are present in Late Pleistocene deposits; they include two large slumps and several sand dikes, convolutions, pseudonodules, faults, dish structures and diapirs in the basal part of a shallow-lacustrine succession in the El Acequión River area. The water-saturated state of these sediments favoured deformation.

  11. The role of alluvial valley deposits in groundwater–surface water exchange in a Chalk river

    OpenAIRE

    Abesser, Corinna; Shand, Paul; Gooddy, Daren; Peach, Denis

    2008-01-01

    To understand the processes of surface water–groundwater exchange in Chalk catchments, a detailed hydrogeochemical study was carried out in the Lambourn catchment in southeast England. Monthly monitoring of river flow and groundwater levels and water chemistry has highlighted a large degree of heterogeneity at the river-corridor scale. The data suggest an irregular connection between the river, the alluvial deposits, and the Chalk aquifer at the study site. The groundwaters in the alluvial gr...

  12. Soil development on Late Quaternary river terraces in a high montane valley in Bhutan, Eastern Himalayas

    NARCIS (Netherlands)

    Tshering Dorji,; Caspari, T.; Bäumler, R.; Veldkamp, A.; Jongmans, A.G.; Kado Tshering,; Tsheten Dorji,; Baillie, I.

    2009-01-01

    We examined the geochemistry and micromorphology of the soils on a suite of morphologically well-defined and visually distinct fluvial terraces, up to 40 m elevation above the current riverbed, at Thangbi in the upper Bumthang Valley, Bhutan. The alluvia forming each of the terraces are lithological

  13. Quality of groundwater and surface water, Wood River Valley, south-central Idaho, July and August 2012

    Science.gov (United States)

    Hopkins, Candice B.; Bartolino, James R.

    2013-01-01

    Residents and resource managers of the Wood River Valley of south-central Idaho are concerned about the effects that population growth might have on the quality of groundwater and surface water. As part of a multi-phase assessment of the groundwater resources in the study area, the U.S. Geological Survey evaluated the quality of water at 45 groundwater and 5 surface-water sites throughout the Wood River Valley during July and August 2012. Water samples were analyzed for field parameters (temperature, pH, specific conductance, dissolved oxygen, and alkalinity), major ions, boron, iron, manganese, nutrients, and Escherichia coli (E.coli) and total coliform bacteria. This study was conducted to determine baseline water quality throughout the Wood River Valley, with special emphasis on nutrient concentrations. Water quality in most samples collected did not exceed U.S. Environmental Protection Agency standards for drinking water. E. coli bacteria, used as indicators of water quality, were detected in all five surface-water samples and in two groundwater samples collected. Some analytes have aesthetic-based recommended drinking water standards; one groundwater sample exceeded recommended iron concentrations. Nitrate plus nitrite concentrations varied, but tended to be higher near population centers and in agricultural areas than in tributaries and less populated areas. These higher nitrate plus nitrite concentrations were not correlated with boron concentrations or the presence of bacteria, common indicators of sources of nutrients to water. None of the samples collected exceeded drinking-water standards for nitrate or nitrite. The concentration of total dissolved solids varied considerably in the waters sampled; however a calcium-magnesium-bicarbonate water type was dominant (43 out of 50 samples) in both the groundwater and surface water. Three constituents that may be influenced by anthropogenic activity (chloride, boron, and nitrate plus nitrite) deviate from this

  14. Wells measured for water-levels, unconfined and confined aquifers, Wood River Valley aquifer system, south-central Idaho, October 2006 and October 2012.

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Water levels in 93 wells completed in the Wood River Valley aquifer system were measured during October 22–24, 2012; these wells are part of a network established...

  15. Changes in the potentiometric-surface altitude of the confined aquifer, Wood River Valley aquifer system, south-central Idaho, October 2006 to October 2012.

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Water levels in 93 wells completed in the Wood River Valley aquifer system were measured during October 22–24, 2012; these wells are part of a network established...

  16. Changes in the water-table altitude of the unconfined aquifer, Wood River Valley aquifer system, south-central Idaho, October 2006 to October 2012.

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Water levels in 93 wells completed in the Wood River Valley aquifer system were measured during October 22–24, 2012; these wells are part of a network established...

  17. 甘肃白龙江流域的茶渍属地衣%The lichen genus Lecanora from Bailong river valley of Gansu province, China

    Institute of Scientific and Technical Information of China (English)

    吕蕾; 王辰磊; 任强; 史秀莉; 赵遵田

    2008-01-01

    Fourteen species of the lichen genus Lecanora are reported from Bailong river valley of Gansu province. Four of them, L. albella, L. flowersiana, L. garovaglii and L. symmicta are reported from China for the first time. Anatomy, morphology and chemistry descriptions based on our materials for the new records are given.

  18. A luminescence dating study of the sediment stratigraphy of the Lajia Ruins in the upper Yellow River valley, China

    Science.gov (United States)

    Zhang, Yuzhu; Huang, Chun Chang; Pang, Jiangli; Zhou, Yali; Zha, Xiaochun; Wang, Longsheng; Zhou, Liang; Guo, Yongqiang; Wang, Leibin

    2014-06-01

    Pedo-sedimentological fieldwork were carried out in the Lajia Ruins within the Guanting Basin along the upper Yellow River valley. In the eolian loess-soil sections on the second river terrace in the Lajia Ruins, we find that the land of the Qijia Culture (4.20-3.95 ka BP) are fractured by several sets of earthquake fissures. A conglomerated red clay covers the ground of the Qijia Culture and also fills in the earthquake fissures. The clay was deposited by enormous mudflows in association with catastrophic earthquakes and rainstorms. The aim of this study is to provide a luminescence chronology of the sediment stratigraphy of the Lajia Ruins. Eight samples were taken from an eolian loess-soil section (Xialajia section) in the ruins for optically stimulated luminescence (OSL) dating. The OSL ages are in stratigraphic order and range from (31.94 ± 1.99) ka to (0.76 ± 0.02) ka. Combined OSL and 14C ages with additional stratigraphic correlations, a chronological framework is established. We conclude that: (1) the second terrace of the upper part of Yellow River formed 35.00 ka ago, which was followed by the accumulation of the eolian loess-soil section; and (2) the eolian loess-soil section is composed of the Malan Loess of the late last glacial (MIS-2) and Holocene loess-soil sequences.

  19. Inter-epidemic transmission of Rift Valley fever in livestock in the Kilombero River Valley, Tanzania: a cross-sectional survey.

    Directory of Open Access Journals (Sweden)

    Robert D Sumaye

    Full Text Available BACKGROUND: In recent years, evidence of Rift Valley fever (RVF transmission during inter-epidemic periods in parts of Africa has increasingly been reported. The inter-epidemic transmissions generally pass undetected where there is no surveillance in the livestock or human populations. We studied the presence of and the determinants for inter-epidemic RVF transmission in an area experiencing annual flooding in southern Tanzania. METHODOLOGY: A cross-sectional sero-survey was conducted in randomly selected cattle, sheep and goats in the Kilombero river valley from May to August 2011, approximately four years after the 2006/07 RVF outbreak in Tanzania. The exposure status to RVF virus (RVFV was determined using two commercial ELISA kits, detecting IgM and IgG antibodies in serum. Information about determinants was obtained through structured interviews with herd owners. FINDINGS: An overall seroprevalence of 11.3% (n = 1680 was recorded; 5.5% in animals born after the 2006/07 RVF outbreak and 22.7% in animals present during the outbreak. There was a linear increase in prevalence in the post-epidemic annual cohorts. Nine inhibition-ELISA positive samples were also positive for RVFV IgM antibodies indicating a recent infection. The spatial distribution of seroprevalence exhibited a few hotspots. The sex difference in seroprevalence in animals born after the previous epidemic was not significant (6.1% vs. 4.6% for females and males respectively, p = 0.158 whereas it was significant in animals present during the outbreak (26.0% vs. 7.8% for females and males respectively, p15 km from the flood plain were more likely to have antibodies than those living <5 km (OR 1.92; 95% CI 1.04-3.56. Species, breed, herd composition, grazing practices and altitude were not associated with seropositivity. CONCLUSION: These findings indicate post-epidemic transmission of RVFV in the study area. The linear increase in seroprevalence in the post-epidemic annual cohorts

  20. Sustainability Assessment of Large Irrigation Dams in Senegal: A Cost-Benefit Analysis for the Senegal River Valley

    Directory of Open Access Journals (Sweden)

    Stanislaw eManikowski

    2016-03-01

    Full Text Available Starting in the 1970s, the Senegalese Government invested in the development of irrigated schemes in the Senegalese part of the Senegal River Valley (S-SRV. From that time to 2012, the irrigated schemes increased from 10,000 ha to more than 110,000 ha. In the meantime, the economic viability of these schemes started to be questioned. It also appeared that the environmental health and social costs might outweigh the benefits of irrigation. Using a life cycle assessment approach and project cost-benefits modelling, this study (i quantified the costs and benefits of the S-SRV irrigated rice production, (ii evaluated the costs and benefits of its externalities and (iii discussed the irrigated rice support policy. The net financial revenues from the irrigated schemes were positive, but their economic equivalences. The economic return rate (EER was below the expected 12% and the net present value (NPV over 20 years of the project represented a loss of about US$-19.6 million. However, if we also include the project’s negative externalities, such as the reduced productivity of the valley ecosystems, protection cost of human health, environmental degradation and social impacts, then the NPV would be much worse, approximately US$-572.1 million. Therefore, the results show that to stop the economic loss and alleviate the human suffering, the S-SRV development policy should be revised using an integrated approach and the exploitation technology should aim at environmental sustainability. This paper may offer useful insights for reviewing the current Senegalese policies for the valley, as well as for assessing other similar cases or future projects worldwide, particularly in critical zones of developing countries.

  1. Simulation and Analysis about the Effects of Geopotential Height Anomaly in Tropical and Subtropical Region on Droughts or Floods in the Yangtze River Valley and North China

    Institute of Scientific and Technical Information of China (English)

    HUANG Yanyan; QIAN Yongfu; WAN Qilin

    2006-01-01

    Previous study comes to the conclusion: based on the anomalies of the South Asian high (SAH), 100-hPa geopotential height, and 100-hPa circulation over tropical and subtropical regions, we can predict precipita tion anomaly in the Yangtze River Valley and North China. To test its validity, a series of experiments have been designed and operated, which include controlled experiment, sensitivity experiment (which has added anomalies into 100-hPa geopotential height and wind field), and our-composite experiments. Experiments based on the composed initial field such as EPR-CF, EPR-CD, EPR-HF, and EPR-HD, can reproduce the floods or droughts in the Yangtze River Valley and North China. It suggests that anomalies of the SAH, 100- hPa geopotential height, and circulation over tropical and subtropical regions may probably imply summer precipitation anomalies in the two regions. Sensitivity experiment results show that anomalies of the SAH, 100-hPa geopotential height, and southwest flow in the previous period is a signal of droughts or floods for the following summer in the Yangtze River Valley and North China. And it is also one of the factors that have impact on summer precipitation anomaly in the two regions. Positive anomaly of 100-hPa geopotential height and the anomalous intensifying of the SAH and southwest flow will induce floods in the Yangtze River Valley and droughts in North China; while negative anomaly of 100-hPa geopotential height and anomalous weakening of the SAH and southwest flow will induce droughts in the Yangtze River Valley and floods in North China.

  2. LDL (Landscape Digital Library) a Digital Photographic Database of a Case Study Area in the River Po Valley, Northern Italy

    CERN Document Server

    Papotti, D

    2001-01-01

    Landscapes are both a synthesis and an expression of national, regional and local cultural heritages. It is therefore very important to develop techniques aimed at cataloguing and archiving their forms. This paper discusses the LDL (Landscape Digital Library) project, a Web accessible database that can present the landscapes of a territory with documentary evidence in a new format and from a new perspective. The method was tested in a case study area of the river Po valley (Northern Italy). The LDL is based on a collection of photographs taken following a systematic grid of survey points identified through topographic cartography; the camera level is that of the human eye. This methodology leads to an innovative landscape archive that differs from surveys carried out through aerial photographs or campaigns aimed at selecting "relevant" points of interest. Further developments and possible uses of the LDL are also discussed.

  3. GEOTOURISM IN THE NIŠAVA RIVER MIDSTREAM VALLEY, SOUTHEASTERN SERBIA – CURRENT STATE AND ISSUES OF FUTURE DEVELOPMENT

    Directory of Open Access Journals (Sweden)

    Milica Began

    2015-12-01

    Full Text Available The region of East  and Southeast Serbia, has the biggest collection of geoheritage sites in the Republic of Serbia. In the southeastern part of Serbia, following various mineralogical compositions of the rocks, the Nišava river has carved a composite valley. This is an area of extraordinary nature capacity because of large number of natural rarities and phenomena that have great possibilities for geotourism development. Despite exceptional predispositions in terms of the value of geological heritage, geosites of this area are still unknown to a wider audience. Aim of this paper is to analyze current state of geotourism and to highlight the values of geosites in Srednje Ponišavlje using the evaluating model as well to evaluate its quality and give the assessment of geotourism development success. Using GAM model, 7 geosites have been analyzed, the ones with extraordinary geological/geomorphological and hydrological features for geotourism development.

  4. Palms and Palm Communities in the Upper Ucayali River Valley - a Little-Known Region in the Amazon Basin

    DEFF Research Database (Denmark)

    Balslev, Henrik; Eiserhardt, Wolf L.; Kristiansen, Thea;

    2010-01-01

    The Amazon region and its palms are inseparable. Palms make up such an important part of the rain forest ecosystem that it is impossible to imagine the Amazon basin without them. Palms are visible in the canopy and often fill up the forest understory. Palms – because of their edible fruits...... – are cornerstone species for the survival of many animals, and palms contribute substantially to forest inventories in which they are often among the ten most important families. Still, the palms and palm communities of some parts of the Amazon basin remain poorly studied and little known. We travelled to a little......-explored corner of the western Amazon basin, the upper Ucayali river valley. There, we encountered 56 different palms, 18 of which had not been registered for the region previously, and 21 of them were found 150–400 km beyond their previously known limits....

  5. Dynamic mechanism of the upwelling on the west side of the submerged river valley off the Changjiang mouth in summertime

    Institute of Scientific and Technical Information of China (English)

    ZHU Jianrong

    2003-01-01

    Based on the analysis of the field observation data off the Changjiang mouth in August 2000 and satellite image of sea surface temperature (SST) in summer of 1997, it indicates that there exists the upwelling event on the west side of the submerged river valley (SRV) off the Changjiang mouth. The calculated results of the three-dimensional numerical model show that this upwelling is induced by the barotropic effect, baroclinic effect, bottom Ekman effect and their interaction with the slope bottom topography. The baroclinic effect is the main cause producing the upwelling at the northern SRV (on the east side of the South Passage of the Changjiang estuary), while the barotropic effect is the main cause at the southern SRV (on the east side of the center of the Hangzhou Bay mouth). The dynamic mechanism producing the upwelling off the Changjiang mouth is different with the general one along coast and on the continental shelf.

  6. Restoration of partly drained fens in the Biebrza River Valley - questions of water management in protected areas

    Energy Technology Data Exchange (ETDEWEB)

    Byczkowski, Andrzej; Okruszko, Thomasz [Warsaw Agricultural University (SAAW-AR), Dept. of Hydraulic Engineering and Environmental Recultivaton (Poland)

    2004-09-01

    The present paper discusses questions of water management in the protected areas, which should be restored due to the anthropogenic induced changes in natural water regime. The study was performed in the Biebrza Wetlands, which lay in North-East Poland in an ice-marginal valley of the Biebrza River. Due to the exceptional ecological values, part of the wetlands is protected in the form of the national park. Anthropogenic changes introduced 150 years ago have disturbed, piece of the system by draining some of the marshes in the central part of the valley. The channels continued to serve their purpose while the area was under extensive agriculture, as long as harvesting hay from small plots was still economically feasible. At present, this is no longer true for most of the area and farmers have been abandoning some of their plots. The review of existing literature on the natural conditions, transformation and possible restoration action in the this area as well as the discussion with the ecologists helped to elaborate the restoration plan, which hydrological consequences were verified by hydrological modeling including hydraulic model, ground water model and optimization, water distribution model. The results of the modeling indicate the area, which will be affected by the restoration project. This constitutes the base for the discussion with the local farmers about the future use of their grasslands. (orig.)

  7. Microbiological Water Quality in Relation to Water-Contact Recreation, Cuyahoga River, Cuyahoga Valley National Park, Ohio, 2000 and 2002

    Science.gov (United States)

    Bushon, Rebecca N.; Koltun, G.F.

    2004-01-01

    The microbiological water quality of a 23-mile segment of the Cuyahoga River within the Cuyahoga Valley National Park was examined in this study. This segment of the river receives discharges of contaminated water from stormwater, combined-sewer overflows, and incompletely disinfected wastewater. Frequent exceedances of Ohio microbiological water-quality standards result in a health risk to the public who use the river for water-contact recreation. Water samples were collected during the recreational season of May through October at four sites on the Cuyahoga River in 2000, at three sites on the river in 2002, and from the effluent of the Akron Water Pollution Control Station (WPCS) both years. The samples were collected over a similar range in streamflow in 2000 and 2002. Samples were analyzed for physical and chemical constituents, as well as the following microbiological indicators and pathogenic organisms: Escherichia coli (E. coli), Salmonella, F-specific and somatic coliphage, enterovirus, infectious enterovirus, hepatitis A virus, Clostridium perfringens (C. perfringens), Cryptosporidium, and Giardia. The relations of the microorganisms to each other and to selected water-quality measures were examined. All microorganisms analyzed for, except Cryptosporidium, were detected at least once at each sampling site. Concentrations of E. coli exceeded the Ohio primary-contact recreational standard (298 colonies per 100 milliliters) in approximately 87 percent of the river samples and generally were higher in the river samples than in the effluent samples. C. perfringens concentrations were positively and significantly correlated with E. coli concentrations in the river samples and generally were higher in the effluent samples than in the river samples. Several of the river samples that met the Ohio E. coli secondary-contact recreational standard (576 colonies per 100 milliliters) had detections of enterovirus, infectious enterovirus, hepatitis A virus, and

  8. Characterization of Amazon fibers of the peach palm, balsa, and babassu by XDR, TGA and NMR; Caracterizacao das fibras amazonicas de pupunha, babacu e balsa atraves de DRX, TG e RMN

    Energy Technology Data Exchange (ETDEWEB)

    Martins, Maria A.; Marconcini, Jose M., E-mail: mariaalice@cnpdia.embrapa.br [Embrapa Instrumentacao, Sao Carlos-SP (Brazil); Morelli, Carolina L.; Marinelli, Alessandra L.; Bretas, Rosario E.S. [Universidade Federal de Sao Carlos - UFSCar, Sao Carlos, SP (Brazil)

    2011-07-01

    The aim of this work was to present the results by testing X-ray diffraction (XRD), thermogravimetric analysis (TG), nuclear magnetic resonance (NMR) and determining the moisture content of the peach palm, balsa and babassu fibers for assessing the feasibility of composite materials. The fibers of peach palm, balsa and babassu showed characteristic chemical structure of lignocellulosic material, and good thermal stability up to 220 deg C. The fiber with the highest crystallinity index (Ic) is the peach palm (72%) and the less crystalline is the babassu (37%), while the balsa fibers have Ic equal to 64%. The results have shown that these fibers can be used in the manufacture of composite materials. (author)

  9. Coptoborus ochromactonus, n. sp. (Coleoptera: Curculionidae: Scolytinae), an emerging pest of cultivated balsa (Malvales: Malvaceae) in Ecuador.

    Science.gov (United States)

    Stilwell, Abby R; Smith, Sarah M; Cognato, Anthony I; Martinez, Malena; Flowers, R Wills

    2014-04-01

    A new species of xyleborine ambrosia beetle has been found to attack balsa, Ochroma pyramidale (Cavanilles ex Lamarck) Urban, in Ecuador. Coptoborus ochromactonus Smith & Cognato is described and its biology is reported. Large-scale surveys were conducted between 2006 and 2009, and observational studies were carried out between 2010 and 2013 in Ecuadorian commercial plantations to determine life history and host preference characteristics. C. ochromactonus attacked balsa between 1.5 and 3 yr in age. Successful attacks were more prevalent in smaller diameter trees and unhealthy trees. In general, attacks and beetle-caused mortality were more prevalent during the dry summer months when trees were under more moisture and light stress. Fungal mycelia were consistently observed coating beetle galleries and are likely the true damaging agent to balsa trees. PMID:24772549

  10. Bees (Hymenoptera: Apidae) present in the flowers of the balsa wood Ochroma lagopus Swartz, 1788 = Abelhas (Hymenoptera: Apidae) associadas às flores do pau-de-balsa Ochroma lagopus Swartz, 1788

    OpenAIRE

    Carla Regina Guimarães Brighenti; Deodoro Magno Brighenti

    2010-01-01

    The flower of balsa wood holds about 10 to 15 mL of nectar, which helps attracting pollinating agents, since the genus Ochroma is incapable of self-fertilization. However, a high mortality of bees is observed in these flowers. The present study investigated the frequency and constancy of mortality of the individuals of the familyApidae that fed on nectar from the balsa wood. Data was gathered from June to August 2008, in Lavras – Minas Gerais State, Brazil. In addition, the survival of the Af...

  11. The impact of an invasive ambrosia beetle on the riparian habitats of the Tijuana River Valley, California

    Science.gov (United States)

    2016-01-01

    The Tijuana River Valley is the first natural habitat in California to be substantially invaded by the Kuroshio Shot Hole Borer (KSHB, Euwallacea sp.), an ambrosia beetle native to Southeast Asia. This paper documents the distribution of the KSHB in the riparian vegetation in the valley and assesses the damage done to the vegetation as of early 2016, approximately six months after the beetle was first observed in the valley. I divided the riparian habitats into 29 survey units so that the vegetation within each unit was relatively homogenous in terms of plant species composition, age and density. From a random point within each unit, I examined approximately 60 individuals of the dominant plant species for evidence of KSHB infestation and evidence of major damage such as limb breakage. In the 22 forested units,I examined the dominant arroyo and black willows (Salix lasiolepis Benth. and S. gooddingii C.R. Ball), and in the seven scrub units, I examined mule fat (Baccharis salicifolia (Ruiz & Pav.) Pers.). Evidence of KSHB infestation was found in 25 of the 29 units. In the forest units, infestation rates ranged from 0 to 100% and were high (>60%) in 16 of the units. In the scrub units, infestation rates ranged from 0 to 33%. Infestation rates were significantly correlated with the wetness of a unit; wetter units had higher infestation rates. Evidence of major physical damage was found in 24 units, and dense stands of willows were reduced to broken trunks in several areas. Overall, I estimated that more than 280,000 (70%) of the willows in the valley were infested, and more than 140,000 had suffered major limb damage. In addition, I recorded evidence of KSHB infestation in the other common plant species in the valley; of the 23 species examined, 14 showed evidence of beetle attack. The four species with the highest rates of infestation were native trees in the Salicaceae family. The three species considered to be the worst invasive plants in the valley, Ricinus

  12. Comparing meteorological records between mountainous and valley bottom sites in the upper reaches of the Heihe River, northwestern China: implications for dendroclimatology

    Science.gov (United States)

    Zeng, Qiao; Yang, Bao

    2016-01-01

    Tree-ring records from remote upland areas are widely used in climate reconstructions, but they are typically calibrated by meteorological data from low-lying areas. With the aim of assessing relationships between climatic records from mountainous and valley bottoms, this study compared meteorological records between mountainous sites (lower to upper elevations) and valley bottoms (Qilian (QL) and Yeniugou (YNG)) in the upper reaches of the Heihe River, northwestern China. We found that daily, 5-day, 10-day, and monthly mean air temperatures observed during a 4-year observational period in valley bottoms were strongly correlated (R = 0.90-0.99) to their mountainous site counterparts. Additionally, temperature records from the QL meteorological station shared a higher percentage of variance with each mountainous site compared to YNG. Correlations of precipitation totals between valley bottoms and mountainous sites showed a similar pattern to temperatures. Furthermore, different time series of total rainfall in YNG can explain more variance than those from QL and were also more suitable representations of mountainous sites. Our results confirmed the reliability of utilizing monthly climatic records from valley bottoms to calibrate tree-ring records in mountainous sites. We also caution that when conducting fine-scale microcoring and dendrometer monitoring studies, lower correlations of short-term scale precipitation records between valley bottoms and mountainous sites may introduce unavoidable errors.

  13. NUMERICAL AND DIGITAL METHODS IN ANALYSIS OF SPACE-TIME CHANGES AND RENEWAL OF VEGETATION COVER RESOURCES IN THE CZARNA RIVER VALLEY

    Directory of Open Access Journals (Sweden)

    Grażyna Łaska

    2015-09-01

    Full Text Available The study aimed at evaluation of the current state and description of changes in plant communities in wetland habitats in the Czarna river valley and at recommendation of effective methods for the renewal of vegetation on the basis of detail analysis of its space-time changes. The methods applied included a compilation of field studies (inventory, cartographic study and phytosociological analyses, valorisation of nature, numerical syntaxonomy with the use of MVSP program (Cluster Analysis and PCA and digital methods GIS (Geomedia Professional 6.1. The field study of the vegetation cover of the Czarna river valley was performed in the years 2010–2011. The space-time analysis of changes in the vegetation cover and renewal of vegetation was made with the use of archive aerial photographs from 1966, topographic maps from 1982 and 2000 and orthophotomaps from 2011. The vegetation cover of the Czarna river valley was found to be composed of 12 plant communities representing 6 syntaxonomic classes, and to include sites of 8 protected species. The space-time analysis of the vegetation cover of the Czarna river valley, taking into account the changes in the forms of the valley use over the period 1966–2011, showed that the area occupied by forest communities in wetland habitats as a result of secondary succession has increased by 0.16 km2, so by 27% with respect to the area of 0.4406 km2 from 1966. Chronological changes in the vegetation cover over this area analysed on the basis of GIS and digital methods indicate that in the wet meadows in the valley studied the secondary succession leads to the reproduction of the potential forest communities that were growing there once in the past. The renewal of forestless greeneries in the Czarna river valley is related to changes in the use of the area realised by mowing and restoration of the earlier hydrological regime in the entire catchment area, changed by the network of channels and drainage ditches.

  14. Quaternary extensional and compressional tectonics revealed from Quaternary landforms along Kosi River valley, outer Kumaun Lesser Himalaya, Uttarakhand

    Science.gov (United States)

    Luirei, Khayingshing; Bhakuni, S. S.; Kothyari, Girish Ch.; Tripathi, Kavita; Pant, P. D.

    2016-04-01

    A portion of the Kosi River in the outer Kumaun Lesser Himalaya is characterized by wide river course situated south of the Ramgarh Thrust, where huge thickness (~200 m) of the landslide deposits and two to three levels of unpaired fan terraces are present. Brittle normal faults, suggesting extensional tectonics, are recognized in the Quaternary deposits and bedrocks as further supported by surface morphology. Trending E-W, these faults measure from 3 to 5 km in length and are traced as discontinuous linear mini-horst and fault scarps (sackungen) exposed due to cutting across by streams. Active normal faults have displaced the coarsely laminated debris fan deposits at two sites located 550 m apart. At one of the sites, the faults look like bookshelf faulting with the maximum displacement of ~2 m and rotation of the Quaternary boulders along the fault plane is observed. At another site, the maximum displacement measures about 0.60 cm. Thick mud units deposited due to blocking of the streams by landslides are observed within and above the fan deposit. Landslide debris fans and terrace landforms are widely developed; the highest level of fan is observed ~1240 m above mean sea level. At some places, the reworking of the debris fans by streams is characterized by thick laminated sand body. Along the South Almora Thrust and Ramgarh Thrust zones, the valleys are narrow and V-shaped where Quaternary deposits are sparse due to relatively rapid uplift across these thrusts. Along the South Almora Thrust zone, three to four levels of fluvial terraces are observed and have been incised by river exposing the bedrocks due to recent movement along the RT and SAT. Abandoned channel, tilted mud deposits, incised meandering, deep-cut V-shaped valleys and strath terraces indicate rapid uplift of the area. Thick mud sequences in the Quaternary columns indicate damming of streams. A ~10-km-long north-south trending transverse Garampani Fault has offset the Ramgarh Thrust producing

  15. Predicting Recreational Water Quality Using Turbidity in the Cuyahoga River, Cuyahoga Valley National Park, Ohio, 2004-7

    Science.gov (United States)

    Brady, Amie M.G.; Bushon, Rebecca N.; Plona, Meg B.

    2009-01-01

    The Cuyahoga River within Cuyahoga Valley National Park (CVNP) in Ohio is often impaired for recreational use because of elevated concentrations of bacteria, which are indicators of fecal contamination. During the recreational seasons (May through August) of 2004 through 2007, samples were collected at two river sites, one upstream of and one centrally-located within CVNP. Bacterial concentrations and turbidity were determined, and streamflow at time of sampling and rainfall amounts over the previous 24 hours prior to sampling were ascertained. Statistical models to predict Escherichia coli (E. coli) concentrations were developed for each site (with data from 2004 through 2006) and tested during an independent year (2007). At Jaite, a sampling site near the center of CVNP, the predictive model performed better than the traditional method of determining the current day's water quality using the previous day's E. coli concentration. During 2007, the Jaite model, based on turbidity, produced more correct responses (81 percent) and fewer false negatives (3.2 percent) than the traditional method (68 and 26 percent, respectively). At Old Portage, a sampling site just upstream from CVNP, a predictive model with turbidity and rainfall as explanatory variables did not perform as well as the traditional method. The Jaite model was used to estimate water quality at three other sites in the park; although it did not perform as well as the traditional method, it performed well - yielding between 68 and 91 percent correct responses. Further research would be necessary to determine whether using the Jaite model to predict recreational water quality elsewhere on the river would provide accurate results.

  16. Implications of anthropogenic river stage fluctuations on mass transport in a valley fill aquifer

    Science.gov (United States)

    Boutt, D.F.; Fleming, B.J.

    2009-01-01

    In humid regions a strong coupling between surface water features and groundwater systems may exist. In these environments the exchange of water and solute depends primarily on the hydraulic gradient between the reservoirs. We hypothesize that daily changes in river stage associated with anthropogenic water releases (such as those from a hydroelectric dam) cause anomalous mixing in the near-stream environment by creating large hydraulic head gradients between the stream and adjacent aquifer. We present field observations of hydraulic gradient reversals in a shallow aquifer. Important physical processes observed in the field are explicitly reproduced in a physically based two-dimensional numerical model of groundwater flow coupled to a simplistic surface water boundary condition. Mass transport simulations of a conservative solute introduced into the surface water are performed and examined relative to a stream condition without stage fluctuations. Simulations of 20 d for both fluctuating river stage and fixed high river stage show that more mass is introduced into the aquifer from the stream in the oscillating case even though the net water flux is zero. Enhanced transport by mechanical dispersion leads to mass being driven away from the hydraulic zone of influence of the river. The modification of local hydraulic gradients is likely to be important for understanding dissolved mass transport in near-stream aquifer environments and can influence exchange zone processes under conditions of high-frequency stream stage changes. Copyright 2009 by the American Geophysical Union.

  17. White River Falls Fish Passage Project, Tygh Valley, Oregon : Final Technical Report, Volume I..

    Energy Technology Data Exchange (ETDEWEB)

    Oregon. Dept. of Fish and Wildlife; Mount Hood National Forest (Or.)

    1985-06-01

    Studies were conducted to describe current habitat conditions in the White River basin above White River Falls and to evaluate the potential to produce anadromous fish. An inventory of spawning and rearing habitats, irrigation diversions, and enhancement opportunities for anadromous fish in the White River drainage was conducted. Survival of juvenile fish at White River Falls was estimated by releasing juvenile chinook and steelhead above the falls during high and low flow periods and recapturing them below the falls in 1983 and 1984. Four alternatives to provide upstream passage for adult salmon and steelhead were developed to a predesign level. The cost of adult passage and the estimated run size of anadromous fish were used to determine the benefit/cost ratio of the preferred alternative. Possible effects of the introduction of anadromous fish on resident fish and on nearby Oak Springs Hatchery were evaluated. This included an inventory of resident species, a genetic study of native rainbow, and the identification of fish diseases in the basin. 28 figs., 23 tabs.

  18. The Effect of Geologic Structures on the Control of Floods in the Middle Yangtze River Valley

    Institute of Scientific and Technical Information of China (English)

    2000-01-01

    This paper discusses the role of geologic structures in the occurrence of floods and how to prevent flood in the middle reaches of the Yangtze River, and gives the author's suggestion that the Luoshan Qiakou be expanded and the land reclaimed from Dongting Lake be returned to the lake in compliance with the law of geology.

  19. Surface-water/ground-water interaction of the Spokane River and the Spokane Valley/Rathdrum Prairie aquifer, Idaho and Washington

    Science.gov (United States)

    Caldwell, Rodney R.; Bowers, Craig L.

    2003-01-01

    Historical mining in the Coeur d’Alene River Basin of northern Idaho has resulted in elevated concentrations of some trace metals (particularly cadmium, lead, and zinc) in water and sediment of Coeur d’Alene Lake and downstream in the Spokane River in Idaho and Washington. These elevated trace-metal concentrations in the Spokane River have raised concerns about potential contamination of ground water in the underlying Spokane Valley/Rathdrum Prairie aquifer, the primary source of drinking water for the city of Spokane and surrounding areas. A study conducted as part of the U.S. Geological Survey’s National Water-Quality Assessment Program examined the interaction of the river and aquifer using hydrologic and chemical data along a losing reach of the Spokane River. The river and ground water were extensively monitored over a range of hydrologic conditions at a streamflow-gaging station and 25 monitoring wells situated from 40 to 3,500 feet from the river. River stage, ground-water levels, water temperature, and specific conductance were measured hourly to biweekly. Water samples were collected on nearly a monthly basis between 1999 and 2001 from the Spokane River and were collected up to nine times between June 2000 and August 2001 from the monitoring wells.

  20. Ecosystem types of boreal forest in the North Klondike River Valley, Yukon Territory, Canada, and their productivity potentials.

    Science.gov (United States)

    Kojima, S

    1996-01-01

    Vegetation, environmental characteristics, and forest productivity were studied in the boreal forest in the North Klondike River Valley, Yukon Territory, Canada. The concept and approach of biogeoclimatic ecosystem classification were followed. For the treed vegetation, five ecosystem types were distinguished based on vegetation structure and physical and chemical properties of soils. They were: 1) spruce-lichen type, 2) spruce-moss type, 3) spruce-Equisetum type, 4) spruce-willow type, and 5) bog forest type. These types were differentiated mainly by moisture regime and base status of soils. The sequence of the ecosystem types reflected their topographical position from slope summit to valley bottom. The spruce-lichen type developed in the driest and nutritionally impoverished habitats, the spruce-Equisetum type occurred in moist and nutritionally enriched sites, and the spruce-moss type was found in between them. The bog forest type occurred where peat had accumulated sufficiently to generate ombrotrophic conditions in habitats of high water table underlain with permafrost. The spruce-willow type developed along small creeks where substrates were very coarse. Tree growth characteristics were measured, except for the bog forest type that did not have trees over 5 m tall. Total volume of standing trees ranged from 29 to 582 m(3)/ha, with an overall mean of 216.9 m(3)/ha. The spruce-Equisetum type exhibited the highest figure, 413.5 m(3)/ha, while spruce-lichen type the lowest one, 87.7 m(3)/ha. Mean annual increment ranged from 0.15 to 2.66 m(3)/ha, with an overall mean of 1.10 m(3)/ha. A similar tendency was noted for all other forestry characteristics, i.e., the spruce-Equisetum type showed the highest productivity while the spruce-lichen type the lowest. This tendency was considered to be attributed to the availability of moisture and basic cations in soils. PMID:24198010

  1. Influence of interannual variability of Antarctic oscillation on mei-yu along the Yangtze and Huaihe River valley and its importance to prediction

    Institute of Scientific and Technical Information of China (English)

    GAO Hui; XUE Feng1; WANG Huijun1

    2003-01-01

    Both correlation analysis and case study indicate that Antarctic oscillation (AAO) is closely related with summer rainfall in eastern China. When AAO is stronger in boreal spring, especially in May, there is more mei-yu rainfall in summer with a longer period along the Yangtze and Huaihe River valley. In contrast, there is less rainfall with a shorter period corresponding to a weaker AAO. Besides, an anomalous AAO changes the position and intensity of several circulation systems, which are important to summer rainfall along the Yangtze and Huaihe River valley. Furthermore, the Antarctic sea ice is negatively correlated with the intensity of AAO with a 6-month leading time. The result in this study provides a new method for the prediction of mei-yu.

  2. Infrastructure and climate change: Impacts and adaptations for the Zambezi River Valley

    OpenAIRE

    Paul S. Chinowsky; Amy E. Schweikert; Strzepek, Niko L.; Strzepek, Kenneth

    2013-01-01

    The African Development Bank has called for US$40 billion per year over the coming decades to be provided to African countries to address development issues directly related to climate change. The current study addresses a key component of these issues, the effect of climate change on the road infrastructure of Malawi, Mozambique, and Zambia, all located within the Zambezi River Basin. The study incorporates a stressor-response approach to estimate the effects of projected precipitation, temp...

  3. Plio-Pleistocene stratigraphy and relations between marine and non-marine successions in the Middle Valley of the Tiber River (Latium, Umbria)

    OpenAIRE

    Girotti, O.; Università di Roma "La Sapienza", Dipartimento di Scienze della Terra; Mancini, M.; Università di Roma "La Sapienza", Dipartimento di Scienze della Terra

    2003-01-01

    The Middle Valley of the Tiber River (MVT) corresponds to the “Paglia-Tevere Graben”, a “neoautochthonous” basin developed since the latest Early Pliocene. The basin is in part linked with the intrapenninic Tiberino and Rieti Basins to the east, and with the Roman Basin to the south. The filling is mostly made up of Plio-Pleistocene marine deposits, unconformably overlaying the meso-cenozoic substratum. Two outcropping 3rd order depositional sequences have been recognised: 1) the old...

  4. Ground-water data for the Salt Basin, Eagle Flat, Red Light Draw, Green River Valley and Presidio Bolson in westernmost Texas

    Science.gov (United States)

    White, Donald E.; Gates, Joseph S.; Smith, James T.; Fry, Bonnie J.

    1980-01-01

    From October 1971 through October 1974. the U.S. Geological Survey collected ground-water data in the basins in Texas west of the Pecos River drainage area and northwest of the Big Bend country. The basins included are, from east to west: The Presidio Bolson; the Salt Basin; Green River Valley, Eagle Flat, and Red Light Draw. These data, which were collected in cooperation with the Texas Department of Water Resources (formerly Texas Water Development Board), will provide information for a continuing assessment of water availability within the State.

  5. Valley-fill alluviation during the Little Ice Age (ca. A.D. 1400-1880), Paria River basin and southern Colorado Plateau, United States

    Science.gov (United States)

    Hereford, R.

    2002-01-01

    Valley-fill alluvium deposited from ca. A.D. 1400 to 1880 is widespread in tributaries of the Paria River and is largely coincident with the Little Ice Age epoch of global climate variability. Previous work showed that alluvium of this age is a mappable stratigraphic unit in many of the larger alluvial valleys of the southern Colorado Plateau. The alluvium is bounded by two disconformities resulting from prehistoric and historic arroyo cutting at ca. A.D. 1200-1400 and 1860-1910, respectively. The fill forms a terrace in the axial valleys of major through-flowing streams. This terrace and underlying deposits are continuous and interfinger with sediment in numerous small tributary valleys that head at the base of hillslopes of sparsely vegetated, weakly consolidated bedrock, suggesting that eroded bedrock was an important source of alluvium along with in-channel and other sources. Paleoclimatic and high-resolution paleoflood studies indicate that valley-fill alluviation occured during a long-term decrease in the frequency of large, destructive floods. Aggradation of the valleys ended about A.D. 1880, if not two decades earlier, with the beginning of historic arroyo cutting. This shift from deposition to valley entrenchment near the close of the Little Ice Age generally coincided with the beginning of an episode of the largest floods in the preceding 400-500 yr, which was probably caused by an increased recurrence and intensity of flood-producing El Nin??o events beginning at ca. A.D. 1870.

  6. The chemistry of river-lake systems in the context of permafrost occurrence (Mongolia, Valley of the Lakes) Part II. Spatial trends and possible sources of organic composition

    Science.gov (United States)

    Szopińska, Małgorzata; Dymerski, Tomasz; Polkowska, Żaneta; Szumińska, Danuta; Wolska, Lidia

    2016-07-01

    The chemistry of river-lake systems located in Central Mongolia near the southern border of permafrost occurrence has not been well studied. The main aim of this paper is to summarize patterns in water chemistry in supply springs, rivers and lakes in relation to permafrost occurrence, as well as other natural and anthropogenic impacts. The analyses involved water samples taken from two river-lake systems: the Baydrag River-Böön Tsagaan Lake system and the Shargalyuut/Tuyn Rivers-Orog Lake system. Total organic carbon (TOC) and polycyclic aromatic hydrocarbons (PAHs) were detected and quantified. Other organic compounds, such as organic halogen compounds, phthalates, and higher alkanes were also noted. The main factors which influence differences in TOC concentrations in the water bodies involve permafrost occurrence, mainly because compounds are released during active layer degradation (in the upper reach of the Tuyn river), and by intensive livestock farming in river valleys and in the vicinity of lakes. In relation to the concentrations of PAHs, high variability between samples (> 300 ng L- 1), indicates the influence of thermal water and local geology structures (e.g., volcanic and sedimentary deposits), as well as accumulation of suspended matter in lakes transported during rapid surface runoff events. The monitoring of TOC as well as individual PAHs is particularly important to future environmental studies, as they may potentially reflect the degradation of the environment. Therefore, monitoring in the Valley of the Lakes should be continued, particularly in the light of the anticipated permafrost degradation in the 21st century, in order to collect more data and be able to anticipate the response of river-lake water chemistry to changes in permafrost occurrence.

  7. Features of the short-term position variation of the west Pacific subtropical high during the torrential rain in Yangtze-Huaihe river valley and its possible cause

    Science.gov (United States)

    Guan, Zhaoyong; Yu, Bo; Wang, Lijuan; He, Jielin; Zeng, Gang

    2009-08-01

    By using the NCEP/NCAR daily reanalysis data, CMAP precipitation data , daily precipitation data of 740 stations in China and some remote sensing data, features of the short-term position variation of the west Pacific subtropical high(WPSH) during the torrential rain in Yangtze-Huaihe river valley and its possible cause are analyzed. Results show that the short-term position variation of WPSH is closely associated with the diabatic heating. During the torrential rain period, the apparent heating source and apparent moisture sink are exceptionally strong over Yangtze-Huaihe river valley( on the northwest side of WPSH )and the Bay of Bengal (to the west of WPSH). Based on the complete form of vertical vorticity tendency equation, it is found that the heating field over Yangtze-Huaihe river valley during the torrential rain period, which is in favor of the increase of cyclonic vorticity on the north side of WPSH, is unfavorable to the WPSH moving northward. And the heat source over the Bay of Bengal ,which is in favor of the increase of anti-cyclonic vorticity on the west of WPSH, may induce the westward extension of WPSH.

  8. Eocene extension in Idaho generated massive sediment floods into Franciscan trench and into Tyee, Great Valley, and Green River basins

    Science.gov (United States)

    Dumitru, Trevor A.; Ernst, W.G.; Wright, James E.; Wooden, Joseph L.; Wells, Ray E.; Farmer, Lucia P.; Kent, Adam J.R.; Graham, Stephan A.

    2013-01-01

    The Franciscan Complex accretionary prism was assembled during an ∼165-m.y.-long period of subduction of Pacific Ocean plates beneath the western margin of the North American plate. In such fossil subduction complexes, it is generally difficult to reconstruct details of the accretion of continent-derived sediments and to evaluate the factors that controlled accretion. New detrital zircon U-Pb ages indicate that much of the major Coastal belt subunit of the Franciscan Complex represents a massive, relatively brief, surge of near-trench deposition and accretion during Eocene time (ca. 53–49 Ma). Sediments were sourced mainly from the distant Idaho Batholith region rather than the nearby Sierra Nevada. Idaho detritus also fed the Great Valley forearc basin of California (ca. 53–37 Ma), the Tyee forearc basin of coastal Oregon (49 to ca. 36 Ma), and the greater Green River lake basin of Wyoming (50–47 Ma). Plutonism in the Idaho Batholith spanned 98–53 Ma in a contractional setting; it was abruptly superseded by major extension in the Bitterroot, Anaconda, Clearwater, and Priest River metamorphic core complexes (53–40 Ma) and by major volcanism in the Challis volcanic field (51–43 Ma). This extensional tectonism apparently deformed and uplifted a broad region, shedding voluminous sediments toward depocenters to the west and southeast. In the Franciscan Coastal belt, the major increase in sediment input apparently triggered a pulse of massive accretion, a pulse ultimately controlled by continental tectonism far within the interior of the North American plate, rather than by some tectonic event along the plate boundary itself.

  9. Modelling potential landscape sediment delivery due to projected soybean expansion: a scenario study of the Balsas sub-basin, Cerrado, Maranhão state, Brazil.

    Science.gov (United States)

    Barreto, Larissa; Schoorl, Jeroen M; Kok, Kasper; Veldkamp, Tom; Hass, Adriani

    2013-01-30

    In Brazil, agriculture expansion is taking place primarily in the Cerrado ecosystems. With the aim of supporting policy development and protecting the natural environment at relevant hotspots, a scenario study was conducted that concerned not only land-use change, but also the resulting effects on erosion and deposition. This coupled approach helped to evaluate potential landscape impacts of the land-use scenarios. In the study area, the Balsas sub-basin in Maranhão State, a model chain was used to model plausible future soybean expansion locations (CLUE-S model) and resulting sediment mobilization patterns (LAPSUS model) for a business-as-usual scenario. In the scenario, more erosion occurred in areas where the conversion of natural vegetation into soybean cultivation is likely to take place, but the generated sediments tended to accumulate mainly within the conversion areas, thus limiting the offsite effects of the increased erosion. These results indicated that when agricultural expansion is kept away from rivers, Cerrado conversion will have only a limited impact on the sediment loads of local rivers. Where land-use changes are most concentrated are coincident with areas where more new sediments are generated (higher erosion) and where more sediments are re-deposited.

  10. Post-earthquake modification of 2015 Gorkha Earthquake landslides in the Bhote Koshi River valley

    Science.gov (United States)

    Cook, Kristen; Andermann, Christoff; Adhikari, Basanta; Schmitt, Clemens; Marc, Odin

    2016-04-01

    Large earthquakes trigger widespread mass failures, and the estimated volumes of landslide material are often used to estimate seismically triggered erosion, assuming that all landslide material is transported out of the affected area. The expectation that earthquakes can generate a pulse of sediment output from the affected area can also potentially be used to recognize large seismic events in the sedimentary record. However, in order to properly understand the relationship between earthquake triggered landslides, sediment flux, and erosion, we need to consider how and when the landslide debris is mobilized in the fluvial system and exported from the catchment. We present observations from three field excursions to the upper Bhote Koshi River following the April 25 2015 Gorkha earthquake, which triggered extensive landsliding in this region. Our observations, from early June, late July, and Oct 2015, cover the pre-monsoon, mid-monsoon, and post-monsoon periods, allowing us to constrain monsoon-driven changes to seismically triggered landslides.In order to quantify post-earthquake modification of individual landslides and of the transport of landslide materials to the main trunk rivers, we conducted surveys using both terrestrial lidar and SfM. Immediately following the earthquake, a large number of landslides were disconnected from the channels, with significant amounts of material stored on the hillslopes. This was facilitated by the widespread presence of a two-step topography, with steep slopes adjacent to the main river channels and a section of lower gradient hillslope above. The landslides above this step typically did not reach the channel, or only delivered material via preexisting narrow debris flow chutes. As expected, the monsoon caused new landslides, the expansion of existing landslides, and the modification of coseisimic landslide deposits. In late July we observed ongoing mobilization of this stored material, with repeated downslope delivery of

  11. Low-temperature geothermal assessment of the Santa Clara and Virgin River Valleys, Washington County, Utah

    Energy Technology Data Exchange (ETDEWEB)

    Budding, K.E.; Sommer, S.N.

    1986-01-01

    Exploration techniques included the following: (1) a temperature survey of springs, (2) chemical analyses and calculated geothermometer temperatures of water samples collected from selected springs and wells, (3) chemical analyses and calculated geothermometer temperatures of spring and well water samples in the literature, (4) thermal gradients measured in accessible wells, and (5) geology. The highest water temperature recorded in the St. George basin is 42/sup 0/C at Pah Tempe Hot Springs. Additional spring temperatures higher than 20/sup 0/C are at Veyo Hot Spring, Washington hot pot, and Green Spring. The warmest well water in the study area is 40/sup 0/C in Middleton Wash. Additional warm well water (higher than 24.5/sup 0/C) is present north of St. George, north of Washington, southeast of St. George, and in Dameron Valley. The majority of the Na-K-Ca calculated reservoir temperatures range between 30/sup 0/ and 50/sup 0/C. Anomalous geothermometer temperatures were calculated for water from Pah Tempe and a number of locations in St. George and vicinity. In addition to the known thermal areas of Pah Tempe and Veyo Hot Spring, an area north of Washington and St. George is delineated in this study to have possible low-temperature geothermal potential.

  12. Mechanisms for concurrent low-latitude circulation anomalies responsible for persistent extreme precipitation in the Yangtze River Valley

    Science.gov (United States)

    Chen, Yang; Zhai, Panmao

    2016-08-01

    Concurrent position shifts of the mid-level western Pacific subtropical high (WPSH) and the upper-level South Asia high (SAH) are regarded as significant precursors for persistent extreme precipitation events (PEPEs) in the Yangtze River Valley (YRV). By performing composite analyses, accountable vorticity genesis and dissipation are diagnosed based on a potential vorticity-diabatic heating theory. The results indicate that about 1 week preceding precipitation onset, a wave-like pattern of anomalous diabatic heating (Q) initiates its northwestward propagation from equatorial central Pacific. Subsequently, this wave-like pattern induces substantial changes in both horizontal and vertical structure of local Q along the propagating route. Forced negative vorticities in key areas result in the zonal approach between the SAH and the WPSH. During PEPEs, two thermal-induced vertical circulation cells take shape, with common strong ascent centered in the YRV. These anomalous cells are capable of self-maintaining for a few days via positive feedback processes. The WPSH and the SAH are therefore anchored in respective favorable positions for PEPEs. Simultaneously, descending motion of these two cells increases local solar radiation and decreases upward latent heat flux from surface, facilitating warmer underlying surface and swift accumulation of lower-level moisture. Correspondingly, enhanced heating to the north and rapid developing cyclone over warmer sea surface to the south combine to terminate above positive feedback processes. Finally, both the WPSH and the SAH retreat to their normal positions, accompanied by a quick decay of PEPEs.

  13. Principal Disease and Insect Pests of Jatropha curcas L. in the Lower Valley of the Senegal River

    Directory of Open Access Journals (Sweden)

    Terren, M.

    2012-01-01

    Full Text Available Jatropha curcas L. seed oil is proven to be toxic to many microorganisms, insects and animals. Despite its toxicity, Jatropha is not pest and disease resistant. The following major pests and diseases affecting Jatropha in the lower valley of the Senegal river have been identified: the leaf miner Stomphastis thraustica (Meyrick, 1908 (Lepidoptera, Gracillariidae, the leaf and stem miner Pempelia morosalis (Saalmuller, 1880 (Lepidoptera, Pyralidae and the shield-backed bug Calidea panaethiopica (Kirkaldy, 1909 (Heteroptera, Scutelleridae, which can cause flower and fruit abortion. Damage from these pests was particularly great during the second year after the plantations were set up (2009 and before later receding. Nevertheless, the worst attacks were caused by a vascular disease transmitted through the soil, which killed 65% of the plants in four years. It is mainly characterised by collar and root rot, which causes foliage to yellow and wilt, before the plant eventually dies. These threats should increase if larger areas are planted with Jatropha. Considering the scale of the damage caused by these attacks in Bokhol, the development of an integrated pest management programme adapted to the local context should be considered.

  14. Variation of GPS Precipitable Water over the Qinghai-Tibet Plateau: Possible Teleconnection Triggering Rainfall over the Yangtze River Valley

    Directory of Open Access Journals (Sweden)

    Gui-Rong Xu

    2011-01-01

    Full Text Available GPS technologies show many capabilities for monitoring atmospheric water vapor. This study uses GPS data from the Japan International Co-operation Agency (JICA and Hubei GPS network to monitor precipitable water (PW over the Qinghai-Tibet Plateau (QTP and over the middle Yangtze River Valley (YRV. The results show that the southern QTP is wetter than the central area due to the barring effect of the Plateau on the monsoon. PW is higher in summer than other months over either the QTP or the middle YRV. The diurnal variation of PW over the QTP is more complex than that of the middle YRV with fluctuations occurring during the whole day due to the unique topography. The minimum PW over both the QTP and the middle YRV appears in the morning; however, the peak over the QTP occurs at night while the peak over the middle YRV occurs in the early afternoon. Furthermore, PW over the QTP, especially its southern and eastern edges, are positively correlated with PW over the middle YRV. This may imply that the southern and eastern Plateaus are key regions transporting atmospheric vapor to the middle YRV. Our results indicate the possibility of finding early warning signals resulting from the intensification of the QTP atmospheric vapor leading to heavy rainfall events over the middle YRV.

  15. Geochemistry of uranium in ground waters of the Conlara river Valley, San Luis and Cordoba provinces (Argentina)

    International Nuclear Information System (INIS)

    Geochemical characteristics of ground waters related with lixiviation, transport and precipitation of uranium in the Conlara river valley (provinces of San Luis and Cordoba (Argentina)) are studied. Anions and cations' distributions, together with hardness, specific conductivity, pH, Eh, and uranium and vanadium contents, have been studied. Those parameters characterize four hidrogeochemical facies along an E-W profile: a calcic strong bicarbonate facies, an alkaline-calcic bicarbonate facies, an alkaline sulfate facies, and a strong alkaline sulfate facies. An ''Interphase zone'' (transition from bicarbonate water to sulfate water), where changes in composition may define a geochemical environment capable of UO2 precipitation, has been determined. The chemical-Thermodynamic studies give a dominance of UDC and UTC complexs ions (even in sulfate waters), so they represent the 99% of present ions. Besides, the calculated values required for equilibrium with uraninite or carnotite resulted much greater than those obtained in the performed experiments. It means that the precipitation of those minerals requires either the presence of greate amounts of uranium or vanadium, or a reducing environment with Eh values smaller than the observed ones. Finally, the steps to be taken in future investigations are suggested in view to a drilling plan where: 1) Priority to the ''Interphase zone'' areas is given. 2) The deepest aquifers in Tertiary sediments of the basin have to be reached in order to get the convenient environmental conditions (i.e. smallest Eh values) for uranium or uranium-vanadium precipitation. (author)

  16. Geomorphology of the Urümqi River Valley and the uplift of the Tianshan Mountains in Quaternary

    Institute of Scientific and Technical Information of China (English)

    ZHOU; Shangzhe; (周尚哲); JIAO; Keqin; (焦克勤); ZHAO; Jingdong; (赵井东); ZHANG; Shiqiang; (张世强); CUI; Jianxin; (崔建新); XU; Liubing; (许刘兵)

    2002-01-01

    The Shaerqiaoke Gravel, more than 400 m in thickness, on the north piedmont of the Tianshan Mountains, is located at the exit of the Urümqi River Valley and belongs to the Molasse construction of the Tianshan Mountains. Another uplift event with the tectonic boundary expansion ended the deposition of the Shaerqiaoke Gravel, and resulted in folding, faulting and down-erosion in the frontier of the deposit. The ESR dating indicates that the top of the Shaerqiaoke Gravel accumulated before 1148 kaBP, probably responding to the Kunlun-Huanghe movement of the Qinghai-Tibetan plateau. After that time, erosion-deposition cycle occurred and 9 terraces developed. The TL and ESR dating techniques were employed to date these terraces, and the results indicate that Terrace 3 was formed at MIS 6. Terrace 2 at Houxia also developed simultaneously. Terraces 5 and 6 were accumulated in 338 kaBP and 562-591 kaBP, respectively. The oldest glaciation, named Gao Wangfeng, correlates to MIS 12.

  17. Fossil gastropods from the MGS3 stratigraphic segment in the Salawusu River Valley and their climatic and environmental implications

    Institute of Scientific and Technical Information of China (English)

    LI BaoSheng; YE JianPing; GUO YunHai; CHEN DeNiu; David Dian ZHANG; WEN XiaoHao; QIU ShiFan; OU XianJiao; DU ShuHuan; NIU DongFeng; YANG Yi

    2008-01-01

    Contemporaneous with MIS3, the MGS3 segment of the Milanggouwan stratigraphic section in the Salawusu River Valley, Mu Us Desert, China contains fossil gastropods (terrestrial and freshwater snails) in strata 33LS, 35LS, 37FL and 39LS. Examination of these fossils revealed 11 species belonging to 8 families and 10 genera. They can be classified as: (1) assemblage of Gyraulus and Galba mainly consisting of Gyraulus convexiusculus, Gyraulus sibiricus, Galba pervia and Galba superegra Gredler,etc. (2) assemblage of Vallonia mainly consisting of terrestrial snails, such as Vallonia patens, Pupilla muscorum and Discus paupe, etc. Based on the dating results, and the living habits, living conditions,and geographic distribution of their extant species, we suggest that: the ages of 33LS, 35LS, 37FL, and 39LS are 26000, 29000, 33000 and 38000 a, respectively, corresponding well to the interstadial period in GRIP 4,5, 6 and 10 in terms of chronology and climatic characters; 33LS, 35LS and 39LS represent very warm-humid periods, while 37FL represents a less warm-humid period; the four periods of climatic fluctuations recorded in MGS3 were related to the strong impact of the summer monsoon in East Asia in Mu Us Desert of China during the interstadial of MIS3 on a global climatic background.

  18. The Impact of Indian Ocean Variability on HighTemperature Extremes across the Southern Yangtze River Valley in Late Summer

    Institute of Scientific and Technical Information of China (English)

    HU Kaiming; HUANG Gang; QU Xia; HUANG Ronghui

    2012-01-01

    In this study,the teleconnection between Indian Ocean sea surface temperature anomalies (SSTAs) and the frequency of high temperature extremes (HTEs) across the southern Yangtze River valley (YRV) was investigated.The results indicate that the frequency of HTEs across the southern YRV in August is remotely influenced by the Indian Ocean basin mode (IOBM) SSTAs.Corresponding to June-July-August (JJA) IOBM warming condition,the number of HTEs was above normal,and corresponding to IOBM cooling conditions,the number of HTEs was below normal across the southern YRV in August.The results of this study indicate that the tropical IOBM warming triggered low-level anomalous anticyclonic circulation in the subtropical northwestern Pacific Ocean and southern China by emanating a warm Kelvin wave in August.In the southern YRV,the reduced rainfall and downward vertical motion associated with the anomalous low-level anticyclonic circulation led to the increase of HTE frequency in August.

  19. Variation of spring climate in lower-middle Yangtse River Valley and its relation with solar-cycle length

    Energy Technology Data Exchange (ETDEWEB)

    Hameed, S. [State Univ. of New York, Stony Brook, NY (United States); Gaofa Gong [Institute of Geography, Beijing (China)

    1994-12-01

    The relatively large number of historical records originating from the area of the Middle and Lower Yangtse River Valley in the late Ming dynasty and the Qing dynasty allows an estimation of the long term fluctuations of phenological dates. Dates of blossoming of plants, found in personal diaries and other documents, and used in this reconstruction are available, with some gaps, for 1580-1920. Independent estimates of spring conditions during the 18th century using data on last day of snowfall, and during 20th and late 19th centuries using accumulated temperatures in Shanghai are also presented. The results show that the spring weather in this region was colder than present in the 17th century and during 1790-1820 and 1870-1920. Spring temperature warmer than the present prevailed during 1720-1770 and 1840-1860. This variation agrees in its broad outline with that of the solar cycle length presented by Friis-Christensen and Lassen. 13 refs., 2 figs., 1 tab.

  20. Variation of spring climate in lower-middle Yangtse River Valley and its relation with solar-cycle length

    Science.gov (United States)

    Hameed, Sultan; Gong, Gaofa

    1994-12-01

    The relatively large number of historical records originating from the area of the Middle and Lower Yangtse River Valley in the late Ming dynasty and the Qing dynasty allows an estimation of the long term fluctuations of phenological dates. Dates of blossoming of plants, found in personal diaries and other documents, and used in this reconstruction are available, with some gaps, for 1580-1920. Independent estimates of spring conditions during the 18th century using data on last day of snowfall, and during 20th and late 19th centuries using accumulated temperatures in Shanghai are also presented. The results show that the spring weather in this region was colder than present in the 17th century and during 1790-1820 and 1870-1920. Spring temperature warmer than the present prevailed during 1720-1770 and 1840-1860. This variation agrees in its broad outline with that of the solar cycle length presented by Friis-Christensen and Lassen (1991).

  1. Preliminary Study on Biological Characteristics of Degraded Soil Ecosystems in Dry Hot Valley of the Jinsha River

    Institute of Scientific and Technical Information of China (English)

    2002-01-01

    Distribution characteristics of soil animals, microorganisms and enzymatic activity were studied in thedry red soil and Vertisol ecosystems with different degradation degrees in the Yuanmou dry hot valley of theJinsha River, China. Results showed that Hymenoptera, Araneae and Collembola were the dominant groupsof soil animals in the plots studied. The numbers of groups and individuals and density of soil animals in thedry red soil series were higher than those in the Vertisol series, and the numbers of individuals and density ofsoil animals decreased with the degree of soil degradation. Bacteria dominated microbiocoenosis not only inthe dry red soils but also in the Vertisols. Microbial numbers of the dry red soil series were higher than thoseof Vertisol series, and decreased with the degree of soil degradation. The activities of catalase, invertase,urease and alkaline phosphatase declined with the degradation degree and showed a significant decline withdepth in the profiles of both the dry red soils and the Vertisols, but activities of polyphenol oxidase andacid and neutral phosphatase showed the same tendencies only in the Vertisols. It was concluded that thecharacteristics of soil animals, microorganisms and enzymatic activity could be used as the bio-indicators toshow the degradation degree of the dry red soils and Vertisols. Correlation among these soil bio-indicatorswas highly significant.

  2. The Aznalcollar (Spain) tailings pond failure of 1998 and the ecological disaster of Guadiamar river: causes, effects and lessons; La rotura de la balsa de residuos mineros de Aznalcollar (Espana) de 1998 y el desastre ecologico consecuente del rio Guadiamar: causas, efectos y lecciones

    Energy Technology Data Exchange (ETDEWEB)

    Ayala-Carcedo, F. J.

    2004-07-01

    On 1998 a large tailings pond confined by a rock fill dyke in the Aznalcollar metallic mine near Sevilla, at the SW of Spain, failed with a big impact on public opinion due to potential environmental Impact on Donana National Park,a key natural space for birds migration between Europea and Africa. The accident is placed in a comparative way with others in the world, the causes of failure, its dynamics and the spill are analysed and also the actual ecological impacts related to the tailings and acid waters scattered by the Agrio and Guadiamar rivers. The lessons for future design and location of these type of deposits and water dams are also presented. The accident very quick, was caused by shear failure of the foundation formation, a miocene over consolidated marly clay, known as Guadalquivir blue marl, through a vertical point and a bedding plane, as a result of a progressive failure process under high pore pressure. Dynamic liquefaction of tailings due to sudden vertical movement towards the void created by the initial movement was a key factor to increase the outwards movement of the dyke, broken by the movement, and the tailings spill. The double dyke failure (main dyke and internal one) produced a tailings spill with solid and liquid flow. The dynamics of these flows is presented and also the combination of factors driving to failure. the problem posed by the successive human institutional failures, a necessary cause driving to no consideration of the possibility of the progressive failure in these formations, known from 1964, is also analysed. (Author) 67 refs.

  3. Flooding of the Great River during the Common Era: A Paleohydrological Record of High Magnitude Flood Events from the Central Mississippi River Valley

    Science.gov (United States)

    Williams, J. W.; Munoz, S. E.; Gruley, K. E.; Massie, A.

    2014-12-01

    Streamflow characteristics are known to be sensitive to changes in climate, but few continuous records of flooding exist to evaluate the response of hydrological systems to centennial- and millennia-scale climate changes. Here, we present sedimentary records from two oxbow lakes (Horseshoe Lake and Grassy Lake, Illinois, USA) in the central Mississippi River valley (CMRV) that display abrupt shifts in sediment composition and particle-size consistent with deposition by floodwaters immediately following inundation of the floodplain. The sedimentary record at Horseshoe Lake begins ca. AD 100 and displays five major flood events, with four of these occurring after ca. AD 1100. Situated 200 km downstream, the record from Grassy Lake begins later, ca. AD 800, and also shows four major flood events after ca. AD 1100. An analysis of synchronicity using Bayesian age modelling software shows high likelihoods that the four overlapping flood events occurred at the same time, confirming that these events resulted from flooding of the Mississippi River. The most recent event we record at AD 1840 ± 50 corresponds to the AD 1844 flood, the largest flood by discharge (37 m3/s) measured by the gauging station at St. Louis, Missouri, indicating that our sedimentary records document high magnitude flood events. Together, our two sedimentary records show a major shift in the frequency of high magnitude flooding in the central Mississippi River at ca. AD 1100. From AD 100 - AD 1100, only one relatively subtle flood event is recorded, but from AD 1100 - AD 1900, four high magnitude floods deposited distinctive sediment at both sites. The period of infrequent flooding corresponds to a time of agricultural intensification and population growth in the CMRV, while the entire region was abandoned when flood frequency increased. The pronounced shift in flood frequency we observe in our records at ca. AD 1100 begins during the Medieval Climate Anomaly (MCA; AD 950 - AD 1250), a period of

  4. Late Holocene dune activity in the Eastern Platte River Valley, Nebraska

    Science.gov (United States)

    Hanson, P. R.; Joeckel, R. M.; Young, A. R.; Horn, J.

    2009-02-01

    Large-scale dune activity in the Nebraska Sand Hills and elsewhere on the western Great Plains has been linked to prehistoric "megadroughts" that triggered the activation of regional dune fields. The effect of megadroughts on the smaller dune fields east of the Nebraska Sand Hills has never been assessed, however. This study focuses on the Duncan dune field near the confluence of the Loup and Platte rivers in eastern Nebraska. Seventeen optically stimulated luminescence age estimates were obtained and reveal two periods of dune activation that occurred between 4.4 to 3.4 ka and 0.8 to 0.5 ka. Significantly, both periods chronologically overlap large-scale dune activity identified in the Nebraska Sand Hills. Geochemical evidence indicates that the Duncan dunes received sand not only from the terrace underlying them, but also from the Loup River. These data link dune activity in the Duncan area, at least indirectly, to increased sediment supply from streams that drain the Sand Hills during megadroughts, implying the activation of the dunes occurred as an indirect response to regional megadroughts. Calculations of dune migration rates, however, argue in favor of local, drought-driven hydrologic changes as a causative factor in dune activation, in other words, a direct effect of megadroughts. Whether the impact was direct or indirect, it is highly likely that the repeated reactivation of the Duncan dunes resulted in some way from regional, large-magnitude droughts. Other paleoclimate proxies from the Great Plains tend to support this conclusion. We conclude that the megadroughts that have been identified in the Sand Hills and other Great Plains dune fields were indeed regional events with far-reaching effects.

  5. Climatic and geologic controls on suspended sediment flux in the Sutlej River Valley, western Himalaya

    Directory of Open Access Journals (Sweden)

    H. Wulf

    2012-01-01

    Full Text Available The sediment flux through Himalayan rivers directly impacts water quality and is important for sustaining agriculture as well as maintaining drinking-water and hydropower generation. Despite the recent increase in demand for these resources, little is known about the triggers and sources of extreme sediment flux events, which lower water quality and account for extensive hydropower reservoir filling and turbine abrasion. Here, we present a comprehensive analysis of the spatiotemporal trends in suspended sediment flux based on daily data during the past decade (2001–2009 from four sites along the Sutlej River and from four of its main tributaries. In conjunction with satellite data depicting rainfall and snow cover, air temperature, earthquake records, and Schmidt hammer rock strength measurements, we infer climatic and geologic controls of peak suspended sediment concentration (SSC events. Our study identifies three key findings: First, peak SSC events (≥99th SSC percentile coincide frequently (57–80% with heavy rainstorms and account for about 30% of the suspended sediment flux in the semi-arid to arid interior of the orogen. Second, we observe an increase of suspended sediment flux from the Tibetan Plateau to the Himalayan front at mean annual timescales. This sediment-flux gradient suggests that averaged, modern erosion in the western Himalaya is most pronounced at frontal regions, which are characterized by high monsoonal rainfall and thick soil cover. Third, in seven of eight catchments we find an anticlockwise hysteresis loop of annual sediment flux, which appears to be related to enhanced glacial sediment evacuation during late summer. Our analysis emphasizes the importance of unconsolidated sediments in the high-elevation sector that can easily be mobilized by hydrometeorological events and higher glacial-meltwater contributions.

  6. Sulphuric acid speleogenesis and landscape evolution: Montecchio cave, Albegna river valley (Southern Tuscany, Italy)

    Science.gov (United States)

    Piccini, Leonardo; De Waele, Jo; Galli, Ermanno; Polyak, Victor J.; Bernasconi, Stefano M.; Asmerom, Yemane

    2015-01-01

    Montecchio cave (Grosseto province, Tuscany, Italy) opens at 320 m asl, in a small outcrop of Jurassic limestone (Calcare Massiccio Fm.), close to the Albegna river. This area is characterised by the presence of several thermal springs and the outcropping of travertine deposits at different altitudes. The Montecchio cave, with passage length development of over 1700 m, is characterised by the presence of several sub-horizontal passages and many medium- and small-scale morphologies indicative of sulphuric acid speleogenesis (SAS). The thermal aquifer is intercepted at a depth of about 100 m below the entrance: the water temperature exceeds 30 °C and sulphate content is over 1300 mg l- 1. The cave hosts large gypsum deposits from 40 to 100 m below the entrance that are by-products of the reaction between sulphuric acid and the carbonate host rock. The lower part of the cave hosts over 1 m thick calcite cave raft deposits, which are evidence of long-standing, probably thermal, water in an evaporative environment related to significant air currents. Sulphur isotopes of gypsum have negative δ34S values (from - 28.3 to - 24.2‰), typical of SAS. Calcite cave rafts and speleogenetic gypsum both yield young U/Th ages varying from 68.5 ka to 2 ka BP, indicating a rapid phase of dewatering followed by gypsum precipitation in aerate environment. This fast water table lowering is related to a rapid incision of the nearby Albegna river, and was followed by a 20-30 m fluctuation of the thermal water table, as recorded in the calcite raft deposits and gypsum crusts.

  7. Questa baseline and pre-mining ground-water quality investigation. 3. Historical ground-water quality for the Red River Valley, New Mexico

    Science.gov (United States)

    LoVetere, Sara H.; Nordstrom, D. Kirk; Maest, Ann S.; Naus, Cheryl A.

    2003-01-01

    Historical ground-water quality data for 100 wells in the Red River Valley between the U.S. Geological Survey streamflow-gaging station (08265000), near Questa, and Placer Creek east of the town of Red River, New Mexico, were compiled and reviewed. The tabulation included 608 water-quality records from 23 sources entered into an electronic database. Groundwater quality data were first collected at the Red River wastewater-treatment facility in 1982. Most analyses, however, were obtained between 1994 and 2002, even though the first wells were developed in 1962. The data were evaluated by considering (a) temporal consistency, (b) quality of sampling methods, (c) charge imbalance, and (d) replicate analyses. Analyses that qualified on the basis of these criteria were modeled to obtain saturation indices for gypsum, calcite, fluorite, gibbsite, manganite, and rhodocrosite. Plots created from the data illustrate that water chemistry in the Red River Valley is predominantly controlled by calcite dissolution, congruent gypsum dissolution, and pyrite oxidation.

  8. Effects of fluvial processes in different order river valleys on redistribution and storage of particle-bound radioactive caesium-137 in area of significant Chernobyl fallout and impact on linked rivers with lower contamination levels

    Science.gov (United States)

    Belyaev, Vladimir; Golosov, Valentin; Shamshurina, Evgeniya; Ivanov, Maxim; Ivanova, Nadezhda; Bezukhov, Dmitry; Onda, Yuichi; Wakiyama, Yoshifumi; Evrard, Olivier

    2015-04-01

    Detailed investigations of the post-fallout fate of radionuclide contamination represent an important task in terms of environmental quality assessment. In addition, particle-bound radionuclides such as the most widespread anthropogenic isotope caesium-137 can be used as tracers for quantitative assessment of different sediment redistribution processes. In landscapes of humid plains with agriculture-dominated land use the post-fallout redistribution of caesium-137 is primarily associated with fluvial activity of various scales in cascade systems starting from soil erosion on cultivated hillslopes through gully and small dry valley network into different order perennial streams and rivers. Our investigations in the so-called Plavsk hotspot (area of very high Chernobyl caesium-137 contamination within the Plava River basin, Tula Region, Central European Russia) has been continuing for more than 15 years by now, while the time passed since the Chernobyl disaster and associated radioactive fallout (1986) is almost 29 years. Detailed information on the fluvial sediment and associated caesium-137 redistribution has been obtained for case study sites of different size from individual cultivated slopes and small catchments of different size (2-180 km2) to the entire Plava River basin scale (1856 km2). It has been shown that most of the contaminated sediment over the time passed since the fallout has remained stored within the small dry valleys of the 1-4 Hortonian order and local reservoirs (>70%), while only about 5% reached the 5-6 order valleys (main tributaries of the Plava River) and storage of the Plava floodplain itself represents as low as 0.3% of the basin-scale total sediment production from eroded cultivated hillslopes. Nevertheless, it has been shown that contaminated sediment yield from the Plava River basin exerts significant influence on less polluted downstream-linked river system. Recent progress of the investigations involved sampling of 7 detailed depth

  9. Anthropogenic Impacts on the Sediment Flux in the Dry-hot Valleys of Southwest China-an Example of the Longchuan River

    Institute of Scientific and Technical Information of China (English)

    ZHOU Yue; LU Xixi; HUANG Ying; ZHU Yunmei

    2004-01-01

    The sediment flux data, measured from a dry-hot valley of the Longchuan River, a tributary of the lower Jinsha River, were analyzed with Mann-Kendall test, Seasonal Mann-Kendall test and Sen's test. In both the upper reaches (Xiaohekou) and the lower reaches (Xiaohuangguayuan), the sediment fluxes showed a significant increase from 1970 to 2001, despite the fact that the water discharge did not change significantly during the period and numerous reservoir constructions which contribute to the trap of sediment. This can be attributed to the intensification of human activities, especially the activities related to land surface disturbances such as deforestation and afforestation, expansion of agriculture land, and road constructions. This increase is more significant in the lower reaches of the river observed at the place of Xiaohuangguayuan due to the dry-hot climate. The profound increase in sediment flux has significant implications for effective management of the sedimentation problems of the on-going Three Gorges Reservoir.

  10. Hydrologic data for the San Juan and Animas River valleys in the Farmington, Aztec, Bloomfield, and Cedar Hill areas, San Juan County, New Mexico

    Science.gov (United States)

    McAda, D.P.; Shelton, S.G.

    1987-01-01

    In July 1985, the U.S. Geological Survey initiated a three-year study in San Juan County, New Mexico, to determine the concentrations of chemical constituents in the groundwater in the San Juan and Animas River valleys and to determine the direction and rate of groundwater flow and its relation to river stage. The study was conducted in cooperation with the San Juan County Commission and the New Mexico Oil Conservation Division. The data that was collected during the first 1-1/2 yr of the study is completed. The report includes well records for 51 wells and water levels from 23 wells, hydrographs from four observation wells and one river stage site, and available chemical analyses from 50 wells and 14 surface water sites. Water samples from six wells and one surface-water site were analyzed for purgeable organic chemicals; none were detected. (Lantz-PTT)

  11. Regression models of ecological streamflow characteristics in the Cumberland and Tennessee River Valleys

    Science.gov (United States)

    Knight, Rodney R.; Gain, W. Scott; Wolfe, William J.

    2011-01-01

    Predictive equations were developed using stepbackward regression for 19 ecologically relevant streamflow characteristics grouped in five major classes (magnitude, ratio, frequency, variability, and date) for use in the Tennessee and Cumberland River watersheds. Basin characteristics explain 50 percent or more of the variation for 10 of the 19 equations. Independent variables identified through stepbackward regression were statistically significant in 81 of 304 coefficients tested across 19 models (⬚ < 0.0001) and represent four major groups: climate, physical landscape features, regional indicators, and land use. The most influential variables for determining hydrologic response were in the land-use and climate groups: daily temperature range, percent agricultural land use, and monthly mean precipitation. These three variables were major explanatory factors in 17, 15, and 13 models, respectively. The equations and independent datasets were used to explore the broad relation between basin properties and streamflow and its implications for the study of ecological flow requirements. Key results include a high degree of hydrologic variability among least disturbed Blue Ridge streams, similar hydrologic behavior for watersheds with widely varying degrees of forest cover, and distinct hydrologic profiles for streams in different geographic regions.

  12. The biogeochemical behaviour of selenium in 2 lentic environments in the Elk River Valley, British Columbia

    Energy Technology Data Exchange (ETDEWEB)

    Martin, A.J.; Simpson, S. [Lorax Environmental Services Ltd., Vancouver, BC (Canada); Wallschlager, D.; London, J. [Trent Univ., Peterborough, ON (Canada); Wiramanaden, C.I.E.; Pickering, I.J. [Saskatchewan Univ., Regina, SK (Canada); Belzile, N.; Chen, Y.W. [Laurentian Univ., Sudbury, ON (Canada)

    2008-07-01

    An understanding of the mechanisms involved in selenium (Se) cycling within lentic environments is needed to accurately determine the long-term fate of Se and risks to biological receptors. This study investigated the biogeochemical behaviour of Se in Goddar Marsh (GM) and Fording River Oxbow (FRO). Se speciation in bottom water, pore water, and sediment components was examined. The study showed that elemental Se and organo-Se species in pore water are closely linked to redox-sensitive metabolite profiles. The pore water profiles showed that the sediments at both GM and FRO serve as diffusive sinks for Se through the in sit adsorption and precipitation of Se in suboxic horizons. Interfacial peaks in dissolved selenite and organo-Se indicated that the species are recycled back into the water column. Differences in redox conditions at the GM site made it more favourable for the recycling of reduced Se species. The shallower depths of the GM site supported greater fluxes of organo-Se to the water column. It was concluded that the conditions observed at the GM site are more favourable for Se accumulation in sediment-detrital food chains. 23 refs., 1 tab., 4 figs.

  13. The Ohio River Valley CO2 Storage Project AEP Mountaineer Plant, West Virginia Numerical Simulation and Risk Assessment Report

    Energy Technology Data Exchange (ETDEWEB)

    Neeraj Gupta

    2008-03-31

    A series of numerical simulations of carbon dioxide (CO{sub 2}) injection were conducted as part of a program to assess the potential for geologic sequestration in deep geologic reservoirs (the Rose Run and Copper Ridge formations), at the American Electric Power (AEP) Mountaineer Power Plant outside of New Haven, West Virginia. The simulations were executed using the H{sub 2}O-CO{sub 2}-NaCl operational mode of the Subsurface Transport Over Multiple Phases (STOMP) simulator (White and Oostrom, 2006). The objective of the Rose Run formation modeling was to predict CO{sub 2} injection rates using data from the core analysis conducted on the samples. A systematic screening procedure was applied to the Ohio River Valley CO{sub 2} storage site utilizing the Features, Elements, and Processes (FEP) database for geological storage of CO{sub 2} (Savage et al., 2004). The objective of the screening was to identify potential risk categories for the long-term geological storage of CO{sub 2} at the Mountaineer Power Plant in New Haven, West Virginia. Over 130 FEPs in seven main classes were assessed for the project based on site characterization information gathered in a geological background study, testing in a deep well drilled on the site, and general site conditions. In evaluating the database, it was apparent that many of the items were not applicable to the Mountaineer site based its geologic framework and environmental setting. Nine FEPs were identified for further consideration for the site. These FEPs generally fell into categories related to variations in subsurface geology, well completion materials, and the behavior of CO{sub 2} in the subsurface. Results from the screening were used to provide guidance on injection system design, developing a monitoring program, performing reservoir simulations, and other risk assessment efforts. Initial work indicates that the significant FEPs may be accounted for by focusing the storage program on these potential issues. The

  14. Development and Validation of National Cotton Cultivar Registration lndex Model in Yangtze River Valley

    Institute of Scientific and Technical Information of China (English)

    Naiyin XU; Jian Ll

    2014-01-01

    Based on the cotton variety high yielding potential, fiber quality traits, disease resistance, and early maturity characters, a cultivar registration index model was developed to simplify the tedious calculation process in national cotton registration procedure, and thus to enhance the practical application of cultivar regis-tration index in cotton breeding and cotton recommending. [Method] By means of correlation analysis, partial correlation analysis and path analysis methods, the cor-relation of cotton main properties and their effects on cultivar registration index were explored using the dataset of national cotton regional trials in Yangtze River Val ey during 1996-2013. The cultivar registration index model was constructed with step-wise regression statistical technique to ascertain the quantitative relationship of main characters with cultivar registration index, and the regional cotton trial dataset in 2013 was used to validate the model. [Result] Several characters with larger deter-minants to cultivar registration index were screened out, i.e. lint yield increase ratio, pro-frost yield ratio, verticil ium wilt index, fiber strength, fusarium wilt index and mi-cronaire value. The cultivar registration index model defined the functional relation-ship of cultivar registration index with the selected main characters, among which lint yield increase ratio, fiber strength and micronaire value contributed most to culti-var registration index. The model validation with regional cotton trials in 2013 indi-cated the root mean square error, RMSE was only 2.77, and the variation coeffi-cient was 6.77%, which confirmed the model prediction effect was quite perfect. [Conclusion] The developed cultivar registration index model was reliable enough to simulate the complicated scoring system in cultivar registration procedure, also sim-plified cotton registration process, and enhanced the practicability of the cultivar reg-istration index.

  15. [Eco-anatomical characteristics of Sophora davidii leaves along an elevation gradient in upper Minjiang River dry valley].

    Science.gov (United States)

    Li, Fanglan; Bao, Weikai; Liu, Junhua; Wu, Ning

    2006-01-01

    This paper studied the eco-anatomical characteristics of Sorphora davidii leaves at the elevations of 1,650, 1,750, 1,850 and 1,950 m in the upper reaches of Minjiang River dry valley. The indices investigated were leaf length (LL), leaf width (LW), LL/ LW, leaf area, leaf thickness, leaf epidermal thickness, leaf palisade mesophyll thickness (P), leaf spongy mesophyll thickness (S), P/S, leaf cutin membrane thickness, leaf stomatal density and area, leaf epidermis cell density and area, and leaf pubescence length and density. The results showed that the leaves of S. davidii were elliptic, with an area 0.144 approximately 0.208 cm2 and a thickness 171.58 approximately 195.83 microm. The mesophyll was significantly differentiated into palisade and spongy. The thickness of palisade mesophyll was 69.83 approximately 82.42 microm, that of spongy mesophyll was 62.00 approximately 80.67 microm, and P/S was 1.14 approximately 1.01. Upper epidermal thickness was 14.03 approximately 15.33 microm, while lower epidermal thickness was 13.88 approximately 16.17 microm. The stomatal density, stomatal area, epidermis cell density, epidermis cell area, pubescence length, and pubescence density were 13.71 approximately 15.02 mm(-2), 249.86 approximately 280.43 microm2, 160.54 approximately 178.43 mm(-2), 557.43 approximately 626.85 microm2, 186.51 approximately 260.99 microm, and 18.29 approximately 32.27 mm(-2), respectively. With increasing elevation, the leaf area, leaf thickness, palisade mesophyll thickness, spongy mesophyll thickness, stomatal area, epidermis cell area and pubescence density were increased, while cutin membrane thickness, epidermis cell density, pubescence length, and stomatal density were decreased. There was no significant difference in LL/LW, P/S, epidermal thickness and stomatal density along the elevation gradient.

  16. Interdecadal Connection Between Artic Temperature and Summer Precipitation Over the Yangtze River Valley in the CMIP5 Historical Simulations

    Energy Technology Data Exchange (ETDEWEB)

    Li, Yuefeng; Leung, Lai-Yung R.; Xiao, Ziniu; Wei, Min; Li, Qingquan

    2013-10-01

    This study assesses the ability of the Phase 5 Coupled Model Intercomparison Project (CMIP5) simulations in capturing the interdecadal precipitation enhancement over the Yangtze River valley (YRV) and investigates the contributions of Arctic warming to the interdecadal variability of the East Asian summer monsoon rainfall. Six CMIP5 historical simulations including models from Canada (CCCma), China (BCC), Germany (MPI-M), Japan (MRI), United Kingdom (MOHC), and United States (NCAR) are used. The NCEP/NCAR reanalysis and observed precipitation are also used for comparison. Among the six CMIP5 simulations, only CCCma can approximately simulate the enhancement of interdecadal summer precipitation over the YRV in 1990-2005 relative to 1960-1975, and the relationships between the summer precipitation with surface temperature (Ts), the 850hPa winds, and 500hPa height field (H500), and between Ts and H500 using regression, correlation, and SVD analyses. It is found that CCCma can reasonably simulate the interdecadal surface warming over the boreal mid-to high latitudes and the Arctic in winter, spring and summer. The summer Baikal blocking appears to be the bridge that links the winter and spring surface warming over the mid-to high latitude and Arctic with the enhancement of summer precipitation over the YRV. Models that missed some or all of these relationships found in CCCma and the reanalysis failed to simulate the interdecadal enhancement of precipitation over the YRV. This points to the importance of high latitude and Arctic processes on interdecadal variability of the East Asian summer monsoon and the challenge for global climate models to correctly simulate the linkages.

  17. Nitrogen Mineralization of Prunings of Six N2-Fixing Hedgerow Species in a Dry Valley of the Jinsha River

    Institute of Scientific and Technical Information of China (English)

    2002-01-01

    A litterbag experiment of 12 weeks was conducted to study nitrogen mineralization process of prunings of six nitrogen-fixing hedgerow species in a dry valley of the Jinsha River. Prunings were incorporated into soil or used as mulch. The results indicated that pruning N of the six hedgerow species was mineralized fast in the first week and then decreased slowly in the rest of the study period. When prunings were incorporated into soil, the amount of nitrogen mineralized by the end of the first week accounted for 69.9%, 58.2%, 54.5%,43.0%, 29.6% and 20.6% of the total N in prunings of Desmodium rensonii, Tephrosia candida, Leucaena leucocuphala, Albizia yunnanensis, Acacia dealbata, and Acacia mearnsii, respectively. When prunings of L. leucocephala were used as mulch materials, the amount of nitrogen mineralized in the first week was 16.2% less than that of prunings incorporated into soil. The mineralization pattern of pruning N could be simulated by an exponent model Nt% = N01% (1 - exp(-k1t))+ N02% (1 - exp(-k2t)) where Nt% is cumulative mineralized N in time t, N01% and N02 % are readily and less readily mineralizable N in prunings,respectively, and k1 and k2 are rate constants. A half-life period of pruning nitrogen mineralization could ~ be determined by this model. The nitrogen content in the pruning residues decreased quickly in the first week but fluctuated thereafter. The initial C/N ratio was negatively related to the mineralization rate of prunings.``

  18. Channel and landscape dynamics in the alluvial forest mosaic of the Carmanah River valley, British Columbia, Canada

    Science.gov (United States)

    Little, Patrick J.; Richardson, John S.; Alila, Younes

    2013-11-01

    The highly diverse shifting-mosaic of forest patches of an alluvial forest within the Carmanah River valley on the west coast of Vancouver Island, British Columbia was studied to examine the hydrogeomorphic disturbance regime that structures it. We used a landscape-scale analysis to quantify historical channel migrations and changes in the extent of specific forest types. This GIS-based analysis using a 70-year aerial photographic record was complemented by field-based research. Thirty-eight plots containing 4509 trees were sampled for forest structure, age, and elevation above the contemporary channel. These data, including a vegetation chronosequence spanning over 500 years, were used to examine channel and landscape dynamics. Our findings support a general conceptual model that describes cycles of patch development and destruction in unconfined alluvial forests of the Pacific Coastal Ecoregion. Over the past century, Carmanah River has eroded nearly 30% of the alluvial forest in this study area, and approximately 65% over the past 500 years. At least 80% of the 2007 channel was forested area within the past 70 years. Younger landforms were disturbed more frequently than mature forest patches, which suggest that as biogeomorphic succession progresses the likelihood of future disturbance decreases. Estimated half lives of landforms ranged from 24 years for pioneer bars to over 1500 years for old growth terraces. Years of regional high magnitude floods resulted in a net loss of floodplain forest area indicating that disturbance was climate driven in this pluvial watershed, whereby rain events result in flood disturbance that converted forests to channel. These events initiate a subsequent course of vegetation succession and geomorphic development, and often result in the deposition of large wood that modifies the channel environment and contributes to channel avulsion and further hydrogeomorphic disturbance. The composition of the landscape is a reflection of the

  19. Survey of Neolithic Sites in the Banghe River and Laohushan River Valleys in Aohan Banner, Inner Mongolia%内蒙古敖汉旗蚌河、老虎山河流域新石器时代遗址调查简报

    Institute of Scientific and Technical Information of China (English)

    中国社会科学院考古研究所内蒙古工作队; 内蒙古自治区敖汉旗博物馆

    2005-01-01

    In 2001, a full-coverage field survey was carried out to explore sites of the Xinglongwa, Zhaobaogou, Hongshan and Xiaoheyan cultures in the lower Banghe River and the upper Laohushan River valleys in Aohan Banner, Inner Mongolia. The aim of the project was, in the perspective of settlernent archaeology, to inquire into the development of social complexity in the two valleys. The data from the lower Banghe River valley show a sharp increase of settlements both in size and in number in the middle Hongshan period. Twenty-three Hongshan sites with a total area of 75.4 ha were found. Moreover, their variety in grade suggests considerable social complexity. In the upper Laohushan River valley, almost no residential sites were recorded except for seven sacrificial sites. This, following the discovery of the Niuheliang ritual complex, again demonstrates the existence of exclusive sacred places separated from everyday secular life.

  20. Evidence for biologic response to pedogenesis along the Merced River chronosequence, Central Valley, California

    Science.gov (United States)

    Reed, S. E.; Amundson, R.

    2010-12-01

    Long-term soil weathering results in accumulations of clay and reduced hydraulic conductivity. How biology responds to these changes in the physical environment and how the response, in turn, influences landscape development are crucial questions in the effort to elucidate the links between the biologic and physical earth surface domains. Mima mounds are small, circular half-domes of soil that are suspected of being formed by burrowing rodents, as an adaption to saturated soil conditions. In the swales between the mounds, ephemeral wetlands called vernal pools, support a suite of endemic and endangered plant and animal species. Mima mounds, then, may provide a useful model by which to examine the complex feedbacks between landscape and life. In this study, changes in mound characteristics and in biological activity (pocket gopher, Thomomys bottae) are investigated across the Merced River chronosequence, a series of alluvial terraces which have been shown to exhibit an increasing degree of soil and hardpan development with landform age. Mound morphology (size, slope, curvature, concentration, elongation, dispersion) and relation to environmental parameters were analyzed using airborne LIDAR (light detection and ranging) imagery of the mounds. The high-resolution (1m) LIDAR surveys (conducted in 2006 and 2010) cover 65km2 and comprise seven different-aged landforms, ranging from several hundred years to several million years. Minimal filtering was performed on the dataset given the absence of large vegetation or other obstructions. A 20x20m moving window filter was used to smooth out the low frequency signals and accentuate mounded features. To test how and whether the subterranean mammals modify their burrowing habits in response to soil age, biotic sediment transport was measured monthly on 0.01, 0.5, and 2 m.y.o. terraces using RFID (radio frequency identification) technology. Half-liter portions of soil containing five RFID tags were implanted in active gopher

  1. Unraveling the Quaternary river incision in the Moselle valley (Rhenish Massif, Germany): new insights from cosmogenic nuclide dating (10Be/26Al) of the Main Terrace complex

    Science.gov (United States)

    Rixhon, Gilles; Cordier, Stéphane; Harmand, Dominique; May, Simon Matthias; Kelterbaum, Daniel; Dunai, Tibor; Binnie, Steven; Brückner, Helmut

    2014-05-01

    Throughout the whole river network of the Rhenish Massif, the terrace complex of the so-called Main Terrace forms the morphological transition between a wide upper palaeovalley (plateau valley) and a deeply incised lower valley. The youngest level of this Main Terrace complex (YMT), directly located at the edge of the incised valley, represents a dominant geomorphic feature in the terrace flight; it is often used as a reference level to identify the start of the main middle Pleistocene incision episode (Demoulin & Hallot, 2009). The latter probably reflects the major tectonic pulse that affected the whole Massif and was related to an acceleration of the uplift rates (Demoulin & Hallot, 2009). The Main terraces are particularly well preserved in the lower Moselle valley and are characterized by a constant absolute elevation of their base along a 150 km-long reach. Despite that various hypotheses have been proposed to explain this horizontality (updoming, faulting...), all studies assumed an age of ca. 800 ka for the YMT, mainly based on the questionable extrapolation of palaeomagnetic data obtained in the Rhine valley. Therefore, a reliable chronological framework is still required to unravel the spatio-temporal characteristics of the Pleistocene evolution of the Moselle valley. In this study, we apply cosmogenic nuclide dating (10Be/26Al) to fluvial sediments pertaining to the Main Terrace complex or to the upper Middle Terraces. Several sites along the lower Moselle were sampled following two distinct sampling strategies: (i) depth profiles where the original terrace (palaeo-)surface is well preserved and did not experience much postdepositional burial (e.g., loess cover); and (ii) the isochron technique where the sediment thickness exceeds 3 m. Cosmogenic nuclide ages recently obtained for three rivers in the Meuse catchment in the western Rhenish Massif demonstrated that the Main Terraces were younger than expected and their abandonment was diachronic along the

  2. Survey of potential sharpshooter and spittlebug vectors of Xylella fastidiosa to grapevines at the São Francisco River Valley, Brazil

    Directory of Open Access Journals (Sweden)

    Rudiney Ringenberg

    2014-06-01

    Full Text Available Survey of potential sharpshooter and spittlebug vectors of Xylella fastidiosa to grapevines at the São Francisco River Valley, Brazil. Pierce's disease of grapevines, caused by Xylella fastidiosa, is a serious problem in some regions of North America, not yet reported in Brazil. In this study, a survey of potential sharpshooter (Hemiptera, Cicadellidae, Cicadellinae and spittlebug (Hemiptera, Cercopidae vectors of X. fastidiosa was conducted in vineyards at the São Francisco River Valley, a major grape growing region in Brazil. Four vineyards of Vitis vinifera L. were sampled fortnightly from June/2005 to June/2007, using yellow sticky cards, each placed at two different heights (45 cm aboveground and 45 cm above the crop canopy in 10 sampling localities. A total of 4,095 specimens of sharpshooters were collected, nearly all from 3 Proconiini species, Homalodisca spottii Takiya, Cavichioli & McKamey, 2006 (96.8% of the specimens, Tapajosa fulvopunctata (Signoret, 1854 (3.1%, and Tretogonia cribrata Melichar, 1926 (1 specimen. Hortensia similis (Walker, 1851 (2 specimens was the only Cicadellini species. Only 1 cercopid specimen, belonging to Aeneolamia colon (Germar, 1821, was trapped. Even though they are not considered potential Xylella vectors, 2 Gyponini leafhoppers were collected: Curtara samera DeLong & Freytag, 1972 (11 specimens and Curtara inflata DeLong & Freytag, 1976 (1 specimen. Homalodisca spottii was observed feeding and mating on green branches of grapevines, in addition to egg masses. Because of its prevalence on the crop canopy, occurrence throughout the year (with peaks from February to August, and ability to colonize grapevines, H. spottii could be an important vector if a X. fastidiosa strain pathogenic to grapevines becomes introduced at the São Francisco River Valley.

  3. Geologic and geophysical data for wells drilled at Raft River Valley, Cassia County, Idaho, in 1977-1978 and data for wells drilled previously

    Science.gov (United States)

    Nathenson, Manuel; Urban, Thomas C.; Covington, Harry R.

    2014-01-01

    In order to better define the size of the thermal anomaly in the Raft River Valley, Idaho, the U.S. Geological Survey drilled a series of intermediate-depth (nominal 500-ft depth) wells in 1977 and 1978.  This report presents geologic, geophysical, and temperature data for these drill holes, along with data for five wells drilled by the Idaho National Engineering Laboratory with U.S. Department of Energy Funding.  Data previously reported for other drill holes are also included in order to make them available as digital files.

  4. A Study on the Construction of Ecological Protective Screen System in the Arid Valley Area of the Upper Reaches of the Min River

    Institute of Scientific and Technical Information of China (English)

    Zhao Bin

    2015-01-01

    The Min River is a large tributary in the upper reaches of the Yangtze River. Its source is the south range of the Min Mountains in the area where Sichuan and Gansu share a bounda ̄ry. The area consists of five counties in the Aba Tibetan-Qiang Autonomous Prefecture, including Wenchuan, Lixian, Maoxian, Songpan, and He ̄ishui. The area covers 25,426 square kilometers. The area in the upper reaches of the Min River is an arid valley, and its ecological position is very important. This area is not only one that is home to world heritage and national scenic spots, but it is also a poor ethnic minority area with relatively backward economic conditions. Moreover,it is also an important ecological screen and water source for the Chengdu plain,as well as an important part of the ecological protective screen in the upper rea ̄ches of the Yangtze River. As a result of natural disasters,pressure on the carrying capacity of the population and the careless manner of economic development,the resources and environment in this area have been exploited irrationally. This has cre ̄ated a series of serious environmental problems,in ̄cluding environmental pollution, and depletion of resources,etc. Therefore, constructing an ecologi ̄cal protective screen in the upper reaches of the Min River becomes very important.

  5. Use of Remotely Piloted Aircraft System (RPAS) in the analysis of historical landslide occurred in 1885 in the Rječina River Valley, Croatia

    Science.gov (United States)

    Dugonjić Jovančević, Sanja; Peranić, Josip; Ružić, Igor; Arbanas, Željko; Kalajžić, Duje; Benac, Čedomir

    2016-04-01

    Numerous instability phenomena have been recorded in the Rječina River Valley, near the City of Rijeka, in the past 250 years. Large landslides triggered by rainfall and floods, were registered on both sides of the Valley. Landslide inventory in the Valley was established based on recorded historical events and LiDAR imagery. The Rječina River is a typical karstic river 18.7km long, originating from the Gorski Kotar Mountains. The central part of the Valley, belongs to the dominant morphostructural unit that strikes in the northwest-southeast direction along the Rječina River. Karstified limestone rock mass is visible on the top of the slopes, while the flysch rock mass is present on the lower slopes and at the bottom of the Valley. Different types of movements can be distinguished in the area, such as the sliding of slope deposits over the flysch bedrock, rockfalls from limestone cliffs, sliding of huge rocky blocks, and active landslide on the north-eastern slope. The paper presents investigation of the dormant landslide located on the south-western slope of the Valley, which was recorded in 1870 in numerous historical descriptions. Due to intense and long-term rainfall, the landslide was reactivated in 1885, destroying and damaging houses in the eastern part of the Grohovo Village. To predict possible reactivation of the dormant landslide on the south-western side of the Valley, 2D stability back analyses were performed on the basis of landslide features, in order to approximate the position of sliding surface and landslide dimensions. The landslide topography is very steep, and the slope is covered by unstable debris material, so therefore hard to perform any terrestrial geodetic survey. Consumer-grade DJI Phantom 2 Remotely Piloted Aircraft System (RPAS) was used to provide the data about the present slope topography. The landslide 3D point cloud was derived from approximately 200 photographs taken with RPAS, using structure-from-motion (SfM) photogrammetry

  6. Groundwater components in the alluvial aquifer of the alpine Rhone River valley, Bois de Finges area, Wallis Canton, Switzerland

    Science.gov (United States)

    Schürch, Marc; Vuataz, François-D.

    2000-09-01

    Source, type, and quantity of various components of groundwater, as well as their spatial and temporal variations were determined by different hydrochemical methods in the alluvial aquifer of the upper Rhone River valley, Bois de Finges, Wallis Canton, Switzerland. The methods used are hydrochemical modeling, stable-isotope analysis, and chemical analysis of surface water and groundwater. Sampling during high- and low-water periods determined the spatial distribution of the water chemistry, whereas monthly sampling over three years provided a basis for understanding seasonal variability. The physico-chemical parameters of the groundwater have spatial and seasonal variations. The groundwater chemical composition of the Rhone alluvial aquifer indicates a mixing of weakly mineralized Rhone River water and SO4-rich water entering from the south side of the valley. Temporal changes in groundwater chemistry and in groundwater levels reflect the seasonal variations of the different contributors to groundwater recharge. The Rhone River recharges the alluvial aquifer only during the summer high-water period. Résumé. Origine, type et quantité de nombreux composants d'eau de l'aquifère alluvial dans la vallée supérieure du Rhône, Bois de Finges, Valais, Suisse, ainsi que leurs variations spatiales et temporelles ont été déterminés par différentes méthodes hydrochimiques. Les méthodes utilisées sont la modélisation hydrochimique, les isotopes stables, ainsi que l'échantillonnage en période de hautes eaux et de basses eaux pour étudier la distribution spatiale de la composition chimique, alors qu'un échantillonnage mensuel pendant trois ans sert à comprendre les processus de la variabilité saisonnière. Les paramètres physico-chimiques des eaux souterraines montrent des variations spatiales et saisonnières. La composition chimique de l'aquifère alluvial du Rhône indique un mélange entre une eau peu minéralisée venant du Rhône et une eau sulfatée s

  7. A new model of river dynamics, hydroclimatic change and human settlement in the Nile Valley derived from meta-analysis of the Holocene fluvial archive

    Science.gov (United States)

    Macklin, Mark G.; Toonen, Willem H. J.; Woodward, Jamie C.; Williams, Martin A. J.; Flaux, Clément; Marriner, Nick; Nicoll, Kathleen; Verstraeten, Gert; Spencer, Neal; Welsby, Derek

    2015-12-01

    In the Nile catchment, a growing number of site- and reach-based studies employ radiocarbon and, more recently, OSL dating to reconstruct Holocene river histories, but there has been no attempt to critically evaluate and synthesise these data at the catchment scale. We present the first meta-analysis of published and publically available radiocarbon and OSL dated Holocene fluvial units in the Nile catchment, including the delta region, and relate this to changing climate and river dynamics. Dated fluvial units are separated both geographically (into the Nile Delta and White, Blue, and Desert Nile sub-regions) and into depositional environment (floodplain and palaeochannel fills). Cumulative probability density frequency (CPDF) plots of floodplain and palaeochannel units show a striking inverse relationship during the Holocene, reflecting abrupt (civilizations in the Nile Valley.

  8. Towards automating measurements and predictions of Escherichia coli concentrations in the Cuyahoga River, Cuyahoga Valley National Park, Ohio, 2012–14

    Science.gov (United States)

    Brady, Amie M G.; Meg B. Plona,

    2015-07-30

    Nowcasts are systems that can provide estimates of the current bacterial water-quality conditions based on predictive models using easily-measured, explanatory variables; nowcasts can provide the public with the information to make informed decisions on the risk associated with recreational activities in natural water bodies. Previous studies on the Cuyahoga River within Cuyahoga Valley National Park (CVNP) have found that predictive models can be used to provide accurate assessments of the recreational water quality. However, in order to run the previously developed nowcasts for CVNP, manual collection and processing of samples is required on a daily basis to acquire the required explanatory variable data (laboratory-measured turbidity). The U.S. Geological Survey and the National Park Service collaborated to develop a more automated approach to provide more timely results to park visitors regarding the recreational water quality of the river.

  9. Early performance of Pinus radiata provenances in the earthquake-ravaged dry river valley area of Sichuan, southwest China

    Institute of Scientific and Technical Information of China (English)

    Huiquan Bi; Rongwei Li; Zongxing Wu; Quan Huang; Qianli Liu; Yongli; Zhou Yun Li

    2013-01-01

    A provenance experiment involving five native provenances and an Australian landrace of Pinus radiata (D. Don) was established over three sites in the dry river valley area of Sichuan, southwest China in 2004 in order to select the most suitable provenance for environmental planting on the dry, steep and degraded slopes to reduce soil erosion. Although with much lower soil moisture supply and mean minimum temperatures in winter compared to P. radiata provenance trials estab-lished elsewhere in the world, these sites are within the working limits of the species defined by previous climate modelling and matching. Be-cause of the difficult site conditions and severe natural disturbances after the experiment was established, mortality was high across the three sites in comparison to provenance trials in other countries. The average mor-tality rate among the provenance by replicate planting units over the three sites varied from 16% to 76% four years after planting, and from 40%to 88%five years after planting . The repeated measurements of tree size over time were analysed using multilevel linear mixed models to derive growth curves for the mean, median, the 75th and the 90th percen-tiles of the size distribution of each provenance at each site. There were significant site effects on tree growth, but no significant interactions between site and provenance was detected. Among the six provenances, Cambria was the best performer in diameter, height and stem volume growth across all sites. The better than average and the best trees of this provenance, as represented by the 75th and 90th percentiles of the nomi-nal stem volume distribution, were significantly larger than the Austra-lian landrace, Año Nuevo, and the two island provenances, Guadalupe and Cedros. Monterey was overall the second best performer behind Cambria. The Australian landrace, Guadalupe and Año Nuevo had simi-lar performances in general. Cedros was significantly and consistently inferior to all other

  10. Precipitation and runoff simulations of select perennial and ephemeral watersheds in the middle Carson River basin, Eagle, Dayton, and Churchill Valleys, west-central Nevada

    Science.gov (United States)

    Jeton, Anne E.; Maurer, Douglas K.

    2011-01-01

    The effect that land use may have on streamflow in the Carson River, and ultimately its impact on downstream users can be evaluated by simulating precipitation-runoff processes and estimating groundwater inflow in the middle Carson River in west-central Nevada. To address these concerns, the U.S. Geological Survey, in cooperation with the Bureau of Reclamation, began a study in 2008 to evaluate groundwater flow in the Carson River basin extending from Eagle Valley to Churchill Valley, called the middle Carson River basin in this report. This report documents the development and calibration of 12 watershed models and presents model results and the estimated mean annual water budgets for the modeled watersheds. This part of the larger middle Carson River study will provide estimates of runoff tributary to the Carson River and the potential for groundwater inflow (defined here as that component of recharge derived from percolation of excess water from the soil zone to the groundwater reservoir). The model used for the study was the U.S. Geological Survey's Precipitation-Runoff Modeling System, a physically based, distributed-parameter model designed to simulate precipitation and snowmelt runoff as well as snowpack accumulation and snowmelt processes. Models were developed for 2 perennial watersheds in Eagle Valley having gaged daily mean runoff, Ash Canyon Creek and Clear Creek, and for 10 ephemeral watersheds in the Dayton Valley and Churchill Valley hydrologic areas. Model calibration was constrained by daily mean runoff for the 2 perennial watersheds and for the 10 ephemeral watersheds by limited indirect runoff estimates and by mean annual runoff estimates derived from empirical methods. The models were further constrained by limited climate data adjusted for altitude differences using annual precipitation volumes estimated in a previous study. The calibration periods were water years 1980-2007 for Ash Canyon Creek, and water years 1991-2007 for Clear Creek. To

  11. Land degradation trends in upper catchments and morphological developments of braided rivers in drylands: the case of a marginal graben of the Ethiopian Rift Valley

    Science.gov (United States)

    Demissie, Biadgilgn; Frankl, Amaury; Haile, Mitiku; Nyssen, Jan

    2014-05-01

    Braided rivers have received relatively little attention in research and development activities in drylands. However, they strongly impact agroecology and agricultural activities and thereby local livelihoods. The Raya Graben (3750 km² including the escarpment) is a marginal graben of the Ethiopian Rift Valley located in North Ethiopia. In order to study the dynamics of braided rivers and the relationship with biophysical controls, 20 representative catchments were selected, ranging between 15 and 311 km². First, the 2005 morphology (length, area) of the braided rivers was related to biophysical controls (vegetation cover, catchment area and slope gradient in the steep upper catchments and gradient in the graben bottom). Second, the changes in length of the braided rivers were related to vegetation cover changes in the upper catchments since 1972. Landsat imagery was used to calculate the Normalized Difference Vegetation Index (NDVI), and to map vegetation cover and the total length of the braided rivers. Spot CNES imagery available from Google Earth was used to identify the total area of the braided rivers in 2005. A linear regression analysis revealed that the length of braided rivers was positively related to the catchment area (R²=0.32, p<0.01), but insignificantly related to vegetation cover in the upper catchments. However, there is an indication that it is an important factor in the relationship calculated for 2005 (R²=0.2, p=0.064). Similarly, the area occupied by the braided rivers was related to NDVI (R²=0.24, p<0.05) and upper catchment area (R²=0.447, p<0.01). Slope gradient is not an important explanatory factor. This is related to the fact that slope gradients are steep (average of 38.1%) in all upper and gentle (average of 3.4%) in graben bottom catchments. The vegetation cover in the upper catchments shows a statistically insignificant increasing trend (R²=0.73, p=0.067) over the last 40 years, whereas length of rivers in the graben bottom

  12. Groundwater Quality, Age, and Probability of Contamination, Eagle River Watershed Valley-Fill Aquifer, North-Central Colorado, 2006-2007

    Science.gov (United States)

    Rupert, Michael G.; Plummer, L. Niel

    2009-01-01

    The Eagle River watershed is located near the destination resort town of Vail, Colorado. The area has a fastgrowing permanent population, and the resort industry is rapidly expanding. A large percentage of the land undergoing development to support that growth overlies the Eagle River watershed valley-fill aquifer (ERWVFA), which likely has a high predisposition to groundwater contamination. As development continues, local organizations need tools to evaluate potential land-development effects on ground- and surface-water resources so that informed land-use and water management decisions can be made. To help develop these tools, the U.S. Geological Survey (USGS), in cooperation with Eagle County, the Eagle River Water and Sanitation District, the Town of Eagle, the Town of Gypsum, and the Upper Eagle Regional Water Authority, conducted a study in 2006-2007 of the groundwater quality, age, and probability of contamination in the ERWVFA, north-central Colorado. Ground- and surface-water quality samples were analyzed for major ions, nutrients, stable isotopes of hydrogen and oxygen in water, tritium, dissolved gases, chlorofluorocarbons (CFCs), and volatile organic compounds (VOCs) determined with very low-level laboratory methods. The major-ion data indicate that groundwaters in the ERWVFA can be classified into two major groups: groundwater that was recharged by infiltration of surface water, and groundwater that had less immediate recharge from surface water and had elevated sulfate concentrations. Sulfate concentrations exceeded the USEPA National Secondary Drinking Water Regulations (250 milligrams per liter) in many wells near Eagle, Gypsum, and Dotsero. The predominant source of sulfate to groundwater in the Eagle River watershed is the Eagle Valley Evaporite, which is a gypsum deposit of Pennsylvanian age located predominantly in the western one-half of Eagle County.

  13. Management of invasive plant species in the valley of the River Ślepiotka in Katowice – the example of the REURIS project

    Directory of Open Access Journals (Sweden)

    Frelich Małgorzata

    2014-06-01

    Full Text Available In recent years, programmes aimed at improving environmental conditions in river valleys within urban spaces have been initiated in many of the European Community countries. An example is the project “Revitalization of Urban River Spaces – REURIS” which was implemented in 2009-2012. Its main aim was to revitalize a part of the valley of the River Ślepiotka in Katowice. One of the tasks of the project was a comprehensive treatment to combat invasive plant species occurring in this area, carried out by using a combination of chemical and mechanical methods. Chemical treatment involved the application of herbicide mixtures, and mechanical treatment included, among others, mowing and/or removal of the undesirable plants. The work focused primarily on reducing the spread of two species of the Impatiens genus: I. glandulifera and I. parviflora, and the species Padus serotina, Reynoutria japonica and Solidago canadensis. Currently, the maintenance works on this section of the river are performed by the Urban Greenery Department in Katowice, which continues the elimination of invasive plants, according to the objectives of the REURIS program. In 2012 the Department of Botany and Nature Protection at the Faculty of Biology and Environmental Protection started to monitor the implementation and the effects of the implemented actions for elimination and participated in the action of removal of selected invasive plant species: Impatiens parviflora and Reynoutria japonica within specific areas. These actions led to a reduction in the area occupied by invasive plants and a weakening of their growth rate and ability to reproduce.

  14. Spatial relations between floodplain environments and land use - land cover of a large lowland tropical river valley: Pánuco basin, México.

    Science.gov (United States)

    Hudson, Paul F; Colditz, René R; Aguilar-Robledo, Miguel

    2006-09-01

    Large lowland river valleys include a variety of floodplain environments that represent opportunities and constraints for human activities. This study integrates extensive field observations and geomorphic data with analysis of satellite remote sensing data to examine spatial relations between land use/land cover (LULC) and floodplain environments in the lower Pánuco basin of eastern Mexico. The floodplain of the lower Pánuco basin was delineated by combining a digital elevation model with a satellite image of a large flood event. The LULC was classified by combining a hybrid classification strategy with image stratification, applied to 15-m-resolution ASTER data. A geomorphic classification of floodplain environments was performed using a dry-stage image (ASTER data) and a 1993 Landsat image acquired during a large flood event. Accuracy assessment was based on aerial photographs (1:38,000), global positioning satellite ground-truthing, and a Landsat 7ETM(+) image from 2000, which resulted in an overall accuracy of 82.9% and a KHAT of 79.8% for the LULC classification. The geomorphic classification yielded 83.5% overall accuracy, whereas the KHAT was 81.5%. LULC analysis was performed for the entire floodplain and individually within four valley segments. The analysis indicates that the study area is primarily utilized for grazing and farming. Agriculture is primarily associated with coarse-grained (sandy/silty) natural levee and point bar units close to the river channel, whereas cattle grazing occurs in distal and lower-lying reaches dominated by cohesive fine-grained (clayey) deposits, such as backswamps. In the Pánuco valley, wetlands and lakes occur within backswamp environments, whereas in the Moctezuma segments, wetlands and lakes are associated with relict channels. This study reveals considerable variation in LULC related to spatial differences in floodplain environments and illustrates the importance of considering older anthropogenic influences on the

  15. Meridional seesaw-like distribution of the Meiyu rainfall over the Changjiang-Huaihe River Valley and characteristics in the anomalous climate years

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    Although Meiyu rainfall has its in-phase spatial variability over the Changjiang-Huaihe River Valley (CHRV) in most years, it is distributed in some years like a seesaw to the north and south of the Changjiang River, when the precipitation tends to be nearly normal throughout the valley, which would inevitably increase difficulties of making short-term prediction of the rainfall. For this reason, EOF analysis is made on 15 related stations' precipitation from June to July during 1951─2004, revealing that the EOF2 mode shows largely a north-south seesaw-like pattern, and thereby classifying Meiyu patterns into two types: "northern drought and southern flood (NDSF)" and "northern flood and southern drought (NFSD)". Afterwards, the authors investigated ocean-atmospheric characteristics when these two anomalous types occurred using the NCEP reanalysis (version 1) and the extended reconstructed SSTs (version 2). The results show that in the NDSF years, the low-level frontal area and moisture convergence center lie more southward, accompanied by weaker subtropical summer monsoon over East Asia, with the western Pacific subtropical high and 200 hPa South Asia High being more southward. Both the Northern and Southern Hemisphere Annular Modes are stronger than normal in preceding February; SST is higher off China during boreal winter and spring and the opposite happens in the NFSD years. Also, this seesaw-form Meiyu rainfall distribution might be affected to some degree by the previous ENSO event.

  16. Levels of Organisation in agent-based modelling for renewable resources management. Agricultural water management collective rules enforcement in the French Drome River Valley Case Study

    International Nuclear Information System (INIS)

    Levels of Organisation in agent-based modelling for renewable resources management. Agricultural water management collective rules enforcement in the French Dr me River Valley Case Study. In the context of Agent-Based Modelling for participative renewable resources management, this thesis is concerned with representing multiple tangled levels of organisation of a system. The Agent-Group-Role (AGR) formalism is borrowed from computer science research. It has been conceptually specified to handle levels of organisation, and behaviours within levels of organisation. A design methodology dedicated to AGR modelling has been developed, together with an implementation of the formalism over a multi-agent platform. AGR models of agricultural water management in the French Dr me River Valley have been built and tested. This experiment demonstrates the AGR formalism ability to (1) clarify usually implicit hypothesis on action modes, scales or viewpoints (2) facilitate the definition of scenarios with various collective rules, and various rules in enforcement behaviours (3) generate bricks for generic irrigated catchment models. (author)

  17. Impacts of the Thermal Effects of Sub-grid Orography on the Heavy Rainfall Events Along the Yangtze River Valley in 1991

    Institute of Scientific and Technical Information of China (English)

    FENG Lei; ZHANG Yaocun

    2007-01-01

    A P - σ regional climate model using a parameterization scheme to account for the thermal effects of the sub-grid scale orography was used to simulate the three heavy rainfall events that occurred within the Yangtze River Valley during the mei-yu period of 1991. The simulation results showed that by considering the sub-grid scale topography scheme, one can significantly improve the performance of the model for simulating the rainfall distribution and intensity during these three heavy rainfall events, most especially the second and third. It was also discovered that the rainfall was mainly due to convective precipitation. The comparison between experiments, either with and without the sub-grid scale topography scheme, showed that the model using the scheme reproduced the convergence intensity and distribution at the 850 hPa level and the ascending motion and moisture convergence center located at 500 hPa over the Yangtze River valley.However, some deviations still exist in the simulation of the atmospheric moisture content, the convergence distribution and the moisture transportation route, which mainly result in lower simulated precipitation levels. Further analysis of the simulation results demonstrated that the sub-grid topography scheme modified the distribution of the surface energy budget components, especially at the south and southwest edges of the Tibetan Plateau, leading to the development and eastward propagation of the negative geopotential height difference and positive temperature-lapse rate difference at 700 hPa, which possibly led to an improved precipitation simulation over eastern China.

  18. Questa Baseline and Pre-Mining Ground-Water-Quality Investigation 22 - Ground-Water Budget for the Straight Creek Drainage Basin, Red River Valley, New Mexico

    Science.gov (United States)

    McAda, Douglas P.; Naus, Cheryl A.

    2008-01-01

    In April 2001, the U.S. Geological Survey (USGS) and the New Mexico Environment Department (NMED) began a cooperative study to infer the pre-mining ground-water chemistry at the Molycorp molybdenum mine site in the Red River Valley. The Molycorp mine has been in operation since the 1920s. Because ground-water conditions prior to mining are not available, sites analogous to the pre-mining conditions at the mine site must be studied to infer those pre-mining conditions. The Straight Creek drainage basin (watershed) was selected as the primary analog site for this study because of its similar terrain and geology to the mine site, accessibility, potential for well construction, and minimal anthropogenic activity. The purpose of this report is to present results of a water-budget analysis of the debris-flow aquifer in the Straight Creek watershed. The water budget is based on mean annual conditions and is assumed to be steady state. For this study, the Straight Creek watershed was divided into sub-watersheds on the basis of locations of seismic lines, which were used to calculate cross-section area through the Straight Creek debris-flow deposits and underlying fractured and weathered bedrock (regolith). Water-budget components were calculated for areas upstream from and between the seismic lines. Components of the water budget were precipitation, evapotranspiration, surface-water flow, and ground-water flow under a steady-state mean annual condition. Watershed yield, defined as precipitation minus evapotranspiration, was separated into surface-water flow, ground-water flow through the debris-flow deposits and regolith, and ground-water flow through fractured bedrock. The approach to this calculation was to use Darcy?s Law to calculate the flow through the cross-section area of the saturated debris-flow deposits and underlying regolith as defined by the interpreted seismic data. The amount of watershed yield unaccounted for through this section then was attributed to

  19. Growth and production of Donax striatus (Bivalvia: Donacidae) from Las Balsas beach, Gibara, Cuba.

    Science.gov (United States)

    Ocaña, Frank A

    2015-09-01

    Clams of the genus Donax are worldwide the dominating group of the invertebrate community on sandy beaches. They are primary consumers that provide a significant abundance and biomass to the ecosystem. In the Caribbean, Donax striatus has an important role for nature and human, nonetheless studies on the population dynamics of this beach clam are scarce and no information exists on secondary production of this species. Growth parameters and secondary production of D. striatus were estimated from February 2008 to November 2009 at Las Balsas beach, Northeastern Cuba, in order to provide basic information for management purposes. In each month 45 samples were taken by means of a PVC corer of 0.025 m2 area and sieved with a 1 mm mesh. Animals were measured and weighted with and without shell. A total of 5 471 specimens were collected during the sampling period. Shell length ranged from 2.7-33.3 mm. Growth parameters estimated from length frequency data were L∞ = 36.1 mm, K= 0.8/yr and t0= 0.2/yr. The growth performance resulted in values of Φ'= 3.02. Life span was 2.4 yrs and mortality rate was 3.07 /yr. In 2008, mean abundance of D. striatus ranged between 17.1 - 770.7 ind./m2. In 2009 the lowest mean abundance was 34.4 and the highest was 892.5 ind./m2. During 2009 biomass and production was more than twice higher in comparison with 2008. Individual production showed highest values in the 24 mm shell size (3.74 g/m2.yr) and 25 mm (0.71 g/m2.yr), considering mass with shell and without shell, respectively. During 2009 abundance of individuals with 15 mm shell length or more increased resulting in higher biomass and production, compared to 2008. Using the conversion factor of wet mass to ash free dry mass (AFDM), annual production ranged between 2.87-6.11 g AFDM/m2.yr, resulting in a turnover rate (P/B) between 5.11 and 3.47 in 2008 and 2009, respectively. The rapid growth and high turnover rate of D. striatus suggest a rapid recovery of the population. These

  20. Growth and production of Donax striatus (Bivalvia: Donacidae) from Las Balsas beach, Gibara, Cuba.

    Science.gov (United States)

    Ocaña, Frank A

    2015-09-01

    Clams of the genus Donax are worldwide the dominating group of the invertebrate community on sandy beaches. They are primary consumers that provide a significant abundance and biomass to the ecosystem. In the Caribbean, Donax striatus has an important role for nature and human, nonetheless studies on the population dynamics of this beach clam are scarce and no information exists on secondary production of this species. Growth parameters and secondary production of D. striatus were estimated from February 2008 to November 2009 at Las Balsas beach, Northeastern Cuba, in order to provide basic information for management purposes. In each month 45 samples were taken by means of a PVC corer of 0.025 m2 area and sieved with a 1 mm mesh. Animals were measured and weighted with and without shell. A total of 5 471 specimens were collected during the sampling period. Shell length ranged from 2.7-33.3 mm. Growth parameters estimated from length frequency data were L∞ = 36.1 mm, K= 0.8/yr and t0= 0.2/yr. The growth performance resulted in values of Φ'= 3.02. Life span was 2.4 yrs and mortality rate was 3.07 /yr. In 2008, mean abundance of D. striatus ranged between 17.1 - 770.7 ind./m2. In 2009 the lowest mean abundance was 34.4 and the highest was 892.5 ind./m2. During 2009 biomass and production was more than twice higher in comparison with 2008. Individual production showed highest values in the 24 mm shell size (3.74 g/m2.yr) and 25 mm (0.71 g/m2.yr), considering mass with shell and without shell, respectively. During 2009 abundance of individuals with 15 mm shell length or more increased resulting in higher biomass and production, compared to 2008. Using the conversion factor of wet mass to ash free dry mass (AFDM), annual production ranged between 2.87-6.11 g AFDM/m2.yr, resulting in a turnover rate (P/B) between 5.11 and 3.47 in 2008 and 2009, respectively. The rapid growth and high turnover rate of D. striatus suggest a rapid recovery of the population. These

  1. Geologic investigation of the Virgin River Valley salt deposits, Clark County, southeastern Nevada, to investigate their suitability for possible storage of radioactive waste material as of September 1977

    International Nuclear Information System (INIS)

    The results from a geologic investigation of the Virgin River Valley salt deposits, Clark County, southeastern Nevada, to examine their suitability for further study and consideration in connection with the possible storage of radioactive waste material are given. The results indicate that (1) approximately one-half of the salt body underlies the Overton Arm of Lake Mead and that the dry land portion of the salt body that has a thickness of 1,000 feet or more covers an area of about four and one-half square miles; (2) current tectonic activity in the area of the salt deposits is believed to be confined to seismic events associated with crustal adjustments following the filling of Lake Mead; (3) detailed information on the hydrology of the salt deposit area is not available at present but it is reported that a groundwater study by the U.S. Geological Survey is now in progress; (4) there is no evidence of exploitable minerals in the salt deposit area other than evaporites such as salt, gypsum, and possibly sand and gravel; (5) the salt deposit area is located inside the Lake Mead Recreation Area, outlined on the accompanying Location Plat, and several Federal, State, and Local agencies share regulatory responsibilities for the activities in the area; (6) other salt deposit areas of Arizona and Nevada, such as the Detrital Valley, Red Lake Dome, Luke Dome, and Mormon Mesa area, and several playa lake areas of central Nevada may merit further study; and (7) additional information, as outlined, is needed to more thoroughly evaluate the salt deposits of the Virgin River Valley and other areas referred to above

  2. Critical controlling of PRED system of oasis ecology in the arid region of central Asia: a case study of Keriya River Valley oases, Xinjiang

    Science.gov (United States)

    Chen, Rui; Liu, Jiaqi; Niu, Wenyuan; Deng, Xiangzheng; Mu, Guijin; Wagner, Mayke; Geldmacher, Karl

    2003-07-01

    Oases is a special ecosystem formed in arid climate and hungriness environment, in which resident, water and soil are the principal factor and exchanges of materials, energy and information are the main functional characteristics. The oases regions in central Asia are not only the basilic cradle of civilization of human beings, but also the important strategic places in world growing awareness of the potential benefits. We choose Keriya River Basin oases in south of Xinjiang as a case to study critical controlling of Oases Evolution, Based on the theories and methods used for environmental geology, physical geography, land resource research, and oases ecology. This study try to indicate the essential factors driving the oases ecosystem and the interactional dynamic mechanism in different scales and levels, confirm the optimal equilibrium aggregate of harmonious development between Population, Resources, Environment and Development, and establish the critical controlling pattern of sustainable development. We advance the indicator system to research the evolution of the PRED System of oases in Keriya River valley oases, in basis of the information derived from the field investigation and local materials. According to inquisitional result based on technical support of Geographic Information System (GIS) and Remote Sense (RS), the comparisons and analyses are carried out in land use at the upper reaches, vegetation change in the middle reaches, and desertification at the lower reaches, which narrates the regulations of Keriya River Valley oases land cover dynamic change. The main land cover types represent distinct characteristics of the local place. On the basis of field survey and statistical data, we use ARCINFO software to preprocess these data and the 2 TM satellite images. Through analyzing these images resulting from post-classification compare, we sums up the concrete quantificational dynamic distributed data of 13 land types covering a span of 15 years and

  3. Analysis of frequency and duration of the functional periods on the basis of long-term variability of limnetic processes within the Bug River valley

    Science.gov (United States)

    Dawidek, J.; Ferencz, B.

    2014-12-01

    Floodplain lakes (FPLs) constitute a very important element of river valleys, both in terms of ecology and hydrology. Dynamic physicochemical, morphometric and biological changes of lake waters are determined by the variability of the functional periods of lakes: limnophases, potamophases and inundations. This paper presents factors that shape long-term dynamics of the frequencies and durations of potamophases and limnophases in 20 selected FPLs. The study area included the left fraction of the Bug River valley located at the European Union's eastern border stretched along countries like Poland, Ukraine, and Belarus. The analysis covered the water years 1952 to 2013. Assigning the value of Limnological Effective Rise (LER) was essential for determining the functional periods for each of the study lakes. The dynamics of the phenomenon was analysed using volatility indicators, while factors determining functional periods were distinguished using Principal Component Analysis (PCA). Results showed that short (0-8 days) and medium-length limnophases were observed most frequently during the study period. In the case of potamophases they most often lasted from 8 to 30 days, continuously. Double-mass curves showed four periods of increasing significance of one of the functional phases: 1952-1962 (limnophases), 1963-1982 (potamophases), 1983-1997 (limnophases) and 1998-2013 (potamophases). A variability that was observed in each floodplain lake under study resulted from two main factors: water input and lake basin morphometry. The major role in FPLs' input was played by potamic supply (inflow of water from the parent river), which was a derivative of Bug River water stages and discharge. Atmospheric precipitation played a smaller role. However, the role of local precipitation was marginal in relation to precipitation in the upper part of the Bug River catchment. Spatial variability of the frequencies and durations of potamophases and limnophases was also associated with the

  4. Local Farmers' Perceptions of Climate Change and Local Adaptive Strategies: A Case Study from the Middle Yarlung Zangbo River Valley, Tibet, China

    Science.gov (United States)

    Li, Chunyan; Tang, Ya; Luo, Han; Di, Baofeng; Zhang, Liyun

    2013-10-01

    Climate change affects the productivity of agricultural ecosystems. Farmers cope with climate change based on their perceptions of changing climate patterns. Using a case study from the Middle Yarlung Zangbo River Valley, we present a new research framework that uses questionnaire and interview methods to compare local farmers' perceptions of climate change with the adaptive farming strategies they adopt. Most farmers in the valley believed that temperatures had increased in the last 30 years but did not note any changes in precipitation. Most farmers also reported sowing and harvesting hulless barley 10-15 days earlier than they were 20 years ago. In addition, farmers observed that plants were flowering and river ice was melting earlier in the season, but they did not perceive changes in plant germination, herbaceous vegetation growth, or other spring seasonal events. Most farmers noticed an extended fall season signified by delays in the freezing of rivers and an extended growing season for grassland vegetation. The study results showed that agricultural practices in the study area are still traditional; that is, local farmers' perceptions of climate change and their strategies to mitigate its impacts were based on indigenous knowledge and their own experiences. Adaptive strategies included adjusting planting and harvesting dates, changing crop species, and improving irrigation infrastructure. However, the farmers' decisions could not be fully attributed to their concerns about climate change. Local farming systems exhibit high adaptability to climate variability. Additionally, off-farm income has reduced the dependence of the farmers on agriculture, and an agricultural subsidy from the Chinese Central Government has mitigated the farmers' vulnerability. Nevertheless, it remains necessary for local farmers to build a system of adaptive climate change strategies that combines traditional experience and indigenous knowledge with scientific research and government

  5. Application of LANDSAT Data for Field-Scale Comparisons and Basin-Scale Estimates of Evapotranspiration in the Wood River Valley, Upper Klamath Basin, Oregon.

    Science.gov (United States)

    Peterson, S. T.; Cuenca, R. H.

    2006-12-01

    30 meter resolution LANDSAT data were used to evaluate the effects of irrigation management decisions in the Wood River Valley, Upper Klamath Basin, Oregon. The Klamath Basin is well known as an over-allocated system that strains to provide adequate water for agriculture, recreational, and wildlife needs. In an effort to provide increased stream flows after the water shutoff to irrigators in 2001 and disastrous fish kills in 2002, a program was established with cooperative ranchers to withhold irrigation from their cattle pastures in the Wood River Valley, just above Upper Klamath Lake. From 2003 to 2006, ground-based measurements over one irrigated and one unirrigated pasture site were used to monitor the difference in evapotranspiration using the Bowen ratio energy balance method. These data sets represent point measurements of the response to irrigation, but do not allow for the spatial integration of effects of irrigated versus unirrigated lands. The SEBAL and later METRIC algorithms were developed to evaluate evapotranspiration on a field- or basin-wide scale using LANDSAT data. Four LANDSAT scenes of the Wood River basin during the 2004 growing season were evaluated using re-derived and updated METRIC algorithms. The Bowen ratio station micrometeorological data were utilized in the METRIC algorithms. Comparisons of METRIC algorithm output with ground-based data for all components of the energy balance, including net radiation, soil heat flux, sensible heat flux and evapotranspiration, were made for the four scenes. The excellent net radiation estimates, along with less accurate estimates of the other components, is demonstrated. The ability to integrate the effects of withholding irrigation on evapotranspiration and the water balance on irrigated and unirrigated lands within the basin is demonstrated. The results exhibit application of the METRIC algorithms to partition water balance components at the watershed scale.

  6. Heavy metals in surface soils of the Warta river valley in an urban area; Schwermetalle in Oberboeden des Warthetals unter staedtischem Einfluss

    Energy Technology Data Exchange (ETDEWEB)

    Lewandowski, P.; Ilnicki, P. [Akademia Rolnicza, Katedra Ochrony i Ksztaltowania Srodowiska, Poznan (Poland); Burghardt, W. [Essen Univ. (Gesamthochschule) (Germany). Inst. fuer Oekologie

    1998-12-31

    In the urban area of the city of Poznan the contamination with heavy metals was investigated. From the top soil layers of five cross-sections of the valley of the Warta river 87 samples were collected. Beside common soil characteristics the contents of arsenic, barium, cadmium, chromium, copper, iron, lead, manganese, phosphorus and zinc were analyzed. Predominantly the level of contamination with heavy metals is low in the valley soils. A higher level was found in the area of the old city centre. Especially the contents of lead, copper and zinc were raised. Downstream of the sewage plant discharge into the river Warta increased contents of lead and cadmium were found. The distribution of heavy metals in the river Warta sediments indicates that the reason of the local increase of heavy metal contents is the sewage water discharge. Correlations between the content of different heavy metals and other soil properties (pH, clay and P-content, C/N-ratio) were calculated. (orig.) [Deutsch] Im staedtischen Bereich der Stadt Poznan wurde die Schwermetallkontamination der Boeden im Tal der Warthe untersucht. Aus fuenf Talquerschnitten wurden 87 Proben der obersten Bodenschichten entnommen. Neben allgemeinen Bodenkennwerten wurde Gehalte an Arsen, Barium, Blei, Cadmium, Chrom, Eisen, Kupfer, Mangan, Phosphat und Zink bestimmt. Die Talboeden weisen keine hohen Gehalte an Schwermetallen auf. Nur unterhalb von Abwassereinleitungen befinden sich erhoehte Gehalte an Blei und Cadmium. Eine starke Bodenkontamination wurde im Bereich der Altstadt gemessen. Dort wurden die hoechsten Gehalte an Blei, Kupfer und Zink gefunden. Die Verteilung von Schwermetallen in Flusssedimenten weist darauf hin, dass als Ursache das Einbringen von Abwaessern angesehen werden muss. Korrelationen zwischen den Elementgehalten und weiterer Bodenkennwerten (pH, Ton- und P-Gehalt, C/N-Verhaeltnis) werden vorgestellt. (orig.)

  7. Ground-Water Quality Data in the Santa Clara River Valley Study Unit, 2007: Results from the California GAMA Program

    Science.gov (United States)

    Montrella, Joseph; Belitz, Kenneth

    2009-01-01

    Ground-water quality in the approximately 460-square-mile Santa Clara River Valley study unit (SCRV) was investigated from April to June 2007 as part of the statewide Priority Basin project of the Ground-Water Ambient Monitoring and Assessment (GAMA) Program. The GAMA Priority Basin project was developed in response to the Groundwater Quality Monitoring Act of 2001 and is being conducted by the U.S. Geological Survey (USGS) in cooperation with the California State Water Resources Control Board (SWRCB). The study was designed to provide a spatially unbiased assessment of the quality of raw ground water used for public water supplies within SCRV, and to facilitate a statistically consistent basis for comparing water quality throughout California. Fifty-seven ground-water samples were collected from 53 wells in Ventura and Los Angeles Counties. Forty-two wells were selected using a randomized grid-based method to provide statistical representation of the study area (grid wells). Eleven wells (understanding wells) were selected to further evaluate water chemistry in particular parts of the study area, and four depth-dependent ground-water samples were collected from one of the eleven understanding wells to help understand the relation between water chemistry and depth. The ground-water samples were analyzed for a large number of synthetic organic constituents (volatile organic compounds [VOC], pesticides and pesticide degradates, potential wastewater-indicator compounds, and pharmaceutical compounds), a constituent of special interest (perchlorate), naturally occurring inorganic constituents (nutrients, major and minor ions, and trace elements), radioactive constituents, and microbial constituents. Naturally occurring isotopes (tritium, carbon-13, carbon-14 [abundance], stable isotopes of hydrogen and oxygen in water, stable isotopes of nitrogen and oxygen in nitrate, chlorine-37, and bromine-81), and dissolved noble gases also were measured to help identify the source

  8. Comparison of land-atmosphere interaction at different surface types in the mid- to lower Yangzi River Valley

    Science.gov (United States)

    Guo, Weidong; Wang, Xueqian; Sun, Jianning; Ding, Aijun; Zou, Jun

    2016-04-01

    The mid- to lower Yangzi River Valley is located within the typical monsoon zone. Rapid urbanization, industrialization, and development of agriculture have led to fast and complicated land use and land cover changes in this region. To investigate land-atmosphere interaction in this region where human activities and monsoon climate are highly interactive with each other, micro-meteorological elements over four different surface types, i.e. urban surface represented by the observational site at Communist Party School in Nanjing (hereafter DX), suburban surface represented by the ground site at Xianling (XL), and grassland and farmland represented by field sites at Lishui County (LS-grass and LS-crop), are analyzed and their differences are revealed. Impacts of different surface parameters applied for different surface types on the radiation budget and surface-atmosphere heat, water, and mass exchanges are investigated. Results indicate that (1) the largest differences in daily average surface air temperature (Ta), surface skin temperature (Ts), and relative humidity (RH) , which are found during the dry periods between DX and LS-crop, can be up to 3.21°C, 7.26°C, and 22.79% respectively. During the growing season, the diurnal ranges of the above three elements are the smallest at DX and the largest at LS-grass, XL and LS-crop; (2) differences in radiative fluxes are mainly reflected in upward shortwave radiation (USR) that is related to surface albedo and upward longwave radiation (ULR) that is related to Ts. USR is the smallest and ULR is the largest at DX. During the growing season, the average difference in ULR between the DX site and other sites with vegetation cover can be up to 20Wm-2. The USR variability is the largest at LS-crop, while the diurnal variation of ULR is the same as that of Ts at all the four sites; (3) the differences in daily average sensible heat (H) and latent heat (LE) between DX and LS-crop are larger than 45 and 95Wm-2, respectively

  9. COHORT OF WOMEN LIVING IN OR NEAR A HIGHLY INDUSTRIALIZED AREA OF KANAWHA RIVER VALLEY IN WEST VIRGINIA: ENDOMETRIOSIS AND BLOOD LEVELS OF DIOXIN AND DIOXIN-LIKE CHEMICALS

    Science.gov (United States)

    Introduction Historical releases of dioxin and dioxin-like chemicals with subsequent impacts to environmental media in the Kanawha River Valley (KRV) of West Virginia have been well documented.' The bulk of dioxin found in this area appears to be derived from the production of 2,...

  10. ENDOMETRIOSIS IN A COHORT OF WOMEN LIVING IN THE KANAWHA RIVER VALLEY IN WEST VIRGINIA: BLOOD LEVELS OF NON-DIOXIN-LIKE PCBs AND RELATIONSHIP WITH BMI AND AGE

    Science.gov (United States)

    Industrial activities, specifically from petroleum and chemical manufacturing facilities, in the Kanawha River Valley (KRV) of West Virginia have resulted in releases of dioxin and dioxin-like chemicals (DLCs). I Most of the dioxin found in this region has resulted from the produ...

  11. Time of travel, water quality, and bed-material quality in the Cuyahoga River within the Cuyahoga Valley National Recreation area, Ohio

    Science.gov (United States)

    Childress, C.J.

    1985-01-01

    Three studies were conducted in the Cuyahoga Valley National Recreation by the U. S. Geological Survey to (1) establish the relationship between time of travel and discharge through the park reach of the Cuyahoga River, (2) characterize water quality of the Cuyahoga River within the park over a 24-hour period, and (3) determine general areas where the streambed might be contaminated by trace metals. Time of Travel between Botzum and Independence is described by the equation T = 46.9-0.038Q, where T = time, in hours, and Q = discharge at Independence, in cubic feet per second. On the main stem of the Cuyahoga River, dissolved-oxygen saturation was highest and ultimate carbonaceous biochemical oxygen demand was lowest on the upstream and downstream ends of the reach. Dissolved-oxygen saturation was more than 80 percent in all the tributaries except Furnace Run, Brandywine Creek, and Langes Run. The number of fecal coliform counts per 100 milliliters of sample was high throughout the study area and ranged from 38 to 1,200,000. Concentrations of all metals and non-metals investigated by means of analysis of bed material were not anomalously high. (USGS)

  12. Predictive simulation of alternatives for managing the water resources of North Fork Solomon River Valley between Kirwin Dam and Waconda Lake, north-central Kansas

    Science.gov (United States)

    Burnett, R.D.

    1984-01-01

    Since 1974 water levels in the alluvial aquifer of the North Fork Solomon River Valley in north-central Kansas have decreased due to increases in ground-water pumpage, decreases in availability of surface water for irrigation, and below-average precipitation. A finite-element model was developed in cooperation with the U.S. Bureau of Reclamation to simulate changing conditions between 1970-79. Model results indicate that annual recharge to the aquifer due to precipitation, applcation of water for irrigation, and canal leakage averaged about 22,825 acre-feet and that annual ground-wate discharge to the river averaged about 16,590 acre-feet. Predictive simulations for 1980-2000 were made using management alternatives that involved clay-lining of irrigation ditches, reduction of surface-water availability with and without an increase in ground-water pumping, and continuation of 1979 pumping conditions. The simulations indicated that as much as 5.5 feet of additional average water-level drawdown in wells would occur by 2000 if surface-water supply were reduced 100 percent and ground-water pumpage increased. The simulations also indicated that a decrease in average drawdown of 0.55 foot would occur by 2000 and that base flow to the river would decrease to 12,300 acre-feet per year if 1979 conditions remained constant. (USGS)

  13. Tecnologia alternativa para a quebra de dormência das sementes de pau-de-balsa (Ochroma lagopus Sw., Bombacaceae) Alternative technology for breaking dormancy of balsa wood (Ochroma lagopus Sw., Bombacaceae) seeds

    OpenAIRE

    Antenor P. Barbosa; Paulo de .T. B. Sampaio; Moacir. A. A. Campos; Vânia P. Varela; Cláudia de Q. B. Gonçalves; Shigeo Iida

    2004-01-01

    Este trabalho, teve como objetivo estudar a germinação das sementes de pau-de-balsa (Ochroma lagopus Sw., Bombacaceae) em diferentes estágios de maturação aparente dos frutos; a germinação das sementes provenientes de árvores com diferentes diâmetros a altura do peito (DAP) e a germinação das sementes tratadas para quebra de dormência. No primeiro experimento, avaliou-se a germinação das sementes dos frutos verdes, verdosos (verde amarelado), negros (fruto fechado) e negros deiscentes (fruto ...

  14. POPULATION STRUCTURE AND PRODUCTION OF COPAIBA OLEORESIN BETWEEN VALLEYS AND HILLSIDES OF THE MINING AREA OFTROMBETAS RIVER - PARÁ1

    Directory of Open Access Journals (Sweden)

    Jonas Gebara

    2016-02-01

    Full Text Available ABSTRACT We aimed in this work to study natural populations of copaiba (Copaifera multijuga Hayne on the Monte Branco mountain at Porto Trombetas-PA, in order to support sustainable management and the exploitation of oleoresin from copaiba. We studied the population structure of copaiba on hillsides and valleys of the south face of Monte Branco, within Saracá Taquera National Forest, where bauxite ore was extracted in the biennium 2013-2014 by Mineração Rio do Norte (MRN. We produced a 100% forest inventory of the specie and of oleoresin extraction in order to quantify the potential production of the remaining area. The density of copaiba individuals with DBH > 30 cm was 0.33 individuals per hectare in the hillside and 0.25 individuals per hectare in the valley. Both environments presented a density of 0.28 individuals per hectare. The average copaiba oleoresin yield was 0.661±0.334 liters in the hillside and 0.765±0.280 liters in the valley. The average value of both environments together (hillside and valley was 0.714±0.218 liters. From all individuals with DBH over 30 cm, 38 (58% produced some amount of oleoresin, averaging 1.113±0.562 liters in the hillside, 1.329±0.448 liters in the valley and 1.190±0.355 liters in both environments together. The results show the need for planning the use of the surroundings of the study area in order to reach the required volume of copaiba to make feasible the sustainable management of oleoresin extraction in the region.

  15. The organic and mineral matter contents in deposits infilling floodplain basins: Holocene alluviation record from the Kłodnica and Osobłoga river valleys, southern Poland

    Science.gov (United States)

    Wójcicki, K. J.; Marynowski, L.

    2012-07-01

    The work examines the timing and environmental conditions of floodplain sedimentation in the valleys of the upland Kłodnica and piedmont Osobłoga rivers in the Upper Odra River basin. A distribution of 52 14C-ages shows relatively high floodplain sedimentation at the Late Glacial-Holocene transition, more stable floodplain environments since the Early (in the Kłodnica Valley) and Middle Holocene (in the Osobłoga Valley) and a gradual increase in floodplain deposition in the Late Holocene (since hydrological events) as well as factors affecting the local record of sedimentation (i.e. valley morphology, hydrologic conditions and episodes of local erosion). A clear relationship is shown between an increase in alluviation and climate- or human-induced extension of unforested areas. The deposition of mineral-rich sediments increases rapidly during periods characterized by non-arboreal pollen values exceeding approximately 8% in pollen diagrams. On the other hand, the results obtained do not confirm significant interactions between Holocene changes in forest composition and alluviation. Despite the settlement of agrarian groups, the sedimentary record of human activity in the Osobłoga catchment is very poor during the Neolithic and early Bronze Age. A large-scale alluviation of the Osobłoga and Kłodnica valleys was initiated during the settlement of people of the Lusatian culture from the middle Bronze Age and escalated in the early Middle Ages and Modern Times. The deposition of products of soil erosion was limited to between ca. 1.9-1.2 kyr BP, probably due to demographic regression during the Migration Period. Comparison of OM/MM fluctuations with phases of increased fluvial activity does not show a relationship between Holocene wetter phases and catchment sediment yield. Sedimentary episodes in the Upper Odra basin also show a low degree of correlation with the probability density curve of the 14C-ages. The results obtained in the Kłodnica and Osob

  16. Conservação e vigor de sementes de pau-de-balsa (Ochroma pyramidale) Conservation and vigour of balsawood seeds (Ochroma pyramidale)

    OpenAIRE

    Antonio Moçambite Pinto; Mario Takao Inoue; Antonio Carlos Nogueira

    2004-01-01

    Ochroma pyramidale, Bombacaceae, conhecida popularmente como pau-de-balsa, é utilizada para construção de jangadas, balsas, salva-vidas, bóias, brinquedos e na fabricação de papel e celulose. O objetivo deste estudo foi definir um método de acondicionamento de sementes de O. pyramidale, visando a conservação da viabilidade e vigor destas para sua utilização e comercialização em épocas de baixa produção. Sementes de O. pyramidale foram embaladas em sacos de papel tipo kraft e sacos de plástico...

  17. Isolation and Characterization of Microsatellite Loci for Hibiscus aridicola (Malvaceae, an Endangered Plant Endemic to the Dry-Hot Valleys of Jinsha River in Southwest China

    Directory of Open Access Journals (Sweden)

    Kaiyun Guan

    2011-09-01

    Full Text Available Hibiscus aridicola (Malvaceae is an endangered ornamental shrub endemic to the dry-hot valleys of Jinsha River in southwest China. Only four natural populations of H. aridicola exist in the wild according to our field investigation. It can be inferred that H. aridicola is facing a very high risk of extinction in the wild and an urgent conservation strategy is required. By using a modified biotin-streptavidin capture method, a total of 40 microsatellite markers were developed and characterized in H. aridicola for the first time. Polymorphisms were evaluated in 39 individuals from four natural populations. Fifteen of the markers showed polymorphisms with two to six alleles per locus; the observed heterozygosity ranged from 0.19 to 0.72. These microsatellite loci would be useful tools for population genetics studies on H. aridicola and other con-generic species which are important to the conservation and development of endangered species.

  18. THE REALIZATION OF THE AGRI-ENVIRONMENTAL MANAGEMENT SCHEME IN THE AREA OF NATURA 2000 IN THE VALLEY OF BIEBRZA RIVER

    Directory of Open Access Journals (Sweden)

    Wojciech Gotkiewicz

    2015-12-01

    Full Text Available The aim of the research was to analyse the functioning of agricultural farms located in the areas of Natura 2000 network. The research was conducted in 2015 among 70 farmers whose lands were located in the Valley of Biebrza River in Podlaskie Voivodeship. The main research method was a questionnaire. According to the results of the research, the agri-environmental scheme is a proper tool that combines the environmental protection and local producers’ interests; however, it requires the implementation of a supplement adjusted to the nature of the areas. It is also indicated that even though the economic part of the program does not raise any doubts, the natural eff ects are practically not recognized, which may lead to an incomplete protection of precious species and habitats.

  19. Dynamics of spatial clustering of schistosomiasis in the Yangtze River Valley at the end of and following the World Bank Loan Project.

    Science.gov (United States)

    Hu, Yi; Xiong, Chenglong; Zhang, Zhijie; Luo, Can; Ward, Michael; Gao, Jie; Zhang, Lijuan; Jiang, Qingwu

    2014-06-01

    The 10-year (1992-2001) World Bank Loan Project (WBLP) contributed greatly to schistosomiasis control in China. However, the re-emergence of schistosomiasis in recent years challenged the long-term progress of the WBLP strategy. In order to gain insight in the long-term progress of the WBLP, the spatial pattern of the epidemic was investigated in the Yangtze River Valley between 1999-2001 and 2007-2008. Two spatial cluster methods were jointly used to identify spatial clusters of cases. The magnitude and number of clusters varied during 1999-2001. It was found that prevalence of schistosomiasis had been greatly reduced and maintained at a low level during 2007-2008, with little change. Besides, spatial clusters most frequently occurred within 16 counties in the Dongting Lake region and within 5 counties in the Poyang Lake region. These findings precisely pointed out the prior places for future public health planning and resource allocation of schistosomiasis.

  20. AIRS Impact on Analysis and Forecast of an Extreme Rainfall Event (Indus River Valley 2010) with a Global Data Assimilation and Forecast System

    Science.gov (United States)

    Reale, O.; Lau, W. K.; Susskind, J.; Rosenberg, R.

    2011-01-01

    A set of data assimilation and forecast experiments are performed with the NASA Global data assimilation and forecast system GEOS-5, to compare the impact of different approaches towards assimilation of Advanced Infrared Spectrometer (AIRS) data on the precipitation analysis and forecast skill. The event chosen is an extreme rainfall episode which occurred in late July 11 2010 in Pakistan, causing massive floods along the Indus River Valley. Results show that the assimilation of quality-controlled AIRS temperature retrievals obtained under partly cloudy conditions produce better precipitation analyses, and substantially better 7-day forecasts, than assimilation of clear-sky radiances. The improvement of precipitation forecast skill up to 7 day is very significant in the tropics, and is caused by an improved representation, attributed to cloudy retrieval assimilation, of two contributing mechanisms: the low-level moisture advection, and the concentration of moisture over the area in the days preceding the precipitation peak.

  1. SHRIMP study of zircons from Early Archean rocks in the Minnesota River Valley: Implications for the tectonic history of the Superior Province

    Science.gov (United States)

    Bickford, M.E.; Wooden, J.L.; Bauer, R.L.

    2006-01-01

    Interest in Paleoarchean to early Mesoarchean crust in North America has been sparked by the recent identification of ca. 3800-3500 Ma rocks on the northern margin of the Superior craton in the Assean Lake region of northern Manitoba and the Porpoise Cove terrane in northern Quebec. It has long been known that similarly ancient gneisses are exposed on the southern margin of the Superior craton in the Minnesota River Valley and in northern Michigan, but the ages of these rocks have been poorly constrained, because methods applied in the 1960s through late 1970s were inadequate to unravel the complexities of their thermotectonic history. Rocks exposed in the Minnesota River Valley include a complex of migmatitic granitic gneisses, schistose to gneissic amphibolite, metagabbro, and paragneisses. The best-known units are the Morton Gneiss and the Montevideo Gneiss. The complex of ancient gneisses is intruded by a major younger, weakly deformed granite body, the Sacred Heart granite. Regional geophysical anomalies that extend across the Minnesota River Valley have been interpreted as defining boundaries between distinct blocks containing the various gneissic units. New sensitive high-resolution ion microprobe (SHRIMP) U-Pb data from complex zircons yielded the following ages: Montevideo Gneiss near Montevideo, 3485 ?? 10 Ma, granodiorite intrusion, 3385 ?? 8 Ma; Montevideo Gneiss at Granite Falls, 3497 ?? 9 Ma, metamorphic event, 3300-3350 Ma, mafic intrusion, 3141 ?? 2 Ma, metamorphic overprint (rims), 2606 ?? 4 Ma; Morton Gneiss: 3524 ?? 9 Ma, granodiorite intrusion, 3370 ?? 8 Ma, metamorphic overprints (growth of rims), 3140 ?? 2 Ma and 2595 ?? 4 Ma; biotite-garnet paragneiss, 2619 ?? 20 Ma; and Sacred Heart granite, 2604 ?? 4 Ma. Zircons from a cordierite-bearing feldspar-biotite schist overlying the Morton Gneiss yielded well-defined age peaks at 3520, 3480, 3380, and 3140 Ma, showing detrital input from most of the older rock units; 2600 Ma rims on these zircons

  2. [Study of interaction of wild soybean subpopulations (Glycine soja) in the valley of the Tsukanovka river in the south of Far East of Russia].

    Science.gov (United States)

    Tikhonov, A V; Martynov, V V; Dorokhov, D B

    2011-01-01

    A comparative study of the genetic structure of natural and anthropogenic populations of G. soja gives significant information about formation of different populations, and allows developing measures for preservation of unique natural gene bank of wild soybean, the species closely related to cultivated soybean. In this study, ISSR markers were used to carry out a comparative analysis of genetic structure of natural and anthropogenic subpopulations of G. soja for studying possible mutual influence of subpopulations of anthropogenic and natural phytocenosis on the formation of their genetic diversity and to study genetic structure of natural subpopulations of wild soybean in the contact places between the two types ofcenoses. As a result, the characteristics that describe the genetic diversity of studied populations have been identified and the important role of an interaction between subpopulations of different phytocenoses on formation of the spatial genetic structure of population in the valley of Tsukanovka river has been demonstrated.

  3. Phases of Environmental Evolution Indicated by Primary Chemical Elements and Paleontological Records in the Upper Pleistocene-Holocene Series for the Salawusu River Valley, China

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    Studies of lithology, sedimentary facies and the distribution regularity of SiO2 and Al2O3 contents and Al2O3/SiO2 ratio allow us to divide the Upper Pleistocene-Holocene Series represented by the Milanggouwan section in China's Salawusu River valley into six segments: MGS1, MGS2, MGS3,MGS4, MGS5 and MGS6. The boundary ages for MGS1 (the Dishaogouwan and Dagouwan Formations), MGS2 (the upper Chengchuan Formation), MGS3 (the middle Chengchuan Formation),MGS4 (the lower Chengchuan Formation), MGS5 (most strata of the Salawusu Formation) and MGS6 (the bottom of the Salawusu Formation and the top of the Lishi Formation) correspond to those of MIS1, MIS2, MIS3, MIS4, MIS5 and MIS6, respectively, from deep sea sediments or continental glaciers. MGS5 can be subdivided into five subsegments (MGS5a, MGS5b, MGS5c,MGS5d and MGS5e) and the boundary ages of these subsegments correspond to those of MIS5a,MIS5b, MIS5c, MIS5d and MIS5e, respectively. Based on the paleoenvironment and paleoecology indicated by the primary chemical elements, fossil vertebrates, mollusks and pollen grains, we hypothesize that MGS1, MGS2, MGS3, MGS4, MGS5 and MGS6 and the subsegments of MGS5 match the corresponding stages for oxygen isotopes in the deep sea sediments and continental glaciers,and the substages of MIS5 in terms of climatic characters, further explaining the phenomena that determined the formation of the late Quaternary strata and the paleontology of the Salawusu River valley. These phenomena relate to fluctuations in the global climate (and particularly in the East Asian monsoon) during the glacial and interglacial periods.

  4. A Summary of the Symposium on the Civilizing Course in the Upper Yangtze River Valley%长江上游地区文明化进程学术研讨会纪要

    Institute of Scientific and Technical Information of China (English)

    陈剑; 于春

    2005-01-01

    In 22 - 24 April, 2004, the Research Center of Ancient Civilization, IA, CASS, the Suchuan Provincial Institute of Cultural Relics and Archaeology, and the Chengdu Municipal Institute of Cultural Relics and Archaeology jointly held the “Symposium on the Civilizing Course in the Upper Yangtze River Valley.” At the meeting, exchanges and discussions were carried out mainly on the following topics: The Neolithic culture in Northwestern China. The southward spread of painted pottery from the upper Yellow River valley. The ritual institution in the Longshan period. Prehistoric city-sites on the Chengdu Plain. An analysis of the Sanxingdui culture elements. A Compositional analysis of the bronzes from the Jinsha site and those from the Three Gorges area. The chronology of the Paleolithic to the Qin-Han cultures in the Three Gorges and Yangtze River area. The origin and development of the Ba people and the Ba culture.

  5. Methods and applications of electrical simulation in ground-water studies in the lower Arkansas and Verdigris River Valleys, Arkansas and Oklahoma

    Science.gov (United States)

    Bedinger, M.S.; Reed, J.E.; Wells, C.J.; Swafford, B.F.

    1970-01-01

    The Arkansas River Multiple-Purpose Plan will provide year-round navigation on the Arkansas River from near its mouth to Muskogee, Okla., and on the Verdigris River from Muskogee to Catoosa, Okla. The altered regimen in the Arkansas and Verdigris Rivers will affect ground-water conditions in the adjacent alluvial aquifers. In 1957 the U.S. Geological Survey and U.S. Army Corps of Engineers entered into a cooperative agreement for a comprehensive ground-water study of the lower Arkansas and Verdigris River valleys. At the request of the Corps of Engineers, the Geological Survey agreed to provide (1) basic ground-water data before, during, and after construction of the Multiple-Purpose Plan and (2) interpretation and projections of postconstruction ground-water conditions. The data collected were used by the Corps of Engineers in preliminary foundation and excavation estimates and by the Geological Survey as the basis for defining the hydrologic properties of, and the ground-water conditions in, the aquifer. The projections of postconstruction ground-water conditions were used by the Corps of Engineers in the planning, design, construction, and operation of the Multiple-Purpose Plan. Analysis and projections of ground-water conditions were made by use of electrical analog models. These models use the analogy between the flow of electricity in a resistance-capacitance circuit and the flow of a liquid in a porous and permeable medium. Verification provides a test of the validity of the analog to perform as the aquifer would, within the range of historic forces. The verification process consists of simulating the action of historic forces which have acted upon the aquifer and of duplicating the aquifer response with the analog. The areal distribution of accretion can be treated as an unknown and can be determined by analog simulation of the piezometric surface in an aquifer. Comparison of accretion with depth to piezometric surface below land surface shows that

  6. 甘肃白龙江流域鸡皮衣属地衣的研究%The lichen genus Pertusaria from Bailong River valley of Gansu,China

    Institute of Scientific and Technical Information of China (English)

    杨芳; 任强; 史秀莉; 张权; 赵遵田

    2008-01-01

    @@ 1 INTRODUCTION Bailong River,a tributary of Jialing River belonging to the Yangtse River system,is located in the southern part of Gansu Province and the northeast rimland of Qinghai-Tibet Plateau,with total length of over 600kin and drainage area of about 31,800km2.Originating from Dagcanglhamo,Luqu of Gansu Province,the river flows through Min Shan Mountains from northwest to southeast,and passes through Tewo,Zhugqu,Wudu and Wenxian.The annual temperature of the river valley is around 4.7-12.7℃,and annual precipitation is 448.9-911.6mm.The climate of the upper reaches is temperate-humid,of the middle reaches warm-humid,and the lower reaches subtropic-humid.

  7. Standard practice for acoustic emission examination of pressurized containers made of fiberglass reinforced plastic with balsa wood cores

    CERN Document Server

    American Society for Testing and Materials. Philadelphia

    2007-01-01

    1.1 This practice covers guidelines for acoustic emission (AE) examinations of pressurized containers made of fiberglass reinforced plastic (FRP) with balsa cores. Containers of this type are commonly used on tank trailers for the transport of hazardous chemicals. 1.2 This practice is limited to cylindrical shape containers, 0.5 m [20 in.] to 3 m [120 in.] in diameter, of sandwich construction with balsa wood core and over 30 % glass (by weight) FRP skins. Reinforcing material may be mat, roving, cloth, unidirectional layers, or a combination thereof. There is no restriction with regard to fabrication technique or method of design. 1.3 This practice is limited to containers that are designed for less than 0.520 MPa [75.4 psi] (gage) above static pressure head due to contents. 1.4 This practice does not specify a time interval between examinations for re-qualification of a pressure container. 1.5 This practice is used to determine if a container is suitable for service or if follow-up NDT is needed before that...

  8. Indicators used to assess the quantity and quality of water in Special Area of Conservation located in the valleys of large lowland rivers - case study

    Science.gov (United States)

    Utratna, Marta; Okruszko, Tomasz

    2016-04-01

    One of the aims of Ecological network Natura 2000 is to protect rare habitats from complete disappearance in Europe. That is why natural and transformed river valleys were and still are often included into this form of protection. The problem of influences on Natura 2000 areas an their impact on the conservation status of protected habitats within the network is well known. Solving this issue may have a significant impact on the planning of protection tasks, as well as on assessing the impact of new and existing investments on protected areas. The aim of this study was to build a statistical model for assessing the impact of selected external factors related to the quantity and quality of water on the conservation status of habitats in large lowland river areas protected under the Natura 2000 network. The method used in the study is based on a structural study which uses the knowledge and experience of experts in the field of Phytosociology as well as indicators used to assess the quantity and quality of water in the analyzed area.

  9. Deglacial Record in the Illinois River Valley Explains Asynchronous Phases of Meltwater Pulses and Clay Mineral Excursions in the Gulf of Mexico

    Science.gov (United States)

    Wang, H.

    2014-12-01

    One prominent event of the Bølling/Allerød (B/A) interstadial was the large meltwater release to global oceans. The Laurentide Ice Sheet (LIS) is usually considered the main source. But, the large LIS meltwater discharge conflicts with the marine record showing an active North Atlantic meridional overturning circulation (AMOC) during the B/A interval. Continuous dune-lacustrine successions in the Illinois River Valley (IRV) have shown complete records of the last deglacial chronozones. Their grain-size distributions and accurate B/A age 14C dates of plant fossils from 15 m deep lacustrine sediment in the IRV suggest that most of the IRV and parts of the adjacent upland were inundated by water. The inundation was caused by a sediment dam interpreted to have been constructed and followed by a breach at the confluence of the Mississippi and Illinois Rivers during the B/A interval due to sediment mobilization by the large meltwater release. The grain size distributions correlate with meltwater pulses and mineralogical excursions in sediments from the Gulf of Mexico (GOM) very well. The blockage and release of illite and chlorite rich fine-grained sediments from the Lake Michigan basin changed the relative abundance of clay minerals and thus the ratio of smectite/(illite + chlorite) in the sediment of the GOM. This finding explains why the meltwater episodes from the LIS and the associated detrital discharges are not synchronous in the sediments in the GOM. The finding also ties meltwater pulses and associated detrital discharges in the GOM closely to the LIS discharges via the Mississippi River Valley on chronozonal scales. Three arguments can be made from this result: 1) unaffected AMOC during B/A interval resulted potentially from the hyperpycnal inflow into the GOM floor; 2) limited volume of the meltwater discharge did not significantly influence the AMOC; and 3) the freshwater input into the GOM from the LIS at this particular location did not significantly

  10. Questa Baseline and Pre-Mining Ground-Water Quality Investigation. 25. Summary of Results and Baseline and Pre-Mining Ground-Water Geochemistry, Red River Valley, Taos County, New Mexico, 2001-2005

    Science.gov (United States)

    Nordstrom, D. Kirk

    2008-01-01

    Active and inactive mine sites are challenging to remediate because of their complexity and scale. Regulations meant to achieve environmental restoration at mine sites are equally challenging to apply for the same reasons. The goal of environmental restoration should be to restore contaminated mine sites, as closely as possible, to pre-mining conditions. Metalliferous mine sites in the Western United States are commonly located in hydrothermally altered and mineralized terrain in which pre-mining concentrations of metals were already anomalously high. Typically, those pre-mining concentrations were not measured, but sometimes they can be reconstructed using scientific inference. Molycorp?s Questa molybdenum mine in the Red River Valley, northern New Mexico, is located near the margin of the Questa caldera in a highly mineralized region. The State of New Mexico requires that ground-water quality standards be met on closure unless it can be shown that potential contaminant concentrations were higher than the standards before mining. No ground water at the mine site had been chemically analyzed before mining. The aim of this investigation, in cooperation with the New Mexico Environment Department (NMED), is to infer the pre-mining ground-water quality by an examination of the geologic, hydrologic, and geochemical controls on ground-water quality in a nearby, or proximal, analog site in the Straight Creek drainage basin. Twenty-seven reports contain details of investigations on the geological, hydrological, and geochemical characteristics of the Red River Valley that are summarized in this report. These studies include mapping of surface mineralogy by Airborne Visible-Infrared Imaging Spectrometry (AVIRIS); compilations of historical surface- and ground- water quality data; synoptic/tracer studies with mass loading and temporal water-quality trends of the Red River; reaction-transport modeling of the Red River; environmental geology of the Red River Valley; lake

  11. Late Pleistocene and Holocene palaeoflood events recorded by slackwater deposits in the upper Hanjiang River valley, China

    Science.gov (United States)

    Liu, Tao; Huang, Chun Chang; Pang, Jiangli; Zha, Xiaochun; Zhou, Yali; Zhang, Yuzhu; Ji, Lin

    2015-10-01

    Slackwater palaeoflood deposits (SWDs) were identified in a bedrock gorge in the upper reaches of the Hanjiang River of central China. The Hanjiang River is the longest tributary of the Yangtze River, one of the most flood-prone rivers in China, and the main source of water for the South-to-North Water Transfer Project (SNWTP). Three main loess-soil profiles with late Pleistocene and Holocene palaeoflood SWD bedsets were found. Palaeoflood SWDs identified interbedded in the loess-soil sequence of late Pleistocene and Holocene age within the cliff riverbanks were studied by field observations and laboratory analysis, including particle-size distribution and Optically Stimulated Luminescence (OSL) dating. At least eight extreme flood events documented by palaeoflood SWDs occurred in the Wufeng reaches of the upper Hanjiang River. The discharge estimation associated with palaeoflood SWDs, indicates that the minimum flood peak discharges of these flood episodes range from 42,220 to 63,400 m3/s. The SWDs were OSL dated to between 12,600-12,400, 4200-4000, 3200-2800 and 1900-1700 a BP and these dates were corroborated with pottery remains retrieved from the profiles and dated by archaeological methods. These periods of increased flood magnitude coincide with contemporaneous global climatic events dated to 12,500, 4200, 3100 and 1900 a BP worldwide. These findings are of great significance in understanding the interactions between hydrological systems and climatic change in monsoonal zones.

  12. POPULATION STRUCTURE AND PRODUCTION OF COPAIBA OLEORESIN BETWEEN VALLEYS AND HILLSIDES OF THE MINING AREA OFTROMBETAS RIVER - PARÁ1

    OpenAIRE

    Jonas Gebara; Antenor Pereira Barbosa; Isabel Maria Gonçalves Azevedo; Bruno Oliva Gimenez

    2016-01-01

    ABSTRACT We aimed in this work to study natural populations of copaiba (Copaifera multijuga Hayne) on the Monte Branco mountain at Porto Trombetas-PA, in order to support sustainable management and the exploitation of oleoresin from copaiba. We studied the population structure of copaiba on hillsides and valleys of the south face of Monte Branco, within Saracá Taquera National Forest, where bauxite ore was extracted in the biennium 2013-2014 by Mineração Rio do Norte (MRN). We produced a 100%...

  13. Evaluation of mechanical properties and low velocity impact characteristics of balsa wood and urethane foam applied to impact limiter of nuclear spent fuel shipping cask

    International Nuclear Information System (INIS)

    The paper aims to evaluate the low velocity impact responses and mechanical properties of balsa wood and urethane foam core materials and their sandwich panels, which are applied as the impact limiter of a nuclear spent fuel shipping cask. For the urethane foam core, which is isotropic, tensile, compressive, and shear mechanical tests were conducted. For the balsa wood core, which is orthotropic and shows different material properties in different orthogonal directions, nine mechanical properties were determined. The impact test specimens for the core material and their sandwich panel were subjected to low velocity impact loads using an instrumented testing machine at impact energy levels of 1, 3, and 5J. The experimental results showed that both the urethane foam and the balsa wood core except in the growth direction (z-direction) had a similar impact response for the energy absorbing capacity, contact force, and indentation. Furthermore, it was found that the urethane foam core was suitable as an impact limiter material owing to its resistance to fire and low cost, and the balsa wood core could also be strongly considered as an impact limiter material for a lightweight nuclear spent fuel shipping cask

  14. Probable hydrologic effects of a hypothetical failure of Mackay Dam on the Big Lost River Valley from Mackay, Idaho to the Idaho National Engineering Laboratory

    Science.gov (United States)

    Druffel, Leroy; Stiltner, Gloria J.; Keefer, Thomas N.

    1979-01-01

    Mackay Dam is an irrigation reservoir on the Big Lost River, Idaho, approximately 7.2 kilometers northwest of Mackay, Idaho. Consequences of possible rupture of the dam have long concerned the residents of the river valley. The presence of reactors and of a management complex for nuclear wastes on the reservation of the Idaho National Engineering Laboratory (INEL), near the river , give additional cause for concern over the consequences of a rupture of Mackay Dam. The objective of this report is to calculate and route the flood wave resulting from the hypothetical failure of Mackay Dam downstream to the INEL. Both a full and a 50 percent partial breach of this dam are investigated. Two techniques are used to develop the dam-break model. The method of characteristics is used to propagate the shock wave after the dam fails. The linear implicit finite-difference solution is used to route the flood wave after the shock wave has dissipated. The time of travel of the flood wave, duration of flooding, and magnitude of the flood are determined for eight selected sites from Mackay Dam, Idaho, through the INEL diversion. At 4.2 kilometers above the INEL diversion, peak discharges of 1,550.2 and 1,275 cubic meters per second and peak flood elevations of 1,550.3 and 1,550.2 meters were calculated for the full and partial breach, respectively. Flood discharges and flood peaks were not compared for the area downstream of the diversion because of the lack of detailed flood plain geometry. (Kosco-USGS)

  15. Post-glacial landform evolution in the middle Satluj River valley, India: Implications towards understanding the climate tectonic interactions

    Indian Academy of Sciences (India)

    Shubhra Sharma; S K Bartarya; B S Marh

    2016-04-01

    Late Quaternary landform evolution in monsoon-dominated middle Satluj valley is reconstructed using the fragmentary records of fluvial terraces, alluvial fans, debris flows, paleo-flood deposits, and epigenetic gorges. Based on detailed field mapping, alluvial stratigraphy, sedimentology and optical chronology, two phases of fluvial aggradations are identified. The older aggradation event dated between ∼13 and 11 ka (early-Holocene), occurred in the pre-existing topography carved by multiple events of erosion and incision. Climatically, the event corresponds to the post-glacial strengthened Indian summer monsoon (ISM). The younger aggradation event dated between ∼5 and 0.4 ka (mid- to late-Holocene), was duringthe declining phase of ISM. The terrain witnessed high magnitude floods during transitional climate (∼6.5–7 ka). The fluvial sedimentation was punctuated by short-lived debris flows and alluvial fans during the LGM (weak ISM), early to mid-Holocene transition climate and mid- to late-Holocene decliningISM. Based on the terrace morphology, an event of relatively enhanced surface uplift is inferred after late Holocene. The present study suggests that post-glacial landforms in the middle Satluj valley owe their genesis to the interplay between the climate variability and local/regional tectonic interactions.

  16. Questa Baseline and Pre-Mining Ground-Water Quality Investigation. 17. Geomorphology of the Red River Valley, Taos County, New Mexico, and Influence on Ground-Water Flow in the Shallow Alluvial Aquifer

    Science.gov (United States)

    Vincent, Kirk R.

    2008-01-01

    In April 2001, the U.S. Geological Survey (USGS) and the New Mexico Environment Department (NMED) began a cooperative study to infer the pre-mining ground-water chemistry at the Molycorp molybdenum mine site in the Red River Valley of north-central New Mexico. This report is one in a series of reports that can be used to determine pre-mining ground-water conditions at the mine site. Molycorp?s Questa molybdenum mine in the Red River Valley, northern New Mexico, is located near the margin of the Questa caldera in a highly mineralized region. The bedrock of the Taos Range surrounding the Red River is composed of Proterozoic rocks of various types, which are intruded and overlain by Oligocene volcanic rocks associated with the Questa caldera. Locally, these rocks were altered by hydrothermal activity. The alteration zones that contain sulfide minerals are particularly important because they constitute the commercial ore bodies of the region and, where exposed to weathering, form sites of rapid erosion referred to as alteration scars. Over the past thousand years, if not over the entire Holocene, erosion rates were spatially variable. Forested hillslopes eroded at about 0.04 millimeter per year, whereas alteration scars eroded at about 2.7 millimeters per year. The erosion rate of the alteration scars is unusually rapid for naturally occurring sites that have not been disturbed by humans. Watersheds containing large alteration scars delivered more sediment to the Red River Valley than the Red River could remove. Consequently, large debris fans, as much as 80 meters thick, developed within the valley. The geomorphology of the Red River Valley has had several large influences on the hydrology of the shallow alluvial aquifer, and those influences were in effect before the onset of mining within the watershed. Several reaches where alluvial ground water emerges to become Red River streamflow were observed by a tracer dilution study conducted in 2001. The aquifer narrows

  17. Evaluation of the Emission, Transport, and Deposition of Mercury and Fine Particulate Matter from Coal-Based Power Plants in the Ohio River Valley Region

    Energy Technology Data Exchange (ETDEWEB)

    Kevin Crist

    2008-12-31

    As stated in the proposal: Ohio University, in collaboration with CONSOL Energy, Advanced Technology Systems, Inc (ATS) and Atmospheric and Environmental Research, Inc. (AER) as subcontractors, evaluated the impact of emissions from coal-fired power plants in the Ohio River Valley region as they relate to the transport and deposition of mercury and associated fine particulate matter. This evaluation involved two interrelated areas of effort: ambient air monitoring and regional-scale modeling analysis. The scope of work for the ambient air monitoring included the deployment of a surface air monitoring (SAM) station in southeastern Ohio. The SAM station contains sampling equipment to collect and measure mercury (including speciated forms of mercury and wet and dry deposited mercury), particulate matter (PM) mass, PM composition, and gaseous criteria pollutants (CO, NOx, SO2, O3, etc.). Laboratory analyses of time-integrated samples were used to obtain chemical speciation of ambient PM composition and mercury in precipitation. Nearreal- time measurements were used to measure the ambient concentrations of PM mass and all gaseous species including Hg0 and RGM. Approximately 30 months of field data were collected at the SAM site to validate the proposed regional model simulations for episodic and seasonal model runs. The ambient air quality data provides mercury, and fine particulate matter data that can be used by Ohio Valley industries to assess performance on multi-pollutant control systems. The scope of work for the modeling analysis includes (1) development of updated inventories of mercury emissions from coal plants and other important sources in the modeled domain; (2) adapting an existing 3-D atmospheric chemical transport model to incorporate recent advancements in the understanding of mercury transformations in the atmosphere; (3) analyses of the flux of Hg0, RGM, and fine particulate matter in the different sectors of the study region to identify key transport

  18. EVALUATION OF THE EMISSION, TRANSPORT, AND DEPOSITION OF MERCURY, FINE PARTICULATE MATTER, AND ARSENIC FROM COAL-BASED POWER PLANTS IN THE OHIO RIVER VALLEY REGION

    Energy Technology Data Exchange (ETDEWEB)

    Kevin Crist

    2004-04-02

    Ohio University, in collaboration with CONSOL Energy, Advanced Technology Systems, Inc. (ATS) and Atmospheric and Environmental Research, Inc. (AER) as subcontractors, is evaluating the impact of emissions from coal-fired power plants in the Ohio River Valley region as they relate to the transport and deposition of mercury, arsenic, and associated fine particulate matter. This evaluation will involve two interrelated areas of effort: ambient air monitoring and regional-scale modeling analysis. The scope of work for the ambient air monitoring will include the deployment of a surface air monitoring (SAM) station in southeastern Ohio. The SAM station will contain sampling equipment to collect and measure mercury (including speciated forms of mercury and wet and dry deposited mercury), arsenic, particulate matter (PM) mass, PM composition, and gaseous criteria pollutants (CO, NOx, SO{sub 2}, O{sub 3}, etc.). Laboratory analysis of time-integrated samples will be used to obtain chemical speciation of ambient PM composition and mercury in precipitation. Near-real-time measurements will be used to measure the ambient concentrations of PM mass and all gaseous species including Hg{sup 0} and RGM. Approximately 18 months of field data will be collected at the SAM site to validate the proposed regional model simulations for episodic and seasonal model runs. The ambient air quality data will also provide mercury, arsenic, and fine particulate matter data that can be used by Ohio Valley industries to assess performance on multi-pollutant control systems. The scope of work for the modeling analysis will include (1) development of updated inventories of mercury and arsenic emissions from coal-fired power plants and other important sources in the modeled domain; (2) adapting an existing 3-D atmospheric chemical transport model to incorporate recent advancements in the understanding of mercury transformations in the atmosphere; (3) analyses of the flux of Hg{sup 0}, RGM, arsenic

  19. Instability in eight sub-basins of the Chilliwack River Valley, British Columbia, Canada: A comparison of natural and logging-related landslides

    Science.gov (United States)

    Wolter, Andrea; Ward, Brent; Millard, Tom

    2010-08-01

    Logging causes increased landslide frequency in British Columbia. In this study, the slope, type, initiation location, aspect, rate, bedrock geology, and size of mass movements located in eight logged tributary valleys of the Chilliwack River Valley are investigated. A landslide inventory was created by digitizing landslides identified on aerial photographs dating from 1941 to 2002. This database was analysed using qualitative observations and simple statistical tests, and a comparison between natural and logging-related landslides was made. Slope tests displayed a significant difference between natural and logging-related events, indicating that, on average, logging-related landslides require lower slope gradients to initiate than natural events. Although aspect, initiation location, and landslide type did not show a significant relationship between natural and logging-related landslides, they do suggest subtle differences. Landslide rate was calculated and compared for natural and logging-related landslides. It was significantly higher for logging-related events, attaining a maximum of 31 times the natural rate in 1978 and an overall average increase of nine times the natural rate. Logging-related landslides were on average smaller than natural landslides but this nevertheless resulted in a 3.1 times increase in area affected by logging-related landslides compared to natural landslides. Geology may influence landslide frequency as well; it appears to be higher over the less resistive sedimentary rocks of the Cultus Formation and Chilliwack Group and lower in granodioritic areas. Finally, roads affected slope stability more than clearcuts in the early decades of the study, but this effect decreased over time, suggesting a correlation with improved road construction.

  20. Bees (Hymenoptera: Apidae) present in the flowers of the balsa wood Ochroma lagopus Swartz, 1788 - doi: 10.4025/actascibiolsci.v32i4.7103 Bees (Hymenoptera: Apidae) present in the flowers of the balsa wood Ochroma lagopus Swartz, 1788 - doi: 10.4025/actascibiolsci.v32i4.7103

    OpenAIRE

    Deodoro Magno Brighenti; Carla Regina Guimarães Brighenti

    2010-01-01

    The flower of balsa wood holds about 10 to 15 mL of nectar, which helps attracting pollinating agents, since the genus Ochroma is incapable of self-fertilization. However, a high mortality of bees is observed in these flowers. The present study investigated the frequency and constancy of mortality of the individuals of the family Apidae that fed on nectar from the balsa wood. Data was gathered from June to August 2008, in Lavras – Minas Gerais State, Brazil. In addition, the survival of the A...

  1. Agricultural reclamations in Xiliao River Valley,China since the Holocene%西辽河流域全新世以来的农业垦殖活动

    Institute of Scientific and Technical Information of China (English)

    HAN Maoli; ZHAO Yuhui; ZHANG Dan

    2012-01-01

    @@%The agricultural reclamations in the Xiliao River Valley since the Holocene have led to a huge landscape change from grassland to farmland.In this paper we reconsider the man-land relationship in the Xiliao River Valley by analyzing three major agricultural reclamations in prehistory,the Liao-Jin Dynasty and the period since the Qing Dynasty.We argue that when the demographic pressure appears in this area,especially during the last reclamation,the intraregional migration (second migration) is the major response to relieve such pressure,which also distinguishes two different settlement locations:"the initial area" and "the secondary area".Due to the environmental differences between these two areas,the cultivation on the latter one has caused more serious disturbance to the local environment.Thus the secondary area has become the key region which needs environmental management seriously.

  2. A Simulation Study of a Heavy Rainfall Process over the Yangtze River Valley Using the Two-Way Nesting Approach

    Institute of Scientific and Technical Information of China (English)

    WANG Shuzhou; YU Entao; WANG Huijun

    2012-01-01

    In this study,the major features of a heavy rainfall event in the Yangtze River region on 3-7 June 2011 and its event-related large-scale circulation and predictability were studied.Both observational analysis and model simulation were used,the latter being based on the Weather Research and Forecasting (WRF) model forced by NCEP Global Forecast System (GFS) datasets.It was found that,during 3-5 June,the western Pacific subtropical high apparently extended to the west and was much stronger,and the Indian summer monsoon trough was slightly weaker than in normal years.The east-west oriented shear line over the middle and lower reaches of the Yangtze River was favorable for the transportation and convergence of water vapor,and the precipitation band was located slightly to the south of the shear line.During 6-7 June,the western Pacific subtropical high retreated eastward,while the trough over the Okhotsk Sea deepened. The low vortex in Northeast China intensified,bringing much more cold air to the middle and lower reaches of the Yangtze River,and the shear line over this area moved slightly southward.The convection band moved southward and became weaker,so the rainfall during 6-7 June weakened and was located slightly to the south of the previous precipitation band.Many of the observed features,including background circulation and the distribution and amount of precipitation,were reproduced reasonably by the WRF,suggesting a feasibility of this model for forecasting extreme weather events in the Yangtze River region.

  3. The rK39 immunochromatic dipstick testing: A study for K39 seroprevalence in dogs and human leishmaniasis patients for possible animal reservoir of cutaneous and visceral leishmaniasis in endemic focus of Satluj river valley of Himachal Pradesh (India)

    OpenAIRE

    Sharma Nand; Mahajan Vikram; Negi Ajit; Verma Ghanshyam

    2009-01-01

    Background: The newly recognized endemic focus of leishmaniasis in Satluj river valley of Himachal Pradesh (India) has both localized cutaneous leishmaniasis (LCL) and visceral leishmaniasis (VL) predominantly caused by Leishmania donovani. Rapid rK39 immunochromatographic dipstick test detects circulating antibodies to recombinant K39 antigen of L. donovani-infantum complex and is highly specific/sensitive in diagnosing symptomatic or asymptomatic infection in humans and dogs. Methods: Th...

  4. Technogenic magnetic particles in soils as evidence of historical mining and smelting activity: A case of the Brynica River Valley, Poland.

    Science.gov (United States)

    Magiera, Tadeusz; Mendakiewicz, Maria; Szuszkiewicz, Marcin; Jabłońska, Mariola; Chróst, Leszek

    2016-10-01

    In the area of Brynica River basin (Upper Silesia, southern Poland) the exploitation and smelting of iron, silver and lead ores was historically documented since early Middle Ages. First investigations showed that metallurgy industry had a large impact from 9th century (AD) until the Second World War. The aim of the study was to use magnetic prospection to detect traces of past mining and ore smelting in Brynica River Valley located in Upper Silesia (southern Poland). The field screening was performed by measurement magnetic susceptibility (κ) on surface and in vertical profiles and was supported locally by gradiometric measurements. Vertical distribution of magnetic susceptibility values was closely associated with the type of soil use. Historical technogenic magnetic particles resulting from exploitation, processing, and smelting of iron, silver, and lead ores were accumulated in the soil layer at the depth 10 to 25cm. They were represented by sharp-edged particles of slag, coke, as well as various mineralogical forms of iron minerals and aggregates composed of carbon particles, aluminosilicate glass, and single particles of metallic iron. The additional geochemical study in adjacent peat bog supported by radiocarbon dating was also performed. The application of integrated geochemical-magnetic methods to reconstruct the historical accumulation of pollutants in the studied peat bog was effective. The magnetic peak, which was pointed out by magnetic analyses, is consistent with the presence of charcoal and pollution from heavy metals, such as Ag, Cd, Cu, Fe, Pb, or Sn. The results of this work will be helpful for the further study of human's impact on the environment related to the historical and even pre-historical ore exploitation and smelting and also used for better targeting the archeological excavations on such areas. PMID:27236619

  5. Technogenic magnetic particles in soils as evidence of historical mining and smelting activity: A case of the Brynica River Valley, Poland.

    Science.gov (United States)

    Magiera, Tadeusz; Mendakiewicz, Maria; Szuszkiewicz, Marcin; Jabłońska, Mariola; Chróst, Leszek

    2016-10-01

    In the area of Brynica River basin (Upper Silesia, southern Poland) the exploitation and smelting of iron, silver and lead ores was historically documented since early Middle Ages. First investigations showed that metallurgy industry had a large impact from 9th century (AD) until the Second World War. The aim of the study was to use magnetic prospection to detect traces of past mining and ore smelting in Brynica River Valley located in Upper Silesia (southern Poland). The field screening was performed by measurement magnetic susceptibility (κ) on surface and in vertical profiles and was supported locally by gradiometric measurements. Vertical distribution of magnetic susceptibility values was closely associated with the type of soil use. Historical technogenic magnetic particles resulting from exploitation, processing, and smelting of iron, silver, and lead ores were accumulated in the soil layer at the depth 10 to 25cm. They were represented by sharp-edged particles of slag, coke, as well as various mineralogical forms of iron minerals and aggregates composed of carbon particles, aluminosilicate glass, and single particles of metallic iron. The additional geochemical study in adjacent peat bog supported by radiocarbon dating was also performed. The application of integrated geochemical-magnetic methods to reconstruct the historical accumulation of pollutants in the studied peat bog was effective. The magnetic peak, which was pointed out by magnetic analyses, is consistent with the presence of charcoal and pollution from heavy metals, such as Ag, Cd, Cu, Fe, Pb, or Sn. The results of this work will be helpful for the further study of human's impact on the environment related to the historical and even pre-historical ore exploitation and smelting and also used for better targeting the archeological excavations on such areas.

  6. The cultural analysis in the environmental impact studies. Jepirachi wind pilot project and connecting road between the Aburra valley and Cauca River

    International Nuclear Information System (INIS)

    This article is synthesis of the investigation to choose I in environment title of Master and Development of the National University of Host Colombia Medellin, on the speech, the social images and representations that emerge in the Studies from environmental Impact -EIA- from the cultural systems from communities affected by the implantation and operation. From two macro projects, that are part of the Plans of national Development, regional and local in Colombia: one, the Project Pilot of Generation of Aeolian Energy Jepirachi, in Colombian the Guajira discharge that affects indigenous communities of several establishments Wayuu in the sector of Average Moon. The other, the project of Road Connection between Valleys of the Aburra River - and the Cauca River, which it affects communities that inhabit an axis of rural transition - urban, whose cultural composition is diverse in its origin, mobility and interactions. It was left from two hypotheses: one, is that the analysis made in the cultural dimension of the EIA, is insufficient lo identify, lo evaluate and to handle the impacts on the cultural systems; second, front lo the treatment of the cultural systems is the existence of fundamental differences. There is cultural systems in Colombia which status is recognized greater and category than to others. The analysis of the speech allowed to obtain a diagnosis on semantic the rhetorical structure and - formal and textual cohesion, coherence, correlations and associations in the EIA and to identify the social images and representations that emerge on the populations taken part by the projects. Finally conclusions. That consider they leave to the debate on the cultural analyses that have been made in the EIA ,their emptiness and limitations and the different courses open that can take futures works from investigation

  7. Landscape pattern of seed banks and anthropogenic impacts in forested wetlands of the northern Mississippi River Alluvial Valley

    Science.gov (United States)

    Middleton, B.; Wu, X.B.

    2008-01-01

    Agricultural development on floodplains contributes to hydrologic alteration and forest fragmentation, which may alter landscape-level processes. These changes may be related to shifts in the seed bank composition of floodplain wetlands. We examined the patterns of seed bank composition across a floodplain watershed by looking at the number of seeds germinating per m2 by species in 60 farmed and intact forested wetlands along the Cache River watershed in Illinois. The seed bank composition was compared above and below a water diversion (position), which artificially subdivides the watershed. Position of these wetlands represented the most variability of Axis I in a Nonmetric Multidimensional Scaling (NMS) analysis of site environmental variables and their relationship to seed bank composition (coefficient of determination for Axis 1: r2 = 0.376; Pearson correlation of position to Axis 1: r = 0.223). The 3 primary axes were also represented by other site environmental variables, including farming status (farmed or unfarmed), distance from the mouth of the river, latitude, and longitude. Spatial analysis based on Mantel correlograms showed that both water-dispersed and wind/water-dispersed seed assemblages had strong spatial structure in the upper Cache (above the water diversion), bur the spatial structure of water-dispersed seed assemblage was diminished in the lower Cache (below the water diversion), which lost floodpulsing. Bearing analysis also Suggested that water-dispersal process had a stronger influence on the overall spatial pattern of seed assemblage in the upper Cache, while wind/water-dispersal process had a stronger influence in the lower Cache. An analysis of the landscapes along the river showed that the mid-lower Cache (below the water diversion) had undergone greater land cover changes associated with agriculture than did the upper Cache watershed. Thus, the combination of forest fragmentation and hydrologic changes in the surrounding landscape may

  8. SELENIUM IN SALSODISOLS LOCATED IN THE CĂLMĂŢUI AND BUZĂU RIVERS VALLEYS

    Directory of Open Access Journals (Sweden)

    Radu Lacatusu

    2012-12-01

    Full Text Available Selenium contents were determined in the A horizon of the Salsodisols (Solonchaks and Solonetzplaced along the Călmăţui and Buzău Valleys. The total selenium content oscillated between 480 and 1140g·kg-1, with an average value of 800 g·kg-1. This value is 2.1 times higher than the selenium total content inthe upper horizon of the World’s non-halomorphic soils. It is also higher than the selenium total content in the upper horizon of the soils from Dobrogea and the South-Eastern Romanian Plain, 5.6 respectively 3.4 times. The mobile selenium content, soluble in the EDTA-CH3COONH4 solution at pH = 7, ranged in the 13-25 g·kg-1 interval, with an average value of 18 g·kg-1, 4 times higher than the mobile selenium contents of the Dobrogea soils upper horizon and 1.2 times higher than the ones in the South-Eastern part of the Romanian Plain. Between the selenium total contents and some Salsodisols physical and chemical properties proportionality relations were established, statistically ensured. Most of these soils’ selenium content is to be found as calcium, sodium, or magnesium (secondary selenates. The presence of the same cations’ selenites is not excluded.

  9. [Effects of grazing disturbance on soil active organic carbon in mountain forest-arid valley ecotone in the upper reaches of Minjiang River].

    Science.gov (United States)

    Liu, Shan-Shan; Zhang, Xing-Hua; Gong, Yuan-Bo; Li, Yuan; Wang, Yan; Yin, Yan-Jie; Ma, Jin-Song; Guo, Ting

    2014-02-01

    Effects of grazing disturbance on the soil carbon contents and active components in the four vegetations, i.e., artificial Robinia pseudoacacia plantation, artificial poplar plantation, Berberis aggregate shrubland and grassland, were studied in the mountain forest-arid valley ecotone in the upper Minjiang River. Soil organic carbon and active component contents in 0-10 cm soil layer were greater than in 10-20 cm soil layer at each level of grazing disturbance. With increasing the grazing intensity, the total organic carbon (TOC), light fraction organic carbon (LFOC), particulate organic carbon (POC) and easily oxidized carbon (LOC) contents in 0-10 cm soil layer decreased gradually in the artificial R. pseudoacacia plantation. The LFOC content decreased, the POC content increased, and the TOC and LOC contents decreased initially and then increased with increasing the grazing intensity in the artificial poplar plantation. The POC content decreased, and the TOC, LFOC and LOC contents decreased initially and then increased with increasing the grazing intensity in the B. aggregate shrubland. The POC and TOC contents decreased, and the LFOC and LOC contents decreased initially and then increased with increasing the grazing intensity in the grassland. The decreasing ranges of LOC, LFOC and POC contents were 0.1-7.9 times more than that of TOC content. There were significant positive relationships between TOC and LOC, LFOC and POC, suggesting that the active organic carbon components could reflect the change of soil total carbon content.

  10. A STUDY ON THE RELATION BETWEEN THE VARIATION OF THE PRECIPITATION IN EASTERN JIANGHUAI WATERSHED AND SEDIMENT TRANSPORT IN CHIHE RIVER VALLEY

    Institute of Scientific and Technical Information of China (English)

    ZAHNGJian-chun; PENGPu-zhuo

    2002-01-01

    Rainfall resource is very important to the development of society and economy,especially to eastern Jianghuai watershed which is now facing serious challenge of water shortage.Based on the observational records covering the period from 1957 to 1999,the characteristics of precipitation changing over eastern JiangHuai watershed and its connection to sediment discharge in Chibe River valley were studied using tendency analysis and correlation analysis.Results show that the rainfall in this area had a declining tendency in Spring at a rate of -21.2mm/10a,annual and Summer precipitation was increasing at the rate of 10.6mm/10a and 14.8mm/10a.The gray correlation analysis shows that sediment discharge correlated most closely with runoffs and the frequency of the rainstorm with a daily precipitation of 50-100mm,on the second place,with the number of rainy days.In addition,the paper suggests the major countermeasures and methods for controlling of soil and water losses in this area.

  11. A STUDY ON THE RELATION BETWEEN THE VARIATION OF THE PRECIPITATION IN EASTERN JIANGHUAI WATERSHED AND SEDIMENT TRANSPORT IN CHIHE RIVER VALLEY

    Institute of Scientific and Technical Information of China (English)

    2002-01-01

    Rainfall resource is very important to the development of society and economy, especially to easternJianghuai watershed which is now facing serious challenge of water shortage. Based on the observational records coveringthe period from 1957 to 1999, the characteristics of precipitation changing over eastern JiangHuai watershed and its connec-tion to sediment discharge in Chihe River valley were studied using tendency analysis and correlation analysis . Resultsshow that the rainfall in this area had a declining tendency in Spring at a rate of -21.2mm/ 10a, annual and Sum-mer precipitation was increasing at the rate of 10. 6mm/10a and 14. 8mm/10a. The gray correlation analysis shows thatsediment discharge correlates most closely with runoffs and the frequency of the rainstorm with a daily precipitation of50- 100mm, on the second place, with the rainfall and the frequency of the rainstorm of a daily precipitation no lessthan 100mm; and thirdly with the number of rainy days. In addition, the paper suggests the major countermeasures andmethods for controlling of soil and water losses in this area.

  12. Analysis of the Profitability and Marketing Channels of Rice: A Case Study of Menchum River Valley, North-West Region, Cameroon

    Directory of Open Access Journals (Sweden)

    Bime, M. J.

    2014-06-01

    Full Text Available The study carried out in Menchum River valley, Northwest Region of Cameroon had as objective to analyze the profitability and establish the marketing channels of rice in this zone. The study in-terviewed a total of 126 respondents, selected purposively and using the snow ball sampling tech-nique. Results showed that the main actors involved in the rice marketing channel were; produc-ers, wholesalers, hullers, retailers and consumers. The production and marketing of rice in the zone is a profitable venture. In terms of profitability in the rice business, millers obtain a relatively large profit margin as a percentage of the cost price (18.69% followed by the producers (12.77%, wholesalers (8.5% then retailers (8.33%. The average profit margin per bag of 50kg was; 1054.5FCFA (franc Communauté financière d'Afrique for producers, 1963.5 FCFA for millers; 1100 FCFA for the wholesalers and 1250FCFA for the retailers. The principal constraints identi-fied by the study that affects actors of the rice channel were, bad condition of the roads, lack of capital, poor quality of rice. It was recommended that there should be improvement in infrastruc-ture.

  13. Millennial-centennial Scales Climate Changes of Holocene Indicated by Magnetic Susceptibility of High-resolution Section in Salawusu River Valley China

    Institute of Scientific and Technical Information of China (English)

    LU Yingxia; LI Baosheng; WEN Xiaohao; QIU Shifan; WANG Fengnian; NIU Dongfeng; LI Zhiwen

    2010-01-01

    The upmost segment(Holocene series)of the Milanggouwan stratigraphic section(MGS1)in the Salawusu River valley shows 11 sedimentary cycles of dune sands and fluvio-lacustrine facies,or dune sands and paleosols.The analysis of the magnetic susceptibility of this segment suggests that there are 11 magnetic susceptibility cycles with the value alternating from low to high,in which the layers of the dune sands correspond to the lower value of the magnetic susceptibility and the layers of fluvio-lacustrine facies and paleosols correspond to the higher peaks.The study reveals that the low and high magnetic susceptibility values indicate the climate dominated by cold-arid winter monsoon and warm-humid summer monsoon of East Asia,respectively,and the study area has experienced at least 22 times of mil-lennial-centennial scales climate alternation from the cold-arid to the warm-humid during the Holocene.In terms of the time and the climate nature,the variations basically correspond to those of the North Atlantic and some records of cold-warm changes in China as well.They might be caused by the alternation of winter and summer monsoons in the Mu Us Desert induced by global climate fluctuations in the Holocene.

  14. CHANGES IN THE MOISTURE CONTENT OF THE MIDDLE FEN SOILS IN THE ODRA RIVER VALLEY IN THE REGION OF BRZEG DOLNY IN THE VEGETATION PERIODS 2004–2009

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    Leszek Pływaczyk

    2014-10-01

    Full Text Available In soils, where the water table is deeply located and has a minor impact on the moisture content of the surface layer, we are dealing with the precipitation-and-water type of water management. If underground water level is close to the surface, the top stratum of the soil, apart from precipitation, is additionally fed by water absorption from underground waters. Then we are dealing with ground-and-water type of management. We consider such types of water management of soil in the area of the left-bank valley of the Odra river, above and below the dam in Brzeg Dolny. The dominant soil types here are middle fen soils, based on middle clay and heavy clay as well as loam, which, in conditions of either excess or deficiency of moisture, are difficult to cultivate. The work compares water management of two soil profiles in vegetation periods between 2004 and 2009. The formation of underground waters, meteorological conditions and the course of the water reserves in the strata 0–50 cm and 0–100 cm were estimated with various supplying conditions of the active stratum of the soil. The volume of the supply with percolated water from underground water of the layer 50–100 cm on approximately 75–90 mm was also estimated. This value was mainly dependent on the depth of the retention of the water table of the soil profile above the level in Brzeg Dolny.

  15. Grain-size distribution characteristics of red sandy sediments in Dongjiang River valley, southern Nanling Mountains,during the MIS2 stage

    Institute of Scientific and Technical Information of China (English)

    ShuHuan Du; BaoSheng Li; DongFeng Niu; XiaoHao Wen; FengNian Wang; XianJiao Ou; Yi Yang; YueJun Si; XinNan Zhao

    2009-01-01

    Layer LJ3 of Linjiang sttrigraphic section in Dongjiang River valley in the south of the Nanling Mountains is a set of red sandy sediments.Measured by thermoluminescence (TL) dating, it was found to be formed in MIS2-9,500±800 yr to 19,600±1,800 yr B.P. After analysis of the grain sizes of the 16 samples (LJ3-100 to LJ3-85) in this layer, it was discovered that (1) The contents of each grain group in different samples are similar. (2) The values of Md, Mz,σ,Sk and Kg vary from LJ3-100 to LJ3-85 in a narrow range. (3) The segments of each sample in the accumulative curves extend parallel with similar slopes. All the three aspects reveal the Aeolian characteristics of Layer LJ3.Therefore, it is thought that Layer LJ3 consists of red sandy sediments formed in MIS2 in the south of Nanling Mountain, which reflects the arid climate at that time.

  16. DETERMINATION OF AGRICULTURAL POTENTIAL BY GEO SPATIAL MODELING AND MULTI CRITERIA ANALYSIS FOR “BALSAS MEZCALA” WATERSHED

    Directory of Open Access Journals (Sweden)

    Anastacio Espejel-García

    2015-07-01

    Full Text Available The use of geographic information systems (GIS facilitates the modeling of specific information allowing faster, lower costs and accuracy for the planning of the agricultural activities for large territories. The objective for this paper was to use GIS as a support for the approach of the land use potential for the “Balsas Mezcala” watershed; for this purpose the multi criteria analysis was used, that allows to consider decision make issues with multiples objectives and considering the following criteria: geo-pedological (geomorphology and soil, climatology (thermal models and rainfall and the edapho-climatological requirements of the crops, the “Balsas Mezcala” hydrological region was chosen as the study area; through cartographic material the area was delimited and climate information was obtained from weather stations, geographic information and the data bases was collected from many different government agencies (INEGI, SEMARNAT, CONABIO, CONAGUA, IMTA, such information was processed in the ArcGIS software version 10.2.2, to obtained the geodatabases and geo spatial matrix which served as a cartographic input for the multi criteria analysis. The result of this investigation is a system that from geo spatial matrix and vectorial data originates raster dataset, same that were submitted to a modeling process with geo statistical algorithms, with that from a structure language, identify the potential zones with the highest aptness level, through the variable attributes that assign a weighted value using the methodology proposed by the United States Department of Agriculture (USDA in 1971 and taken by Food and Agriculture Organization of the United Nations (FAO for case studies since 1977 as an Agro-ecological Zoning System (AEZ. The result of the modeling of the soil aptness level in the watershed are 4 classes with 6 levels of aptness (very apt, apt, moderately apt, little apt, very little apt, unapt: Lands with irrigation potential

  17. White River Falls Fish Passage Project, Tygh Valley, Oregon : Final Technical Report, Volume II, Appendix A, Fisheries Habitat Inventory.

    Energy Technology Data Exchange (ETDEWEB)

    Oregon. Dept. of Fish and Wildlife; Mount Hood National Forest (Or.)

    1985-06-01

    Stream habitat inventories on 155 stream miles in the White River drainage on the Mt. Hood National Forest are summarized in this report. Inventory, data evaluation, and reporting work were accomplished within the framework of the budgetary agreements established between the USDA Forest Service, Mt. Hood National Forest, and the Bonneville Power Administration, in the first 2 years of a multiyear program. One hundred forty-two stream miles of those inventoried on the Forest appear suitable for anadromous production. The surveyed area appears to contain most or all of the high quality fish habitat which would be potentially available for anadromous production if access is provided above the White River Falls below the Forest boundary. About 34 stream miles would be immediately accessible without further work on the Forest with passage at the Falls. Seventy-two additional miles could be made available with only minor (requiring low investment of money and planning) passage work further up the basin. Thirty-six miles of potential upstream habitat would likely require major investment to provide access.

  18. Hydrogeology of the Scioto River Valley near Piketon, South-Central Ohio a quantitative study of ground-water yield and induced infiltration in a glacial outwash aquifer

    Science.gov (United States)

    Norris, Stanley Eugene; Fidler, Richard E.

    1969-01-01

    A systematic study was made of one of Ohio's principal aquifers, a sand and gravel outwash in the Scioto River Valley, to determine the feasibility of developing a ground-water supply of 20 million gallons per day at a site near Piketon. The first part of the study was spent in determining the thickness and physical properties of the sand and gravel aquifer and in drilling test wells to determine the best site for the supply wells. The second part of the investigation was an aquifer infiltration test to determine the hydraulic properties of the aquifer and the conditions of stream recharge. A well 83 feet deep was drilled on the flood plain and was pumped for 9 days at the rate of 1,000 gallons per minute. Tile effect on the hydrologic system during and after the pumping was determined by measuring the water levels in an array of deep and shallow observation wells and in 8 drive-point wells installed in the bed of the river. Seldom have more comprehensive data been collected showing the effects of pumping on a natural, unconfined, hydrologic system. From these data were calculated the coefficient of transmissibility (215,000 gallons per day per foot) and the rate of streambed infiltration (0.235 million gallons per day per acre per foot). The aquifer was tested near the end of a long drought; so the ground-water levels and the river stage were very nearly following a level trend. Because the ground-water levels were essentially unaffected by extraneous influences, the test data are probably as precise and uncomplicated as is practical to obtain in the field. These data proved to be valid for use as design criteria for the location, spacing, and construction of four supply wells. The third part of the investigation was the testing and quantitative evaluation of the four supply wells before they were put into service. The wells were found to perform about as predicted, indicating that the hydraulic properties of the aquifer, as determined by standard methods, are

  19. Estimates of consumptive use and ground-water return flow and the effect of rising and sustained high river stage on the method of estimation in Cibola Valley, Arizona and California, 1983 and 1984

    Science.gov (United States)

    Owen-Joyce, Sandra J.

    1990-01-01

    In Cibola Valley, Arizona, water is pumped from the Colorado River to irrigate crops and to maintain wildlife habitat. Unused water percolates to the water table and, as groundwater, moves downgradient into areas of phreatophytes, into a drainage ditch, out of the flood plain, and back to the river. In 1983 and 1984, groundwater return flow was negligible because in most of Cibola Valley the river lost water to the aquifer. Evapotranspiration was used as an approximation for consumptive use by vegetation. Evapotranspiration was calculated as the sum of the products of the area of vegetation types and water-use rate by vegetation type. Evapotranspiration was estimated to be 70,100 acre-ft in 1983 and 62,600 acre-ft in 1984. These estimates may be in error because of the effect of sustained inundation on the rate of water use by phreatophytes. The effects cannot be quantified and therefore adjustments to rates calculated for dry-surface conditions could not be made. The method of estimating consumptive use of water by vegetation and groundwater return flow is affected by changing conditions during years of rising and sustained high river stage caused by flood-control releases at Parker Dam. Most of the bank storage that will return to the river when the high river stage subsides did not originate as irrigation water. High river stage caused some areas to be flooded directly or raised groundwater levels above the land surface. No crops could be grown in flooded fields. The decreased depth to water and inundation with fresh water resulted in new phreatophyte growth in some areas. In some areas that were flooded, many phreatophytes died. Changes in the inundated and flooded areas throughout the years made it difficult to estimate the evaporation losses from the increased water surface. (USGS)

  20. Records of wells, water levels, and chemical quality of water in the lower Santiam River basin, middle Willamette Valley, Oregon

    Science.gov (United States)

    Helm, Donald C.

    1968-01-01

    Basic water data on the lower Santiam River basin is preliminary to a comprehensive hydrologic study of this productive and intensely irrigated area where expanding population and industry increases the demand for water. Highest yielding wells are in shallow alluvial aquifers near the main streams; yields range from several hundred to more than a thousand gpm. Wells in lacustrine and older alluvial aquifers that underlie low, flat terraces have yields from a few tens to a few hundred gpm. Wells in the Salem Hills and in the Cascade Range foothills yield moderate to small quantities of water and tap a variety of geologic units. Tabulated material includes records of representative wells, drillers' logs, and chemical and spectrographic analyses of the ground water.

  1. Process interpretation of laminated lacustrine sediments from the valley of the river Alf, Quaternary West Eifel Volcanic Field, Germany

    Science.gov (United States)

    Eichhorn, Luise; Pirrung, Michael; Zolitschka, Bernd; Büchel, Georg

    2016-04-01

    High-resolution annually laminated sediment archives from lakes Holzmaar and Meerfelder Maar located in the Quaternary West Eifel Volcanic Field are in the focus of many investigations (e.g. Brauer et al. 2001, Zolitschka 1991). These publications are related to predominantly biogenic varves covering the last ca. 14 ka years, i.e. the Lateglacial and the Holocene. In our study, laminated sediments consisting of clay-silt couplets are presented from paleolake Alf. This paleolake formed in a valley dammed by volcanic products, and covers the Pleniglacial between 31 and 24 ka BP (Pirrung et al. 2007). The focus of our study is the characterization of the structure of clay-silt couplets and the determination of their origin. The applied granulometry revealed mean grain sizes of 10 μm for the light laminae (colors refer to core scan photo) and 14 μm for the dark laminae (both middle silt). X-ray diffraction confirms identical mineral phases for light and dark laminae, with light laminae being clay-enriched containing a higher amount of sericite and chlorite while dark laminae are enriched in quartz. X-ray fluorescence and detrital microfacies analysis on thin sections indicate that calcite dominates in the dark laminae. Microscopically, three different types of silt layers are present. Type I are laminae with homogeneous sublayers, Type II are graded laminae and Type III are laminae with graded sublayers. Processes causing the formation of these silt lamination types can be attributed to repeatedly occurring snow melting, permafrost thawing or rain events linked with sediment delivery from the catchment into the lake. The amount of precipitation and melt water, sediment discharge and density stratification lead to gravity suspension fall out, partial erosion of previously deposited unconsolidated sediments and resuspension in the lake. Brauer, A., et al. (2001). Lateglacial varve chronology and biostratigraphy of lakes Holzmaar and Meerfelder Maar, Germany. Boreas 30

  2. Hydraulic and Geomorphic Assessment of the Merced River and Historic Bridges in Eastern Yosemite Valley, Yosemite National Park, California: Sacramento, California

    Science.gov (United States)

    Minear, J. Toby; Wright, Scott A.

    2013-01-01

    The Merced River in the popular and picturesque eastern-most part of Yosemite Valley in Yosemite National Park, California, USA, has been extensively altered since the park was first conceived in 1864. Historical human trampling of streambanks has been suggested as the cause of substantial increases in stream width, and the construction of undersized stone bridges in the 1920s has been suggested as the major factor leading to an increase in overbank flooding due to deposition of bars and islands between the bridges. In response, the National Park Service at Yosemite National Park (YNP) requested a study of the hydraulic and geomorphic conditions affecting the most-heavily influenced part of the river, a 2.4-km reach in eastern Yosemite Valley extending from above the Tenaya Creek and Merced River confluence to below Housekeeping Bridge. As part of the study, present-day conditions were compared to historical conditions and several possible planning scenarios were investigated, including the removal of an elevated road berm and the removal of three undersized historic stone bridges identified by YNP as potential problems: Sugar Pine, Ahwahnee and Stoneman Bridges. This Open-File Report will be superseded at a later date by a Scientific Investigations Report. A two-dimensional hydrodynamic model, the USGS FaSTMECH (Flow and Sediment Transport with Morphological Evolution of Channels) model, within the USGS International River Interface Cooperative (iRIC) model framework, was used to compare the scenarios over a range of discharges with annual exceedance probabilities of 50-, 20-, 10-, and 5- percent. A variety of topographic and hydraulic data sources were used to create the input conditions to the hydrodynamic model, including aerial LiDAR (Light Detection And Ranging), ground-based LiDAR, total station survey data, and grain size data from pebble counts. A digitized version of a historical topographic map created by the USGS in 1919, combined with estimates of

  3. Holocene alluvial stratigraphy and response to climate change in the Roaring River valley, Front Range, Colorado, USA

    Science.gov (United States)

    Madole, Richard F.

    2012-09-01

    Stratigraphic analyses and radiocarbon geochronology of alluvial deposits exposed along the Roaring River, Colorado, lead to three principal conclusions: (1) the opinion that stream channels in the higher parts of the Front Range are relics of the Pleistocene and nonalluvial under the present climate, as argued in a water-rights trial USA v. Colorado, is untenable, (2) beds of clast-supported gravel alternate in vertical succession with beds of fine-grained sediment (sand, mud, and peat) in response to centennial-scale changes in snowmelt-driven peak discharges, and (3) alluvial strata provide information about Holocene climate history that complements the history provided by cirque moraines, periglacial deposits, and paleontological data. Most alluvial strata are of late Holocene age and record, among other things, that: (1) the largest peak flows since the end of the Pleistocene occurred during the late Holocene; (2) the occurrence of a mid- to late Holocene interval (~ 2450-1630(?) cal yr BP) of warmer climate, which is not clearly identified in palynological records; and (3) the Little Ice Age climate seems to have had little impact on stream channels, except perhaps for minor (~ 1 m) incision.

  4. Holocene alluvial stratigraphy and response to climate change in the Roaring River valley, Front Range, Colorado, USA

    Science.gov (United States)

    Madole, Richard F.

    2012-01-01

    Stratigraphic analyses and radiocarbon geochronology of alluvial deposits exposed along the Roaring River, Colorado, lead to three principal conclusions: (1) the opinion that stream channels in the higher parts of the Front Range are relics of the Pleistocene and nonalluvial under the present climate, as argued in a water-rights trial USA v. Colorado, is untenable, (2) beds of clast-supported gravel alternate in vertical succession with beds of fine-grained sediment (sand, mud, and peat) in response to centennial-scale changes in snowmelt-driven peak discharges, and (3) alluvial strata provide information about Holocene climate history that complements the history provided by cirque moraines, periglacial deposits, and paleontological data. Most alluvial strata are of late Holocene age and record, among other things, that: (1) the largest peak flows since the end of the Pleistocene occurred during the late Holocene; (2) the occurrence of a mid- to late Holocene interval (~2450–1630(?) cal yr BP) of warmer climate, which is not clearly identified in palynological records; and (3) the Little Ice Age climate seems to have had little impact on stream channels, except perhaps for minor (~1 m) incision. Published

  5. Bees (Hymenoptera: Apidae present in the flowers of the balsa wood Ochroma lagopus Swartz, 1788 = Abelhas (Hymenoptera: Apidae associadas às flores do pau-de-balsa Ochroma lagopus Swartz, 1788

    Directory of Open Access Journals (Sweden)

    Carla Regina Guimarães Brighenti

    2010-10-01

    Full Text Available The flower of balsa wood holds about 10 to 15 mL of nectar, which helps attracting pollinating agents, since the genus Ochroma is incapable of self-fertilization. However, a high mortality of bees is observed in these flowers. The present study investigated the frequency and constancy of mortality of the individuals of the familyApidae that fed on nectar from the balsa wood. Data was gathered from June to August 2008, in Lavras – Minas Gerais State, Brazil. In addition, the survival of the Africanized bees that fed on the nectar of this flower was compared to those that fed on 50% aqueous solution of honey. Forty flowers were analyzed, and 949 individuals of the orders Hymenoptera (98.1%, Hemiptera (0.95%, Coleoptera (0.74% and Diptera (0.21% were collected. Most Hymenoptera individuals were bees of the genera Partamona and Trigona (677 individuals, which were considered of constant occurrence. Flowers producing up to 16.7 nectar mL were found. The nectar diet contained 16.44% of total sugar, and resulted in low survival of the bees in laboratory (31.32 . 2.37 hours, compared to a diet of 50% aqueous solution of honey (112.32 .2.03 hours.A flor do pau-de-balsa produz cerca de 10 a 15 mL de néctar, útil na atração de polinizadores, uma vez que o gênero Ochroma é incapaz de fazer autofecundação. É observada intensa mortalidade de abelhas em suas flores. Objetivou-se realizar o levantamento da frequência e constância de mortalidade de indivíduos da família Apidae, sendo os dados levantados no período de junho a agosto de 2008 em Lavras, MinasGerais, Brasil. Além disso, avaliou-se a sobrevivência de abelhas africanizadas alimentadas com o néctar desta flor quando comparados com aquelas alimentadas com solução aquosa de mel a 50%. Foram analisadas 40 flores e coletados 949 indivíduos das Ordens: Hymenoptera (98,1%, Hemiptera (0,95%, Coleoptera (0,74% e Diptera (0,21%. Dentre os himenópteros os mais frequentes foram dos g

  6. Status of Water Levels and Selected Water-Quality Conditions in the Mississippi River Valley Alluvial Aquifer in Eastern Arkansas, 2004

    Science.gov (United States)

    Schrader, T.P.

    2006-01-01

    During the spring of 2004, water levels were measured in 684 wells completed in the Mississippi River Valley alluvial aquifer in eastern Arkansas. Ground-water levels are affected by intense ground-water withdrawals resulting in extensive potentiometric depressions. In 2004, the highest water-level altitude measured was 293 feet above National Geodetic Vertical Datum of 1929 in northeastern Clay County. The lowest water-level altitude measured was 76 feet above National Geodetic Vertical Datum of 1929 in the center of Arkansas County. A large depression in the potentiometric surface was located in Arkansas, Lonoke, and Prairie Counties during 1998 and persisted to 2002. The area enclosed in the 100-foot contour in Arkansas County in 2004 is about the same as in 2002, however, the area enclosed in the 100-foot contour in Lonoke and Prairie Counties in 2004 has receded. Two shallower cones of depressions were located in Craighead, Cross, and Poinsett Counties and St. Francis, Woodruff, Lee, and Monroe Counties west of Crowleys Ridge during 1998. The 2004 potentiometricsurface map shows that the areas enclosed by the 140-foot contour have continued to expand. A map of changes in water-level measurements between 2000 and 2004 was constructed using the difference between water-level measurements from 625 wells reported in this report and the 2000 Mississippi River Valley alluvial aquifer report. Water-level changes between 2000 and 2004 ranged from -31.1 feet to 16.3 feet, with a mean of -0.7 feet (negative changes indicating water-level declines, positive changes indicating water-level rises). The largest rise of 16.3 feet is in Arkansas County and the largest decline of -31.1 feet is in Prairie County. Long-term water-level changes were calculated for 134 wells in the alluvial aquifer for the period from 1980 to 2004. The mean annual decline in water level for the entire study area was -0.31 feet per year with a range of -1.35 feet per year to 0.84 feet per year. The

  7. Chemical changes in argisols under irrigated grape production in the central São Francisco river valley, Brazil

    Directory of Open Access Journals (Sweden)

    R. J. Heck

    2002-03-01

    Full Text Available This study compares the chemical composition of the solution and exchange complex of soil in a 3-year-old irrigated vineyard (Vitis vinifera L., Red Globe cultivar with that of adjacent clearing in the native hyperxerophyllic 'caatinga' vegetation. The soils are classified as Plinthic Eutrophic Red-Yellow Argisol; according to Soil Taxonomy they are isohyperthermic Plinthustalfs. Detailed physiographic characterization revealed an impermeable gravel and cobble covering the crystalline rocks; the relief of this layer was more undulating than the level surface. Significant higher concentrations of extractable Na, K, Mg and Ca were observed within the vineyard. Lower soil acidity, higher Ca/Mg ratios, as well as lower sodium adsorption and Na/K ratios reflected additions of dolomitic lime, superphosphate and K-bearing fertilizers. As the water of the São Francisco River is of good quality for irrigation (C1S1, the increases in Na were primarily attributed to capillary rise from the saline groundwater table. None of the soil in the study area was found to be sodic. About 62% of the vineyard had an Ap horizon with salinity levels above 1.5dSm-1 (considered detrimental for grape production; according to average values for this horizon, a potential 13% reduction in grape production was predicted. Differences in chemical composition in function of distance to the collector canals were observed in the clearing, but not in the vineyard. The influence of differences in the elevations of the surface and impermeable layers, as well as pediment thickness, was generally weaker under irrigation. Under irrigation, soil moisture was greater in points of convergent surface waterflow; the effect of surface curvature on chemical properties, though less consistent, was also stronger in the vineyard.

  8. Pesticides in Water and Suspended Sediment of the Alamo and New Rivers, Imperial Valley/Salton Sea Basin, California, 2006-2007

    Science.gov (United States)

    Orlando, James L.; Smalling, Kelly L.; Kuivila, Kathryn M.

    2008-01-01

    Water and suspended-sediment samples were collected at eight sites on the Alamo and New Rivers in the Imperial Valley/Salton Sea Basin of California and analyzed for both current-use and organochlorine pesticides by the U.S. Geological Survey. Samples were collected in the fall of 2006 and spring of 2007, corresponding to the seasons of greatest pesticide use in the basin. Large-volume water samples (up to 650 liters) were collected at each site and processed using a flow-through centrifuge to isolate suspended sediments. One-liter water samples were collected from the effluent of the centrifuge for the analysis of dissolved pesticides. Additional samples were collected for analysis of dissolved organic carbon and for suspended-sediment concentrations. Water samples were analyzed for a suite of 61 current-use and organochlorine pesticides using gas chromatography/mass spectrometry. A total of 25 pesticides were detected in the water samples, with seven pesticides detected in more than half of the samples. Dissolved concentrations of pesticides observed in this study ranged from below their respective method detection limits to 8,940 nanograms per liter (EPTC). The most frequently detected compounds in the water samples were chlorpyrifos, DCPA, EPTC, and trifluralin, which were observed in more than 75 percent of the samples. The maximum concentrations of most pesticides were detected in samples from the Alamo River. Maximum dissolved concentrations of carbofuran, chlorpyrifos, diazinon, and malathion exceeded aquatic life benchmarks established by the U.S. Environmental Protection Agency for these pesticides. Suspended sediments were analyzed for 87 current-use and organochlorine pesticides using microwave-assisted extraction, gel permeation chromatography for sulfur removal, and either carbon/alumina stacked solid-phase extraction cartridges or deactivated Florisil for removal of matrix interferences. Twenty current-use pesticides were detected in the suspended

  9. 西藏拉萨河谷地土壤中的暗色丝孢菌%Soil dematiaceous hyphomycetes from Lhasa River Valley, Tibet, China

    Institute of Scientific and Technical Information of China (English)

    耿月华; 张天宇

    2010-01-01

    A total of 38 isolates of soil dernatiaceous hyphomycetes belonging to 25 species in 15 genera were obtained from 17 soil samples in the Lhasa River Valley. Among them, Gliomastix tibetensis, Monodictys tibetensis and Phialomyces microsporus are new species. Chrysosporium keratinophilum is a new record for China. The other 21 species previously known from China are also included.All descriptions and illustrations provided were based on Chinese isolates. The holotype and isotype specimens are deposited in the Herbarium of Sbandong Agricultural University: Plant Pathology (HSAUP) and the Herbarium Mycologieum, Academiae Sinicae (HMAS), respectively. The other specimens are kept in HSAUP.%从采自拉萨河谷地的17份土样中,分离获得38个暗色丝孢菌分离物,经鉴定分别属于15属中的25种,其中包括3个新种,即西藏粘鞭霉Gliomastix tibetensis,西藏单格孢Monodictys tibetensis和小孢瓶梗霉Phialomyces microsporus,1个中国新记录种嗜毛金色孢Chrysosporium keratinophilum.对新种和中国新记录种进行了描述和图示,对其他21个中国已报道种作了分离地点和生境的引证.主模式和等模式标本(干制培养物)分别保藏在山东农业大学植物病理学标本室(HSAUP)和中国科学院菌物标本馆(HMAS).其余研究过的标本(干制培养物)与活菌种保存在HSAUP.

  10. Interdecadal Modulation of the Influence of La Ni(n)a Events on Mei-yu Rainfall over the Yangtze River Valley

    Institute of Scientific and Technical Information of China (English)

    WANG Xin; WANG Dongxiao; ZHOU Wen; LI Chongyin

    2012-01-01

    The aim of this study was to investigate changes in the relationship between mei-yu rainfall over East China and La Ni(n)a events in the late 1970s,a period concurrent with the Pacific climate shift,using meiyu rainfall data and the National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis.This relationship was modulated by the climate shift:Before the 1977/1978 climate shift and after the 1992/1993 climate shift,mei-yu rainfall levels were above normal in most La Ni(n)a years,whereas during the period 1979-1991,mei-yu rainfall was usually below normal levels in La Ni(n)a years.Both composite analyses and results from an atmospheric general circulation model show remarkable detail in terms of La Ni(n)a's impacts on mei-yu rainfall in the late 1970s due to the change in the mean climatic state over the tropical Pacific.After the late 1970s.the tropical Pacific SSTs were warmer,and the mean state of low-level anticyclone circulation over the western North Pacific (WNP) weakened.Superimposed on La Ni(n)a related cyclonic anomaly over the WNP.anticyclonic circulation weakened.Prior to the late 1970s,the mean state of low-level anticyclone circulation over the WNP was stronger and was less affected by La Ni(n)a-related anomalous cyclones.Anticyclone circulation may have brought moisture to the Yangtze River valley,leading to above-normal rainfall.

  11. Factors influencing temporal changes in chemical composition of biogenic deposits in the middle Tążyna River Valley (Kuyavian Lakeland, central Poland)

    Science.gov (United States)

    Okupny, Daniel; Rzepecki, Seweryn; Borówka, Ryszard Krzysztof; Forysiak, Jacek; Twardy, Juliusz; Fortuniak, Anna; Tomkowiak, Julita

    2016-06-01

    The present paper discusses the influence of geochemical properties on biogenic deposits in the Wilkostowo mire near Toruń, central Poland. The analysed core has allowed the documentation of environmental changes between the older part of the Atlantic Period and the present day (probably interrupted at the turn of the Meso- and Neoholocene). In order to reconstruct the main stages in the sedimentation of biogenic deposits, we have used stratigraphic variability of selected litho-geochemical elements (organic matter, calcium carbonate, biogenic and terrigenous silica, macro- and micro-elements: Na, K, Mg, Ca, Fe, Mn, Cu, Zn, Pb, Cr and Ni). The main litho-geochemical component is CaCO3; its content ranges from 4.1 per cent to 92 per cent. The variability of CaCO3 content reflects mainly changes in hydrological and geomorphological conditions within the catchment area. The effects of prehistoric anthropogenic activities in the catchment of the River Tążyna, e.g., the use of saline water for economic purposes, are recorded in a change from calcareous gyttja into detritus-calcareous gyttja sedimentation and an increased content of lithophilous elements (Na, K, Mg and Ni) in the sediments. Principal component analysis (PCA) has enabled the distinction the most important factors that affected the chemical composition of sediments at the Wilkostowo site, i.e., mechanical and chemical denudation processes in the catchment, changes in redox conditions, bioaccumulation of selected elements and human activity. Sediments of the Wilkostowo mire are located in the direct vicinity of an archaeological site, where traces of intensive settlement dating back to the Neolithic have been documented. The settlement phase is recorded both in lithology and geochemical properties of biogenic deposits which fill the reservoir formed at the bottom of the Parchania Canal Valley.

  12. Warm season heavy rainfall events over the Huaihe River Valley and their linkage with wintertime thermal condition of the tropical oceans

    Science.gov (United States)

    Li, Laifang; Li, Wenhong; Tang, Qiuhong; Zhang, Pengfei; Liu, Yimin

    2016-01-01

    Warm season heavy rainfall events over the Huaihe River Valley (HRV) of China are amongst the top causes of agriculture and economic loss in this region. Thus, there is a pressing need for accurate seasonal prediction of HRV heavy rainfall events. This study improves the seasonal prediction of HRV heavy rainfall by implementing a novel rainfall framework, which overcomes the limitation of traditional probability models and advances the statistical inference on HRV heavy rainfall events. The framework is built on a three-cluster Normal mixture model, whose distribution parameters are sampled using Bayesian inference and Markov Chain Monte Carlo algorithm. The three rainfall clusters reflect probability behaviors of light, moderate, and heavy rainfall, respectively. Our analysis indicates that heavy rainfall events make the largest contribution to the total amount of seasonal precipitation. Furthermore, the interannual variation of summer precipitation is attributable to the variation of heavy rainfall frequency over the HRV. The heavy rainfall frequency, in turn, is influenced by sea surface temperature anomalies (SSTAs) over the north Indian Ocean, equatorial western Pacific, and the tropical Atlantic. The tropical SSTAs modulate the HRV heavy rainfall events by influencing atmospheric circulation favorable for the onset and maintenance of heavy rainfall events. Occurring 5 months prior to the summer season, these tropical SSTAs provide potential sources of prediction skill for heavy rainfall events over the HRV. Using these preceding SSTA signals, we show that the support vector machine algorithm can predict HRV heavy rainfall satisfactorily. The improved prediction skill has important implication for the nation's disaster early warning system.

  13. Out-of-phase decadal changes in boreal summer rainfall between Yellow-Huaihe River Valley and southern China around 2002/2003

    Science.gov (United States)

    Ha, Yao; Zhong, Zhong; Chen, Haishan; Hu, Yijia

    2016-07-01

    This study investigates the decadal variability of rainfall over China in boreal summer (June-August) since the early 1990s. Results show that the rainfall experiences an abrupt decadal change at around 2002/2003. The decadal change is statistically significant and characterized by an out-of-phase pattern between southern China (SC) and the Yellow-Huaihe River Valley (YHRV). The rainfall over SC decreases during the decade 2003-2012 compared to that in the preceding decade 1993-2002. A simultaneous decadal increase in rainfall has occurred over the YHRV. Meanwhile, a significant sea surface temperature warming appears over the western Pacific Ocean and the northern Indian Ocean after 2002 on the decadal time scale. Further analysis reveals that enhanced convections are activated over the tropical regions between 130°E and 160°E and west of 80°E due to the SST anomalies, which induce the dry air in an area of anomalous subsidence located over SC and the northern South China Sea (SCS) via zonal circulation. Accompanied by the anomalous descending flow over the northern SCS, tropical cyclone (TC) activities in the SCS also experience a concurrent decadal reduction. The decrease in landfall TCs contributes to the decadal decrease in SC rainfall since 2003. Corresponding to the anomalous descending motion that is dominant south of 30°N, an anomalous moist ascending flow develops over the YHRV at around 35°N. Meanwhile, the western Pacific subtropical high becomes stronger and extends further westward during 2003-2012, leading to enhanced moisture transport by the southwesterly in the northwestern flank of subtropical high. As a result, more precipitation occurs over the YHRV. The above analysis has revealed the physical-dynamical processes involved in the decadal changes in rainfall over China. The mechanisms behind the out-of-phase pattern of rainfall changes between SC and the YHRV that occurred at 2002/2003 are explored.

  14. Sedimentos arcillosos en un suelo del valle inferior del río Colorado (Argentina Clay sediments in a soil of the lower Colorado river valley (Argentina

    Directory of Open Access Journals (Sweden)

    Norman Peinemann

    2008-12-01

    Full Text Available Se describe la presencia de capas sedimentarias ricas en minerales de arcilla en un subsuelo del valle inferior del río Colorado por su importancia para el régimen hídrico de suelos bajo riego. Difractogramas de rayos X efectuados sobre la fracción arcilla fina de estos sedimentos revelaron que está compuesta por smectitas con muy buena cristalización. La caracterización fisicoquímica del perfil de suelo mostró que el fuerte incremento de minerales de arcilla en el subsuelo estuvo vinculado con un aumento de pH y PSI y en consecuencia una marcada disminución en la conductividad hidráulica, motivo por el cual la eventual presencia de estas capas sedimentarias debe ser muy tenida en cuenta en la programación de las prácticas de riego para evitar el posible deterioro de los suelos.The presence of sedimentary clay layers in subsoils of the lower Colorado river valley are described due to their impact on the water balance of soils under irrigation. X-ray difractograms of the fine clay fraction of these sediments show that they are composed of smectites with a very good crystallization. The physicochemical characterization of the soil profile indicates that the abrupt increase of clay minerals was associated with high pH and ESP values as well as a sharp decrease in hydraulic conductivity. Therefore, the presence of sedimentary clay layers in soils has to be considered when planning irrigation practices to avoid soil degradation.

  15. Riqueza y diversidad de especies leñosas del bosque tropical caducifolio El Tarimo, Cuenca del Balsas, Guerrero Richness and diversity of woody species in the tropical dry forest of El Tarimo, Cuenca del Balsas, Guerrero

    Directory of Open Access Journals (Sweden)

    Fernando Pineda-García

    2007-06-01

    Full Text Available Se describe la composición florística, la riqueza y la diversidad de especies de un bosque tropical caducifolio en la provincia florística Cuenca del Balsas, México. Se seleccionaron 4 sitios de 1000 m² cada uno, censándose los árboles, arbustos y lianas con d.a.p. >1 cm. En total se registraron 1456 individuos, pertenecientes a 82 especies, 56 géneros y 24 familias. Independientemente del sitio y de la forma de crecimiento, Leguminosae fue la familia con mayor número de especies y de individuos. Los géneros más diversos fueron Bursera (Burseraceae y Cordia (Boraginaceae con 9 y 4 especies, respectivamente. La riqueza entre los sitios varió de 43 a 55 especies y su similitud fue más alta en el nivel de familia que en el de especie. Los árboles fueron la forma de crecimiento con mayor riqueza de especies. Respectoa otros bosques tropicales caducifolios de México y del mundo, los sitios que se estudiaron en este bosque ocupan una posición baja en cuanto a sus valores de riqueza y estructura.Floristic composition, species richness, and diversity of the seasonally dry tropical forest in the floristic province of the Balsas Depression, México, is described. We sampled four 1,000 m² sites and recorded species and dbh of trees, shrubs and lianas >1 cm dbh. Data from 1,456 individuals were recorded, representing 82 species, 56 genera, and 24 families. Independently of site or growth form, Leguminosae was the family with the highest number of species and individuals. Bursera (Burseraceae and Cordia (Boraginaceae were the most speciose genera, with nine and four species, respectively. Species richness among sites ranged from 43-55 species and their similarity was higher at the family level than the species level. Trees had higher numbers of species than shrubs and lianas. Our results indicate that these forests have low values of species richness and structure attributes in relation with other tropical dry forests of Mexico and the world.

  16. Spring migration ecology of the mid-continent sandhill crane population with an emphasis on use of the Central Platte River Valley, Nebraska

    Science.gov (United States)

    Krapu, Gary L.; Brandt, David A.; Kinzel, Paul J.; Pearse, Aaron T.

    2014-01-01

    We conducted a 10-year study (1998–2007) of the Mid-Continent Population (MCP) of sandhill cranes (Grus canadensis) to identify spring-migration corridors, locations of major stopovers, and migration chronology by crane breeding affiliation (western Alaska–Siberia [WA–S], northern Canada–Nunavut [NC–N], west-central Canada–Alaska [WC–A], and east-central Canada–Minnesota [EC–M]). In the Central Platte River Valley (CPRV) of Nebraska, we evaluated factors influencing staging chronology, food habits, fat storage, and habitat use of sandhill cranes. We compared our findings to results from the Platte River Ecology Study conducted during 1978–1980. We determined spring migration corridors used by the breeding affiliations (designated subpopulations for management purposes) by monitoring 169 cranes marked with platform transmitter terminals (PTTs). We also marked and monitored 456 cranes in the CPRV with very high frequency (VHF) transmitters to evaluate length and pattern of stay, habitat use, and movements. An estimated 42% and 58% of cranes staging in the CPRV were greater sandhill cranes (G. c. tabida) and lesser sandhill cranes (G. c. canadensis), and they stayed for an average of 20 and 25 days (2000–2007), respectively. Cranes from the WA–S, NC–N, WC–A, and EC–M affiliations spent an average of 72, 77, 52, and 53 days, respectively, in spring migration of which 28, 23, 24, and 18 days occurred in the CPRV. The majority of the WA–S subpopulation settled in the CPRV apparently because of inadequate habitat to support more birds upstream, although WA–S cranes accounted for >90% of birds staging in the North Platte River Valley. Crane staging duration in the CPRV was negatively correlated with arrival dates; 92% of cranes stayed >7 days. A program of annual mechanical removal of mature stands of woody growth and seedlings that began in the early 1980s primarily in the main channel of the Platte River has allowed distribution of crane

  17. Geochemical correlation and 40Ar/39Ar dating of the Kern River ash bed and related tephra layers: Implications for the stratigraphy of petroleum-bearing formations in the San Joaquin Valley, California

    Science.gov (United States)

    Baron, D.; Negrini, R.M.; Golob, E.M.; Miller, D.; Sarna-Wojcicki, A.; Fleck, R.J.; Hacker, B.; Erendi, A.

    2008-01-01

    The Kern River ash (KRA) bed is a prominent tephra layer separating the K and G sands in the upper part of the Kern River Formation, a major petroleum-bearing formation in the southern San Joaquin Valley (SSJV) of California. The minimum age of the Kern River Formation was based on the tentative major-element correlation with the Bishop Tuff, a 0.759??0.002 Ma volcanic tephra layer erupted from the Long Valley Caldera. We report a 6.12??0.05 Ma 40Ar/39Ar date for the KRA, updated major-element correlations, trace-element correlations of the KRA and geochemically similar tephra, and a 6.0??0.2 Ma 40Ar/39Ar age for a tephra layer from the Volcano Hills/Silver Peak eruptive center in Nevada. Both major and trace-element correlations show that despite the similarity to the Bishop Tuff, the KRA correlates most closely with tephra from the Volcano Hills/Silver Peak eruptive center. This geochemical correlation is supported by the radiometric dates which are consistent with a correlation of the KRA to the Volcano Hills/Silver Peak center but not to the Bishop Tuff. The 6.12??0.05 Ma age for the KRA and the 6.0??0.2 Ma age for the tephra layer from the Volcano Hills/Silver Peak eruptive center suggest that the upper age of the Kern River Formation is over 5 Ma older than previously thought. Re-interpreted stratigraphy of the SSJV based on the new, significantly older age for the Kern River Formation opens up new opportunities for petroleum exploration in the SSJV and places better constraints on the tectonostratigraphic development of the SSJV. ?? 2007 Elsevier Ltd and INQUA.

  18. Tecnologia alternativa para a quebra de dormência das sementes de pau-de-balsa (Ochroma lagopus Sw., Bombacaceae Alternative technology for breaking dormancy of balsa wood (Ochroma lagopus Sw., Bombacaceae seeds

    Directory of Open Access Journals (Sweden)

    Antenor P. Barbosa

    2004-01-01

    Full Text Available Este trabalho, teve como objetivo estudar a germinação das sementes de pau-de-balsa (Ochroma lagopus Sw., Bombacaceae em diferentes estágios de maturação aparente dos frutos; a germinação das sementes provenientes de árvores com diferentes diâmetros a altura do peito (DAP e a germinação das sementes tratadas para quebra de dormência. No primeiro experimento, avaliou-se a germinação das sementes dos frutos verdes, verdosos (verde amarelado, negros (fruto fechado e negros deiscentes (fruto aberto com painas expostas. No segundo, a germinação das sementes de árvores da mesma idade e com diferentes DAP's: pequeno (5,4 cm, médio (9,1 cm e grande (13,2 cm. No terceiro, a germinação das sementes com diferentes quebra de dormência: testemunha; água por 24 e 48 horas; água a 80ºC até esfriar; H2SO4 por ½ e 1 minuto com e sem paina; queima da paina em peneira metálica; e semeio de sementes com a paina. As sementes germinaram em gerbox sobre papel de filtro, em câmara de germinação, nas temperaturas de 20ºC, 30ºC e 25ºC, no primeiro, segundo e terceiro experimentos, respectivamente. As sementes de pau-de-balsa germinaram melhor e mais rápido quando coletadas de frutos negros a negros deiscentes, ou quando coletadas de árvores com menor e médio diâmetros, ou quando tratadas com água quente a 80ºC até esfriar, ou com ácido sulfúrico por ½ ou 1 minuto com ou sem paina. Os tratamentos com ácido tem a vantagem de quebrar a dormência da semente e dissolver a paina. As sementes recém colhidas e germinadas não apresentaram dormência tegumentar.The objective of this study was to evaluate the germination of "pau-de-balsa" (Ochroma lagopus Sw., Bombacaceae seed as a function of maturation stages of fruits, the germination of seeds harvested from trees with different diameters at height breast (DBH, and the germination of seed with different treatments to break dormancy. In the first experiment, the germination of seeds

  19. The quality of our Nation's waters: water quality in the Mississippi embayment-Texas coastal uplands aquifer system and Mississippi River Valley alluvial aquifer, south-central United States, 1994-2008

    Science.gov (United States)

    Kingsbury, James A.; Barlow, Jeannie R.; Katz, Brian G.; Welch, Heather L.; Tollett, Roland W.; Fahlquist, Lynne S.

    2015-01-01

    About 8 million people rely on groundwater from the Mississippi embayment—Texas coastal uplands aquifer system for drinking water. The Mississippi River Valley alluvial aquifer also provides drinking water for domestic use in rural areas but is of primary importance to the region as a source of water for irrigation. Irrigation withdrawals from this aquifer are among the largest in the Nation and play a key role in the economy of the area, where annual crop sales total more than $7 billion. The reliance of the region on both aquifers for drinking water and irrigation highlights the importance of long-term management to sustain the availability and quality of these resources.

  20. Lowland river systems - processes, form and function

    DEFF Research Database (Denmark)

    Pedersen, M. L.; Kronvang, B.; Sand-Jensen, K.;

    2006-01-01

    Present day river valleys and rivers are not as dynamic and variable as they used to be. We will here describe the development and characteristics of rivers and their valleys and explain the background to the physical changes in river networks and channel forms from spring to the sea. We seek to ...

  1. Petrogenesis, geochronology, and tectonic significance of granitoids in the Tongshan intrusion, Anhui Province, Middle-Lower Yangtze River Valley, eastern China

    Science.gov (United States)

    Zhang, Zhi-Yu; Du, Yang-Song; Teng, Chuan-Yao; Zhang, Jing; Pang, Zhen-Shan

    2014-01-01

    The Tongshan copper deposit in Anhui Province is a typical mid-sized skarn and porphyry type deposit in the Anqing-Guichi district along the Middle-Lower Yangtze River Valley, eastern China. The Tongshan intrusion is closely related to this mineralization. The intrusion mainly comprises rocks that are quartz diorite porphyry, quartz monzonite porphyry, and granodiorite porphyry. Plagioclase in these rocks is mostly andesine (An = 31.0-42.9), along with minor oligoclase. Biotite is magnesium-rich [Mg/(Mg + Fe) = 0.52-0.67] and aluminum-poor (Al2O3 = 12.32-14.09 wt.%), and can be classified as magnesio-biotite. Hornblende is TiO2-poor ( 0.60], and is magnesio-hornblende or edenite. The SHRIMP zircon U-Pb age of the quartz monzonite porphyry is 145.1 ± 1.2 Ma, which corresponds to the middle Yanshanian period. Whole-rock geochemical results show that the rocks are silica-rich (SiO2 = 60.23-66.23 wt.%) and alkali-rich (K2O + Na2O = 4.97-8.72 wt.%), and low in calcium (CaO = 2.61-5.66 wt.%). Trace element results show enrichments in large ion lithophile element (e.g., K, Rb, and Ba) and depletions in some high field strength elements (e.g., Nb, Ta, P, and Ti). The total rare earth element (REE) content of the rocks is low (ΣREE 10] and small positive Eu anomalies (average δEu = 1.16). These mineralogical, geochronological, and geochemical results show that the intrusion has a mixed crust-mantle source. The Tongshan intrusion was formed by multiple emplacements of crustally contaminated basaltic magma generated by varying degrees of partial melting of enriched lithospheric mantle and lower crust. Hornblende thermobarometry yielded magmatic crystallization temperatures of 652-788 °C and an average crystallization pressure of 1.4 kbar, which corresponds to a depth of approx. 4.7 km. Biotite thermobarometry yielded similar temperatures and lower pressures of 735-775 °C and 0.6 kbar (depth 2.1 km), respectively. The parental magma had a high oxygen fugacity and was

  2. Geological, geochronological, and mineralogical constraints on the genesis of the Chengchao skarn Fe deposit, Edong ore district, Middle-Lower Yangtze River Valley metallogenic belt, eastern China

    Science.gov (United States)

    Yao, Lei; Xie, Guiqing; Mao, Jingwen; Lü, Zhicheng; Zhao, Caisheng; Zheng, Xianwei; Ding, Ning

    2015-04-01

    The Edong ore district is located within the westernmost Middle-Lower Yangtze River Valley metallogenic belt (MLYRB), and hosts the largest concentration of skarn Fe deposits in China, although the origin of these deposits remains controversial. The Chengchao deposit is the largest skarn Fe deposit so far discovered within the MLYRB, and provides a good opportunity to address the debate surrounding the origin of these skarn Fe deposits. Here, we present geological, geochronological, and mineralogical data from the Chengchao skarn deposit and associated intrusions, and discuss the relationships between granitoids and mineralization in the Chengchao deposit. The NW-SE-striking orebodies in the study area have porphyritic quartz monzonite and/or granite footwalls, and Triassic marble or diorite hangingwalls, indicating a spatial relationship between these intrusions and Fe mineralization. Zircon U-Pb data from the granite, porphyritic quartz monzonite, diorite, and porphyritic diabase dike within the deposit show ages of 129 ± 1, 128 ± 1, 140 ± 1, and 126 ± 1 Ma, respectively. These ages and the previously reported ages on the timing of mineralization suggest that the porphyritic quartz monzonite and granite are coeval with the formation of the skarn Fe deposit. Our data confirm that the granitic rocks are temporally associated with Fe mineralization. The prograde substage of skarn development is characterized by two stages of andradite (Adr98-38Grs61-2Prp2-0Sps1-0Alm1-0) and diopside (Di95-61Hd37-5Jo3-0), including an early stage of garnet and pyroxene formation that is genetically associated with the mineralization. The early stage garnets are more andradite-rich (Adr98-50Grs49-2Prp1-0Sps1-0Alm0) than the late veinlet garnets characterized by intermediate grandite compositions (Adr67-37Grs61-31Prp2-0Sps1-0Alm1-0). The early stage pyroxenes (Di95-74Hd26-5Jo1-0) are compositionally distinct from the late stage pyroxenes (Di84-61Hd37-16Jo3-0). Compositional

  3. Comparison of land-atmosphere interaction at different surface types in the mid- to lower reaches of the Yangtze River valley

    Science.gov (United States)

    Guo, Weidong; Wang, Xueqian; Sun, Jianning; Ding, Aijun; Zou, Jun

    2016-08-01

    The mid- to lower reaches of the Yangtze River valley are located within the typical East Asian monsoon zone. Rapid urbanization, industrialization, and development of agriculture have led to fast and complicated land use and land cover change in this region. To investigate land-atmosphere interaction in this region where human activities and monsoon climate have considerable interaction with each other, micrometeorological elements over four sites with different surface types around Nanjing, including urban surface at Dangxiao (hereafter DX-urban), suburban surface at Xianling (XL-suburb), and grassland and farmland at Lishui County (LS-grass and LS-crop), are analyzed and their differences are revealed. The impacts of surface parameters of different surface types on the radiation budget and land surface-atmosphere heat, water, and mass exchanges are investigated and compared. The results indicate the following. (1) The largest differences in daily average surface air temperature (Ta), surface skin temperature (Ts), and relative humidity (RH), which are found during the dry periods between DX-urban and LS-crop, can be up to 3.21 °C, 7.26 °C, and 22.79 %, respectively. The diurnal ranges of the above three elements are the smallest at DX-urban and the largest at LS-grass, XL-suburb, and LS-crop. (2) Differences in radiative fluxes are mainly reflected in upward shortwave radiation (USR) that is related to surface albedo and upward longwave radiation (ULR) that is related to Ts. When comparing four sites, it can be found that both the smallest USR and the largest ULR occur at the DX-urban site. The diurnal variation in ULR is same as that of Ts at all four sites. (3) The differences in daily average sensible heat (H) and latent heat (LE) between DX-urban and LS-crop are larger than 45 and 95 Wm-2, respectively. The proportion of latent heat flux in the net radiation (LE/Rn) keeps increasing with the change in season from the spring to summer. (4) Human activities

  4. The Role of Non-Formal Education in Rural Development: A 10-year Case Study of the Cauca River Valley, Colombia.

    Science.gov (United States)

    Garcia, Alvardo Pedrosa

    1980-01-01

    Details several agricultural and health development programs initiated during the past decade in the Cauca Valley in Colombia. Introduced through nonformal educational strategies making use of media, these programs have had mixed results. (LLS)

  5. Revised geologic cross sections of parts of the Colorado, White River, and Death Valley regional groundwater flow systems, Nevada, Utah, and Arizona

    Science.gov (United States)

    Page, William R.; Scheirer, Daniel S.; Langenheim, V.E.; Berger, Mary A.

    2006-01-01

    This report presents revisions to parts of seven of the ten cross sections originally published in U.S. Geological Survey Open-File Report 2006-1040. The revisions were necessary to correct errors in some of the original cross sections, and to show new parts of several sections that were extended and (or) appended to the original section profiles. Revisions were made to cross sections C-C', D-D', E-E', F-F', G-G', I-I', and J-J', and the parts of the sections revised or extended are highlighted below the sections on plate 1 by red brackets and the word "revised," or "extended." Sections not listed above, as well as the interpretive text and figures, are generally unchanged from the original report. Cross section C-C' includes revisions in the east Mormon Mountains in the east part of the section; D-D' includes revisions in the Mormon Mesa area in the east part of the section; E-E' includes revisions in the Muddy Mountains in the east part of the section; F-F' includes revisions from the Muddy Mountains to the south Virgin Mountains in the east part of the section; and J-J' includes some revisions from the east Mormon Mountains to the Virgin Mountains. The east end of G-G' was extended about 16 km from the Black Mountains to the southern Virgin Mountains, and the northern end of I-I' was extended about 45 km from the Muddy Mountains to the Mormon Mountains, and revisions were made in the Muddy Mountains part of the original section. This report contains 10 interpretive cross sections and an integrated text describing the geology of parts of the Colorado, White River, and Death Valley regional groundwater flow systems in Nevada, Utah, and Arizona. The primary purpose of the report is to provide geologic framework data for input into a numerical groundwater model. Therefore, the stratigraphic and structural summaries are written in a hydrogeologic context. The oldest rocks (basement) are Early Proterozoic metamorphic and intrusive crystalline rocks that are considered

  6. Analysis of the influence of tectonics on the evolution valley network based on the SRTM DEM and the relationship of automatically extracted lineaments and the tectonic faults, Jemma River basin, Ethiopia

    Science.gov (United States)

    Kusák, Michal

    2016-04-01

    The Ethiopian Highland is good example of high plateau landscape formed by combination of tectonic uplift and episodic volcanism (Kazmin, 1975; Pik et al., 2003; Gani et al., 2009). Deeply incised gorges indicate active fluvial erosion which leads to instabilities of over-steepened slopes. In this study we focus on Jemma River basin which is a left tributary of Abay - Blue Nile to assess the influence of neotectonics on the evolution of its river and valley network. Tectonic lineaments, shape of valley networks, direction of river courses and intensity of fluvial erosion were compared in six subregions which were delineate beforehand by means of morphometric analysis. The influence of tectonics on the valley network is low in the older deep and wide canyons and in the and on the high plateau covered with Tertiary lava flows while younger upper part of the canyons it is high. Furthermore, the coincidence of the valley network with the tectonic lineaments differs in the subregions. The fluvial erosion along the main tectonic zones (NE-SW) direction made the way for backward erosion possible to reach far distant areas in E for the fluvial erosion. This tectonic zone also separates older areas in the W from the youngest landscape evolution subregions in the E, next to the Rift Valley. We studied the functions that can automatically extract lineaments in programs ArcGIS 10.1 and PCI Geomatica. The values of input parameters and their influence of the final shape and number of lineaments. A map of automated extracted lineaments was created and compared with 1) the tectonic faults by Geology Survey of Ethiopia (1996); and 2) the lineaments based on visual interpretation of by the author. The comparation of lineaments by automated visualization in GIS and visual interpretation of lineaments by the author proves that both sets of lineaments are in the same azimuth (NE-SW) - the same direction as the orientation of the rift. But it the mapping of lineaments by automated

  7. 基于遥感技术的陕西省渭河流域污染演变研究%Research on contamination evolution in Weihe River valley in Shaanxi province based on remote sensing technology

    Institute of Scientific and Technical Information of China (English)

    李思; 崔晨风; 梁宁

    2013-01-01

    Water pollution is one of the great issues in todays society. The paper analyzed the application of remote sensing technology especially with NDVI and water quality change trend in Weihe River valley in Shaanxi Province. The result indicated that water quality is one of the important factors which influence the growth of plants. The extremum of vegetation index went down in Weihe River valley, witch reflected that water quality turned into integral downtrend from 1998 to 2008 and pollution is more serious on high levels. The paper confirmed the feasibility of remote sensing technology to conduct water quality monitoring.%水污染是当今社会面临的一个重大问题.论文应用遥感技术,以NDVI为指标,对陕西省渭河流域水质变化趋势进行了分析.结果表明:水质是影响植物生长的重要的因素之一.渭河流域的植被指数极值下降,反映出渭河流域的水质从1998年到2008年整体呈下降趋势,污染日趋严重,且污染程度居高不下.证实了遥感技术进行水质监测的可行性.

  8. Triterpenes, Phenols, and Other Constituents from the leaves of Ochroma pyramidale(Balsa Wood, Bombacaceae). Preferred Conformations of 8-C-b-D-Glucopyranosyl-apigenin (vitexin)

    OpenAIRE

    Erika Vázquez; Esteban M. Martínez; Juan Antonio Cogordán; Guillermo Delgado

    2002-01-01

    Lupeol, oleanolic acid, stigmasterol, b-sitosterol, b- sitosteryl-b-D-glucopyranoside, catechin, epi-catechin, and 8-C-b-Dglucopyranosylapigenin (vitexin) were isolated from the acetonic extract of the leaves of Ochroma pyramidale(balsa wood, Bombacaceae), a tree noted by its exceedingly light wood. 1H and 13C NMR of 8-C-b-D-glucopyranosyl-apigenin (vitexin) at room temperature exhibited doubling of some signals, suggesting the presence of atropisomers. 1H NMR spectra at 70 °C showed one set ...

  9. EL GÉNERO FICUS (MORACEAE) EN LA PROVINCIA BIOGEOGRÁFICA DE LA DEPRESIÓN DEL BALSAS, MÉXICO

    OpenAIRE

    NAHÚ GONZÁLEZ-CASTAÑEDA; GUADALUPE CORNEJO-TENORIO; GUILLERMO IBARRA-MANRÍQUEZ

    2010-01-01

    Con base en colectas de campo, revisión de literatura florística y taxonómica, así como en la revisión de ejemplares depositados en diversos herbarios se registraron 11 especies de Ficus (Moraceae) en la Provincia Biogeográfica de la Depresión del Balsas. Las especies registradas pertenecen a los subgéneros Pharmacosycea (F. insipida y F. maxima) y Urostigma (F. citrifolia, F. cotinifolia, F. crocata, F. membranacea, F. obtusifolia, F. pertusa, F. petiolaris, F. pringlei y F. velutina), y en ...

  10. 历史时期长江流域农业生态变迁述论%A Study of Change in Agro-Ecology in Yangtze River Valley from Historical Perspective

    Institute of Scientific and Technical Information of China (English)

    惠富平; 李琦珂

    2011-01-01

    The ecological changes of the Yangtze River Valley in history,such as those in the climate,soil,water,forest vegetation and other environmental factors,have been closely linked with the human social activities,particularly with the agricultural activities of rice production as its center.On the one hand,the ecological environment has been limiting the development of rice agriculture;on the other hand,agricultural activities can exert certain effects on the ecological environment to some extent.Since Song Dynasty and Yuan Dynasty,the lager-scale agricultural economic development mainly focusing on land reclamation around lakes and from hills in the south in China has gradually had great negative influence on the ecological environment of the Yangtze River Valley,resulting in soil erosion,silting rivers and lakes,and frequent floods and droughts.At the same time,the agricultural production and people's lives,therefore,have been subject to great harm.In modern times,the economic development of the Yangtze River Valley has been further strengthened in a broad and deep sense,leading to serious river and lake silt waste,the increasing forest destruction and the severe chemical contamination of soil and water environment.Fortunately,the government has paid great attention to these problems,which have also aroused the public attention.The Yangtze River Valley is the cradle of Chinese rice civilization and the main place of rice production in china.Here,the study on the relationship between the changes of environmental factors and the development of rice agriculture will pose important academic significance to the protection of the regional ecological environment and the sustainable development of local agriculture.%历史时期长江流域气候、水土和森林植被等生态环境要素的变迁,与人类活动尤其是以稻空大点作生产为中心的农业活动有密切关系。一方面生态环境制约着稻作农业的发展变化,另一方面,农业活动

  11. Simulation of climate change in San Francisco Bay Basins, California: Case studies in the Russian River Valley and Santa Cruz Mountains

    Science.gov (United States)

    Flint, Lorraine E.; Flint, Alan L.

    2012-01-01

    As a result of ongoing changes in climate, hydrologic and ecologic effects are being seen across the western United States. A regional study of how climate change affects water resources and habitats in the San Francisco Bay area relied on historical climate data and future projections of climate, which were downscaled to fine spatial scales for application to a regional water-balance model. Changes in climate, potential evapotranspiration, recharge, runoff, and climatic water deficit were modeled for the Bay Area. In addition, detailed studies in the Russian River Valley and Santa Cruz Mountains, which are on the northern and southern extremes of the Bay Area, respectively, were carried out in collaboration with local water agencies. Resource managers depend on science-based projections to inform planning exercises that result in competent adaptation to ongoing and future changes in water supply and environmental conditions. Results indicated large spatial variability in climate change and the hydrologic response across the region; although there is warming under all projections, potential change in precipitation by the end of the 21st century differed according to model. Hydrologic models predicted reduced early and late wet season runoff for the end of the century for both wetter and drier future climate projections, which could result in an extended dry season. In fact, summers are projected to be longer and drier in the future than in the past regardless of precipitation trends. While water supply could be subject to increased variability (that is, reduced reliability) due to greater variability in precipitation, water demand is likely to steadily increase because of increased evapotranspiration rates and climatic water deficit during the extended summers. Extended dry season conditions and the potential for drought, combined with unprecedented increases in precipitation, could serve as additional stressors on water quality and habitat. By focusing on the

  12. Significant cooling effect on the surface due to soot particles over Brahmaputra River Valley region, India: An impact on regional climate.

    Science.gov (United States)

    Tiwari, S; Kumar, R; Tunved, P; Singh, S; Panicker, A S

    2016-08-15

    Black carbon (BC) is an important atmospheric aerosol constituent that affects the climate by absorbing (directly) the sunlight and modifying cloud characteristics (indirectly). Here, we present first time yearlong measurements of BC and carbon monoxide (CO) from an urban location of Guwahati located in the Brahmaputra River valley (BRV) in the northeast region of India from 1st July 2013 to 30th June 2014. Daily BC concentrations varied within the range of 2.86 to 11.56μgm(-3) with an annual average of 7.17±1.89μgm(-3), while, CO varied from 0.19 to 1.20ppm with a mean value of 0.51±0.19ppm during the study period. The concentrations of BC (8.37μgm(-3)) and CO (0.67ppm) were ~39% and ~55% higher during the dry months (October to March) than the wet months (April to September) suggesting that seasonal changes in meteorology and emission sources play an important role in controlling these species. The seasonal ΔBC/ΔCO ratios were highest (lowest) in the pre-monsoon (winter) 18.1±1.4μgm(-3)ppmv(-1) (12.6±2.2μgm(-3)ppmv(-1)) which indicate the combustion of biofuel/biomass as well as direct emissions from fossil fuel during the pre-monsoon season. The annual BC emission was estimated to be 2.72Gg in and around Guwahati which is about 44% lower than the mega city 'Delhi' (4.86Gg). During the study period, the annual mean radiative forcing (RF) at the top of the atmosphere (TOA) for clear skies of BC was +9.5Wm(-2), however, the RF value at the surface (SFC) was -21.1Wm(-2) which indicates the net warming and cooling effects, respectively. The highest RF at SFC was in the month of April (-30Wm(-2)) which is coincident with the highest BC mass level. The BC atmospheric radiative forcing (ARF) was +30.16 (annual mean) Wm(-2) varying from +23.1 to +43.8Wm(-2). The annual mean atmospheric heating rate (AHR) due to the BC aerosols was 0.86Kday(-1) indicates the enhancement in radiation effect over the study region. The Weather Research and Forecasting model

  13. Significant cooling effect on the surface due to soot particles over Brahmaputra River Valley region, India: An impact on regional climate.

    Science.gov (United States)

    Tiwari, S; Kumar, R; Tunved, P; Singh, S; Panicker, A S

    2016-08-15

    Black carbon (BC) is an important atmospheric aerosol constituent that affects the climate by absorbing (directly) the sunlight and modifying cloud characteristics (indirectly). Here, we present first time yearlong measurements of BC and carbon monoxide (CO) from an urban location of Guwahati located in the Brahmaputra River valley (BRV) in the northeast region of India from 1st July 2013 to 30th June 2014. Daily BC concentrations varied within the range of 2.86 to 11.56μgm(-3) with an annual average of 7.17±1.89μgm(-3), while, CO varied from 0.19 to 1.20ppm with a mean value of 0.51±0.19ppm during the study period. The concentrations of BC (8.37μgm(-3)) and CO (0.67ppm) were ~39% and ~55% higher during the dry months (October to March) than the wet months (April to September) suggesting that seasonal changes in meteorology and emission sources play an important role in controlling these species. The seasonal ΔBC/ΔCO ratios were highest (lowest) in the pre-monsoon (winter) 18.1±1.4μgm(-3)ppmv(-1) (12.6±2.2μgm(-3)ppmv(-1)) which indicate the combustion of biofuel/biomass as well as direct emissions from fossil fuel during the pre-monsoon season. The annual BC emission was estimated to be 2.72Gg in and around Guwahati which is about 44% lower than the mega city 'Delhi' (4.86Gg). During the study period, the annual mean radiative forcing (RF) at the top of the atmosphere (TOA) for clear skies of BC was +9.5Wm(-2), however, the RF value at the surface (SFC) was -21.1Wm(-2) which indicates the net warming and cooling effects, respectively. The highest RF at SFC was in the month of April (-30Wm(-2)) which is coincident with the highest BC mass level. The BC atmospheric radiative forcing (ARF) was +30.16 (annual mean) Wm(-2) varying from +23.1 to +43.8Wm(-2). The annual mean atmospheric heating rate (AHR) due to the BC aerosols was 0.86Kday(-1) indicates the enhancement in radiation effect over the study region. The Weather Research and Forecasting model

  14. The 20-30-day oscillation of the global circulation and heavy precipitation over the lower reaches of the Yangtze River valley

    Institute of Scientific and Technical Information of China (English)

    YANG QiuMing

    2009-01-01

    Based on the observational data in summer, the variations of intraseasonal oscillation (ISO) of the daily rainfall over the lower reaches of the Yangtze River valley (LYRV) were studied by using the non-integer spectrum analysis. The NCEP/NCAR reanalysis data for the period of 1979-2005 were analyzed by principal oscillation pattern analysis (POP) to investigate the spatial and temporal characteristics of principal ISO patterns of the global circulation. The relationships of these ISO patterns to the rainfall ISO and the heavy precipitation process over LYRV were also discussed. It is found that the rainfall over LYRV in May-August is mainly of periodic oscillations of 10-20, 20-30 and 60-70 days, and the interannual variation of the intensity of its 20-30-day oscillation has a strongly positive correlation with the number of the heavy precipitation process. Two modes (POP1, POP2) are revealed by POP for the 20-30-day oscillation of the global 850 hPa geopotential height. One is a circumglobal telecon-nection wave train in the middle latitude of the Southern Hemisphere (SCGT) with an eastward propa-gation, and the other is the southward propagation pattern in the tropical western Pacific (TWP). The POP modes explain 7.72% and 7.66% of the variance, respectively. These two principal ISO patterns are closely linked to the low frequency rainfall and heavy precipitation process over LYRV, in which the probability for the heavy precipitation process over LYRV is 54.9% and 60.4% for the positive phase of the imaginary part of POP1 and real part of POP2, respectively. Furthermore, the models of the global atmospheric circulation for the 20-30-day oscillation in association with or without the heavy pre-cipitation process over LYRV during the Northern Hemisphere summer are set up by means of the composite analysis method. Most of the heavy precipitation processes over LYRV appear in Phase 4 of SCGT or Phase 6 of TWP. When the positive phases of 20-30-day oscillations for

  15. The 20―30-day oscillation of the global circulation and heavy precipitation over the lower reaches of the Yangtze River valley

    Institute of Scientific and Technical Information of China (English)

    2009-01-01

    Based on the observational data in summer, the variations of intraseasonal oscillation (ISO) of the daily rainfall over the lower reaches of the Yangtze River valley (LYRV) were studied by using the non-integer spectrum analysis. The NCEP/NCAR reanalysis data for the period of 1979―2005 were analyzed by principal oscillation pattern analysis (POP) to investigate the spatial and temporal characteristics of principal ISO patterns of the global circulation. The relationships of these ISO patterns to the rainfall ISO and the heavy precipitation process over LYRV were also discussed. It is found that the rainfall over LYRV in May―August is mainly of periodic oscillations of 10―20, 20―30 and 60―70 days, and the interannual variation of the intensity of its 20―30-day oscillation has a strongly positive correlation with the number of the heavy precipitation process. Two modes (POP1, POP2) are revealed by POP for the 20―30-day oscillation of the global 850 hPa geopotential height. One is a circumglobal telecon-nection wave train in the middle latitude of the Southern Hemisphere (SCGT) with an eastward propagation, and the other is the southward propagation pattern in the tropical western Pacific (TWP). The POP modes explain 7.72% and 7.66% of the variance, respectively. These two principal ISO patterns are closely linked to the low frequency rainfall and heavy precipitation process over LYRV, in which the probability for the heavy precipitation process over LYRV is 54.9% and 60.4% for the positive phase of the imaginary part of POP1 and real part of POP2, respectively. Furthermore, the models of the global atmospheric circulation for the 20―30-day oscillation in association with or without the heavy pre-cipitation process over LYRV during the Northern Hemisphere summer are set up by means of the composite analysis method. Most of the heavy precipitation processes over LYRV appear in Phase 4 of SCGT or Phase 6 of TWP. When the positive phases of 20―30-day

  16. Valley of the Brahmaputra, India

    Science.gov (United States)

    2002-01-01

    In this true-color MODIS image from October 23, 2001, the semi-arid Tibetan Plateau (upper left) meets up with the Himalayas to the south. From the heights of the Himalayas, snow-covered on their northern flanks, and lush with vegetation to the south, numerous rivers, brown with churned up sediment, flow into the valley of the Brahmaputra River in Assam, India. The Brahmaputra turns southward at the border of Bangladesh and is soon joined by the Ganges River, flowing in from image left. The mighty river splits into numerous channels as it runs out toward the Bay of Bengal, giving the region the name 'Mouths of the Ganges.' Vast amounts of sediment are being emptied into the Bay by the river, and greenish blue swirls could be a mixture of sediment and phytoplankton. Image courtesy Jacques Descloitres, MODIS Land Rapid Response Team at NASA GSFC

  17. Contribution of Soil Fauna to Foliar Litter-Mass Loss in Winter in an Ecotone between Dry Valley and Montane Forest in the Upper Reaches of the Minjiang River.

    Directory of Open Access Journals (Sweden)

    Yan Peng

    Full Text Available Litter decomposition during winter can provide essential nutrients for plant growth in the subsequent growing season, which plays important role in preventing the expansion of dry areas and maintaining the stability of ecotone ecosystems. However, limited information is currently available on the contributions of soil fauna to litter decomposition during winter in such ecosystems. Therefore, a field experiment that included litterbags with two different mesh sizes (0.04 mm and 3 mm was conducted to investigate the contribution of soil fauna to the loss of foliar litter mass in winter from November 2013 to April 2014 along the upper reaches of the Minjiang River. Two litter types of the dominant species were selected in each ecosystem: cypress (Cupressus chengiana and oak (Quercus baronii in ecotone; cypress (Cupressus chengiana and clovershrub (Campylotropis macrocarpa in dry valley; and fir (Abies faxoniana and birch (Betula albosinensis in montane forest. Over one winter incubation, foliar litter lost 6.0%-16.1%, 11.4%-26.0%, and 6.4%-8.5% of initial mass in the ecotone, dry valley and montane forest, respectively. Soil fauna showed obvious contributions to the loss of foliar litter mass in all of the ecosystems. The highest contribution (48.5%-56.8% was observed in the ecotone, and the lowest contribution (0.4%-25.8% was observed in the montane forest. Compared with other winter periods, thawing period exhibited higher soil fauna contributions to litter mass loss in ecotone and dry valley, but both thawing period and freezing period displayed higher soil fauna contributions in montane forest. Statistical analysis demonstrated that the contribution of soil fauna was significantly correlated with temperature and soil moisture during the winter-long incubation. These results suggest that temperature might be the primary control factor in foliar litter decomposition, but more active soil fauna in the ecotone could contribute more in litter

  18. 基于HA-GGE双标图的长江流域棉花区域试验环境评价%Evaluation of Cotton Regional Trial Environments Based on HA-GGE Biplot in the Yangtze River Valley

    Institute of Scientific and Technical Information of China (English)

    许乃银; 张国伟; 李健; 周治国

    2012-01-01

    The latest heritability adjusted GGE (HA-GGE) biplot analysis was adopted to evaluate cotton regional trial environments (trial locations) in terms of the discriminating ability, representative ability, desirability index and superiority index for cotton lint yield selection in 27 independent sets of cotton variety trials in the Yangtze River Valley during 2000-2010 periods. The results showed that Huanggang, Nanjing and Jinzhou were the most ideal trial environments and therefore were the most effective locations for developing and/or recommending cultivars for broad adaptation selection in the target region. However, Shehong, Jianyang, Xiangyang and Nanyang were not desirable for cotton lint yield selection in the whole regions. The desirable test environments were all located in the middle and lower reaches of the Yangtze River Valley, while among the undesirable test environments Nanyang and Xiangyang were located at the inland Nan-Xiang Basin bordering with the Yellow River Valley in the north, where the first frost came early and temperature declined sharply in the late autumn, and Shehong and Jianyang were located at the mountainous Sichuan Basin in the west area, where cotton planting density was higher and cotton matured earlier. Therefore, this article fully displayed the HA-GGE biplot application efficiency in regional trial environment evaluation and also provided the theory background for the decision-making in national cotton scheme implementation and cotton megaenvironment investigation in the Yangtze River Valley.%采用遗传力校正的GGE (HA-GGE)双标图方法对2000-2010年间27个独立的长江流域棉花品种区域试验的15个试验环境(试验点)在皮棉产量选择上的鉴别力、代表性、理想指数和离优度指数进行分析和综合评价.结果表明,湖北黄冈、江苏南京和湖北荆州是最理想的试验环境,对以长江流域为目标环境的广适性新品种选育和作为区域试验点鉴别理想品

  19. Bedrock geologic map of the Spring Valley, West Plains, and parts of the Piedmont and Poplar Bluff 30'x60' quadrangles, Missouri, including the upper Current River and Eleven Point River drainage basins

    Science.gov (United States)

    Weary, David J.; Harrison, Richard W.; Orndorff, Randall C.; Weems, Robert E.; Schindler, J. Stephen; Repetski, John E.; Pierce, Herbert A.

    2015-01-01

    This map covers the drainage basins of the upper Current River and the Eleven Point River in the Ozark Plateaus physiographic province of southeastern Missouri. The two surface drainage basins are contiguous in their headwaters regions, but are separated in their lower reaches by the lower Black River basin in the southeast corner of the map area. Numerous dye-trace studies demonstrate that in the contiguous headwaters areas, groundwater flows from the Eleven Point River basin into the Current River basin. Much of the groundwater discharge of the Eleven Point River basin emanates from Big Spring, located on the Current River. This geologic map and cross sections were produced to help fulfill a need to understand the geologic framework of the region in which this subsurface flow occurs.

  20. Questa baseline and pre-mining ground-water quality investigation 4. Historical surface-water quality for the Red River Valley, New Mexico, 1965 to 2001

    Science.gov (United States)

    Maest, Ann S.; Nordstrom, D. Kirk; LoVetere, Sara H.

    2004-01-01

    Historical water-quality samples collected from the Red River over the past 35 years were compiled, reviewed for quality, and evaluated to determine influences on water quality over time. Hydrologic conditions in the Red River were found to have a major effect on water quality. The lowest sulfate concentrations were associated with the highest flow events, especially peak, rising limb, and falling limb conditions. The highest sulfate concentrations were associated with the early part of the rising limb of summer thunderstorm events and early snowmelt runoff, transient events that can be difficult to capture as part of planned sampling programs but were observed in some of the data. The first increase in flows in the spring, or during summer thunderstorm events, causes a flushing of sulfide oxidation products from scars and mine-disturbed areas to the Red River before being diluted by rising river waters. A trend of increasing sulfate concentrations and loads over long time periods also was noted at the Questa Ranger Station gage on the Red River, possibly related to mining activities, because the same trend is not apparent for concentrations upstream. This trend was only apparent when the dynamic events of snowmelt and summer rainstorms were eliminated and only low-flow concentrations were considered. An increase in sulfate concentrations and loads over time was not seen at locations upstream from the Molycorp, Inc., molybdenum mine and downstream from scar areas. Sulfate concentrations and loads and zinc concentrations downstream from the mine were uniformly higher, and alkalinity values were consistently lower, than those upstream from the mine, suggesting that additional sources of sulfate, zinc, and acidity enter the river in the vicinity of the mine. During storm events, alkalinity values decreased both upstream and downstream of the mine, indicating that natural sources, most likely scar areas, can cause short-term changes in the buffering capacity of the Red

  1. A Typical Mode of Seasonal Circulation Transition: A Climatic View of the Abrupt Transition from Drought to Flood over the Middle and Lower Reaches of the Yangtze River Valley in the Late Spring and Early Summer of 2011%A Typical Mode of Seasonal Circulation Transition: A Climatic View of the Abrupt Transition from Drought to Flood over the Middle and Lower Reaches of the Yangtze River Valley in the Late Spring and Early Summer of 2011

    Institute of Scientific and Technical Information of China (English)

    ZONG Hai-Feng; BUEH Cholaw; CHEN Lie-Ting; JI Li-Ren; WEI Jie

    2012-01-01

    In this study, the seasonal transition of precipitation over the middle and lower reaches of the Yangtze River Valley (YRV) from late spring to early summer is investigated. The results show that the seasonal transition of precipitation exhibits multi-modes. One of these modes is characterized by an abrupt transition from drought to flood (ATDF) over the middle and lower reaches of the YRV in the seasonal transition of precipita- tion. It is shown that the ATDF event from May to June 2011 is simply one prominent case of the ATDF mode. The ATDF mode exhibits an obvious decadal variability. The mode has occurred more frequently since 1979, and its amplitude has apparently strengthened since 1994. From the climatic view, the ATDF mode configures a typical seasonal circulation transition from winter to summer, for which the winter circulations are prolonged, and the summer circulations with the rainy season are built up early over the YRV.

  2. Probability of Elevated Volatile Organic Compound (VOC) Concentrations in Groundwater in the Eagle River Watershed Valley-Fill Aquifer, Eagle County, North-Central Colorado, 2006-2007

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This raster data set delineates the predicted probability of elevated volatile organic compound (VOC) concentrations in groundwater in the Eagle River watershed...

  3. Report on Red-shouldered Hawk nesting within the Milan Bottoms and Pools 9-16 of the Upper Mississippi River Valley during 1999

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — During our investigations along the Upper Mississippi River during 1999 we located Red-shouldered Hawks (Buteo lineatus) in a total of 32 of the 51 areas searched....

  4. Genetic Damage of Root Tip Cells in Broad Bean Plant (Vicia faba) Induced by Water in Liao River Valley%辽河流域水诱发蚕豆根尖细胞遗传损伤的研究

    Institute of Scientific and Technical Information of China (English)

    张利红; 徐成斌; 陈忠林; 苏丹; 王家懿

    2009-01-01

    以辽河流域12个不同断面的河水为诱变剂,运用蚕豆根尖微核检测技术和染色体畸变实验方法,测定蚕豆根尖细胞的有丝分裂指数、微核率和染色体畸变率.结果表明:不同断面的河水均能降低蚕豆根尖细胞有丝分裂指数,能诱发较高频率的微核和染色体畸变,产生染色体断片、核突起和核碎裂.所有样点微核率和染色体畸变率均高于对照组.根据采样点水质污染指数分析町知,福德店水质属重度污染,东辽河、条子河、红庙子水质属中度污染,招苏台河水质属轻度污染.%Water in 12 sections of Liao River Valley was sampled as mutagen and micronucleus test and chromosome aberration assay were used to detect mitotic index,micronucleus ratio and chromosome aberration ratio of root tip cells in broad bean plant(Viciafaba).Results showed that water in different sections can decrease the mitotic index in Vicia faba root tip ceHs,induce higher raftos of either micronucleus or chromosome aberration and produce chromosomal segments,nuclear protuberances and fragments.Micronucleus ratio and chromosome aberration ratio in different sections were higher than those of the control group.Analysis of pollution index in 12 sections showed that water quality Was graded as heavy pollution in Fudedian River,moderate pollution in Dongliao River,Tiaozi River and Hongmiaozi River and light pollution in Zhaosutai River.

  5. Bees (Hymenoptera: Apidae present in the flowers of the balsa wood Ochroma lagopus Swartz, 1788 - doi: 10.4025/actascibiolsci.v32i4.7103 Bees (Hymenoptera: Apidae present in the flowers of the balsa wood Ochroma lagopus Swartz, 1788 - doi: 10.4025/actascibiolsci.v32i4.7103

    Directory of Open Access Journals (Sweden)

    Deodoro Magno Brighenti

    2010-11-01

    Full Text Available The flower of balsa wood holds about 10 to 15 mL of nectar, which helps attracting pollinating agents, since the genus Ochroma is incapable of self-fertilization. However, a high mortality of bees is observed in these flowers. The present study investigated the frequency and constancy of mortality of the individuals of the family Apidae that fed on nectar from the balsa wood. Data was gathered from June to August 2008, in Lavras – Minas Gerais State, Brazil. In addition, the survival of the Africanized bees that fed on the nectar of this flower was compared to those that fed on 50% aqueous solution of honey. Forty flowers were analyzed, and 949 individuals of the orders Hymenoptera (98.1%, Hemiptera (0.95%, Coleoptera (0.74% and Diptera (0.21% were collected. Most Hymenoptera individuals were bees of the genera Partamona and Trigona (677 individuals, which were considered of constant occurrence. Flowers producing up to 16.7 nectar mL were found. The nectar diet contained 16.44% of total sugar, and resulted in low survival of the bees in laboratory (31.32 ± 2.37 hours, compared to a diet of 50% aqueous solution of honey (112.32 ± 2.03 hours.The flower of balsa wood holds about 10 to 15 mL of nectar, which helps attracting pollinating agents, since the genus Ochroma is incapable of self-fertilization. However, a high mortality of bees is observed in these flowers. The present study investigated the frequency and constancy of mortality of the individuals of the family Apidae that fed on nectar from the balsa wood. Data was gathered from June to August 2008, in Lavras – Minas Gerais State, Brazil. In addition, the survival of the Africanized bees that fed on the nectar of this flower was compared to those that fed on 50% aqueous solution of honey. Forty flowers were analyzed, and 949 individuals of the orders Hymenoptera (98.1%, Hemiptera (0.95%, Coleoptera (0.74% and Diptera (0.21% were collected. Most Hymenoptera individuals were bees of the

  6. On Chishui River Valley mental health status and personality characteristics of the children left behind%赤水河流域留守儿童心理健康状况与人格特征的关系探究

    Institute of Scientific and Technical Information of China (English)

    邵义萍

    2013-01-01

    Chishui River Valley children left behind lack of communication with their parents, as well as a lack of parent-child education and family education, which leads to personality characteristics and mental health compared with normal children with differences. To summarize the author of the main personality characteristics and psychological problems of children left behind in the Red River Basin, and put forward a strategy to improve such situation, hoping to be helpful.%  赤水河流域留守儿童与父母缺乏足够的交流,同时也缺乏亲子教育和家庭教育,这导致其人格特征和心理健康状况与正常儿童相比具有差异性。笔者对赤水河流域留守儿童的主要人格特点和心理问题加以总结,并提出了改善此类状况的策略,希望能有所帮助。

  7. The chemistry of river-lake systems in the context of permafrost occurrence (Mongolia, Valley of the Lakes). Part I. Analysis of ion and trace metal concentrations

    Science.gov (United States)

    Szopińska, Małgorzata; Szumińska, Danuta; Polkowska, Żaneta; Machowiak, Katarzyna; Lehmann, Sara; Chmiel, Stanisław

    2016-07-01

    This study provides a description of water chemistry in river-lake systems located in central Mongolia, at the borderline of permafrost occurrence. The analysis involved water samples collected from two river-lake systems: Baydrag River-Böön Tsagaan Lake system, and Shargalyuut/Tuyn Rivers-Orog Lake system. In the water samples, ions and trace elements were detected and quantified. Additionally, the parameters of pH, electrical conductivity (SEC), total dissolved solids (TDS) and total organic carbon (TOC) were determined. Principal Component Analysis (PCA) was performed on the sample results. Water chemistry is mostly influenced by geochemical and hydrometeorological processes. Permafrost thawing could increase the concentration of nitrogen (NH4+, NO3-) as well as Na+ and Ca2+, Cl- and SO42 -. However, it may also be an effect of other factors such as livestock farming. Seasonal drying out of lakes (e.g., Lake Orog) may also influence water chemistry by deflation of evaporites from exposed lake beds and, at the same time, with lower concentration of chemical compounds in water. The PCA shows that water samples can be divided into two groups. The first group contains lake samples, where water chemistry is shaped by prevailing evaporation processes, whereas the second includes samples from rivers and springs. Water chemistry of the latter is predominantly influenced by geochemical and hydro-meteorological processes.

  8. Wonder Valley

    OpenAIRE

    Hillyard, William

    2013-01-01

    You might have passed through here, maybe. Thought you'd stick to the blue roads, hit the casinos of Vegas by the back way. As you blew through this nowhere corner of the Mojave Desert you might have noticed the rat-trap shacks rotting into the sparse hardscrabble of greasewood scrub. And you'd have thought, "What the hell is this place?" Wonder Valley. Out here, thousands of dilapidated cabins crumble into the desert, each one 12 by 20, an outhouse out back. They sit on a grid of five acre p...

  9. Archaeological salvage excavations at Patoka Lake, Indiana: prehistoric occupations of the upper Patoka River Valley. Research report (final) no. 6, Aug 77-May 80

    Energy Technology Data Exchange (ETDEWEB)

    Munson, C.A.

    1980-03-01

    An archaeological data recovery project at Patoka Lake, Indiana, was aimed toward the goals of providing a cultural-historical base for a little known area of the hill country of south-central Indiana and relating project findings to broader questions about prehistoric man's substance and settlement behaviors. Data for project studies are the result of environmental reconstructions, surface surveys at 192 sites, and salvage excavations at 11 sites. Various studies concern the cultural dimensions of both the excavated sites and the Upper Patoka Valley as a region and are based on the construction of a radiocarbon and artifact chronology, and analyses of tools and debris, features, chert utilization, botanical remains, and site location characteristics. Project findings indicate the bulk of the prehistoric occupation of the Upper Patoka Valley occurred during the Archaic, with major seasonal settlements being made during the Late Archaic, around 3,000 - 1,500 BC. For this period, the French Lick phase is defined, and a model of interregional, seasonally shifting settlements is proposed. Other interregional comparisons are identifying cultural and environmental factors which likely influenced several recognized patterns of regional land use changes between 10,000 BC and AD 1,600.

  10. 黑龙港流域油葵-夏玉米套播高效栽培模式研究%Research of Oil Sunflower and Summer Maize Interplanted Cultivation Mode in Heilonggang River Valley

    Institute of Scientific and Technical Information of China (English)

    李积铭; 宋聪敏; 李爱国; 李和平

    2014-01-01

    For against the serious shortage of groundwater due to drought and over-exploitation in Heilonggang river valley.According to the production and climatic characteristics of the area, within the region two major water-saving crops oil sunflower and summer maize were taking as the materials, the maize sowed on July 5 with rotation was using as control, in the interplanted conditions, the effects of different cultivation mode (60 cm of row spacing, 40 cm +80 cm of narrow and wide row spacing) and different sowing date (June 20, 25 and 30 of maize on economic benefit of unit area were studied.The results showed that in the condition of oil sunflower and summer maize interplanted, using the narrow and wide row spacing and sowed maize on June 25, in which the economic benefit of unit area was highest (40 080 yuan /hm2 ), in Heilonggang river valley, the cultivation mode of oil sunflower and summer maize interplanted could be used to partially replace the wheat and summer maize rotation mode with huge water consumption at present.%针对黑龙港流域干旱少雨、地下水资源由于超量开采而严重匮乏的局面,河北省农林科学院旱作农业研究所立足于黑龙港流域的生产和气候特点,以区域内两大主要节水作物---油葵和夏玉米为试验材料,以7月5日轮作直播玉米为对照,在套播条件下研究了不同种植模式(60 cm 等行距,40 cm +80 cm宽窄行)和玉米不同播期(6月20日、25日和30日)对单位面积经济效益的影响。结果表明:油葵-夏玉米套播时,采用宽窄行种植、6月25日播种玉米,单位面积经济效益最高,达到了40080元/hm2。在黑龙港流域可以采用油葵-夏玉米套播种植模式,部分替代目前耗水量巨大的小麦-夏玉米轮作模式。

  11. Species composition and diversity characteristics of Quercus franchetii communities in dry-hot valley of Jinsha River%金沙江干热河谷锥连栎群落物种组成与多样性特征

    Institute of Scientific and Technical Information of China (English)

    刘方炎; 王小庆; 李昆; 孙永玉; 张志翔; 张春华

    2012-01-01

    金沙江干热河谷元谋段残存的锥连栎群落中植物种类组成较为简单,共发现68种植物,隶属于35科60属,其中,禾本科、蝶形花科、菊科、唇形科等科植物占有较大优势;从植物生活型和功能型来看,群落内以草本植物和多年生植物数量居多,分别占所有植物种类的58.8%和63.2%.不同类型群落中,除了扭黄茅始终为各群落中最为重要的优势种之外,同一草本植物在不同群落中的作用和地位存在较大差异;群落物种多样性及相似性程度较为低下,其Shannon-Weiner指数在1.7~2.6之间,且与群落受干扰程度存在较大关联.%Species composition and diversity characteristics of different Quercus franchetii communities in dry-hot valley of Jinsha River were studied based on the plots data. The results showed that there was a simple plant species composition in remained Q. franchetii communities in Jinsha River dry-hot valley of YuanMou section. In communities,68 plant species were found,which belong to 35 families 60 genera,and Poaceae,Papilionaceae, Asteraceae,and Lamiaceae plants had a large advantage; in the plant life form and functional type,the majority of the plants within communities were herbs and perennials,which occupied respectively 58. 8% and 63. 2%. In Q. franchetii communities , excepted that Heteropogon contortus was eventually the most important dominant species, the same herb in different communities were quite different in the role and status. Simultaneously,Q. franchetii communities had lower species diversity and similarity,and Shannon-Weiner index was between 1. 7 and 2. 6,which was correlated with the degree of disturbance of communities.

  12. An evaluation of the evolution of the latest miocene to earliest pliocene bouse lake system in the lower Colorado river valley, southwestern USA

    Science.gov (United States)

    Spencer, J.E.; Pearthree, P.A.; House, P.K.

    2008-01-01

    The upper Miocene to lower Pliocene Bouse Formation in the lower Colorado River trough of the American Southwest was deposited in three basins - from north to south, the Mohave, Havasu, and Blythe Basins - that were formed by extensional fault ing in the early to middle Miocene. Fossils of marine, brackish, and freshwater organ isms in the Bouse Formation have been interpreted to indicate an estuarine environment associated with early opening of the nearby Gulf of California. Regional uplift since 5 Ma is required to position the estuarine Bouse Formation at present elevations as high as 555 m, where greater uplift is required in the north. We present a compilation of Bouse Formation elevations that is consistent with Bouse deposition in lakes, with an abrupt 225 m northward increase in maximum Bouse elevations at Topock gorge north of Lake Havasu. Within Blythe and Havasu Basins, maximum Bouse elevations are 330 m above sea level in three widely spaced areas and reveal no evidence of regional tilting. To the north in Mohave Basin, numerous Bouse outcrops above 480 m elevation include three widely spaced sites where the Bouse Formation is exposed at 536-555 m. Numerical simulations of initial Colorado River inflow to a sequence of closed basins along the lower Colorado River corridor model a history of lake filling, spilling, evaporation and salt concentration, and outflow-channel incision. The simulations support the plausibility of evaporative concentration of Colorado River water to seawater-level salinities in Blythe Basin and indicate that such salinities could have remained stable for as long as 20-30 k.y. We infer that fossil marine organ isms in the Bouse Formation, restricted to the southern (Blythe) basin, reflect coloniza tion of a salty lake by a small number of species that were transported by birds.

  13. Recalibration of a ground-water flow model of the Mississippi River Valley alluvial aquifer of northeastern Arkansas, 1918-1998, with simulations of water levels caused by projected ground-water withdrawals through 2049

    Science.gov (United States)

    Reed, Thomas B.

    2003-01-01

    A digital model of the Mississippi River Valley alluvial aquifer in eastern Arkansas was used to simulate ground-water flow for the period from 1918 to 2049. The model results were used to evaluate effects on water levels caused by demand for ground water from the alluvial aquifer, which has increased steadily for the last 40 years. The model results showed that water currently (1998) is being withdrawn from the aquifer at rates greater than what can be sustained for the long term. The saturated thickness of the alluvial aquifer has been reduced in some areas resulting in dry wells, degraded water quality, decreased water availability, increased pumping costs, and lower well yields. The model simulated the aquifer from a line just north of the Arkansas-Missouri border to south of the Arkansas River and on the east from the Mississippi River westward to the less permeable geologic units of Paleozoic age. The model consists of 2 layers, a grid of 184 rows by 156 columns, and comprises 14,118 active cells each measuring 1 mile on a side. It simulates time periods from 1918 to 1998 along with further time periods to 2049 testing different pumping scenarios. Model flux boundary conditions were specified for rivers, general head boundaries along parts of the western side of the model and parts of Crowleys Ridge, and a specified head boundary across the aquifer further north in Missouri. Model calibration was conducted for observed water levels for the years 1972, 1982, 1992, and 1998. The average absolute residual was 4.69 feet and the root-mean square error was 6.04 feet for the hydraulic head observations for 1998. Hydraulic-conductivity values obtained during the calibration process were 230 feet per day for the upper layer and ranged from 230 to 730 feet per day for the lower layer with the maximum mean for the combined aquifer of 480 feet per day. Specific yield values were 0.30 throughout the model and specific storage values were 0.000001 inverse-feet throughout

  14. Evolution of Nitrogen, Phosphorus and Potassium Fertilizer Application Rates in Cotton Fields and lts lnfluences on Cotton Yield in the Yangtze River Valley

    Institute of Scientific and Technical Information of China (English)

    Naiyin XU; Jian Ll

    2014-01-01

    Objective] The historical evolution pattern of nitrogen (N), phosphorus (P) and potassium (K) fertilizer application rate and its effects on lint cotton yield were explored to provide the theoretical basis for reasonable fertilizer management strate-gy in the cotton planting region of the Yangtze River Val ey. [Method] GGE biplot analysis method was adopted to analyze the correlation among N, P and K fertilizer application rate and lint cotton yield with the dataset of national cotton regional trials of the Yangtze River Val ey during 1991-2013. The linear and nonlinear regression analysis method was used to reveal the evolution of the fertilizer applying patterns, and analyze the effects of N, P, K application rates on cotton lint yield. [Result] The application rates of N, P and K fertilizer presented highly significant positive corre-lation with lint cotton yield, among which the potassium fertilizer was the strongest relative factor with lint cotton yield, fol owed by phosphorus fertilizer, while nitrogen fertilizer was the weakest factor. The application rate of nitrogen fertilizer was relat-ed with the test year in the pattern of a quadratic function, while phosphate and potassium had progressive increase linear relation with the test year in the cotton planting region of the Yangtze River Val ey. Meanwhile, cotton lint yield was in re-sponse to nitrogen fertilizer content increase with a quadratic parabola function, and increased with the applying phosphate fertilizer and potassium fertilizer content with linearly increasing function. [Conclusion] The increasing application amount of N, P and K fertilizer was general y beneficial to cotton yield improvements, however, ex-orbitant applying nitrogen fertilizer was unfavorable for cotton production, and a reasonable mixture formula of N, P and K fertilizer was better in terms of cotton yield-increasing effect.

  15. Evaluation on the High Yielding, Stability and Comprehensive Performances of Check Cultivars in National Cotton Regional Trials in the Yangtze River Valley

    Institute of Scientific and Technical Information of China (English)

    Shiqiao JIN; Naiyin XU

    2014-01-01

    Objective] This study was to analyze the high yielding, stability, adaptabil-ity and main characteristics of check cultivars in national cotton regional trials in the Yangtze River Val ey in 2000-2013, with the aim to provide theoretical basis for the reasonable selection of check cultivars for cotton regional trials. [Method] GGE biplot analysis method was used to carry out the intensive analysis and comprehensive comparisons on the performances and differences of the 9 major characters of check cultivars, namely, lint cotton yield , stability, and other main traits including bol weight, bol number, lint percentage, fiber length, fiber strength, micronaire val-ue, plant height and seed index. [Result] Ezamian 10 was suitable in the majority of cotton planting regions in the Yangtze River Val ey, with the best high yielding abili-ty and perfect yield stability. The yielding ability of Xiangzamian 8 ranked the sec-ond, but its stability was the poorest. Xiangzamian 8 was of the specific adaptive cultivar with relatively good performance in high yielding but the poorest stability. The suitable planting areas of Xiangzamian 8 were limited to the cotton planting re-gion around Dongting Lake in Hunan province, Poyang Lake in Jiangxi Province, the Coastal region in Jiangsu Province and Wuhan district in Hubei Province. Xi-angzamian 2 performanced poorer in both yielding and stability, while Simian 3 ranked first in stability but the last in yielding ability. The dominant character of Xi-angzamian 8 and Xiangzamian 2 were high cotton plants and big bol s. Simian 3 performanced super in lint percentage and fiber length. Ezamian 10 was strong in cotton bol formation ability, lint cotton yielding, fiber strength and seed size, as wel as high micronaire value. [Conclusion] The outstanding performance of Ezamian 10 in high and stable yield in the Yangtze River Val ey in recent years has effectively promoted the high yielding ability of candidate varieties in cotton regional

  16. 岷江上游干旱河谷旱地土壤斥水性特征初步研究%Preliminary Study on the Characteristics of Soil Repellency in the Dry Valley of Minjiang River

    Institute of Scientific and Technical Information of China (English)

    秦纪洪; 赵利坤; 孙辉; 李沙

    2012-01-01

    土壤斥水性是土壤颗粒不易被水滴浸润的现象,对土壤水分特征曲线、土壤溶质运移、土壤优先流、土壤导水率以及地表径流和土壤侵蚀等具有重要影响。研究结果表明,3月份岷江上游干旱河谷0-5cm土层具斥水性的土壤在空间上的分布概率约为34%,其中强度斥水性土壤分布比例为5%;在时间分布上,土壤斥水性主要表现在7月,轻度以下斥水性概率为91%,强度以上斥水性概率为58%;从各粒级土壤斥水性的研究结果来看,斥水性与土壤粒级呈显著负相关,粒级越小,土壤斥水性越高。因此,岷江上游干旱河谷旱地土壤斥水性具有明显的时空分布差异,并且粒级越小土壤斥水性越强,7月份土壤表层的土壤斥水性强度与分布比例高。这可能是导致干旱河谷严重水土流失、土壤砂砾化的一个重要原因。%Soil water repellency is a widespread hydrologic phenomenon in different soils all over the world,and its implications encompass hysteresis of the water retention curve,unstable wetting fronts with fingered flow,reduced infiltration capacity as compared to wettable soils,and accelerated hillslope runoff and erosion.The results show that probability of 0-5 cm layer of soil with slight and strong repellency is about 34% in total,of which soil with strong water repellency is 5% in the dry valley of Minjiang River in March.In July,the probability of soil with slight and strong repellency is 91%,in which 58% is strong water repellent soil.The results also show that soil water repellency is significantly negatively related to the ratio of soil particle size.It can be concluded that there are apparently temporal and spatial variability for soil water repellency and water repellent soil distribution in the dry valley of Minjiang River.A higher ratio of strong soil water repellency exhibits in July of monsoon in topsoil,and in soil with higher proportion of fine fraction,which may be one of

  17. Quaternary stratigraphy and tectonics, and late prehistoric agriculture of the Safford Basin (Gila and San Simon river valleys), Graham County, Arizona

    Science.gov (United States)

    Houser, Brenda B.; Pearthree, Phillip A.; Homburg, Jeffry A.; Thrasher, Lawrence C.

    2004-01-01

    This guidebook accompanied the 46th annual meeting of the Rocky Mountain Cell of the Friends of the Pleistocene (FOP) and the 2002 Fall Field Trip of the Arizona Geological Society. The meeting and field trip were held in the Safford Basin, southeastern Arizona. The Friends of the Pleistocene is an informal gathering of Quaternary geologists, geomorphologists, and pedologists who meet annually for a field conference. The first part of the guidebook consists of road logs with descriptions of stops covering the three days of the field trip. An overview of the geology of the Safford Basin is given in Stop 1-1. The second part of the guidebook consists of four short papers that discuss adjacent areas or that expand upon the road log descriptions of the field trip stops. The first paper by Reid and Buffler is a summary of upper Cenozoic depositional facies in the Duncan Basin, the first basin to the east of the Safford Basin. The next three papers expand upon (1) the soil study of the gridded field agricultural complex (Stop 2-3, Homburg and Sandor), (2) the vertebrate fossils of the San Simon Valley in the southeastern part of the Safford Basin (Stop 3-1, Thrasher), and (3) paleoIndian irrigation systems and settlements in Lefthand Canyon at the foot of the Pinaleno Mountains (Stop 3-2, Neely and Homburg).

  18. 萨拉乌苏河流域萨拉乌苏组砂丘砂沉积特征%Sedimentary characteristics of paleo-aeolian dune sands of Salawusu Formation in the Salawusu River Valley

    Institute of Scientific and Technical Information of China (English)

    欧先交; 杨艺; 刘宇飞; 李保生; 靳鹤龄; 董光荣; 章典; 吴正; 温小浩; 曾兰华; 欧阳椿陶

    2008-01-01

    The Salawusu Formation of Milanggouwan section in Salawusu River Valley in-cludes 7 layers of paleo-mobile dune sands, and 4 layers of paleo-fixed and semi-fixed dune sands. Their structures have been observed and their grain size, surface textural features and several main chemical elements have been analyzed. The results showed that: 1) Some of the aeolian structural characteristics of these dune sands are similar to that of the recent dune sands. 2) They are also similar to the recent dune sands in grain size components, and pa-rameters of Mz, σ, Sk and Kg, as well as in several main chemical components. 3) The scattergrams of Mz-σ and SiO2--Al2O3+TOFE and the probability curves of grain size showed that these paleo-dune sands are different from paleosols and fluvio-lacustrine facies, but are consistency with recent dune sands. 4) Quartz sands have well roundness and surface tex-tural features such as dish-shaped pits, crescent-shaped pits, pockmarked pits, upturnedcleavage plates, siliceous precipitates and siliceous crevasses, indicating that they had been carried for a long time by the wind. As the 11 layers of paleo-dune sands possess the aeolian characteristics in structure, grain size, surface textural features and chemical elements, the origin of their formation should be attributed to eolation.

  19. Holocene alluvial fills in the South Loup Valley, Nebraska

    Science.gov (United States)

    May, David W.

    1989-07-01

    Four Holocene alluvial fills are present in Nebraska's South Loup River valley. Fill IV, the oldest and thickest, was deposited between 10,200 and 4800 14C yr B.P.; Fill III has an age of about 3000 14C yr B.P.; Fill II is younger than 2100 and older than 900 14C yr B.P.; and Fill I is younger than 900 14C yr B.P. Regional contemporaneity of valley alluviation in the eastcentral Great Plains suggests that climate has controlled long-term sediment storage in the South Loup River valley.

  20. Avaliação de desempenho ambiental em uma balsa guindaste e de lançamento – BGL

    Directory of Open Access Journals (Sweden)

    Hélio Soibelman

    2009-06-01

    -para-margin-bottom:.0001pt; mso-pagination:widow-orphan; font-size:10.0pt; font-family:"Times New Roman"; mso-ansi-language:#0400; mso-fareast-language:#0400; mso-bidi-language:#0400;} Com o objetivo de auxiliar os gestores de Meio Ambiente de embarcações de obras submarinas na avaliação do desempenho de seus Sistemas de Gestão, e com fundamentação nos princípios da norma ABNT NBR ISO 14001:2004 (Sistema de Gestão Ambiental, bem como em criteriosa pesquisa bibliográfica, o presente trabalho, apresenta uma metodologia que se baseia no que preceitua o item Planejamento da ABNT NBR ISO 14001:2004 de que os objetivos, as metas ambientais e seus indicadores devem estar diretamente relacionados aos aspectos e impactos significativos. Foi realizada uma pesquisa de campo com a finalidade de demonstrar a aplicabilidade da metodologia criada. Esta pesquisa foi desenvolvida em uma Balsa Guindaste e de Lançamento (BGL, utilizada em obras de engenharia. Vale ressaltar que a BGL é um ativo muito importante da empresa estudada, pois ela, além de atuar em lançamentos de dutos rígidos para escoar a produção de óleo e gás, também atua em instalações de plataformas e de grandes estruturas submarinas.

  1. Saline Valley

    Science.gov (United States)

    2001-01-01

    [figure removed for brevity, see original site] [figure removed for brevity, see original site] Figure 1 Figure 2 These images of the Saline Valley area, California, were acquired March 30, 2000 and cover a full ASTER scene (60 by 60 km). Each image displays data from a different spectral region, and illustrates the complementary nature of surface compositional information available as a function of wavelength. This image displays visible and near infrared bands 3, 2, and 1 in red, green, and blue (RGB). Vegetation appears red, snow and dry salt lakes are white, and exposed rocks are brown, gray, yellow and blue. Rock colors mainly reflect the presence of iron minerals, and variations in albedo. Figure 1 displays short wavelength infrared bands 4, 6, and 8 as RGB. In this wavelength region, clay, carbonate, and sulfate minerals have diagnostic absorption features, resulting in distinct colors on the image. For example, limestones are yellow-green, and purple areas are kaolinite-rich. Figure 2 displays thermal infrared bands 13, 12 and 10 as RGB. In this wavelength region, variations in quartz content appear as more or less red; carbonate rocks are green, and mafic volcanic rocks are purple. The image is located at 36.8 degrees north latitude and 117.7 degrees west longitude. The U.S. science team is located at NASA's Jet Propulsion Laboratory, Pasadena, Calif. The Terra mission is part of NASA's Science Mission Directorate.

  2. 三河口水利枢纽工程坝址区河谷应力场分析研究%In-situ Stress in the River Valley of Dam Site of Sanhekou Hydro-Junction

    Institute of Scientific and Technical Information of China (English)

    赵宪民; 尹健民; 李永松; 周春华

    2013-01-01

    Sanhekou Hydro-junction project is located in the river valley of east Qinling area. Complex geological structure and topography determines the complexity of in-situ stress distribution. To investigate the distribution of in-situ stress, hydraulic fracturing test was carried out on 3 boreholes in the slopes of both abutments and the river bed. Measured results show that the stress values are relatively large in buried depth of 0-50m in borehole at the river bed, and elevation of 500-530m in the boreholes at both banks, which can be designated as increased stress zone. Meanwhile, the area of buried depth under 50m in the borehole of river bed and elevation under 500m in the boreholes of both banks can be designated as original stress zone. In the shallow rockmass under the riverbed, the orientation of maximum horizontal principal stress is nearly perpendicular to the river trend, and with the increase of burial depth, it is close to the direction of regional structure. In the surface rockmass of slope, the direction of maximum horizontal principal stress intersects with the river trend at an small angle, and with the increase of burial depth, it transits to the northeast gradually. In deep buried rock mass, the direction of maximum horizontal principal stress is close to the regional tectonic.%三河口水利枢纽工程地处东秦岭地区的河谷地段,复杂地质结构和复杂地形地貌决定了工程区地应力分布的复杂性.为了研究其地应力分布情况,采用水压致裂法在左右坝肩边坡和河床部位3个钻孔进行现场地应力测量.测试结果表明:河床部位测孔埋深0~50 m及两岸边坡测孔500 ~ 530 m高程岩体应力量值较大,可划为应力增高区;而河床测孔埋深50 m以下和边坡测孔500 m高程以下,可归为原岩应力区;河床浅部岩体最大水平主应力方位与河流走向基本垂直,随着埋深的增加而向区域构造方位靠近;边坡浅层岩体最大水平主应力方

  3. Interglacial Extension of the Boreal Forest Limit in the Noatak Valley, Northwest Alaska: Evidence from an Exhumed River-Cut Bluff and Debris Apron

    Science.gov (United States)

    Edwards, M.E.; Hamilton, T.D.; Elias, S.A.; Bigelow, N.H.; Krumhardt, A.P.

    2003-01-01

    Numerous exposures of Pleistocene sediments occur in the Noatak basin, which extends for 130 km along the Noatak River in northwestern Alaska. Nk-37, an extensive bluff exposure near the west end of the basin, contains a record of at least three glacial advances separated by interglacial and interstadial deposits. An ancient river-cut bluff and associated debris apron is exposed in profile through the central part of Nk-37. The debris apron contains a rich biotic record and represents part of an interglaciation that is probably assignable to marine-isotope stage 5. Pollen spectra from the lower part of the debris apron closely resemble modern samples taken from the Noatak floodplain in spruce gallery forest, and macrofossils of spruce are also present at this level. Fossil bark beetles and carpenter ants occur higher in the debris apron. Mutual Climatic Range (MCR) estimates from the fossil beetles suggest temperatures similar to or warmer than today. Together, these fossils indicate the presence of an interglacial spruce forest in the western part of the Noatak Basin, which lies about 80 km upstream of the modern limit of spruce forest.

  4. Analysis of genetic diversity among seven goat populations in the middle and lower valley of Yangtse River and southeast coastal regions in China

    Institute of Scientific and Technical Information of China (English)

    WANG Zhiguo; YANG Zhangping; MA Yuehui; WANG Qinghua; MAO Yongjiang; CHANG Hong; ZHOU Qunlan; XU Ming

    2007-01-01

    The genomes of seven native goat populations were screened by using microsatellites as molecular markers;the populations were Yichang white,Matou,Xiangdong black,Fuqing,Daiyun,Huanghuai and Yangtse River Delta white goats.A total of 23 microsatellite markers were used and genetic diversities and genetic distances were also determined.The results showed that only 21 loci showed polymorphism in all populations.BM0203 was a homozygotic locus in every population,but more than one allele was found among all populations.Alleles of BM6444 were homozygotic in Xiangdong Black and Yichang White goats,but more than one allele was detected in other populations.Average heterozygosity of all populations was 0.819 0,and the mean polymorphism information content (PIC) of all seven populations was 0.630 5-0.691 9.An unweighted pair group method with arithmetic mean (UPGMA) dendrogram was constructed on Nei's standard genetic distance.Matou and Xiangdong black were grouped at first,then Fuqing,Daiyun,Yangtse River Delta white and Huanghuai goats joined them respectively.Finally,Yichang white goats clustered with all of the above.

  5. Questa baseline and pre-mining ground-water quality investigation. 14. Interpretation of ground-water geochemistry in catchments other than the Straight Creek catchment, Red River Valley, Taos County, New Mexico, 2002-2003

    Science.gov (United States)

    Nordstrom, D. Kirk; McCleskey, R. Blaine; Hunt, Andrew G.; Naus, Cheryl A.

    2005-01-01

    The U.S. Geological Survey, in cooperation with the New Mexico Environment Department, is investigating the pre-mining ground-water chemistry at the Molycorp molybdenum mine in the Red River Valley, New Mexico. The primary approach is to determine the processes controlling ground-water chemistry at an unmined, off-site but proximal analog. The Straight Creek catchment, chosen for this purpose, consists of the same Tertiary-age quartz-sericite-pyrite altered andesite and rhyolitic volcanics as the mine site. Straight Creek is about 5 kilometers east of the eastern boundary of the mine site. Both Straight Creek and the mine site are at approximately the same altitude, face south, and have the same climatic conditions. Thirteen wells in the proximal analog drainage catchment were sampled for ground-water chemistry. Eleven wells were installed for this study and two existing wells at the Advanced Waste-Water Treatment (AWWT) facility were included in this study. Eight wells were sampled outside the Straight Creek catchment: one each in the Hansen, Hottentot, and La Bobita debris fans, four in a well cluster in upper Capulin Canyon (three in alluvial deposits and one in bedrock), and an existing well at the U.S. Forest Service Questa Ranger Station in Red River alluvial deposits. Two surface waters from the Hansen Creek catchment and two from the Hottentot drainage catchment also were sampled for comparison to ground-water compositions. In this report, these samples are evaluated to determine if the geochemical interpretations from the Straight Creek ground-water geochemistry could be extended to other ground waters in the Red River Valley , including the mine site. Total-recoverable major cations and trace metals and dissolved major cations, selected trace metals, anions, alkalinity; and iron-redox species were determined for all surface- and ground-water samples. Rare-earth elements and low-level As, Bi, Mo, Rb, Re, Sb, Se, Te, Th, U, Tl, V, W, Y, and Zr were

  6. Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado

    Science.gov (United States)

    Weeks, Edwin P.; Sorey, M.L.

    1973-01-01

    A method to determine evapotranspiration from ground water was tested at four sites in the flood plain of the Arkansas River in Colorado. Approximate ground-water budgets were obtained by analyzing water-level data from observation wells installed in five-point arrays. The analyses were based on finite difference approximations of the differential equation describing ground-water flow. Data from the sites were divided into two groups by season. It was assumed that water levels during the dormant season were unaffected by evapotranspiration of ground water or by recharge, collectively termed 'accretion.' Regression analyses of these data were made to provide an equation for separating the effects of changes in aquifer storage and of aquifer heterogeneity from those due to accretion during the growing season. The data collected during the growing season were thus analyzed to determine accretion.

  7. Ongoing Transmission of Onchocerca volvulus after 25 Years of Annual Ivermectin Mass Treatments in the Vina du Nord River Valley, in North Cameroon.

    Directory of Open Access Journals (Sweden)

    Albert Eisenbarth

    2016-02-01

    Full Text Available Recent reports of transmission interruption of Onchocerca volvulus, the causing agent of river blindness, in former endemic foci in the Americas, and more recently in West and East Africa, raise the question whether elimination of this debilitating disease is underway after long-term treatment of the population at risk with ivermectin. The situation in Central Africa has not yet been clearly assessed.Entomologic data from two former endemic river basins in North Cameroon were generated over a period of 43 and 48 months to follow-up transmission levels in areas under prolonged ivermectin control. Moreover, epidemiologic parameters of animal-borne Onchocerca spp. transmitted by the same local black fly vectors of the Simulium damnosum complex were recorded and their impact on O. volvulus transmission success evaluated. With mitochondrial DNA markers we unambiguously confirmed the presence of infective O. volvulus larvae in vectors from the Sudan savannah region (mean Annual Transmission Potential 2009-2012: 98, range 47-221, but not from the Adamawa highland region. Transmission rates of O. ochengi, a parasite of Zebu cattle, were high in both foci.The high cattle livestock density in conjunction with the high transmission rates of the bovine filaria O. ochengi prevents the transmission of O. volvulus on the Adamawa plateau, whereas transmission in a former hyperendemic focus was markedly reduced, but not completely interrupted after 25 years of ivermectin control. This study may be helpful to gauge the impact of the presence of animal-filariae for O. volvulus transmission in terms of the growing human and livestock populations in sub-Saharan countries.

  8. Comparison of River Terraces in the Middle Reach Valleys of the Yellow River and Analysis on the Multi-Gradational Features of Tectonism in the Formation of Terrace Series

    Institute of Scientific and Technical Information of China (English)

    Xing Chengqi; Ding Guoyu; Lu Yanchou; Shen Xuhui; Tian Qinjian; Yin Gongming; Chai Zhizhang; Wei Kaibo

    2003-01-01

    Where the Yellow River flows through the Haiyuan-Tongxin arc-form tectonic region on thenortheastern side of the Qinghai-Xizang (Tibet) Plateau, as many as 10 ~ 21 basis and erosionterraces have been produced, among which the biggest altitude above river level is 401m andthe formation age of the highest terrace is 1.57 Ma B.P. Based on comparative analysis of theYellow River terraces located separately in the Mijiashan mountain, the Chemuxia gorge, theHeishanxia gorge and the other river terraces in the vast extent of the northern part of China,it has been found that the tectonic processes resulting in the formation of the terrace series isone of multi-gradational features, i.e., a terrace series can include the various terracesproduced by tectonic uplifts of different scopes or scales and different ranks. The Yellow Riverterrace series in the study region can be divided into three grades. Among them, in the firstgrade there are 6 terraces which were formed separately at the same time in the vast extent ofthe northern part of China and represent the number and magnitude of uplift of the Qinghai-Xizang Plateau since 1.6 Ma B. P.; in the second grade there are 5 terraces which wereseparately and simultaneously developed within the Haiyuan-Tianjingshan tectonic region andrepresent the number and magnitude of uplift of this tectonic region itself since 1.6Ma B.P.;in the third grade there are 10 terraces which developed on the eastern slope of the Mijiashanmountain and represent the number and amplitude of uplift of the Haiyuan tectonic belt itselfsince 1. 6Ma B.P. Comparison of the terrace ages with loess-paleosoil sequence has also showedthat the first grade terraces reflecting the vast scope uplifts of the Qinghai-Xizang Plateau arevery comparable with climatic changes and their formation ages all correspond to theinterglacial epochs during which paleosoils were formed. This implies that the vast extenttectonic uplifts resulting in river down-cutting are closely

  9. Winter browse selection by white-tailed deer and implications for bottomland forest restoration in the Upper Mississippi River Valley, USA

    Science.gov (United States)

    Cogger, Benjamin J.; De Jager, Nathan R.; Thomsen, Meredith; Adams, Carrie Reinhardt

    2014-01-01

    White-tailed deer (Odocoileus virginianus) forage selectively, modifying upland forest species composition and in some cases shifting ecosystems to alternative stable states. Few studies, however, have investigated plant selection by deer in bottomland forests. Herbaceous invasive species are common in wetlands and their expansion could be promoted if deer avoid them and preferentially feed on native woody species. We surveyed plant species composition and winter deer browsing in 14 floodplain forest restoration sites along the Upper Mississippi River and tributaries. Tree seedling density declined rapidly with increasing cover of invasive Phalaris arundinacea, averaging less than 1 per m2 in all sites in which the grass was present. Deer browsed ∼46% of available tree seedling stems (branches) at mainland restorations, compared to ∼3% at island sites. Across all tree species, the number of browsed stems increased linearly with the number available and responded unimodally to tree height. Maximum browsing rates were observed on trees with high stem abundances (>10 per plant) and of heights between 50 and 150 cm. Deer preferred Ulmus americana and Acer saccharinum, and avoided Fraxinus pennsylvanica, Acer negundo, and Quercus spp. at mainland sites, and did not browse Phalaris arundinacea if present. Depending on plant growth responses to herbivory and the competitive effects of unbrowsed species, our results suggest that selective foraging could promote the expansion of invasive species and/or alter tree species composition in bottomland forest restorations. Islands may, however, serve as refuges from browsing on a regional scale.

  10. The Preliminary Discussion of the Difference of the Livelihood Models in River Valley Areas during Qijia Culture Period in Qinghai Province%青海河谷地区齐家文化生业模式差异初步探讨

    Institute of Scientific and Technical Information of China (English)

    王倩倩

    2015-01-01

    Many sites of Qijia culture and tombs have been unearthed in recent years ,according to the unearthed archaeological material , this paper chose three typical sites of different river valley areas to process comparative analysis .Through analyzing the means of production and remains of animals which were unearthed from the sites ,it shows that the livelihood models of the ruins of Qijia Culture which are distributed in different river valley areas in Qinghai are different .The production pattern of the Gamatai site at high altitudes in the Yellow River Valley is dominanted by animal husbandry ,combining with agri‐culture and hunting ;The economic pattern of Changning site in the HuangShui valley is dominanted by ag‐riculture ,combining with animal husbandry and hunting ,fishing and hunting ;However ,the economic form of the Jinchankou site in the Datong River Valley is mixed with planting ,hunting and animal hus‐bandry .T he difference of the regional natural resources conditions may be the main reason w hy there are the difference ,meanw hile there may be its ow n factors of culture .%青海省发掘了多处齐家文化遗址和墓葬,根据已发掘的考古资料,本文选择了三个河谷区的典型遗址或墓地进行了对比分析,通过对出土生产工具、动物遗存等分析,表明分布在青海不同河谷区的齐家文化遗址或墓地其生业模式是有差异的,黄河谷地较高海拔的尕马台墓地以畜牧为主、兼有农业与狩猎的生产模式,湟水谷地的长宁遗址则以农业为主,以畜牧狩猎业、渔猎业为辅的混合型经济格局,大通河谷的金禅口遗址是种植业、狩猎和畜牧等多种生产方式的混合经济形态。地域自然资源条件的不同可能是造成这种差异的主要原因,同时可能还有其文化自身的因素。

  11. Planning and execution of Raft River stimulation treatments

    Energy Technology Data Exchange (ETDEWEB)

    Verity, R.V.; Crichlow, H.B. (ed.)

    1980-02-07

    The following topics are discussed for two Raft River Valley wells: well characteristics and treatment objectives, treatment selection and design, treatment history, mechanical arrangements and job costs. (MHR)

  12. 青海省湟水流域红桦林的分布规律%Distribution Law of Betula albo-sinensis Qinghai Huangshui River Valley

    Institute of Scientific and Technical Information of China (English)

    周生华

    2012-01-01

    通过二类资源调查数据总结了青海湟水流域的红桦林的分布及生境、组成与结构、林型、生长规律及更新与演替。调查结果表明:红桦林分布地区气候干湿季分明,分布区海拔2300—2900m;林分结构和组成不稳定且复杂;林型同龄单层纯林居多,主要有为苔草红桦林和灌木红桦林2种,相林不整齐,生长缓慢,树干分叉多枝,干形弯曲,尖削度较大,立木多呈团状分布。林分分层明显,可分为乔木层、下木层、草被层、苔藓层等四个层次;20龄后开始结实,40年后进入盛期,非常有利于天然更新。现有红桦林绝大部分是云杉林被破坏后而形成的次生林,红桦幼树随着年龄的增大,需光量也随之增加,常因不能忍受林内较弱的光照而逐渐衰弱和死亡。属云杉林演替过程中的一个过渡阶段。%Through Two types of resources survey data the paper summarize distribution and habitat, the composition and structure of forest types, growth regulation, and update and succession of Betula albo-sinensis Huangshui valley Qinghai. The survey results show that:distribution of regional climate wet and dry season clearly, the distribution of district elevation 2300-2900 ; stand structure and composition of the instability and complexity; forest types have monolayer pure forest, and shrub birch, forest irregular, slow growth, trunk forked branch, trunk-shaped bend, taper, stump mostly slug distribution. The obvious stand stratification, can be divid- ed into four levels of the tree layer,the understory layer,grass layer, moss layer; strong after 20 age ,40 years after the peak, is very conducive to natural regeneration. Existing birch, most of the spruce forest is destroyed after the formation of secondary forest, with age increases, the required amount of light also increases, often because they can not put up with weak light in the forest and gradually weakened and death

  13. THE ROLE OF THE MALARIA VECTORS IN THE UPPER VALLEY OF MEKONG RIVER IN YUNNAN%云南湄公河流域上游河谷地区疟疾媒介传疟作用研究

    Institute of Scientific and Technical Information of China (English)

    周红宁; 张再兴; 李春富; 吴超; 王丕玉; Chris; Curtis; Nigel; Hill

    2005-01-01

    Objective To study the role of the malaria vectors in the upper valley of Mekong River in Yunnan by studying their seasonal abundance, host preference, biting behaviors and sporozites rates. Methods Mosquitoes were collected by light-traps and human landing catches in villages;sporozoites were detected in the salivary glands under microscopy in the field sites and circumsporozoite proteins (CSP) from mosquito was tested by ELISA. Results A total of 16 Anopheles species were caught in villages. 7 sporozoite positive mosquitoes in the salivary glands were found from 1 010 parous mosquitoes in 7 Anopheles species in the fields;CSP were detected positive in 11 mosquitoes by ELISA out of 5 154 mosquitoes in 8 Anopheles species. sporozoites rate was 0.37%, 0.22% and 0.32% in Anopheles minimus, An. sinensis and An. maculatus respectively (including CSP positive by ELISA and sporozoite positive in the salivary glands), and their entomological inoculation rate was estimated to be 9.82, 3.97 and 2.69 respectively. The biting activity began after dusk and was maintained through the night, but feeding peak of the An. minimus was in the midnight, and that of An. sinensis and An. maculatus occurred before 21:00. The human blood index was over 80% for all 3 mosquitoes. Conclusion It is suggested that An. minimus, An. sinensis and An. maculatus are the most important malaria vectors in the upper valley of Mekong River.%目的通过观察蚊媒季节消长、嗜血习性、叮咬行为和疟疾子孢子率以研究出它们在云南湄公河上游河谷地带传疟作用的关系. 方法村内采取诱蚊灯和人工诱捕方法捕蚊;现场采取显微镜解剖蚊虫的方法观察唾腺子孢子,实验室采用ELISA技术检测蚊虫体内环子孢子蛋白(CSP). 结果村内共捕获16种按蚊.现场显微镜解剖7种按蚊,1 010只经产蚊中,发现了7只唾液腺感染子孢子;ELISA方法检测现场捕回的8种按蚊,5 154只各龄期蚊中,发现11只环子孢子蛋

  14. Recalibration of a ground-water flow model of the Mississippi River Valley alluvial aquifer in Southeastern Arkansas, 1918, with simulations of hydraulic heads caused by projected ground-water withdrawals through 2049

    Science.gov (United States)

    Stanton, Gregory P.; Clark, Brian R.

    2003-01-01

    The Mississippi River Valley alluvial aquifer, encompassing parts of Arkansas, Kentucky, Louisiana, Mississippi, Missouri, and Tennessee supplies an average of 5 billion gallons of water per day. However, withdrawals from the aquifer in recent years have caused considerable drawdown in the hydraulic heads in southeastern Arkansas and other areas. The effects of current ground-water withdrawals and potential future withdrawals on water availability are major concerns of water managers and users as well as the general public. A full understanding of the behavior of the aquifer under various water-use scenarios is critical for the development of viable water-management and alternative source plans. To address these concerns, the U.S. Geological Survey, in cooperation with the U.S. Army Corps of Engineers, Vicksburg District, and the Arkansas Soil and Water Conservation Commission developed and calibrated a ground-water flow model for the Mississippi River valley alluvial aquifer in southeastern Arkansas to simulate hydraulic heads caused by projected ground-water withdrawals. A previously published ground-water flow model for the alluvial aquifer in southeastern Arkansas was updated and recalibrated to reflect more current pumping stresses with additional stress periods added to bring the model forward from 1982 to 1998. The updated model was developed and calibrated with MODFLOW-2000 finite difference numerical modeling and parameter estimation software. The model was calibrated using hydraulic-head data collected during 1972 and 1982 and hydraulic-head measurements made during spring (February to April) of 1992 and 1998. The residuals for 1992 and 1998 have a mean absolute value of 4.74 and 5.45 feet, respectively, and a root mean square error of 5.9 and 6.72 feet, respectively. The effects of projected ground-water withdrawals were simulated through 2049 in three predictive scenarios by adding five additional stress periods of 10 years each. In the three scenarios

  15. Using Native Plants in the Reclamation of Areas Affected of Mining Activities in the Rodrigatos River Valley (El Bierzo, Leon, Spain)

    International Nuclear Information System (INIS)

    It is difficult for sites affected by mining to be colonized by vegetation and thus they suffer a slow recovery to a healthy ecosystem and, as a result, restoration work is necessary. The aim of this report is to propose a set of native species which are conducive to establishing a stable and self-sufficient plant community that will protect the soil and contribute to the rapid integration into the landscape of the areas affected by mining in the upper basin of the river Rodrigatos in the region of El Bierzo (Leon) An analysis of plant communities was undertaken using the phyto sociological method of Braun-Blanquet in order to subsequently select, using ecological criteria, the most suitable species for revegetation. Plant mapping using ortho photos was also developed in order to identify and delineate the location of the different landscape units. Among candidate species, in the first revegetation phase, we suggest a variety of herbs that are able to fix soils and protect them from erosion; species of the genus Cytisus and Genista in areas of moderate slope and species such as Rumex induratus Boiss and Reuter, Erysimum linifolium (Pourr. Ex Pers .) Jay in steeper areas because of their rooting ability. In later stages, the introduction of tree species characteristic for each formation is recommended. Furthermore, in the riverside areas species such as Carex elata subsp.reuteriana (Boiss.) Lucen and Aedo, Alnus glutinosa (L.) and Salix atrocinerea Brot. are proposed for introduction from the fi rst stage onwards. The species proposed in this study include some not commonly used in restoration, so a subsequent more detailed study would be required in order to assess their degree of suitability for this use. (Author) 65 refs.

  16. 近52年太阳活动与江淮梅雨异常关系分析%Analysis of relationship between solar activities and abnormality of plum rains in Changjiang-Huaihe River Valley in recent 52 years

    Institute of Scientific and Technical Information of China (English)

    程国生; 杜亚军; 陈烨

    2012-01-01

    Floods in China mainly occur in the region of Changjiang-Huaihe River Valley. Floods and droughts in June and July are mostly caused by abnormality of plum rains. To study the influence factors of plum rains, the impact of solar activities on plum rains in the region was analyzed based on the data of sunspots and precipitation in the Changjing-Huaihe fiver region during the plum rains period from 1954 to 2005. The results show that, the maximum trend-coefficient of the precipitation of plum rains is located in Hangzhou area, where solar activities has little impact on plum rains. Impact of solar activities on the precipitation and the intensity of plum rains shows obvious regional characteristics in the Changjiang-Huaihe River region. From north to south of the Changjiang-Huaihe River region, the correlations between solar activity and the precipitation of plum rains are negative, positive, and negative, respectively. In anomalous strong solar activity years, precipitation is less in the north and south and more in the middle of the region; while from north to south, the correlations between the solar activity and the intensity of plum rains are positive and negative, i. e. , generally speaking, in anomalous strong solar activity years, the intensity of plum rains is stronger than normal in the north and weaker than normal in the south of the region. Composite analysis results show that, in low solar activity years, the Changjiang-Huaihe River region is prone to have floods.%我国涝灾主要集中在江淮地区,其中6-7月的旱涝,大部分是由梅雨异常引起的。为了研究梅雨的影响因子,利用1954-2005年太阳黑子、江淮地区33站梅雨期降水资料,分析了太阳活动对江淮地区梅雨的影响。研究表明,梅雨量趋势系数的最大值中心位于杭州地区,而太阳活动与杭州地区的梅雨基本上没有关系。太阳活动对江淮地区梅雨量、梅雨强度的影响具有地域性。

  17. 金沙江干热河谷人T林土壤水分研究%A Study on Soil Moisture in Different Plantations in Dry-Hot Valley of Jinsha River

    Institute of Scientific and Technical Information of China (English)

    岳学文; 方海东; 钱坤建; 方晋; 奎建蕊; 潘志贤; 杨艳鲜; 纪中华; 彭辉

    2011-01-01

    以金沙江干热河谷6种人工林为例,采用TRIME-PICO-IPH TDR测定雨季(6-10月)土壤水分,每个样地设3个重复,分析不同人工林内的土壤水分变化特征.罗望子纯林土壤含水量稳定,变异系数小,且含水量较其他人工林高.随着深度的增加,不同人工林之间的土壤含水量差异逐渐变小.根据土壤对降雨的蓄积、利用情况,将0-100cm的土壤剖面分为水分剧烈变化层、弱利用层,草本植物水分利用层、土壤水分微调节层.%Six kinds of plantations in Yuanmou County of Yunnan Province,a typical dry-hot area in the valley of Jinsha River, were selected. Soil moisture was determined with TRIME-PICO-IPH TDR in rainy season (from June to October). Each sample area was selected in triplicate to analysis the variety characteristics of the soil moisture. Soil moisture is vey stable and the variation coefficient is much less in the pure forest of tamarindus indica and its soil moisture content is higher than the others. With the increase of the soil depth,the soil moisture differences among the plantations diminish gradually. The soil profile at 0- 100 cm was divided into 4 layers by saving and using the rainfall of soil, i.e. moisture dramatical-change layer, moisture weak-utilization layer, herbaceous plant moisture utilization layer and soil moisture slight-adjustment layer.

  18. 滇中盆地和金沙江谷地高产水稻的产量形成特点%Yield formation of high yield rice in the middle basin and Jinsha River valley of Yunnan plateau

    Institute of Scientific and Technical Information of China (English)

    路季梅; 杨家庆; 宋令荣; 程在全; 普双有

    2001-01-01

    研究表明,滇中盆地和金沙江谷地高产水稻(10.5~15 t*hm -2)的产量形成特点为:(1)产量结构上具有单位面积穗数多和每穗粒数多的优势,在大群体条件下仍保持高的结实率和大穗优势;(2)水稻的生育期长和高原独特的光温条件有利于植株的稳健生长和产量器官的协调发展;(3)光合速率高,干物质积累量大,库源关系协调。这些特点的形成与高原独特的气候生态条件和栽培管理密切相关。%The characteristics of yield formation of high-yield rice with yield of 10.5-15.0t*hm-2 in the middle basin and Jinsha River valley of Yunnan plateau were studied.The yield formation of high-yield rice in those areas was characterized by the following three aspects:(1)more ears per unit area and more grains per ear,higher seed setting rate and bigger ear;(2)full growth and harmonic development of yield organs due to the long growth duration and favorable photo-thermal conditions in those areas;(3)higher rate of photosynthesis,more dry matter accumulation,and harmonic relation between sink and source.The formation of these characteristics is closely related to the u nique climatic ecological environment in the plateau and the rice cultivation and management.

  19. Creating a catchment perspective for river restoration

    OpenAIRE

    L. Benda; MILLER, D; J. Barquín

    2011-01-01

    One of the major challenges in river restoration is to identify the natural fluvial landscape in catchments with a long history of river control. Intensive land use on valley floors often predates the earliest remote sensing: levees, dikes, dams, and other structures alter valley-floor morphology, river channels and flow regimes. Consequently, morphological patterns indicative of the fluvial landscape including multiple channels, extensive floodplains, wetlands, and fluvial-riparian and tribu...

  20. Influence of the Spring Arctic Oscillation on Midsummer Surface Air Temperature over the Yangtze River Valley%春季北极涛动对盛夏长江流域地表气温的影响

    Institute of Scientific and Technical Information of China (English)

    张乐英; 徐海明; 施宁

    2015-01-01

    本文基于1958至2002年的ERA-40月平均再分析资料,利用年际增量方法分析了春季北极涛动(Arctic Oscillation,简称AO)与我国夏季长江流域地表气温的关系。结果表明,在扣除前期冬季ENSO影响后,5月AO指数与8月长江流域地表气温存在显著正相关。通过回归分析发现,5月AO可通过影响中低纬度的海气相互作用进而影响8月长江流域地表气温。当5月AO处于正位相时,在(10°~15°N)及赤道附近产生异常下沉气流,对应着西太平洋局地Hadley环流减弱,对流层底层出现了异常的反气旋性辐散气流。与之对应,赤道西太平洋地区出现了显著的东风异常。由于该东风异常位于5月气候平均的局地海表面温度(SST)极大值中心位置上,该东风异常可通过平流作用使得高海温不断地向西堆积,最终造成赤道西太平洋SST出现显著正异常。当该SST正异常持续至8月时,它通过 Gill 响应(Gill,1980)在其西北侧激发出气旋性异常环流,它有利于西太平洋副热带高压在我国长江流域的维持,进而造成长江流域地表气温正异常。反之,则相反。%AbstractBased on ERA-40 monthly mean reanalysis data over the period 1958–2002, this paper studies the relationship between the spring Arctic Oscillation (AO) and the summer surface air temperature (SAT) over the Yangtze River valley by adopting the year-to-year increment approach. The winter ENSO signal is filtered out in advance. Results show that the AO in May is significantly and positively correlated with the SAT over the Yangtze River valley in August. The possible physical mechanism for this relationship is investigated by means of regression analysis. The air–ocean interaction over the middle and low latitudes might play an important role. Following a stronger positive AO in May, an anomalous subsidence flow appears over the region 10°–15°N and the Equator

  1. Modeling effects of climatological variability and management practices on conservation of groundwater from the Mississippi River Valley Shallow Alluvial Aquifer in the Mississippi Delta region

    Science.gov (United States)

    Thornton, Robert Frank

    Ninety-eight percent of water taken from the Mississippi River Shallow Alluvial Aquifer, hereafter referred to as "the aquifer" or "MRVA," is used by the agricultural industry for irrigation. Mississippi Delta agriculture is increasingly using more water from the MRVA and the aquifer has been losing about 300,000 acre-feet per year. This research expands on previous work in which a model was developed that simulates the effects of climatic variability, crop acreage changes, and specific irrigation methods on consequent variations in the water volume of the MRVA. This study corrects an identified problem by replacing total growing season precipitation with an irrigation demand driver based on evaporation and crop coefficients and changing the time scale from the entire growing season to a daily resolution. The calculated irrigation demand, as a climatological driver for the model, captures effective precipitation more precisely than the initial growing season precipitation driver. Predictive equations resulting from regression analyses of measured versus calculated irrigation water use showed R2 and correlations of 0.33 and 0.57, 0.77 and 0.88, 0.71 and 0.84, and 0.68 and 0.82 for cotton, corn, soybeans and rice, respectively. Ninety-five percent of the predicted values fall within a range of + or - about 23,000 acre-feet, an error of about 10-percent. The study also adds an additional conservation strategy through the use of surface water from on-farm reservoirs in lieu of groundwater. Analyses show that climate could provide the entire water need of the plants in 70-percent of the years for corn, 65-percent of the years for soybeans and cotton, and even 5-percent of the years for rice. Storing precipitation in on-farm structures is an effective way to reduce reliance of Delta producers on groundwater. If producers adopted, at a minimum, the 97.5:2.5 ratio suggested management practice, this minimal management strategy could potentially conserve 48-percent, 35

  2. Late-glacial to Early Holocene lake basin and river valley formation within Pomeranian moraine belt near Dobbertin (Mecklenburg-Vorpommern, NE Germany)

    Science.gov (United States)

    Zawiska, Izabela; Lorenz, Sebastian; Börner, Andreas; Niessner, Dominique; Słowiński, Michał; Theuerkauf, Martin; Pieper, Hagen; Lampe, Reinhard

    2014-05-01

    In central Mecklenburg-Vorpommern vast areas between the terminal moraine belts of the Frankfurt (W1F) and Pomeranian Phase (W2) were covered by glaciolacustrine basins which were embedded in the outwash plains. With deglaciation of the Pomeranian Phase around 17-18 ka BP the basins north to the villages Dobbertin and Dobbin were part of a glaciofluvial river system in combination with ice-dammed lake basins. During the late-glacial after ~14 ka cal BP the melting of buried dead ice reshaped the lake basin morphology by new depressions, in- and outlets. We study late-glacial basin and landscape development using cores collected along a pipeline trench crossing the Dobbin-Dobbertin basin. Core analysis includes sedimentological (carbon content, grainsize distribution) and palaeoecological (pollen, plant macrofossils, Cladocera) proxies. Radiocarbon dates indicate that peat formation started soon after the start of the Weichselian late-glacial. High resolution analysis of a basal peat layer indicates that initial organic and lacustrine sedimentation started in shallow ponding mires, evolving from buried dead ice sinks in the glaciofluvial sequence, in which telmatic plants (Carex aquatilis, Schoenoplectus lacustris) dominated. Chydorus sphaericus, the only cladocera species recorded, is ubiquitous and can survive in almost all reservoir types in very harsh conditions. Findings of Characeae than point at the formation of shallow lakes. The expansion of rich fen communities, including Scorpidium scorpoides, and a decline in Cladocera diversity show that these lakes soon again terrestrialised with peat formation. The appearance of Alona costata points at a lowering of pH values in that process. A tree trunk of birch (14.2 ka cal. BP) shows that first trees established during this first telmatic period. At this position in the basin, the basal peat layer is covered by minerogenic sediments, which points at a period of higher water levels and fluvial dynamics, possibly

  3. Questa baseline and pre-mining ground-water quality investigation. 5. Well installation, water-level data, and surface- and ground-water geochemistry in the Straight Creek drainage basin, Red River Valley, New Mexico, 2001-03

    Science.gov (United States)

    Naus, Cheryl A.; McCleskey, R. Blaine; Nordstrom, D. Kirk; Donohoe, Lisa C.; Hunt, Andrew G.; Paillet, Frederick L.; Morin, Roger H.; Verplanck, Philip L.

    2005-01-01

    The U.S. Geological Survey, in cooperation with the New Mexico Environment Department, is investigating the pre-mining ground-water chemistry at the Molycorp molybdenum mine in the Red River Valley, northern New Mexico. The primary approach is to determine the processes controlling ground-water chemistry at an unmined, off-site, proximal analog. The Straight Creek drainage basin, chosen for this purpose, consists of the same quartz-sericite-pyrite altered andesitic and rhyolitic volcanic rock of Tertiary age as the mine site. The weathered and rugged volcanic bedrock surface is overlain by heterogeneous debris-flow deposits that interfinger with alluvial deposits near the confluence of Straight Creek and the Red River. Pyritized rock in the upper part of the drainage basin is the source of acid rock drainage (pH 2.8-3.3) that infiltrates debris-flow deposits containing acidic ground water (pH 3.0-4.0) and bedrock containing water of circumneutral pH values (5.6-7.7). Eleven observation wells were installed in the Straight Creek drainage basin. The wells were completed in debris-flow deposits, bedrock, and interfingering debris-flow and Red River alluvial deposits. Chemical analyses of ground water from these wells, combined with chemical analyses of surface water, water-level data, and lithologic and geophysical logs, provided information used to develop an understanding of the processes contributing to the chemistry of ground water in the Straight Creek drainage basin. Surface- and ground-water samples were routinely collected for determination of total major cations and selected trace metals; dissolved major cations, selected trace metals, and rare-earth elements; anions and alkalinity; and dissolved-iron species. Rare-earth elements were determined on selected samples only. Samples were collected for determination of dissolved organic carbon, mercury, sulfur isotopic composition (34S and 18O of sulfate), and water isotopic composition (2H and 18O) during

  4. Study on Climate Characteristics of Seven Great River Valleys and Mechanism of Precipitation Anomaly in July 2011%2011年7月七大江河流域气候特点及降水异常成因分析

    Institute of Scientific and Technical Information of China (English)

    周兵; 王晓敏; 刘秋峰; 王东阡

    2012-01-01

    Based on the precipitation and temperature data at National Climate Centre 723 stations,the JRA-25 and NCEP/NCAR I reanalysis data sets and the NOAA Climate Prediction Centre extended reconstructed SST data,using methods of linear trend,dynamical diagnosis,correlation analysis and wavelet analysis, the climate characteristics and variation features of seven great river valleys(SGRV) in July 2011 were researched,and the mechanism of precipitation anomalies of the Yangtze River Valley(YRV) during the dominant flood season was revealed.Results indicated that the precipitations of SGRV were overall less in July 2011,however,the precipitation of YRV was far less than normal;meanwhile,the temperatures of SGRV were characterized by continued climate warming,especially for Songhua River Valley.The linear trend of precipitation changing showed that Zhujiang River Valley and YRV were in a linearly increased trend,Huaihe River Valley maintained an unchanged condition,and Liaohe,Haihe,Huanghe and Songhua River Valleys where in a linearly decreased trend.In addition to the obvious interannual variability, the decadal changes of precipitation in YRV,Huaihe,Haihe and Huanghe River Valleys were also obvious. The main causes for the below-normal precipitation of YRV in July 2011 were as follows:The atmospheric responses to external forcing of equatorial Middle-Eastern Pacific were the same as those to La Nina pattern;the subtropical high was abnormal and the East Asian southerly wind circulation intensity index(I_(ES)) was weak;besides, the water vapor budget had a deficit and the precipitation efficiency was low.%利用国家气候中心723站降水和气温资料、JRA-25和NCEP/NCAR I再分析资料数据集、NOAA气候预测中心海温资料等,采用线性趋势、动力诊断、相关分析、小波分析等方法,开展2011年7月我国七大江河流域气候特点及其变化特征研究,揭示长江流域主汛期降水异常的

  5. Conservação e vigor de sementes de pau-de-balsa (Ochroma pyramidale Conservation and vigour of balsawood seeds (Ochroma pyramidale

    Directory of Open Access Journals (Sweden)

    Antonio Moçambite Pinto

    2004-01-01

    Full Text Available Ochroma pyramidale, Bombacaceae, conhecida popularmente como pau-de-balsa, é utilizada para construção de jangadas, balsas, salva-vidas, bóias, brinquedos e na fabricação de papel e celulose. O objetivo deste estudo foi definir um método de acondicionamento de sementes de O. pyramidale, visando a conservação da viabilidade e vigor destas para sua utilização e comercialização em épocas de baixa produção. Sementes de O. pyramidale foram embaladas em sacos de papel tipo kraft e sacos de plástico (0,10 mm e armazenadas em ambiente de laboratório (22ºC e 65% U.R., câmara úmida (5ºC e 86% U.R. e câmara seca (15ºC e 40% U.R.. A percentagem de germinação, teor de água e vigor das sementes foram avaliados no início e após períodos de armazenamento. Todos os tratamentos testados foram favoráveis para manutenção do vigor das sementes por 120 dias de armazenamento. As melhores condições de armazenamento para manter a viabilidade por até 400 dias foram: sacos de papel (76,5% de germinação e sacos plásticos (65,5% de germinação em câmara seca, e sacos plásticos em condições de laboratório (63,5% de germinação.Balsawood (Ochroma pyramidale, Bombacaceae is used for construction of rafts, floats, life-savers, buoys, toys and for paper and cellulose production. The objective of this study was to determine a seed storage method for O. pyramidale to conserve seed viability and vigour for use and commercialization during seasonal shortages. Seeds were put in paper (Kraft and plastic bags (0.10 mm, and stored in three environmental conditions: laboratory (22ºC and 65% relative humidity, humid chamber (5ºC and 86% RH and dry chamber (15ºC and 40% RH. Germination percentage, moisture content and vigour of seeds were evaluated at the beginning of the experiment and after the storage periods. All treatments maintained seed vigour for 120 days of storage. The best storage conditions to maintain seed viability for a 400

  6. O Crescimento de duas espécies florestais pioneiras, pau-de-balsa (Ochroma lagopus Sw.) e caroba (Jacaranda copaia D. Don), usadas para recuperação de áreas degradadas pela agricultura na Amazônia Central, Brasil Growth of two forest pioneer species, pau-de-balsa (Ochroma lagopus Sw.) e caroba (Jacaranda copaia D. Don), used for rehabilitation of degraded areas from agriculture in Central Amazon, Brazil

    OpenAIRE

    Antenor Pereira Barbosa; Moacir Alberto Assis Campos; Paulo de Tarso Barbosa Sampaio; Shozo Nakamura; Cláudio de Queiroz Blair Gonçalves

    2003-01-01

    O objetivo deste trabalho foi estudar o crescimento das espécies florestais pioneiras pau-de-balsa (Ochroma lagopus Sw.) e caroba (Jacaranda copaia D. Don) para a recuperação de áreas degradadas pela agricultura. Na área, situada no km 120 da BR-174, tinha sido plantado mandioca e banana e abandonada há 8 anos, formando uma capoeira de porte baixo e rala. O experimento foi instalado em maio/98, com e sem gradagem da área. O espaçamento foi de 3x3m, em covas de 20 cm (diâmetro) x 30 cm (profun...

  7. CO2 concentrations and delta13C (CO2) values in monthly sets of air samples from downtown Parma and the Parma and Taro river valleys, Emilia-Romagna, Italy.

    Science.gov (United States)

    Longinelli, Antonio; Selmo, Enricomaria

    2006-09-01

    Monthly sets of discrete air samples were collected from September 2004 to June 2005 in the town of Parma, along North-South and East-West runs (8 plus 8 samples), using four-litre Pyrex flasks. The CO2 concentrations and delta13C values were determined on these samples with the aim of evaluating quantitatively the contribution of domestic heating to the winter atmospheric CO2 pollution in downtown Parma by comparing autumn and spring atmospheric values with winter values. After separation of CO2 from the other air gases in the laboratory, the CO2 concentrations were calculated from the intensity of the 12C16O2+ ion beam in the mass spectrometer, after calibration with artificial air samples whose CO2 concentration was very carefully determined by the Monte Cimone Observatory (Sestola, Modena, Italy). The reproducibility of these measurements was of approximately +/-0.4 % and, consequently, the most probable error is not higher than+/-2-3 ppmv and does not affect the magnitude of the gradients between different samples. The standard deviation of delta13C measurements ranges from+/-0.02 to +/-0.04 per thousand (1sigma). The results suggest that the contribution of domestic heating to atmospheric CO2 pollution is almost negligible in the case of ground level atmosphere, where the main CO2 pollution is essentially related to the heavy car traffic. This is probably because of the fact that the gases from the domestic heating systems are discharged tens of metres above ground level at a relatively high temperature so that they rise quickly to the upper atmospheric layers and are then displaced by air masses dynamics. Monthly sets of discrete air samples were also collected from October 2004 to June 2005 along North-South runs from the town of Parma to the Apennine ridge following the Parma and the Taro river valleys (8 samples and 7 samples per set, respectively) and measured using the same technique. The aim of this study was the comparison between the town samples

  8. 云南金沙江干热河谷地区麻疯树生物量的变化%Biomass Change of Jatropha curcs in Dry-hot Valley Areas of Jinsha River in Yunnan

    Institute of Scientific and Technical Information of China (English)

    陈喜英; 谷勇; 殷瑶; 吴昊; 齐泮仑

    2011-01-01

    为实现麻疯树资源的可持续利用和科学管理,并为估算麻疯树生态系统的碳汇提供依据,于2009年7月对云南省金沙江干热河谷地区的元谋、永胜、华坪3县半野生的麻疯树进行了生物量调查.结果表明:6~15年生麻疯树生理活动达到高峰期,生物量迅速增加;地上部分生物量与主干、叶、枝条的生物量符合线性模型,各构件生物量与树龄的关系符合生长曲线模型,其中地上部分生物量与树龄的关系符合3次曲线方程,地下部分生物量与树龄的关系符合逻辑曲线方程;地上部分各构件生物量比率随树龄的变化呈不同的变化规律;根系中主根生物量最大,占全根系的58.7%~82.6%,须根最小,仅占0.7%~6.2%.%The biomass of semi-wild Jatropha curcas in Yuanmou, Yongsheng and Huaping counties (dry-hot valley areas of Jinsha River in Yunnan) was surveyed in 2009 to realize sustainable utilization and scientific management of Jatropha curcas resource and provide the basis for estimating carbon sink ofJatropha curcas ecological system. The results showed that the physiological activity of Jatropha curcas with 6~15 years old reached the peak, its biomass increased rapidly, there was a linear model in biomass between the aerial part and trunk, leaf, branch, the relationship between biomass of different parts and tree age fitted the growth curve model, the relationship between aerial part biomass and tree age fitted the cubic curve equation, the relationship between biomass of underground part and tree age fitted the logic curve equation, the biomass ratio between different aerial parts showed different variation regulation with change of tree age, the biomass of main root was maximum (58.7~82.6%) and the biomass of fibrous root was minimum (0.7%~6.2%).

  9. Cultivable Bacterial Diversity in A Small Area of Natural Populus Euphractica Forest of Tarim River Valley, China%塔河天然胡杨林地可培养细菌的生态分布研究

    Institute of Scientific and Technical Information of China (English)

    孜来古丽·米吉提; 马相如; 阿不都外力·阿布都热依木; 玛丽帕·吐达洪; 古丽斯玛依·艾拜都拉; 艾尔肯·热合曼

    2009-01-01

    Objective: Investigate the bacteria community diversity in a small area of Natrural Populus euphractica Forest of Tarim River Valley, China. Method: Using phenotypic and biochemical characterization, and finally molecular identification by analysis of polymerase chain reaction(PCR)-amphfied 16S rRNA gene sequence.Result: 22 cultivable different bacteria had isolated from soil, waste water and secretion liquid the Poptdus euphractica stand by culturing with LB medium, respectively. Among them 17 strains were gram-positive, 5 strains were gram-negative. Based on analysis of 16S rRNA gene sequence showed that 15 strains found to be Bacilli, 4 strains were Acinetobacter, other than Ba-cilli and Acinetobacter there is one Pseudomonas strain(W1-1), one Planococcus strain (W2-3), and one Agrococcus strain (M5). Conclu-sion:There is a high diversity of Bacilli species in this small area, while some potential novel species were found belong to the Bacillus genus and ornithinibacillus.%目的:研究塔里木河天然胡杨林部分地区可培养细菌的生态分布.方法:通过塔里木河胡杨林采样,可培养菌分离及16S rDNA序列鉴定.结果:从3种不同样品(水样、土样和胡杨树杆分泌物)中分离筛选了22株细菌,其中17株菌为革兰氏阳性菌,5株为革兰氏阴性菌.根据生理生化特征与16S rDNA序列分析结果表明,其中15株菌属于芽孢杆菌属,4株属于不动杆菌属、假单胞菌属、动性球菌属和Agrococcus属各含有1个分离株.结论:塔里木河胡杨林可培养微生物中芽孢杆菌比较丰富,其中有3个可能的新种.

  10. Geochemical characteristics of the Shujiadian Cu deposit related intrusion in Tongling: Petrogenesis and implications for the formation of porphyry Cu systems in the Middle-Lower Yangtze River Valley metallogenic belt, eastern China

    Science.gov (United States)

    Wang, Shiwei; Zhou, Taofa; Yuan, Feng; Fan, Yu; Cooke, David R.; Zhang, Lejun; Fu, Bin; White, Noel C.

    2016-05-01

    Porphyry Cu deposits can form in intracontinental or post-collision settings; however, both the genesis of fertile magmas and the mechanism of metal enrichment remain controversial. The Shujiadian porphyry Cu deposit is located in the Tongling area of the Middle-Lower Yangtze River Valley metallogenic belt. It is hosted by the Shujiadian complex, which mainly consists of quartz diorite porphyry (143.7 ± 1.7 Ma) and pyroxene diorite (139.8 ± 1.6 Ma). They both belong to the calc-alkaline series, with enrichment in large-ion lithophile elements (LILE) and light rare earth elements (LREE), depletion in high field-strength elements (HFSE) and heavy rare earth elements (HREE), and slightly negative Eu anomalies. Both quartz diorite porphyry and pyroxene diorite have geochemical affinities with adakite, and their low MgO (1.5-3.7 wt%), and Ni (3.7-6.9 ppm), Cr (2.0-44 ppm), and Th/Ce contents (0.06-0.11) indicate that the intrusive rocks have some characteristics of adakite-like rocks derived from thickened lower crust and melts from metabasaltic rocks and eclogites. Plagioclases from the quartz diorite porphyry are andesine (An value = 31.8-40.5) and from the pyroxene diorite are felsic albite and oligoclase with large-scale zones and variable An value (An value = 8.9-18.3), Fe and Sr contents, which indicate that mixing of mafic and felsic magma may have occurred in the shallow magma chamber. Compared to the barren quartz diorite porphyry, relatively lower SiO2 contents (49.5-55.2 wt.%), higher εNd(t) values (- 7.4 to - 6.9), εHf(t) values (- 11.0 to - 9.1) compositions, Ti-in-zircon temperatures (714-785 °C), and variations of HREE contents of the mineralization-related pyroxene diorite suggest mixing with high-temperature mafic magma. Calculated Ce4 +/Ce3 + values of pyroxene diorite plot between the Ni-NiO buffer (NNO) and magnetite-hematite buffer (MH), and barren quartz diorite porphyry samples plot below the Ni-NiO buffer (NNO). Geochemical features of

  11. The Shoreline Management Tool - an ArcMap tool for analyzing water depth, inundated area, volume, and selected habitats, with an example for the lower Wood River Valley, Oregon

    Science.gov (United States)

    Snyder, Daniel T.; Haluska, Tana L.; Respini-Irwin, Darius

    2013-01-01

    within each parcel. The Shoreline Management Tool is highly transferable, using easily generated or readily available data. The capabilities of the tool are demonstrated using data from the lower Wood River Valley adjacent to Upper Klamath and Agency Lakes in southern Oregon.

  12. 美国切诺基文化传播对淮河流域弱势文化外宣的启示%The enlightenment of Cherokee culture communication on university-based publicity of weak culture in Huai River Valley

    Institute of Scientific and Technical Information of China (English)

    樊继群

    2015-01-01

    As a sect of aboriginal Indian culture, Cherokee culture has been staying at an inferior position for a long History. Northeastern State University has been an important player in the protection and inheritance of Cherokee culture. The culture in the Huai River Valley is also weak, and its preservation is facing severe challenges. Universities along the Huai River are also expected to shoulder their due responsibilities of preserving and publicizing the Huai River culture. The practice and experience of Northeastern State University on cultural communication will be of great inspiration for universities concerned to the preservation and publicity of weak culture in the Huai River Valley.%切诺基文化是美国印第安族裔文化,在美国属于弱势文化。美国东北州立大学是切诺基语言文化传播的重要阵地,在切诺基文化传播方面做出了大量卓有成效的工作。淮河流域文化也属于弱势文化,其在本地区的传播与发展也面临着严峻的挑战。沿淮高校在保护、传播淮河流域文化方面有义不容辞的责任。东北州立大学在弘扬切诺基弱势文化中的经验做法值得借鉴,对相关高校保护、传播淮河流域文化具有积极的启示意义。

  13. 长江中下游麦区小麦品质改良设想%Concept on Wheat Quality Improvement in Middle and Lower Reaches of Yangtze River Valley

    Institute of Scientific and Technical Information of China (English)

    高德荣; 张晓; 张伯桥; 朱冬梅; 吕国锋

    2013-01-01

    长江中下游麦区是我国唯一的弱筋小麦优势产业带,该麦区的沿江、沿海地区适宜发展弱筋小麦,其他地区适宜发展中筋小麦.弱筋、中筋小麦品种的品质遗传改良是该麦区重要育种方向之一.目前该麦区虽然育成并推广了一批弱筋、中筋小麦品种,基本满足了生产上对优质小麦品种的需求,但还存在一定的问题.如新育成的弱筋小麦品质并不优于扬麦9号和宁麦9号,中筋小麦面筋含量和强度还需提高.针对存在的问题,提出该麦区小麦品质改良的3个设想:(1)利用高分子量谷蛋白亚基缺失,降低面筋强度,培育优质弱筋小麦;(2)利用优质高分子量麦谷蛋白亚基组合,改善蛋白质组分,提高面筋强度,培育优质中筋小麦;(3)利用Wx蛋白亚基缺失,培育弱筋和中筋兼用型小麦,使该麦区小麦品种在蛋白质含量和面筋含量偏高而不能作为弱筋小麦使用时,利用其优良的淀粉品质加工品质较优的面条.%The middle and lower reach of Yangtze River Valley is the only main region for planting weak gluten wheat.In which,coastal area and region along the Yangtze River is the most suitable area for developing weak gluten wheat and other regions are suitable for growing moderate gluten wheat.The quality improvement of weak gluten and moderate gluten wheat are the main breeding objectives.Although a number of weak gluten and moderate gluten wheat varieties have been released to meet the market requirement for quality wheat generally,the progress is not significant,since the quality of new released weak gluten varieties is not superior than that of Yangmai 9 and Ningmai 9,moreover,the gluten strength of moderate gluten wheat is not enough.In order to resolve these problems,three approaches were suggested:(1) Use the null of HMW-GS to reduce wheat gluten strength,thus breed weak gluten wheat with high quality.(2) Use preferable HMW-GS combinations improving protein

  14. Geo morphological setting and main technological features of new Middle and Upper Pleistocene sites in the Lower Manzanares River Valley (Madrid, Spain); Contexto geomorfologico y principales rasgos tecnologicos de nuevos yacimientos del Pleistoceno Medio y Superior en el Valle Inferior del Manzanares (Madrid, Espana)

    Energy Technology Data Exchange (ETDEWEB)

    Silva, P. G.; Lopez Recio, M.; Cuartero, F.; Baena, J.; Tapias, F.; Manzano, I.; Martin, D.; Morin, J.; Roquero, E.

    2012-11-01

    The archaeological works developed during the years 1996 in the site of Tafesa, 2005 in the 12 de Octubre Metro Station site and 2006 in the confluence of the Butarque Stream (Villaverde-Barrio de Butarque site) located south of the Madrid City (Spain), have provided new lithic assemblages. These assemblages have been stratigraphic ally contextualized in the Pleistocene deposits of the Lower Manzanares river valley within the so-called Manzanares Complex Terrace (TCMZ). This fluvial terrace constitutes an anomalous thickened (20-15m) deposit at {+-}22-16m above the present river thalweg mainly developed along the right (southern) valley margin. This fluvial level has been traditionally considered of middle Pleistocene age on the basis of the acheulian lithics and faunal assemblages typically located within its lower stratigraphic layers. Certainly, the Tafesa is a fluvial terrace site at {+-}22 m with acheulian industry and middle Pleistocene faunal remains at its lower sedimentary sequence. However, the upper sedimentary levels of this same terrace in the 12 de Octubre y Villaverde-Butarque sites throw lithic assemblages of the lower and upper Paleolithic belonging to upper Pleistocene, as suggested by the available set of TL and OSL dates for the zone. The analyses developed in this study indicate that the development of this thickened fluvial terrace started during the end of the middle Pleistocene, but also comprise the whole Oxygen Isotopic Stage OIS 5 during the upper Pleistocene. (Author) 95 refs.

  15. Sandy Beach Hammering Block Nursing and High Efficiency Seedling Nursing Techniques of Walnut Improved Variety in Jinsha River Valley Area%金沙江河谷地区核桃沙滩育砧高效育苗技术试验

    Institute of Scientific and Technical Information of China (English)

    杨根林; 和善程; 高云

    2011-01-01

    Walnuts is a kind of woody oil plant with high economic worth. Sandy beach hammering block nursing, bud grafting and field seedling nursing of walnut was studied in Lijiang Jinsha river valley area. The results show that the techniques have many advantages, such as short cycle, strong seedling and flourishing roots, neat emerging, short slowing seedling period, high survival rate. Because of saving the step of putting up breeding and shortening the time of growing seedlings, the new approach can save lots of cost and satisfy demands of production. The techniques have high value to popularize in Lijiang Jinsha river valley area.%在丽江市金沙江河谷地区进行核桃沙滩育砧、移砧芽苗嫁接、大田育苗的研究.结果认为,该方法具有周期短,嫁接口愈合好,苗木生长健壮,根系发达,发苗整齐,砧木苗生长粗壮、种植后缓苗期短,成活率高等特点,而且成本低,无须搭建育砧苗床,能在短时间内培育出大量优质苗木.

  16. Ecological Adaptability of Eight Tree Species in Dry and Hot Valley of Jinsha River%金沙江干热河谷区8个造林树种的生态适应性变化

    Institute of Scientific and Technical Information of China (English)

    李昆; 孙永玉; 张春华; 崔永忠

    2011-01-01

    The water ecophysiology of eight tree species growing in dry and hot valley of Jinsha River was studied. The result showed that in rain season the index of water saturation deficit ( WSD) of indigenous tree species Dodonaea viscosa Jacg, and three eucalyptus species were higher than that of the other tree species. The plant with high WSD index and low relative water content (RWC) has strong drought tolerance. Enlargement of the rate of leaf area and fresh leaf weight is beneficial to enhance the drought tolerance of a plant, while increasing the accumulation of dry materials and the density of cytoplasm is also an effective way. Dry and hot stress may induce chlorophyll content reduced, while the chlorophyll content may increase in rainy seasons with increasing the rate of chlorophyll a and chlorophyll b. In dry seasons, the sugar content of test trees is higher than that in rainy seasons and the starch and sugar contents are lower in dry reasons than in rainy reasons except Acacia manguim De Willd. Under the arid condition, the free proline content of 7 tree species increased with different degrees except Eucalyptus urophylla S. T. Blake. The tree species which are prone to wither and defoliation in dry seasons can accumulate more free pro-line. There are more ecophysiological similarities among the seven tree species which are suitable for afforestation except Acacia manguim De Willd. ; and there exists obvious consistency in ecophysiological characteristics amongsame genus. Some ecophysiological characteristics of D. Viscosa Jacg. , the indigenous tree species, are similar to that of Acacia and some others are similar to that of Eucalyptus. Three Eucalyptus species, three Acacia species and D. Viscosa Jacg. Showed stronger ecological adaptability and grow well in dry and hot valley of Jinsha River.%对金沙江干热河谷区8个造林树种的有关生理生态特性进行了研究.结果表明:相思类树种在旱季水分自然饱和亏

  17. Rift Valley Fever Virus

    Science.gov (United States)

    Rift Valley fever virus (RVFV) is a mosquito-transmitted virus or arbovirus that is endemic in sub-Saharan Africa. In the last decade, Rift Valley fever (RVF) outbreaks have resulted in loss of human and animal life, as well as had significant economic impact. The disease in livestock is primarily a...

  18. Silicon Valley Ecosystem

    Institute of Scientific and Technical Information of China (English)

    Joseph Leu

    2005-01-01

    @@ It is unlikely that any industrial region of the world has received as much scrutiny and study as Silicon Valley. Despite the recent crash of Internet and telecommunications stocks,Silicon Valley remains the world's engine of growth for numerous high-technology sectors.

  19. Lithologic controls on valley width and strath terrace formation

    Science.gov (United States)

    Schanz, Sarah A.; Montgomery, David R.

    2016-04-01

    Valley width and the degree of bedrock river terrace development vary with lithology in the Willapa and Nehalem river basins, Pacific Northwest, USA. Here, we present field-based evidence for the mechanisms by which lithology controls floodplain width and bedrock terrace formation in erosion-resistant and easily friable lithologies. We mapped valley surfaces in both basins, dated straths using radiocarbon, compared valley width versus drainage area for basalt and sedimentary bedrock valleys, and constructed slope-area plots. In the friable sedimentary bedrock, valleys are 2 to 3 times wider, host flights of strath terraces, and have concavity values near 1; whereas the erosion-resistant basalt bedrock forms narrow valleys with poorly developed, localized, or no bedrock terraces and a channel steepness index half that of the friable bedrock and an average channel concavity of about 0.5. The oldest dated strath terrace on the Willapa River, T2, was active for nearly 10,000 years, from 11,265 to 2862 calibrated years before present (cal YBP), whereas the youngest terrace, T1, is Anthropocene in age and recently abandoned. Incision rates derived from terrace ages average 0.32 mm y- 1 for T2 and 11.47 mm y- 1 for T1. Our results indicate bedrock weathering properties influence valley width through the creation of a dense fracture network in the friable bedrock that results in high rates of lateral erosion of exposed bedrock banks. Conversely, the erosion-resistant bedrock has concavity values more typical of detachment-limited streams, exhibits a sparse fracture network, and displays evidence for infrequent episodic block erosion and plucking. Lithology thereby plays a direct role on the rates of lateral erosion, influencing valley width and the potential for strath terrace planation and preservation.

  20. Turnover Rates of Fall Migrating Pectoral Sandpipers Through the Lower Mississippi Alluvial Valley

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The Mississippi Alluvial Valley (MA V) is the historic alluvial floodplain of the Lower Mississippi River. Most of the MAV is located in Arkansas, Louisiana, and...

  1. 76 FR 24914 - Digital River Education Services, Inc., a Division of Digital River, Inc., Including Workers...

    Science.gov (United States)

    2011-05-03

    ... Employment and Training Administration Digital River Education Services, Inc., a Division of Digital River... Marketing (JEM), Including On-Site Lease Workers From Serenity Staffing, Accountemps, Silicon Valley, and... Assistance on January 28, 2011, applicable to workers of Digital River Education Services, Inc., a...

  2. 78 FR 48716 - Notice of Availability of the Final Environmental Impact Statement for the Arkansas Valley...

    Science.gov (United States)

    2013-08-09

    ... Arkansas River Basin, groundwater, climate change, recreation biological resources, human environment... Valley Conduit and Long-Term Excess Capacity Master Contract, Fryingpan-Arkansas Project; Bent, Chaffee... statement (EIS) for the Arkansas Valley Conduit (AVC) and Long-Term Excess Capacity Contract,...

  3. Volume of Valley Networks on Mars and Its Hydrologic Implications

    Science.gov (United States)

    Luo, W.; Cang, X.; Howard, A. D.; Heo, J.

    2015-12-01

    Valley networks on Mars are river-like features that offer the best evidence for water activities in its geologic past. Previous studies have extracted valley network lines automatically from digital elevation model (DEM) data and manually from remotely sensed images. The volume of material removed by valley networks is an important parameter that could help us infer the amount of water needed to carve the valleys. A progressive black top hat (PBTH) transformation algorithm has been adapted from image processing to extract valley volume and successfully applied to simulated landform and Ma'adim Valles, Mars. However, the volume of valley network excavation on Mars has not been estimated on a global scale. In this study, the PBTH method was applied to the whole Mars to estimate this important parameter. The process was automated with Python in ArcGIS. Polygons delineating the valley associated depressions were generated by using a multi-flow direction growth method, which started with selected high point seeds on a depth grid (essentially an inverted valley) created by PBTH transformation and grew outward following multi-flow direction on the depth grid. Two published versions of valley network lines were integrated to automatically select depression polygons that represent the valleys. Some crater depressions that are connected with valleys and thus selected in the previous step were removed by using information from a crater database. Because of large distortion associated with global dataset in projected maps, the volume of each cell within a valley was calculated using the depth of the cell multiplied by the spherical area of the cell. The volumes of all the valley cells were then summed to produce the estimate of global valley excavation volume. Our initial result of this estimate was ~2.4×1014 m3. Assuming a sediment density of 2900 kg/m3, a porosity of 0.35, and a sediment load of 1.5 kg/m3, the global volume of water needed to carve the valleys was

  4. 伊犁河谷新垦区土壤有机质、全氮、全磷特征%On Features of SOM、Total - N、 Total - P in New Reclamation Area of Yili River Valley

    Institute of Scientific and Technical Information of China (English)

    马鹏; 李志忠

    2012-01-01

    对伊犁河谷新垦区不同土地利用方式下土壤剖面有机质、全氮、全磷含量进行分析,结果表明:不同土地利用方式,土壤有机质、全氮含量明显不同,都是未开垦荒地最大,杨树林地、树上干杏林地次之,油葵地(耕地)最小,撂荒地因弃耕比油葵地稍大;土壤全磷则是树上干杏林地最大,油葵地最小。新垦区土壤有机质、全氮、全磷含量随着深度变大含量都有所减小,表现出的表聚的特征,并且有机质与全氮含量随深度增加差异也逐渐减小。研究区土壤有机质含量与全氮、全磷含量相关性较好,尤其是有机质与全氮具有更高的相关度。为了防止土地肥力逐渐退化,研究区应提倡以林草为主的土地利用方式,并且在耕作中适量增施有机肥。%This paper analyzes the contents of soil organic matter(SOM) 、total - N,total - P of different types of land use in new reclamation area of Yili River valley. Studies show that the soil property has significant influence over different types of land use. According to the contents of SOM, total - N, the wasteland is maximum, while the poplar forest and the apricot land follow, and the cultivated land with sunflower oil is minimum, and the abandoned land is higher than the cultivated one. According to the contents of total - P, the maximum is the apricot land, the minimum is also the cultivated land. All of the contents of soil organic matter(SOM) ,total -N,total -P in new reclamation area reduce with the depth increasing, show the character of surface gathering, the content diversity in different types of land use of SOM and total - N also decrease with the depth increasing. The content of SOM has relevance with total -N and total -P, especially more obvious to the total -N. The experimental area should advocate the types of land use of woods and grass, and add organic fertilizers in cultivated land, in order to prevent the

  5. Caracterização de matérias-primas cerâmicas do Vale do Rio Caí Characterization of ceramic raw materials from the Caí River Valley, RS, Brazil

    Directory of Open Access Journals (Sweden)

    J. E. Zorzi

    2012-12-01

    Full Text Available Este trabalho tem como objetivo a caracterização química e mineralógica de matérias-primas argilosas utilizadas pelas indústrias cerâmicas do Vale do Rio Caí, RS. Essa região, situada entre Porto Alegre e a Serra Gaúcha, é o maior centro produtor cerâmico para construção civil do estado do Rio Grande do Sul. Apesar da importância da indústria cerâmica para a economia local e do Estado, a grande maioria das argilas disponíveis para consumo nunca foi caracterizada satisfatoriamente e não existem dados técnicos e científicos que possam orientar tanto a correta exploração das jazidas quanto o desenvolvimento de produtos cerâmicos de maior valor agregado. Neste trabalho foram feitas análises por fluorescência e difração de raios X das principais argilas utilizadas pela indústria cerâmica da região. De acordo com o método de análise hierárquica de agrupamentos e tendo como base a composição química das amostras, foram identificados três grupos de matérias-primas: argilas residuais (ou primárias e dois grupos de argilas transportadas (ou secundárias. A diferenciação das matérias-primas em grupos se manifesta também na composição de fases das amostras, tal como determinada por difração de raios X e análise racional.This work aims to characterize the chemistry and mineralogy of clay raw materials used in the heavy clay industry of the Caí River Valley, in southern Brazil. This region lies between Porto Alegre and Serra Gaúcha and is regarded as the major production center of brick and tiles in the Rio Grande do Sul. Despite the importance of this activity for both the local and state economy, the vast majority of clay raw materials have never been satisfactorily characterized, so there is not adequate data to guide its correct exploitation or to allow the development of ceramic products of higher quality. In this work X-ray fluorescence and diffraction were applied to analyze the clays largely used by

  6. 九龙瀑布群喀斯特河谷区的苔藓植物区系及生态学特征%Flora and Ecology of the Bryophytes in Jiulong-Waterfalls Karst River Valley

    Institute of Scientific and Technical Information of China (English)

    李晓娜; 张朝晖; 龙明忠

    2014-01-01

    In order to comprehensively grasp the flora status of the bryophytes in Jiulong-waterfalls karst river valley,the bryophytes information of the studied area were extracted and reprocessed from the research findings in 2006 and 2010.The results were shown as follows: 1 )A total of 106 species (including subspecies and varieties)in 48 genera,19 families were found.Both the dominant bryophyte families and genera suggested that this area was with transitional characteristics between tropics and temperate zone.2)The bryoflora was dominated by East Asian elements (52%)and tropical elements (31%),in which areal patterns of East Asia (27%),tropical Asia (26%)and endemic to China (25%) occupied the highest percentages.Therefore,the bryoflora was with both characteristics of the warm temperate and south subtropical elements, and possessed very high endemism. 3 ) The ecological environment types of bryophytes in the study area were dominated by soil (67.92%),tufa (40.57%)and carbonate rock (33.02%).Because there was a large amount of silt deposited in the tufa,some soil and tufa environment types were difficult to be distinguished.4)70 species of bryophytes in 36 genera,17 families living on tufa or carbonate rocks played a part in karstic ecological processes of the study area though they were not very specific to the calcium environment.%为全面掌握云南苔藓植物区系状况,在2006年和2010年研究的基础上单独抽提云南省罗平县九龙瀑布群喀斯特河谷区的苔藓数据进行苔藓植物区系及其生态学特征分析。结果表明:1)该区共有苔藓植物19科48属106种(含变种和亚种),其优势科、属均体现了该地区由温带向热带过渡的特征。2)区内苔藓区系地理成分并不复杂,以东亚成分(52%)和热带成分(31%)占绝对优势,其中又以东亚分布型(27%)、热带亚洲分布型(26%)和中国特有分布型(25%)所占比例最高,反映了该区系

  7. Características produtivas de genótipos de cebola no Vale do São Francisco Yield characteristics of onion genotypes in the São Francisco River Valley

    Directory of Open Access Journals (Sweden)

    Nivaldo D Costa

    2007-06-01

    . The fresh mass of bulbs varied from 86 to 160 g and the genotypes EX-07593000 and Granex 429 showed the highest number of commercial bulbs per plot (126 and 124 bulbs, respectively. Based on the evaluated characteristics, the genotypes EX-19013, EX-07595002, Encino, IPA-11, Brisa, TPC 91923, TPR 91970 and EX-075593000, in 2003, and the genotypes EX-0759300, Granex-429, IPA-11, IPA-04 and Texas Grano 502, in 2004, were the best adapted and with the highest potential for planting in the São Francisco River Valley.

  8. Initiation of large-volume silicic centers in the Yellowstone hotspot track: insights from H2O- and F-rich quartz-hosted rhyolitic melt inclusions in the Arbon Valley Tuff of the Snake River Plain

    Science.gov (United States)

    Drew, Dana L.; Bindeman, Ilya N.; Loewen, Matthew W.; Wallace, Paul J.

    2016-01-01

    During the onset of caldera cluster volcanism at a new location in the Snake River Plain (SRP), there is an increase in basalt fluxing into the crust and diverse silicic volcanic products are generated. The SRP contains abundant and compositionally diverse hot, dry, and often low-δ18O silicic volcanic rocks produced through time during the formation of individual caldera clusters, but more H2O-rich eruptive products are rare. We report analyses of quartz-hosted melt inclusions from pumice clasts from the upper and lower Arbon Valley Tuff (AVT) to gain insight into the initiation of caldera cluster volcanism. The AVT, a voluminous, caldera-forming rhyolite, represents the commencement of volcanism (10.44 Ma) at the Picabo volcanic field of the Yellowstone hotspot track. This is a normal δ18O rhyolite consisting of early and late erupted members (lower and upper AVT, respectively) with extremely radiogenic Sr isotopes and unradiogenic Nd isotopes, requiring that ~50 % of the mass of these elements is derived from melts of Archean upper crust. Our data reveal distinctive features of the early erupted lower AVT melt including: variable F concentrations up to 1.4 wt%, homogenous and low Cl concentrations (~0.08 wt%), H2O contents ranging from 2.3 to 6.4 wt%, CO2 contents ranging from 79 to 410 ppm, and enrichment of incompatible elements compared to the late erupted AVT, subsequent Picabo rhyolites, SRP rhyolites, and melt inclusions from other metaluminous rhyolites (e.g., Bishop Tuff, Mesa Falls Tuff). We couple melt inclusion data with Ti measurements and cathodoluminescence (CL) imaging of the host quartz phenocrysts to elucidate the petrogenetic evolution of the AVT rhyolitic magma. We observe complex and multistage CL zoning patterns, the most critical being multiple truncations indicative of several dissolution-reprecipitation episodes with bright CL cores (higher Ti) and occasional bright CL rims (higher Ti). We interpret the high H2O, F, F/Cl, and

  9. Edge effects of grasshopper communities in the North-Luo River Valley of Yan'an%延安北洛河流域蝗虫群落的边缘效应

    Institute of Scientific and Technical Information of China (English)

    李亚妮; 王文强; 廉振民

    2011-01-01

    蝗虫作为重要的昆虫,研究其边缘效应,有助于更详细和准确地把握其分布格局,从而为蝗虫的边缘效应及其强度的分析和其防治提供理论基础.根据延安北洛河流域的生态特点,选取农田一草地、农田一灌草丛、农田-.道路和草地-道路4种边缘类型进行调查与分析.结果表明:草地-道路边缘利于蝗虫孳生,其物种数(25种)和多样性指数H′(2.574 5)都高于其他3种边缘;边缘效应强度除农田-灌草丛(0.9160<1)边缘外,其余类型均呈边缘正效应(>1).说明在进行蝗虫防治工作时,应将边缘效应作为一种重要影响因子考虑在内,同时结合不同种类蝗虫在边缘反应类型上的差异,采取有针对性的防治措施与手段,才能达到理想的防治效果.%With the advance of biodiversity and landscape research, the studies on edge effect has enter a new phase since the concept of edge effect came into being, and the study on the response of creature to edge effect has become a hot research topic too. Grasshopper as one group of the important insects, the study on the edge effect would help us to grasp their distribution patterns precisely and hence offer some of basic theory on the analysis on grasshoppers' edge response and its intensity . Four types of edge zones: farmland-grassland, farmland-shrub, farmland-road, and grassland-road, were selected and analyzed based on ecological characteristics of the North-Luo River Valley of Yah'an using the Shannon-Wiener biodiversity index (H'), Pielou index(J), Simpson index(C)and species quantity. Results showed that both species quantity (25 species) and H' of 2.574 5 for the grassland-road treatment were highest. Edge effects with four edges for the farmland-shrub treatment was below 1 (0.916 0); whereas the other three treatments had positive effects(> 1 ). Thus, for effective grasshopper prevention and control, edge effects should be considered as an important factor so as to

  10. Comportamento de cultivares de uva sem sementes no submédio São Francisco Behavior of grape seedless varieties in the valley of São Francisco River

    Directory of Open Access Journals (Sweden)

    Patrícia Coelho de Souza Leão

    2002-12-01

    Full Text Available Com o objetivo de introduzir, avaliar e selecionar variedades de uva sem sementes, adaptadas às condições tropicais semi-áridas e oferecer novas alternativas aos viticultores do Vale do São Francisco, implantou-se, em 1994, uma coleção com dezenove variedades de uvas sem sementes no Campo Experimental de Bebedouro, da Embrapa Semi-Árido, em Petrolina - PE. Foram avaliadas treze variedades ao longo dos anos de 1997 e 1998, correspondendo a cinco ciclos de produção. As variedades utilizadas foram Vênus, Arizul, Beauty Seedless, Thompson Seedless, Marroo Seedless, Canner, CG 39915, Pasiga, Saturn, Emperatriz, A1581, Paulistinha e Loose Perlette, enxertadas sobre o porta-enxerto IAC 572 ('Campinas'. Foram avaliados aspectos relacionados ao desenvolvimento vegetativo e produtivo das plantas e características e composição química dos frutos. Todas as variedades apresentaram cachos com tamanho pequeno. As variedades Vênus e Marroo Seedless destacaram-se em relação ao diâmetro de bagas, apresentando, respectivamente, 17,83 e 18,26 mm, sem a necessidade de aplicação de reguladores de crescimento. O teor de sólidos solúveis totais foi elevado na maioria das variedades, enquanto a acidez total titulável foi reduzida, resultando em relações SST/ATT satisfatórias. As variedades Vênus e Marroo Seedless foram as mais produtivas, com produtividades anuais de 24 t/ha e 20 t/ha, respectivamente.The present work aimed at evaluating and selecting seeddless grape varieties adapted to the semi-arid tropical conditions of the São Francisco River Valley, Northeastern - Brazil. The experiment was carried out in an experimental vineyard which belongs to Embrapa Semi-Árid, in Petrolina, Pernambuco State, Brazil during five growing seasons in 1997 and 1998. The varieties tested were: Vênus, Arizul, Beauty Seedless, Thompson Seedless, Marroo Seedless, Canner, CG 39915, Pasiga, Saturn, Emperatriz, A1581, Paulistinha and Loose Perlette, grafted

  11. A Characteristic Analysis on Diurnal Variations of Convective Rainfall Along the Yangtze River Middle Valleys in 2010 Flooding Season%2010年汛期长江中游对流降水日变化特征分析

    Institute of Scientific and Technical Information of China (English)

    赵玉春; 徐明; 王叶红; 徐桂荣; 崔春光

    2012-01-01

    Abstract: With hourly intensive surface observations, satellite remote-sensed temperature of black body (TBB) and 3-hourly radio-soundings, an analysis is carried out to investigate the diurnal changes of convective rainfall and atmospheric physical variables along the middle valleys of Yangtze River. The result are as follows: the convective rainfall is of obvious diurnal changes, with a rainfall maximum (minimum at 1500 BT (0100 BT). The surface and sounding physical variables are also of clear diurnal changes. Th diurnal variation of surface temperature is the most obvious, with a mean diurnal range of 9℃, while th diurnal range of dew point temperature is only about 1℃. The diurnal change of relative humidity is mainl caused by the temperature diurnal variation. The spatial distribution of surface temperature diurnal changes is influenced by the topography. The temperature rising (dropping) in the mountainous areas is large than in the plain areas in the daytime (nighttime). The diurnal change of temperature gradient due to tin topographic difference can drive topographically near-surface thermal flow. The convergence (divergence flows occur in the mountainous areas (plain areas) in the daytime, vice versa in the nighttime. The stabilty decrease in the lower atmosphere and the CAPE increase are beneficial to the afternoon thermal convection initiation in the daytime. The lowering of lifting condensation level (LCL), the increase of relative humidity and the increase of air-column precipitable water vapor (PW) are favorable for the development of long-life early-morning convective systems in the nighttime.%利用2010年6月16日至7月31日每3h一次的探空资料、逐小时地面加密观测和卫星云图黑体辐射亮温(TBB)等资料,对长江中游的对流降水及大气物理量的日变化特征进行了分析。结果发现:对流降水具有明显的日变化特征,降水在15时(01时)左右具有峰(谷)值。地面气象

  12. Foliar carbohydrates content and invertase activity in vines at São Francisco River Valley - Brazil Teores foliares de carboidratos e atividade de invertases em videiras no Vale do Rio São Francisco- Brasil

    Directory of Open Access Journals (Sweden)

    Barbara França Dantas

    2005-08-01

    Full Text Available The irrigated agriculture at the São Francisco River Valley, Northeast Brazil, shows an increasing production of grapes for winery. Among the wines produced there the one obtained from Vitis vinifera L., cultivar Syrah, stands out due to its adaptation to the climatic conditions of the region. However, little is known about carbohydrates metabolism of vines cultivated in this region. The objective of this work was to evaluate sugar and starch contents and the invertase activity in vines leaves during two consecutive growing seasons. The experiment was carried out at Embrapa Semi-Árido and at Santa Maria Winery, respectively located in Petrolina and Lagoa Grande, Pernambuco-Brazil. Leaves were collected weekly from January to December of 2003 and assessed for reducing sugars, total soluble sugars and starch contents, as well as for acid (AI and neutral invertases (NI. The results showed that reducing sugars, total soluble sugars and starch contents increased during fruit maturation and are influenced by temperature, radiation and insolation variations. The second growing season showed higher reducing sugars and total soluble sugars content and lower starch content in the leaves than the first one. AI activity was higher than NI activity and these also varied according to weather conditions. During berries ripening, leaves showed higher sugar content and invertase activity, suggesting a higher sugar metabolism and transport during this phase.O pólo de agricultura irrigada do Vale do Rio São Francisco apresenta um crescente aumento na produção de uvas para vinificação. Entre os vinhos finos produzidos na região, destaca-se aquele obtido da cultivar Syrah, que se adaptou bem às condições climáticas da região. Pouco se conhece, no entanto, sobre o metabolismo de carboidratos das videiras nessa região. O objetivo deste trabalho foi avaliar os teores de açúcares e de amido, bem como a atividade de invertases durante dois ciclos de

  13. Spatial prediction of soil organic carbon based on RS and GIS in West River Valley%基于RS和GIS的西河流域土壤有机碳含量的空间反演

    Institute of Scientific and Technical Information of China (English)

    周稀; 潘洪旭; 邓欧平; 邓良基

    2016-01-01

    基于遥感( RS)和地理信息系统( GIS)方法掌握土壤有机碳含量是当前土壤学科的发展趋势。本文利用西河流域Landsat 8 OLI遥感影像及121个样点土壤表层(0~20 cm)有机碳含量和地面辅助数据建立预测模型并进行了空间反演。结果表明,仅用遥感光谱信息建立的土壤有机碳含量预测模型均达极显著水平( P=0.000),表明遥感光谱信息能用于表层土壤有机碳含量的预测建模。在引入成土母质、地貌类型和农地利用方式等地面辅助因子后,预测模型决定系数R2明显增大(P=0.000),由0.385提高到了0.579,这表明地面辅助因子能有效改善模型精度。空间反演显示,最优模型的插值图能较好地表现区域土壤有机碳含量分布的基本格局,但对于个别值区的反演效果仍有待进一步提升。%Understanding of soil organic carbon content ( SOC ) based on remote sensing ( RS ) and geographic information system ( GIS) techniques becomes the development trend of current discipline. In this research, remotely sensed spectral data from Landsat 8 OLI, soil organic carbon content (121 samples from 0~20 cm soil layer) and the related ground parameters in the West River Valley were integrated to construct models for spatial prediction in the area. Space inversion was employed to check the model reliability. Results indicated that evaluation of SOC content was achieved by the constructed models using re-mote sensing data (P=0. 000), implying that it was potentially reliable to predict SOC content. When the related ground pa-rameters of soil parent material, landforms and agricultural land use were considered, respectively, the R2 values of prediction models were significantly improved (P=0. 000). Concretely, the R2 was increased from 0. 385 to 0. 579, indicating the in-volvement of ground parameters was beneficial to prediction accuracy. In contrast to the determined content, optimal interpola-tion model better

  14. Fine-scale Spatial Pattern Typical Vegetation at the Dry Minjiang River Valley%岷江干旱河谷中心地段植被微尺度空间格局特征

    Institute of Scientific and Technical Information of China (English)

    王晶; 包维楷

    2011-01-01

    微尺度景观格局是景观生态学的一个研究热点.干旱河谷是横断山区一类特殊的生态系统类型,生态脆弱,生态退化潜在风险大.选择四川茂县两河口典型样地干旱河谷微尺度景观格局进行研究.研究表明,样地上分布的景观类型多样,斑块类型有19个,植被景观总斑块达3 383个,以基质分布为主,植被斑块状镶嵌其中,主要以中生性耐旱植物为主,植被覆盖度为42.25%.植被景观类型大部分为豆科类灌丛景观,整个景观由川甘亚菊、刺蓬、瓦松、茂汶韭、狗尾草、小角柱花、侧柏、臭椿、滇柏、卷柏、元宝枫、岷江柏景观斑块控制.植被景观分布特征为,帚菊斑块面积最大且分布均匀,小马鞍羊蹄甲斑块最大且聚集度最高,狗尾草斑块破碎化程度最大,蚊子草斑块多样性程度最大,小角柱花多样性程度最小且分布最散.通过空间自相关性分析,研究区植物分布呈现较高的正相关性和空间聚集性,在尺度2m×2m空间自相关值最大,未来干旱河谷区微尺度空间格局研究尺度在这个尺度较适宜.%The dry Minjiang river valley is a special kind of cross-sectional type of ecological system, with its ecological fragility, the potential risks of degradation. We analyzed land cover categories(20 m ×20 m of extent and 1 mm of resolution) and images of vegetation index in MAO county. This study showed that the landscape diversity in the experimental plots are significant with 19 patch types and total 3 383 patches of vegetation. The regional distribution was matrix-based, patchy mosaic of vegetation in which endogenous drought-tolerant plants predominated. The vegetation coverage is 42. 25%. Most of the vegetation in the landscape are shrub legumes, the vegetation types include Pertya phylicoides, Sophora viciifolia Hance ,Ajania potaninii, Herba Euphorbiae Milii, W. Stnophylla, Iudigofera lenticellata,Orostachys fimbriatus,Bauhiniafaberi var

  15. Blitzen Valley Management Plan

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The 64,000 acre Blitzen Valley unit of Malheur National Wildlife Refuge is not producing enough wildlife to meet the refuge's migratory bird objectives. The area...

  16. Geometry of Valley Growth

    CERN Document Server

    Petroff, Alexander P; Abrams, Daniel M; Lobkovsky, Alexander E; Kudrolli, Arshad; Rothman, Daniel H

    2011-01-01

    Although amphitheater-shaped valley heads can be cut by groundwater flows emerging from springs, recent geological evidence suggests that other processes may also produce similar features, thus confounding the interpretations of such valley heads on Earth and Mars. To better understand the origin of this topographic form we combine field observations, laboratory experiments, analysis of a high-resolution topographic map, and mathematical theory to quantitatively characterize a class of physical phenomena that produce amphitheater-shaped heads. The resulting geometric growth equation accurately predicts the shape of decimeter-wide channels in laboratory experiments, 100-meter wide valleys in Florida and Idaho, and kilometer wide valleys on Mars. We find that whenever the processes shaping a landscape favor the growth of sharply protruding features, channels develop amphitheater-shaped heads with an aspect ratio of pi.

  17. 金沙江干热河谷人工林地表的蚂蚁群落%Communities of Ground-Dwelling Ants in Different Plantation Forests in Arid-Hot Valleys of Jinsha River,Yunnan Province,China

    Institute of Scientific and Technical Information of China (English)

    李巧; 卢志兴; 张威; 马艳滟; 冯萍

    2015-01-01

    Objective]Because of the fragile ecological environment in arid-hot valleys of Jinsha River,Yunnan Province,China,the region has been the hot spots of vegetation restoration for which plantation is the main model. To reveal the diversity status of these plantations,and the potential role in biodiversity protection,the ground-dwelling ant community was studied in 7 different plantations in Jinsha River arid-hot valleys,by comparing the difference of ground-dwelling ant community in terms of species composition and diversity. It would be reference for revegetation and biodiversity protection in the arid-hot valleys.[Method]The experimental sites were in the Desert Ecosystem Observation Station of the State Forestry Administration in Yuanmou County. The sampled plots were set in the following tree plantations: Eucalyptus spp.; Jatropha carcas; Jatropha carcas +Leucaena leucocephala; Azadirachta indica; Azadirachta indica + Acacia auriculiformis; Azadirachta indica + Acacia glauca and Azadirachta indica + Leucaena leucocephala. Investigation of ground-dwelling ant community was carried out by pitfall trappings in all 7 plantations in April ( dry season) and August (wet season),2011,respectively. At each plot,two-three 200 m transects were established for ant collection. The 20 pitfall traps with 50ml 50% glycerol were set along each transect at 10 m intervals at ground level.Pitfall traps were made from plastic containers,8 cm diameter and 15 cm deep,covered by a stone plate to protect the trap from rain. Traps were set for 5 days. The contents of each transect were placed separately in plastic bottles and deposited in 95% alcohol.[Results]The resultswere as follows: 1 ) Ant community composition: 4001 ant individuals were collected,representing 36 species in 17 genera and 5 subfamilies. The collected Myrmicinae subfamily had the most abundant genus and species,with 18 species in 6 genera,followed by Formicinae with 10 species in 5 genera,then Dolichoderinae with 6

  18. On the Changes of Agriculture and Animal Husbandry Environment in Sanggan River Valley in Middle Ancient Times --Discussing the Reason Why the Northern Wei Dynasty Makes Pingeheng Be Its Capital at the Same Time%中古时期桑干河流域农牧环境的变迁——兼论北魏为何定都平城

    Institute of Scientific and Technical Information of China (English)

    孙靖国

    2012-01-01

    Since the Late Han Dynasty, there have been the differences of economic forms in the Sanggan River Valley. In the south, farming economy is maintained or recovered in different periods and the farmers immigrated in the period of the Northern Wei settled. While in the north, it has been the complete animal husbandry economy since the Late Han Dynasty and the nomadic, fishing and hunting tribes settled. As a result, the economic structure of infertile north Sanggan River is formed in the Northern Wei Dynasty. Among the cities in Daibei region, Pingcheng lies in the north of Yinshan Mountain, the middle of the three roads for Xianbei tribe to enter Sanggan River Valley. At the same time, it is also the settlement of immigranted Xianbei tribe. Therefore, it is convenient to communicate farming and animal husbandry economy and to control the whole valley and even the whole north. Because of these, it begins to be built since Yilu and finally becomes the capital.%汉末以来,桑干河(湮水)流域内的经济形态存在一定的差别:桑干河南,在不同时期保留或恢复了不同程度的农耕经济,北魏时期迁徙畿内的农耕居民多安置于此地;而在其北部,自汉末以来就完全畜牧和狩猎化,北魏时期更是迁徙了大批游牧、渔猎民族于此,并修建了规模宏大的苑囿。更适合作为牧民和猎手的“国人”居住。所以在北魏时期,形成了“漫北地瘠”的经济格局。在代北地区的众多城市中,平城位于阴山以北拓跋鲜卑故地进入桑干河流域的三条主要陉道中居中者,地处漫北的国人聚居区,便于沟通草原游牧社会与中原农耕区域,控制整个桑干河流域乃至华北地区.所以自猗卢时代即开始经营。最终定都于此。

  19. Creating a catchment scale perspective for river restoration

    OpenAIRE

    L. Benda; MILLER, D; J. Barquín

    2011-01-01

    One of the major challenges in river restoration is to identify the natural fluvial landscape in catchments with a long history of river control. Intensive land use on valley floors often predates the earliest remote sensing: levees, dikes, dams, and other structures alter valley-floor morphology, river channels and flow regimes. Consequently, morphological patterns indicative of the fluvial landscape including multiple channels, extensive floodplains, wetlands, and fluvial-riparian and tribu...

  20. Environmental Contaminants in River Otter (Lontra canadensis) Collected from the Willamette River, Oregon, 1996-99

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The Willamette River originates in the Cascade Mountains southeast of Eugene, Oregon and makes a 300 mile northward journey through the Willamette Valley, joining...

  1. Composición, estructura y diversidad de la comunidad arbórea del bosque tropical caducifolio en Tziritzícuaro, Depresión del Balsas, Michoacán, México

    OpenAIRE

    Moisés Méndez-Toribio; Juan Martínez-Cruz; Jorge Cortés-Flores; Francisco Javier Rendón-Sandoval; Guillermo Ibarra-Manríquez

    2014-01-01

    Se describe la composición, estructura y diversidad de los árboles del bosque tropical caducifolio en Tziritzícuaro, municipio de La Huacana, en la Depresión del Balsas, Michoacán. Se censaron todos los árboles enraizados dentro de 36 parcelas de 100 m 2 (0.36 ha) con un diámetro a la altura del pecho (DAP) 1 cm. Se registraron 78 especies, incluidas en 50 géneros y 24 familias. La familia Fabaceae fue la más importante respecto a su número de especies (24), géneros (14) e individuos (274). ...

  2. Valley Density Evaluation and Typical Development Pattern in Mountainous Areas of Beijing

    Institute of Scientific and Technical Information of China (English)

    MU Song-lin; ZHANG Yi-feng; WANG Kai-yong; TANG Cheng-cai; WANG Ling-en; LIU Yu

    2012-01-01

    Based on geographical differences and space differentiation, valley economy is a new pattern and new perspective for the development of mountainous areas, integrating ecological protection, industrial nurture, and village integration. On the basis of natural and geographical differentiation of valley, we give an overview of the spatial distribution of valley in mountainous areas of Beijing and spatial difference in valley density, and sum up the typical development pattern of valley economy, using DEM data. The results show that the spatial distribution of valley presents an asymmetric shape of inverted V or branch; Miyun, Yanqing, and Changping have high valley density, while Pinggu, Fangshan and Mentougou have low valley density; there is a significant positive relationship between valley density and the spatial distribution of river and reservoir. The development pattern of valley economy is divided into five types: leisure and high-end upgrade-based pattern, ecological development and transition demonstration-based pattern, folk culture and creation-driven pattern, scenic spots-driven and valley-linked pattern and leisure agriculture and specialty-led pattern.

  3. On the Origin and Function of Moat-surrounded Settlements in the Middle Changjiang River Valley in the Light of the Moat-surrounded Settlement at Menbanwan%从门板湾城壕聚落看长江中游地区城壕聚落的起源与功用

    Institute of Scientific and Technical Information of China (English)

    王红星

    2003-01-01

    The present paper analyzes the moat-surrounded settlement at Menbanwan and on this basis makes a comprehensive study of Neolithic moat-surrounded settlements in the middle Changjiang River valley. Referring to the available information of the environmental changes, the paper comes to the conclusion that moat-surrounded settlements originated from ditch-surrounded settlements and came into being as a necessary result of environmental changes and the evolution of settlement pattern. The main function of the moat was to control floods and to resist the intrusion of external disaster victims. Actually these settlements constituted a type of central settlement in special geographical settings and essentially differed from cities of the civilized period. Their emergence played a very important role in the birth of civilization.

  4. Ocorrência de infecção natural de Fasciola hepatica Linnaeus, 1758 em Lymnaea columella Say, 1817 no Vale do Paraíba, SP, Brasil Natural infection by Fasciola hepatica in Lymnaea columella in the Paraíba river valley, S. Paulo, Brazil

    Directory of Open Access Journals (Sweden)

    Marlene Tiduko Ueta

    1980-06-01

    Full Text Available Foram registradas em Piquete, no vale do rio Paraíba do Sul (SP, Brasil, taxas de 1,22% e 0,14% de infecção natural em Lymnaea columella, por Fasciola hepatica. Em um único exemplar de Lymnaea columella dentre os 1.052 examinados, foram observadas rédias com xifidiocercárias, rédias com cercárias de Fasciola hepatica e metacercárias de Echinostomatidae.Infection rates of 1.22% and 0.14% were obtained in Lymnaea columella snails naturally infected by Fasciola hepatica. Samples of the snails were collected in Piquete, a municipality of Paraíba do Sul, a river valley area in the State of S. Paulo. Also observed was one of the 1052 specimen of the Lymnaea columella rediae which had xiphidiocercariae and rediae with Fasciola hepatica cercariae and metacercariae of Echinostomatidae.

  5. Valley-contrasting orbital angular momentum in photonic valley crystals

    CERN Document Server

    Chen, Xiaodong; Dong, Jianwen

    2016-01-01

    Valley, as a degree of freedom, has been exploited to realize valley-selective Hall transport and circular dichroism in two-dimensional layered materials. On the other hand, orbital angular momentum of light with helical phase distribution has attracted great attention for its unprecedented opportunity to optical communicagtions, atom trapping, and even nontrivial topology engineering. Here, we reveal valley-contrasting orbital angular momentum in all-dielectric photonic valley crystals. Selective excitation of valley chiral bulk states is realized by sources carrying orbital angular momentum with proper chirality. Valley dependent edge states, predictable by nonzero valley Chern number, enable to suppress the inter-valley scattering along zigzag boundary, leading to broadband robust transmission in Z-shape bend without corner morphological optimization. Our work may open up a new door towards the discovery of novel quantum states and the manipulation of spin-orbit interaction of light in nanophotonics.

  6. O Crescimento de duas espécies florestais pioneiras, pau-de-balsa (Ochroma lagopus Sw. e caroba (Jacaranda copaia D. Don, usadas para recuperação de áreas degradadas pela agricultura na Amazônia Central, Brasil Growth of two forest pioneer species, pau-de-balsa (Ochroma lagopus Sw. e caroba (Jacaranda copaia D. Don, used for rehabilitation of degraded areas from agriculture in Central Amazon, Brazil

    Directory of Open Access Journals (Sweden)

    Antenor Pereira Barbosa

    2003-01-01

    Full Text Available O objetivo deste trabalho foi estudar o crescimento das espécies florestais pioneiras pau-de-balsa (Ochroma lagopus Sw. e caroba (Jacaranda copaia D. Don para a recuperação de áreas degradadas pela agricultura. Na área, situada no km 120 da BR-174, tinha sido plantado mandioca e banana e abandonada há 8 anos, formando uma capoeira de porte baixo e rala. O experimento foi instalado em maio/98, com e sem gradagem da área. O espaçamento foi de 3x3m, em covas de 20 cm (diâmetro x 30 cm (profundidade, com adubação de 150g/cova de NPK (4-16-8 e calcário dolomítico na proporção de 3:1. Para a avaliação do crescimento, foram medidas a altura e o diâmetro das plantas aos 2 meses (julho/98 e a cada ano aproximadamente (junho/99, setembro/00 e maio/01. Os dados foram analisados através do delineamento inteiramente casualisado. A sobrevivência do pau-de-balsa foi maior em área gradeada (97,1% do que em area não gradeada (92,5%, após o primeiro ano do plantio; da caroba, foi cerca de 90% e sem diferenças entre as areas. A altura e diâmetro do pau-de-balsa, foram maiores em área gradeada, a partir do primeiro ano, chegando no terceiro ano a 11,85 m de altura e 11,42 cm de diâmetro. Na caroba, a diferença ocorreu a partir do segundo ano e no terceiro chegou a 8,37 m de altura e 11,18 cm de diâmetro. Além de outros fatores inerentes às espécies, o solo mais friável das áreas gradeadas, possibilitou um maior crescimento em altura e diâmetro das duas espécies estudadas.The objective of experiment was study the growth of pioneer forest species pau-de-balsa (Ochroma lagopus and caroba (Jacaranda copaia to rehabilitate degraded areas from agriculture. The experiment carried out at Br-174, km 120. After the use for cassava and banana plantations the area was abandoned for 8 years. The secondary forest that took place was of low height and sparse trees. The experiment was installed at may/98 and composed by harrowed and no harrowed

  7. The dating and interpretation of a Mode 1 site in the Luangwa Valley, Zambia

    DEFF Research Database (Denmark)

    Barham, Lawrence; Phillips, William M.; Maher, Barbara A.;

    2011-01-01

    artefacts in the Luangwa Valley, Zambia. The Manzi River, a tributary of the Luangwa River, has exposed a 4.7 m deep section of fluvial sands with discontinuous but stratified gravel layers bearing Mode 1, possibly Oldowan, artefacts in the basal layers. An unconformity divides the Manzi section, separating...

  8. 沱江流域两种人工针叶林群落结构比较%Comparison of community structure between two artificial coniferous forests in the Tuojiang River Valley

    Institute of Scientific and Technical Information of China (English)

    陈文年; 卿东红; 张轩波

    2011-01-01

    采用样方调查法比较了沱江流域两种人工针叶林群落的结构.结果表明,湿地松林中湿地松幼苗幼树很少;马尾松林中有较多的马尾松幼苗幼树.马尾松种群多度比湿地松种群大38%,而湿地松种群的平均高度、平均冠幅比马尾松种群分别大32.7%和22.2%.从高度结构及径级结构来看,马尾松种群在各个级别上都有分布;而在湿地松种群中,没有Ⅰ级和Ⅱ级的幼苗和小树,种群中以大树为主,呈现出更新不良.马尾松在各个树高级别上都形成一定的盖度,但湿地松在1 m以下不形成盖度,反映出湿地松缺乏幼苗幼树,这与树高及径级研究中得出的结果是一致的.乔木层地上生物产量是湿地松林大于马尾松林;而灌木层地上生物产量却是马尾松林大于湿地松林;草本层地上生物产量则在两种林分中则无明显差异.湿地松林灌木层和草本层的物种多样性都比马尾松林低一些,这与湿地松林乔木层盖度较大,对林下灌草层的阴蔽作用有关.从快速绿化及用材的角度来看,湿地松更适合于当地大面积的推广种植.%By using plot sample method, community structure of two artificial forests were studied in a low mountain area of the Tuojiang River Valley. The results showed that there were less Pinus elliottii seedlings and saplings in P. elliottii community compared with P. massoniana community. Individuals of P. massoniana were 38% more than those of P. elliottii. However, average hight and average diameter of tree crown of P. elliottii were 32. 7% and 22. 2% bigger than that of P. massoniana, respectively. Judged from height and DBH (diameter at breast height)structure,individuals of P. massoniana distributed through all classes. On the contrary, P. elliottii population had no individuals of class Ⅰ and Ⅱ,and was dominated by the biggest trees, suggesting that it was difficult for the population to regenerate in the future. P

  9. Percentage of uric acid calculus and its metabolic character in Dongjiang River valley%广东东江流域泌尿系结石患者中尿酸结石的比例和代谢特点

    Institute of Scientific and Technical Information of China (English)

    钟红兴; 安庚

    2009-01-01

    Objective To study the percentage of uric acid calculus in urolithus and its metabolic character in Dongjiang River valley. Methods To analyze the chemical composition of 290 urinary stones by infrared (IR) spectroscopy and study the ratio changes of uric acid calculus. Uric acid calculus patients and healthy people were studied. Personal characteristics, dietary habits were collected. Conditional logistic regression was used for data analysis and studied the dietary risk factors of uric acid calculus. Patients with uric acid calculus, calcium oxalate and those without urinary calculus were undergone metabolic evaluation analysis. The results of uric acid calculus patients compared to another two groups to analysis the relations between the formation of uric acid calculus and metabolism factors. Results Uric acid calculi were found in 53 cases (18.3%). The multiple logistic regression analysis suggested that low daily water intake, eating more salted and animal food, less vegetable were very closely associated with uric acid calculus. Comparing to calcium oxalate patients, the urine volume, the value of pH, urine calcium, urine oxalic acid were lower, but uric acid was higher than it. The value of pH, urine oxalic acid and citric acid were lower than them, but uric acid and urine calcium were higher than none urinary calculus peoples. Blood potassium and magnesium were lower than them. Conclusions The percentage of uric acid stones had obvious advanced. Less daily water intake, eating salted food, eating more animal food, less vegetables and daily orange juice intake, eating sea food are the mainly dietary risk factors to the formation of uric acid calculus. Urine volume, the value of pH, citric acid, urine calcium, urine uric acid and the blood natrium, potassium, magnesium, calcium, uric acid have significant influence to the information of uric acid stones.%目的 分析广东东江流域泌尿系结石患者中尿酸结石的比例及其代谢特点.方法

  10. Adubação verde com leguminosas em videira no submédio São Francisco Green manuring grapevine with legumes in the submiddle São Francisco River Valley

    Directory of Open Access Journals (Sweden)

    C. M. B. Faria

    2004-08-01

    Full Text Available Os solos do Vale do Submédio São Francisco são, de modo geral, arenosos, com baixa capacidade de retenção de nutrientes e, por se localizarem numa região semi-árida, são muito pobres em matéria orgânica, conseqüentemente, são deficientes em N, tornando-se limitante para produção agrícola. Dessa forma, o uso de leguminosas como adubo verde pode contornar esse problema, porque adiciona C e N ao solo. O trabalho constituiu-se de dois experimentos de leguminosas consorciadas com a cultura da videira (Vitis vinifera irrigada, realizados em um Argissolo Amarelo de textura arenosa, em Petrolina (PE, de junho de 1996 a julho de 2002, com o objetivo de avaliar o efeito da adubação verde nas características químicas do solo e na produtividade e qualidade da uva. O primeiro experimento foi realizado até à quarta safra de uva. Os tratamentos foram representados por duas leguminosas: crotalária (Crotalaria juncea e feijão-de-porco (Canavali