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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. Late Pleistocene and Holocene environmental history of the Iguala Valley, Central Balsas Watershed of Mexico.

    Science.gov (United States)

    Piperno, D R; Moreno, J E; Iriarte, J; Holst, I; Lachniet, M; Jones, J G; Ranere, A J; Castanzo, R

    2007-07-17

    The origin of agriculture was a signal development in human affairs and as such has occupied the attention of scholars from the natural and social sciences for well over a century. Historical studies of climate and vegetation are closely associated with crop plant evolution because they can reveal the ecological contexts of plant domestication together with the antiquity and effects of agricultural practices on the environment. In this article, we present paleoecological evidence from three lakes and a swamp located in the Central Balsas watershed of tropical southwestern Mexico that date from 14,000 B.P. to the modern era. [Dates expressed in B.P. years are radiocarbon ages. Calibrated (calendar) ages, expressed as cal B.P., are provided for dates in the text.] Previous molecular studies suggest that maize (Zea mays L.) and other important crops such as squashes (Cucurbita spp.) were domesticated in the region. Our combined pollen, phytolith, charcoal, and sedimentary studies indicate that during the late glacial period (14,000-10,000 B.P.), lake beds were dry, the climate was cooler and drier, and open vegetational communities were more widespread than after the Pleistocene ended. Zea was a continuous part of the vegetation since at least the terminal Pleistocene. During the Holocene, lakes became important foci of human activity, and cultural interference with a species-diverse tropical forest is indicated. Maize and squash were grown at lake edges starting between 10,000 and 5,000 B.P., most likely sometime during the first half of that period. Significant episodes of climatic drying evidenced between 1,800 B.P. and 900 B.P. appear to be coeval with those documented in the Classic Maya region and elsewhere, showing widespread instability in the late Holocene climate. PMID:17537917

  3. Synthetic River Valleys

    Science.gov (United States)

    Brown, R.; Pasternack, G. B.

    2011-12-01

    The description of fluvial form has evolved from anecdotal descriptions to artistic renderings to 2D plots of cross section or longitudinal profiles and more recently 3D digital models. Synthetic river valleys, artificial 3D topographic models of river topography, have a plethora of potential applications in fluvial geomorphology, and the earth sciences in general, as well as in computer science and ecology. Synthetic river channels have existed implicitly since approximately the 1970s and can be simulated from a variety of approaches spanning the artistic and numerical. An objective method of synthesizing 3D stream topography based on reach scale attributes would be valuable for sizing 3D flumes in the physical and numerical realms, as initial input topography for morphodynamic models, stream restoration design, historical reconstruction, and mechanistic testing of interactions of channel geometric elements. Quite simply - simulation of synthetic channel geometry of prescribed conditions can allow systematic evaluation of the dominant relationships between river flow and geometry. A new model, the control curve method, is presented that uses hierarchically scaled parametric curves in over-lapping 2D planes to create synthetic river valleys. The approach is able to simulate 3D stream geometry from paired 2D descriptions and can allow experimental insight into form-process relationships in addition to visualizing past measurements of channel form that are limited to two dimension descriptions. Results are presented that illustrate the models ability to simulate fluvial topography representative of real world rivers as well as how channel geometric elements can be adjusted. The testing of synthetic river valleys would open up a wealth of knowledge as to why some 3D attributes of river channels are more prevalent than others as well as bridging the gap between the 2D descriptions that have dominated fluvial geomorphology the past century and modern, more complete, 3D

  4. 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...

  5. 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

  6. The Red River Valley archeological project

    Science.gov (United States)

    Bennett, Jack; Smith, Lawson; Laustrup, Mark

    1986-01-01

    The Red River Valley Archeology Project is a long-term effort involving numerous individuals and institutions engaged in archeological investigations in the Texas and Oklahoma portions of the Red River Valley. To date the focus of the project was on site location. The project acquired both Thermal Infrared Multispectral Scanner (TIMS), TMS, and color infrared photographs over a significant portion of the project area in an effort to define signatures for archeological sites and to assist in the detailed geomorphological mapping of the flood plain. Preliminary analysis of acquired data indicates that both the TIMS and TMS can make a substantial contribution to landform definition, the identification of cultural resources, and to the clarification of site-landform correlations in this riverine environment.

  7. 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...

  8. 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,...

  9. 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,...

  10. 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

  11. Segetal flora of the Middle Vistula River Valley

    OpenAIRE

    Maria Ługowska

    2014-01-01

    The objective of the study was to describe the segetal flora of the Middle Vistula River Valley. A total of 367 species were recorded in spring and winter cereals, tuber crops, and stubble fields. Such floristic abundance may be due to the fact that the study area is located in the proximity of a river where semi-natural communities interact directly with communities inhabiting cultivated fields and that fields are fragmented and characterised by different habitats. There were more apophytes ...

  12. Segetal flora of the Middle Vistula River Valley

    Directory of Open Access Journals (Sweden)

    Maria Ługowska

    2014-12-01

    Full Text Available The objective of the study was to describe the segetal flora of the Middle Vistula River Valley. A total of 367 species were recorded in spring and winter cereals, tuber crops, and stubble fields. Such floristic abundance may be due to the fact that the study area is located in the proximity of a river where semi-natural communities interact directly with communities inhabiting cultivated fields and that fields are fragmented and characterised by different habitats. There were more apophytes (62% than anthropophytes (38% in the flora studied. Meadow apophytes were the dominant native species (35% and archeophytes were the dominant anthropophytes (69%. The analysis of the life spectrum revealed that there were more therophytes (50% than hemicryptophytes (39%. What is more, non-perennial species constituted 56% and perennials 44% of the segetal flora established in the Middle Vistula River Valley. The large proportion of archeophytes (26% may indicate that traditional farming predominated in the study area.

  13. Integral ordering of the River Vardar Valley

    International Nuclear Information System (INIS)

    From Skopje to Gevgelia, an annual quantity of 4,5 billions M3 of water flows out of the territory through the Vardar River for only 60 hours. This poses two questions. The first is whether the flowing out of the water can be decelerated, i.e., whether the water can be kept for at least 60 days and the second question is how this can be realized. Construction of 12 hydroelectric power plants is envisaged along Vardar River, i.e., its section extending from Skopje to the border on Greece, which means within a length of 200 km. Two of these are classical hydroelectric power plants (HPP 'Veles' and HPP 'Gradec'), while the remaining 10 hydroelectric power plants are distributed in a cascade along the river course, with small water head of H = 8,20 - 8,50 m and are considered ecological hydroelectric power plants according to European criteria. For us, these represent a new technology of design and construction particularly considering the part referring to the equipment, while in Europe, there is assembly-line production of such equipment. Presented very briefly in the paper shall be the main technical information on these hydroelectric power plants, namely HPP Kukuricani, as a pilot project to be realized by AD ESM. (Author)

  14. 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.

  15. 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,…

  16. 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)

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

    International Nuclear Information System (INIS)

    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)

  18. 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...

  19. 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.

  20. 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.

  1. 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

  2. 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

  3. 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.

  4. Composition patterns of waterbirds from la vieja river, geographic valley of cauca river, colombia

    OpenAIRE

    Laura Milena Ramírez-Urrea; Enrique Arbeláez-Cortés; Oscar Humberto Marín-Gómez; Diego Duque-Montoya

    2014-01-01

    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, t...

  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. Valley heat deficit as a bulk measure of wintertime particulate air pollution in the Arve River Valley

    Science.gov (United States)

    Chemel, Charles; Arduini, Gabriele; Staquet, Chantal; Largeron, Yann; Legain, Dominique; Tzanos, Diane; Paci, Alexandre

    2016-03-01

    Urbanized valleys are particularly vulnerable to particulate air pollution during the winter, when ground-based stable layers or cold-air pools persist over the valley floor. We examine whether the temporal variability of PM10 concentration in the section of the Arve River Valley between Cluses and Servoz in the French Alps can be explained by the temporal variability of the valley heat deficit, a bulk measure of atmospheric stability within the valley. We do this on the basis of temperature profile and ground-based PM10 concentration data collected during wintertime with a temporal resolution of 1 h or finer, as part of the Passy-2015 field campaign conducted around Passy in this section of valley. The valley heat deficit was highly correlated with PM10 concentration on a daily time scale. The hourly variability of PM10 concentrations was more complex and cannot be explained solely by the hourly variability of the valley heat deficit. The interplay of the diurnal cycles of emissions and local dynamics is demonstrated and a drainage mechanism for observed nocturnal dilution of near-surface PM10 concentrations is proposed.

  7. 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.

  8. 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.

  9. 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...

  10. 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...

  11. 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...

  12. 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...

  13. 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...

  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. 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...

  16. 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...

  17. EMISSION CHARACTERIZATION OF MAJOR FOSSIL FUEL POWER PLANTS IN THE OHIO RIVER VALLEY

    Science.gov (United States)

    This study characterizes the atmospheric emissions from five major coal-fired power plant units in the Ohio River Valley between Portsmouth, Ohio, and Louisville, Kentucky. This characterization provides data that are representative of the boiler fuel emission control combination...

  18. 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...

  19. 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...

  20. 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....

  1. Fire Management Plan for Rappahannock River Valley National Wildlife Refuge 2002

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The Rappahannock River Valley National Wildlife Refuge is a relatively new refuge, and does not yet have a Master Plan, or a Comprehensive Conservation Plan....

  2. [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

  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. 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...

  5. 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.

  6. Extraction and characterization of cellulose nano whiskers from balsa wood

    International Nuclear Information System (INIS)

    In this study cellulose nano whiskers were obtained from balsa wood. For this purpose, fibers of balsa wood were subjected to hydrolysis reactions for lignin and hemi cellulose digestion and acquisition of nano-scale cellulose. Cellulose nano crystals obtained had medium length and thickness of 176 nm and 7 nm respectively. Infrared spectroscopy and x-ray diffraction showed that the process used for extracting nano whiskers could digest nearly all the lignin and hemi cellulose from the balsa fiber and still preserve the aspect ratio and crystallinity, satisfactory enough for future application in polymer nano composites. Thermogravimetry showed that the onset temperature of thermal degradation of cellulose nano crystals (226 degree C) was higher than the temperature of the balsa fiber (215 degree C), allowing its use in molding processes with many polymers from the molten state.(author)

  7. 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.

  8. 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.

  9. The evolution of the Shiwanghe River valley in response to the Yellow River incision in the Hukou area, Shaanxi, China

    Science.gov (United States)

    Qiu, Wei-Li; Zhang, Jia-Fu; Wang, Xiao-Yan; Guo, Yu-Jie; Zhuang, Mao-Guo; Fu, Xiao; Zhou, Li-Ping

    2014-06-01

    Tributary response to mainstream incision is an important landscape evolution process. The objective of this study is to examine tributary valley evolution in response to mainstream incision. The Shiwanghe River, a tributary of the Yellow River in the Hukou area, was chosen for a case study. The terraces and knickpoints of the Shiwanghe River were investigated and correlated to those of the mainstream. Optically stimulated luminescence (OSL) was applied to date fluvial terraces. Longitudinal profiles of river and terraces were used to analyze valley evolution. The terrace sequence of the Shiwanghe River near their confluence is almost identical to the Yellow River terraces at the Hukou area. This suggests that terrace formations of the tributary and the mainstream are synchronous, and influenced by similar factors. But the formation age of the same tributary terrace varies from downstream to the upper reaches of the river valley. For such terraces, their formation should be controlled by knickpoint migration. A sudden drop in base-level caused by the Yellow River incision would trigger the formation of a knickpoint in the tributary. A new terrace would be formed as the knickpoint propagated upstream throughout the tributary valley. Due to the different erodibility of bedrock, a set of interbedded sandstone and shale, the major knickpoint would disassemble into a cluster of small ones during its propagation. The age of terrace formation with various valley segments depends on knickpoint migration rate and distance from the confluence. Vertical incision of the Yellow River results in knickpoint recession of its tributaries. The migration rate of knickpoints was affected by climate, lithologic variation, and, to some extent, structural control.

  10. 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.

  11. 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...

  12. 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...

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

    OpenAIRE

    Lesniewska,Malgorzata; Jastrzębski,Piotr; Stańska, Marzena; Hajdamowicz, Izabela

    2015-01-01

    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 (M...

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

    OpenAIRE

    Malgorzata Lesniewska; Piotr Jastrzębski; Marzena Stańska; Izabela Hajdamowicz

    2015-01-01

    Abstract 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. Lit...

  15. 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.

  16. 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

  17. 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

  18. 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...

  19. 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.

  20. Flood Frequency Analysis for Jiya Dhol River of Brahmaputra Valley

    OpenAIRE

    Luna Moni Das; Zahid Husain Qureshi

    2014-01-01

    Flood frequency analysis is an important mathematical modelling technique in determining the return period of the probability of witnessing a particular discharge in a river, especially a peak discharge. Floods as periodic events in a river basin are associated with high discharge. In flood frequency analysis the annual peak discharge in a river is fitted in different probability distributions. Three important statistical methods, most commonly used in flood frequency analysis, are - Gumbel’s...

  1. 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.

  2. First record of Diatraea tabernella in the Cauca River Valley of Colombia

    Science.gov (United States)

    Diatraea tabernella (Dyar) is first recorded in the Cauca River Valley of Colombia. Even though information on its status has been unknown for almost a century in Colombia, its recent register creates concern about its potential economic importance in virtue of its abundance and distribution in the ...

  3. 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...

  4. 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...

  5. 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.

  6. 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

  7. 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

  8. 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

  9. 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...

  10. 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...

  11. 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...

  12. 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....

  13. 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.

  14. 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...

  15. Migrants and AIDS: Risk Management versus Social Control. An Example from the Senegal River Valley

    OpenAIRE

    Richard Lalou; Victor Piché

    2004-01-01

    Even though numerous previous studies have demonstrated the existence of a relationship between mobility and AIDS, the complex mechanisms subjacent to this relationship still remain relatively unknown. The study presented here is based on a survey carried out in 2000 in the Senegal River valley. It specifically examines the link between migration and risky sexual behaviour in the return zone (risk of spread) by using a conceptual framework which takes into consideration (1) various types of m...

  16. [Relationships between biochemical qualities of paddy rice and climate conditions in the Anning River Valley].

    Science.gov (United States)

    Peng, Guozhao; Bai, Jian; Wang, Jingbo

    2004-12-01

    Based on the experimental data of paddy rice planted geographically periodically without control in the Anning River Valley of Sichuan Province, this paper quantitatively analyzed the effects of meteorological conditions from 40 days before heading to ripeness on the biochemical qualities of paddy rice, and developed a model about the integrated relationships between biochemical qualities of paddy rice and mean temperature, daily range of temperature and daylight hours, which would be of significance both for the instruction of paddy distribution in the Anning River Valley and for improving rice qualities via adjusting planting time. The results showed that climate conditions had a great effect on the biochemical qualities of paddy rice, which was different in ways and in critical periods. The period when the correlation between some ingredients of rice and climate conditions was most significant was before or after, or from before to after full heading, which widened the existing knowledge about the period which was important for paddy rice qualities forming. Applying this finding in the Anning River Valley during 2002-2003, the accumulated high-grade paddy farming area stood at 73,000 hm2, 30,000 hm2 more than that in 2001, and brought 0.2 billion yuan increment to the peasants, promoting the development of high-grade paddy greatly. PMID:15825441

  17. 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...

  18. Debris Flow Control on Fluvial Hanging Valley Formation in the South Fork Eel River, CA

    Science.gov (United States)

    Deshpande, N.; Perkins, J.; Finnegan, N. J.

    2012-12-01

    An understanding of how base level signals are transmitted into landscapes is fundamental to interpreting river long profiles in tectonically active settings. Fluvial hanging valleys, locations where waves of incision have apparently arrested at tributary junctions, suggest that base level propagation is an unsteady process in many settings. A recent hypothesis (Wobus et al., 2006) explains the formation of fluvial hanging valleys via an instability in the saltation abrasion model of Sklar and Dietrich (2004). At locations where small steep tributaries join trunk streams, tributary incision rates can actually decrease with increasing channel slope when subjected to downstream base-level fall. However, we note that in mountainous river networks steep tributaries also commonly convey debris flows into trunk channels. Since these tributary junctions mark the upstream limit of channels whose beds are mobilized on a regular basis during flood events, here we hypothesize that transitions from fluvial to debris flow channels control the location of fluvial hanging valleys. To test our hypothesis, we exploit a natural experiment in base level fall and landscape evolution along the South Fork Eel River, which is argued to be responding to an increase in rock uplift rate associated with the passage of the Mendocino Triple Junction. In order to separate debris flow channels from fluvial channels, we use airborne laser swath mapping (ALSM) to quantify channel slopes and concavities. In our analysis, concavity data are noisy and represent a poor metric for determination of debris flow channels. In lieu of this, we choose a more straightforward metric of channel slope to discriminate where debris flows occur on the landscape. We find that, on average, fluvial hanging valleys are only present in tributaries with average gradients above 0.10, consistent with empirical determinations of the gradient at which debris flow channels transition to fluvial channels (0.03-0.10). Field

  19. 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.

  20. 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.

  1. 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.

  2. 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.

  3. 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.

  4. 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.

  5. 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.

  6. Climatic changes and isotopic content along the River Nile valley

    International Nuclear Information System (INIS)

    Full text: The stable isotope composition of rain and snow has considerable variation with climatology, with geography and with time at a given location. This variation primarily results from the lower vapour pressure of water molecules which contain heavy isotopes of deuterium and oxygen-18 compared to molecules consisting of only the lightest. Because of vapour pressure differences, heavier isotopes tend to be enriched in liquid phase relative to vapour phase. Subsequent precipitation formed from the depleted vapour will be progressively 'lighter' in stable isotope composition. Surface waters became enriched in deuterium and oxygen-18 relative to their initial isotopic composition as losses by evaporation occur. According to the IAEA precipitation sampling at Entebbe, which represent the source region of white Nile, with isotopic composition range (-33 to +4 per mille in δD and -5.7 to -1.1 in δ18O). The isotopic composition of precipitation station at Addis Ababa which is the main source of Blue Nile ranges from -8.4 to +7 per mille in δD and from -0.7 to -2.27 per mille in δ18O. Assuming the Central Africa run-off contribution to white Nile downstream of the Sudan represents 20% of natural discharge to Egypt, and the balance 80% is derived from Ethiopia (Blue Nile), we obtain a composite stable isotope composition of δD=-1 per mille and δ18O=-1.8 per mille, as an order of magnitude estimate on the probable long term stable isotope composition of the River Nile reaching upper Egypt under natural condition (before High Dam construction). Stable isotopes were used to estimate the evaporation from Naser Lake at the High Aswan Dam. According to isotopic content, the lake can be divided into two sectors; the first sector with pronounced vertical isotope gradients, and the second with subdued isotope gradients. Isotope content in surface waters varies with time and environmental effects (humidity, wind velocity,temperature, etc.). In order to detect this effect

  7. 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

  8. 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

  9. 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

  10. 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).

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

    Energy Technology Data Exchange (ETDEWEB)

    Ednie, M.; Wright, J.F.; Duchesne, C. [Natural Resources Canada, Ottawa, ON (Canada). Geological Survey of Canada

    2007-07-01

    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. 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

  13. Agronomic and molecular traits of the 'Italia Muscat' clone in Sao Francisco River Valley

    Directory of Open Access Journals (Sweden)

    Patrícia Coelho de Souza Leão

    2011-03-01

    Full Text Available The objective of this study was to evaluate agronomic and molecular traits of the 'Italia Muscat' clone and compare it with the cv. 'Italia', providing information to support the cultivation of 'Italia Muscat' this cultivar in the São Francisco River Valley. Agronomic characteristics of both clones were evaluated for two seasons in 2004. The characteristics were phenology, bud break (%, bud fertility (%, yield (kg mass of bunches (g, length and width of bunches (cm, mass of berries (g, length and diameter of berries (mm, TSS (ºBrix, ATT (% titratable acidity and TSS/TTA. Molecular analysis of seven SSR markers were carried out. The clone 'Italia Muscat' showed larger berries, mass of bunches and better TSS/TA ratio than 'Italia'. The molecular analysis resulted in the same allelic profile in both clones, highlighting the need to use a larger number of microsatellite markers or other molecular technique to allow their discrimination. Based on their morpho-agronomic characteristics, 'Italia Muscat' seems to be a good table grape cultivar alternative for grape growers of São Francisco River Valley.

  14. 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

  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. 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.

  18. 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.

  19. 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)

  20. 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

  1. 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

  2. Radioecological meta-database on the Yenisei river Catchment and Valley

    International Nuclear Information System (INIS)

    Results of development of a sophisticated information system, including a meta-database for assessment of radiation impact on the population and natural environment in the Krasnoyarsk region of the Russian Federation are presented. The radioactive contamination of the Krasnoyarsk region has been formed in a number of stages: - 1954-1958 small global fallout from nuclear tests; - 1958-1969 maximum global fallout jointly with the Mining and Chemical Combine (MCC) radionuclide air releases and discharges of its single-pass nuclear reactors (commissioned in 1958 and 1964) into the Yenisei river; - 1969-1986 - MCC releases and discharges after the Krasnoyarsk hydroelectric plant dam, controlling the river water flow, had been built; - 1986-1992 MCC releases and discharges and long-distance Chernobyl fallout; - after 1992 after ceasing direct MCC discharges into the river (the single-pass reactors were shut-down) the formed contamination has been being redistributed due to natural processes in the valley and on the catchment. Primary data from various institutions and agencies of Russia have been analysed and compiled into files, corresponding to the different periods. The files are described in the metadatabase. The work is being carried out under the ISTC no. 2097 project. (author)

  3. 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...

  4. 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.

  5. 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...

  6. Migration of 137Cs artificial radionuclide in the valley of the Takhtakushuk river of the Degelen massif

    International Nuclear Information System (INIS)

    Study of horizontal and vertical radionuclide distribution in the valley of the Takhtakushuk River of the 'Degelen' Massif is carried out in the framework of ecological and biological investigations of soil and plant cover within radioactive contaminated areas, and radionuclide migration in biological chain 'soil - plant - animal'. For the first time, the pool-type method was used in the studies of soil of the valley that allows tracing solid and liquid substances migrating by means of surface and soil drainage from its head to final part. This paper presents some physical and chemical properties of the study landscape's soils, radionuclide content in soil genetic horizons of the valley. The study results showed that major mass of 137Cs radionuclide is sorbed by soil humus and fine-dispersed clay particles of grass soils within the valley. (author)

  7. 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...

  8. 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.

  9. 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.

  10. Trace element concentrations on fine particles in the Ohio River Valley

    International Nuclear Information System (INIS)

    Atmospheric particles were collected from May, 1980 to Dec., 1981 at 3 sampling sites in the Ohio River Valley (ORV). The collected samples were analyzed by x-ray fluorescence (XRF) for elemental concentrations and their masses determined by β gauging. The XRF data and associated wind trajectories were used to select a subset (200) of ORV samples in the fine fraction for further analysis by instrumental neutron activation analysis (INAA). Combined XRF and INAA data provided concentration values for up to 40 elements. Chemical mass balances with 11 sources were used to fit trace element concentrations. About 90% of the predicted mass arises from the regional sulfate component, which accounts for most of the observed sulfur. Sulfate concentrations are nearly as high at the west station (in KY) as at the center (IN) and east (OH) stations in disagreement with the usual picture of build-up of sulfate in air masses as they move up the valley, picking up SO2, which is slowly converted to sulfate. Even when back trajectories are used to limit consideration to samples of air masses coming from the southwest, the picture remains despite the lack of strong sources upwind in MO, AK and OK. The authors find no reasonable way in which to fit observed sulfate concentrations and SSe ratios with a simple hybrid receptor model

  11. Hazard assessment of landslide and debris flow in the Rjeina river valley, Croatia

    Science.gov (United States)

    Wang, Chunxiang; Watanabe, Naoki; Marui, Hideaki

    2013-04-01

    The Rječina River extends approximately 18.7km long and flows into the Adriatic Sea at the center of Rijeka City, Croatia. Landslide, debris flow and rockfall are main geohazards in the middle part of the Rječina river basin. The zone between the Valići reservoir dam and the Pasac Bridge is particularly the most unstable and hazardous area in the river basin. The Grohovo landslide in the middle part of the river basin is located on the valley's slope facing southwest and situated at just downstream of the Valići dam. This landslide is the largest active landslide along the Adriatic Sea coast in Croatia. Assuming that serious heavy rainfall or earthquake occurs, it is most likely to occur two types of geohazard event. One scenario is that the debris deposited on the Grohovo landslide will move down to the channel of the Rječina River and dam up the river course. Another scenario is that the slope deposits on the landslide will be mixed with water and subsequently turn into a debris flow reaching to Rijeka City. We simulate both two cases of the formation of landslide-dam and the occurrence of debris-flow by two integrated models using GIS to represent the dynamic process across 3D terrains. In the case of the formation of landslide-dam, it is assumed that slope deposits will move downhill after failing along a shear zone. GIS-based revised Hovland's 3D limit equilibrium model is used to simulate the movement and stoppage of the slope deposits to form landslide-dam. The 3D factor of safety will be calculated step by step during the sliding process simulation. Stoppage is defined by the factor of safety much greater than one and the velocity equal to zero. The simulation result shows that the height of the landslide-dam will be nine meters. In case of debris flow, the mixture of slope deposits and water will be differentiated from landslide by fluid-like deformation of the mobilized material. GIS-based depth-averaged 2D numerical model is used to predict the

  12. Groundwater Quality and Nitrogen Use Efficiency in Nebraska's Central Platte River Valley.

    Science.gov (United States)

    Ferguson, Richard B

    2015-03-01

    Groundwater nitrate contamination has been an issue in the Platte River Valley of Nebraska since the 1960s, with groundwater nitrate-N concentrations frequently in excess of 10 mg L. This article summarizes education and regulatory efforts to reduce the environmental impact of irrigated crop production in the Platte River Valley. In 1988, a Groundwater Management Area (GWMA) was implemented in the Central Platte Natural Resources District to encourage adoption of improved management practices. Since 1988, there have been steady declines in average groundwater nitrate-N concentrations of about 0.15 mg NO-N L yr in much of the GWMA (from 19 to 15 mg NO-N L). However, N use efficiency (NUE) (partial factor productivity for N [PFP]) has increased very little from 1988 to 2012 (60-65 kg grain kg N), whereas statewide PFP increased from 49 to 67 kg grain kg N in the same period. Although growers are encouraged to credit N from sources besides fertilizer (e.g., soil residual, legumes, irrigation water, and manure), confidence in and use of credits tended to decrease as credits became larger; there was a tendency toward an average N rate regardless of credit-based recommendations. This information, coupled with data from other studies, suggests that much of the decline in groundwater nitrate can be attributed to improved irrigation management-especially conversion from furrow to sprinkler irrigation-and to a lesser extent to improved timing of N application. The development and adoption of improved N management practices, such as fertigation, controlled-release N formulation, and use of crop canopy sensors for in-season N application may be required for further significant NUE gains in these irrigated systems. PMID:26023964

  13. 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...

  14. Anthropogenic and Geologic Influence on the Downstream Fining Pattern of the Cosumnes River, Central Valley, California

    Science.gov (United States)

    Fehr, C. R.; Mount, J. F.

    2001-05-01

    A geomorphic survey of the Cosumnes River was conducted to identify the effects of anthropogenic change and local geology on downstream changes in grain size. Patterns of downstream fining exhibited by alluvial rivers reflect the processes of abrasion and sediment sorting by selective entrainment, transport and deposition. Longitudinal sorting of gravel is commonly modeled as a downstream exponential decrease in median particle grain size over the length of the profile. This relationship mirrors downstream reduction in gradient and bed shear stress typical of aggrading alluvial channels and is influenced by variations in sediment supply. The impacts of anthropogenic activity on these variables should be reflected by departures in downstream fining patterns from the expected trend. Results from this study show that grain-size change over the longitudinal profile deviates significantly from the predicted model. In addition, grain-size measurements at cross-sections demonstrate poor correlation with average bankfull bed shear stress. At sites where grain size appears unrelated to distance downstream as well as to energy slope, sediment transport may be directly influenced by alterations to the channel such as in-stream mining and the construction of diversion dams. Fluvial response to the cumulative effects of watershed-scale anthropogenic activities has also contributed to the modification of the nature of sediment transport in the channel. Prior to settlement of the Great Valley, the Cosumnes was a shallow, anastomosing alluvial river connected to a broad floodplain. Changes in land-use practices as well as channel regulation have caused rapid river-bed degradation and incision into resistant Quaternary alluvial fan deposits in some locations. Unlike the alluvial reaches studied, those with duripan beds and banks are characterized by a step-pool-like structure and contribute only small volumes of coarse sediment to the river. Data suggest that sediment transport in

  15. 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

  16. 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

  17. Map of water table in Solomon River valley, Waconda Lake to Solomon, north-central Kansas, May 1980

    Science.gov (United States)

    Reed, Thomas B.

    1983-01-01

    A map of the water table in the Solomon River valley from Waconda Lake to Solomon presents current (1980) data on water levels in the unconsolidated deposits. The Solomon River, which originates in western Kansas, flows southeastward from Waconda Lake to its confluence with the Smoky Hill River at Solomon. In the study area, its valley is incised into consolidated rocks that are composed mostly of shale and limestone. The unconsolidated deposits in the valley underlie the flood plain and the terrace. The alluvial deposits generally consist of gravel and sand, grading upward to sand and silt, with clay lenses interbedded throughout. Thickness of the deposits may be as much as 70 feet. Ground water in the unconsolidated deposits is a principal source of supply for domestic, stock, and irrigation use. Water-table contours indicate that ground water moves from the alluvial deposits to the stream. Thus, the Solomon River gains in flow through most of the reach. Water-level measurements for this study were made during the spring of 1980, prior to the irrigation season. (USGS)

  18. One year long measurements of traffic air pollutants in the River Inn valley

    International Nuclear Information System (INIS)

    Full text: To complement the routine data acquisition of NO, NO2, CO and PM10 at an environmental monitoring station in the River Inn valley at Vomp (Austria), measurements of certain volatile organic compounds (VOCs) were carried out at this location between February 2004 and May 2005. In addition, meteorological data (wind, vertical temperature profile, etc.) were used to gain an understanding of dispersion and dilution of pollutants in the local valley atmosphere. Furthermore traffic abundance was used to determine the emission-strengths of certain compounds. Daily variations of pollutant levels arise from both traffic abundance and meteorological influences: on the one hand they are due to variations in emission-strengths (heavy duty vehicles ban during the night, rush-hour traffic); on the other hand they result from changing dispersion and dilution conditions for pollutants, such as during nighttime when a low inversion layer develops, that subsequently breaks up during the day. Fortunately dispersion and dilution conditions are mostly well developed during times of high emission strengths. Only in the morning and evening do high emissions occur when there is a poorly developed air exchange, resulting in maximum pollutant levels. For the known carcinogenic agent benzene the EU introduced a target value of 1.5 ppbV as an annual mean to be met by its member states by 2010. The, during this campaign for the first time, measured annual value (1.4.2004 - 31.3.2005) in Vomp was 0.6 ppbV and thus below the guideline limit, whereas PM10 and NO2 were found to exceed the EU guideline limits. (author)

  19. Uranium favorability of tertiary sedimentary rocks of the Pend Oreille River valley, Washington

    International Nuclear Information System (INIS)

    Tertiary sedimentary rocks in the Pend Oreille River valley were investigated in a regional study to determine the favorability for potential uranium resources of northeastern Washington. This project involved measurement and sampling of surface sections, collection of samples from isolated outcrops, chemical and mineralogical analyses of samples, and examination of available water well logs. The Box Canyon Dam area north of Ione is judged to have very high favorability. Thick-bedded conglomerates interbedded with sandstones and silty sandstones compose the Tiger Formation in this area, and high radioactivity levels are found near the base of the formation. Uranophane is found along fracture surfaces or in veins. Carbonaceous material is present throughout the Tiger Formation in the area. Part of the broad Pend Oreille valley surrounding Cusick, Washington, is an area of high favorability. Potential host rocks in the Tiger Formation, consisting of arkosic sandstones interbedded with radioactive shales, probably extend throughout the subsurface part of this area. Carbonaceous material is present and some samples contain high concentrations of uranium. In addition, several other possible chemical indicators were found. The Tiger-Lost Creek area is rated as having medium favorability. The Tiger Formation contains very hard, poorly sorted granite conglomerate with some beds of arkosic sandstone and silty sandstone. The granite conglomerate was apparently derived from source rocks having relatively high uranium content. The lower part of the formation is more favorable than the upper part because of the presence of carbonaceous material, anomalously high concentrations of uranium, and other possible chemical indicators. The area west of Ione is judged to have low favorability, because of the very low permeability of the rocks and the very low uranium content

  20. 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...

  1. 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...

  2. 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...

  3. 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...

  4. 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...

  5. 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...

  6. Map of the Rinconada and Reliz Fault Zones, Salinas River Valley, California

    Science.gov (United States)

    Rosenberg, Lewis I.; Clark, Joseph C.

    2009-01-01

    The Rinconada Fault and its related faults constitute a major structural element of the Salinas River valley, which is known regionally, and referred to herein, as the 'Salinas Valley'. The Rinconada Fault extends 230 km from King City in the north to the Big Pine Fault in the south. At the south end of the map area near Santa Margarita, the Rinconada Fault separates granitic and metamorphic crystalline rocks of the Salinian Block to the northeast from the subduction-zone assemblage of the Franciscan Complex to the southwest. Northwestward, the Rinconada Fault lies entirely within the Salinian Block and generally divides this region into two physiographically and structurally distinct areas, the Santa Lucia Range to the west and the Salinas Valley to the east. The Reliz Fault, which continues as a right stepover from the Rinconada Fault, trends northwestward along the northeastern base of the Sierra de Salinas of the Santa Lucia Range and beyond for 60 km to the vicinity of Spreckels, where it is largely concealed. Aeromagnetic data suggest that the Reliz Fault continues northwestward another 25 km into Monterey Bay, where it aligns with a high-definition magnetic boundary. Geomorphic evidence of late Quaternary movement along the Rinconada and Reliz Fault Zones has been documented by Tinsley (1975), Dibblee (1976, 1979), Hart (1976, 1985), and Klaus (1999). Although definitive geologic evidence of Holocene surface rupture has not been found on these faults, they were regarded as an earthquake source for the California Geological Survey [formerly, California Division of Mines and Geology]/U.S. Geological Survey (CGS/USGS) Probabilistic Seismic Hazards Assessment because of their postulated slip rate of 1+-1 mm/yr and their calculated maximum magnitude of 7.3. Except for published reports by Durham (1965, 1974), Dibblee (1976), and Hart (1976), most information on these faults is unpublished or is contained in theses, field trip guides, and other types of reports

  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. Preliminary report on the geology of the Red River Valley drilling project, eastern North Dakota and northwestern Minnesota

    International Nuclear Information System (INIS)

    Thirty-two wells, 26 of which penetrated the Precambrian, were drilled along the eastern edge of the Williston Basin in the eastern tier of counties in North Dakota and in nearby counties in northwestern Minnesota. These tests, along the Red River Valley of the North, were drilled to study the stratigraphy and uranium potential of this area. The drilling program was unsuccessful in finding either significant amounts of uranium or apparently important shows of uranium. It did, however, demonstrate the occurrence of thick elastic sections in the Ordovician, Jurassic and Cretaceous Systems, within the Red River Valley, along the eastern margins of the Williston Basin which could serve as host rocks for uranium ore bodies

  9. 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.

  10. 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.

  11. 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...

  12. Application of Artificial Neural Networks in Modelling the Hydrological Balance of the Ploucnice River valley, Northern Bohemia (Czech Republic)

    Czech Academy of Sciences Publication Activity Database

    Neruda, M.; Neruda, Roman

    Praha : Academia, 2007 - (Hartel, H.; Cílek, V.; Herben, T.; Jackson, A.; Williams, R.), s. 90-92 ISBN 978-80-200-1577-8 R&D Projects: GA ČR GA526/03/Z042 Institutional research plan: CEZ:AV0Z10300504 Keywords : rainfall-runoff models * Ploucnice River valley * artificial neural networks Subject RIV: DA - Hydrology ; Limnology

  13. Principal disease and Insect pests of Jatropha curcas L. in the lower valley of the Senegal river

    OpenAIRE

    Terren, Marieke; Mignon, Jacques; De Clerck, Caroline; Jijakli, Haissam; Savery, Sebastien; Jacquet de Haveskercke, Paul; Winandy, Stéphane; Mergeai, Guy

    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 panaet...

  14. 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

  15. 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.

  16. 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

  17. 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)

  18. Monitoring agricultural burning in the Mississippi River Valley region from the moderate resolution imaging spectroradiometer (MODIS).

    Science.gov (United States)

    Korontzi, Stefania; McCarty, Jessica; Justice, Christopher

    2008-09-01

    The 2003 active fire observations from the Moderate Resolution Imaging Spectroradiometer (MODIS), on board NASA's Terra and Aqua satellites, were analyzed to assess burning activity in the cropland areas of the Mississippi River Valley region. Agricultural burning was found to be an important contributor to fire activity in this region, accounting for approximately one-third of all burning. Agricultural fire activity showed two seasonal peaks: the first, smaller peak, occurring in June during the spring harvesting of wheat; and the second, bigger peak, in October during the fall harvesting of rice and soy. The seasonal signal in agricultural burning was predominantly evident in the early afternoon MODIS Aqua fire detections. A strong diurnal agricultural fire signal was prevalent during the fall harvesting months, as suggested by the substantially higher number (approximately 3.5 times) of fires detected by MODIS Aqua in the early afternoon, compared with those detected by MODIS Terra in the morning. No diurnal variations in agricultural fire activity were apparent during the springtime wheat-harvesting season. The seasonal and diurnal patterns in agricultural fire activity detected by MODIS are supported by known crop management practices in this region. MODIS data provide an important means to characterize and monitor agricultural fire dynamics and management practices. PMID:18817116

  19. Evapotranspiration from forage grass replacing native vegetation in the Gila River valley of Arizona

    Science.gov (United States)

    Leppanen, O.E.

    1981-01-01

    Estimates of evapotranspiration from an area of forage grass, which had been planted to replace native vegetation of little economic value, were made daily for a 363-day period in 1969 and 1970. The measurement site was located in the Gila River valley in east-central Arizona. The forage, panigrass (Panicum antidotale Retz.), grew from seed during the early summer of 1969 and after winterkill, regrew in 1970. Daily evapotranspiration estimates, which were based on energy budget measurements, ranged from a maximum of 9.2 millimeters to small amounts of condensation. Two daily values of substantial condensation (0.9 and 0.4 millimeter) were of dubious quality, but were retained in the record. The annual evapotranspiration was 989 millimeters, of which about 332 millimeters came from precipitation at the site. The water table fluctuated between 210 and 280 centimeters below land surface. However, the measurement site was near a wash, so that undocumented, shallower subterranean flows may have occurred. (USGS)

  20. 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.

  1. 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.

  2. 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)

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

    Directory of Open Access Journals (Sweden)

    V. R. Alekseev

    2015-03-01

    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. 

  4. 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.

  5. 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

  6. 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...

  7. 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

  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. 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

  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. A mid to late Holocene history of floodplain and terrace reworking along the middle Delaware River valley, USA

    Science.gov (United States)

    Stinchcomb, Gary E.; Driese, Steven G.; Nordt, Lee C.; Allen, Peter M.

    2012-10-01

    This study tests and refines the traditional floodplain development model for the partly confined middle Delaware River valley, which has shown that the main channel was relatively stable and flanked by a 6000-8000 year old, vertically accreting alluvial terrace. The Holocene alluvial processes and history presented here in 6 fluvial phases were reconstructed using morphostratigraphy, 36 profile descriptions, 332 grain size analyses, and 82 14C ages from soil trenches, auger borings, and archaeological excavations. Fluvial phases I-III largely validate previous reconstructions showing a late Pleistocene (I: > 10.7 ka) braided stream transition into an early Holocene wandering stream with prolonged floodplain stability (II: 10.7-8 ka), followed by early-middle Holocene erosion and then deposition (III: 8-5 ka). The early and middle Holocene changes in alluvial stratigraphy and sedimentology broadly correlate with climatically derived Holocene subdivisions, suggesting climate change partly controls alluvial response along the middle Delaware River valley. This study documents for the first time a middle Holocene episode of channel incision occurring sometime between 6.0 and 5.0 ka. Although the results reconfirm that the majority of alluvial landforms are composed of vertical accretion deposits, we present here new evidence of oblique, abandoned channel, and lateral accretion deposits inset to similar landforms with different formation histories (i.e., polycyclic terrace development), depicting a river valley that has experienced floodplain and terrace reworking. The majority of floodplain and terrace reworking occurs during the late-middle and late Holocene phases IV-VI (5.5-0 ka), following the middle Holocene incision event. These phases demonstrate floodplain reworking processes in the form of channel abandonment, stripping, flood channeling, and convex bank erosion. The subsequent space filled rapidly with evidence of multistory soil formation, and eventually

  12. PIXE analysis of prehistoric and protohistoric Caborn-Welborn phase copper artifacts from the lower Ohio River Valley

    International Nuclear Information System (INIS)

    Particle-induced X-ray emission (PIXE) spectrometry is being used to nondestructively determine the elemental composition of copper-based artifacts excavated from prehistoric/protohistoric sites in the Ohio River Valley. Copper objects from Caborn-Welborn (C-W) and contemporary Fort Ancient sites are being studied so as to differentiate between native American and European copper. The trace element analysis of metal artifacts enables archaeologists to more accurately assess the material culture and chronological development of C-W society (A.D. 1400-1700) with particular reference to geological sources of copper and brass. (author)

  13. 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

  14. 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。

  15. 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

  16. Using GPS to Quantify Three Dimensional Storage and Aquifer Deformation in the Virgin River Valley, Nevada

    Science.gov (United States)

    Warner, S. M.; Burbey, T. J.; Blewitt, G.; Bell, J. W.; Hill, E.; Johnson, M.

    2003-12-01

    Quantifying aquifer storage is important in order to characterize aquifer response and optimize aquifer pumping in large well fields located in thick sedimentary basins like those in the arid southwestern United States. The majority of this water is released from storage because of aquifer-system compaction. Historically this compaction was assumed to occur only in the vertical direction. However, aquifer mechanics and related field investigations indicate that strain is three-dimensional and the amount of water released from storage by horizontal strain can be significant. The development of empirically-based analytical techniques that allow for accurate quantification of storage and an assessment of the strain components at various radii from the pumping well are needed. From May through August, 2003, field scale aquifer testing and land subsidence monitoring were performed in the Virgin River Valley at Mesquite, NV. The goals were to determine the usefulness of storage quantification methods at the field scale and developing an effective inexpensive method to monitor three-dimensional deformation patterns due to removal of water from storage. The ground movement was monitored using choke ring antennas and GPS receivers at 10 different locations at various distances from the pumping well for 100 days. The well was pumped for approximately 12 hours each day at a rate of about 18000 m3/d. Compared to pumping at a steady rate, pulsating pumping (i.e. on and off cycles) has been shown to concentrate vertical deformation closer to the pumping well. The effect of pulsed pumping on horizontal deformation is previously not well documented but can now be investigated. The GPS data and pumping data collected from the aquifer test will be used to quantify aquifer strain in three dimensions at various distances from the well and stages during pumping. These strain patterns will provide information about possible faults in the area that affect groundwater flow, provide

  17. 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

  18. 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.

  19. Pre-and post-Missoula flood geomorphology of the Pre-Holocene ancestral Columbia River Valley in the Portland forearc basin, Oregon and Washington, USA

    Science.gov (United States)

    Peterson, Curt D.; Minor, Rick; Peterson, Gary L.; Gates, Edward B.

    2011-06-01

    Geomorphic landscape development in the pre-Holocene ancestral Columbia River Valley (1-5 km width) in the Portland forearc basin (~ 50 km length) is established from depositional sequences, which pre-date and post-date the glacial Lake Missoula floods. The sequences are observed from selected borehole logs (150 in number) and intact terrace soil profiles (56 in number) in backhoe trenches. Four sequences are widespread, including (1) a vertically aggraded Pleistocene alluvial plain, (2) a steep sided valley that is incised (125-150 m) into the Pleistocene gravel plain, (3) Missoula flood terraces (19-13 ka) abandoned on the sides of the ancestral valley, and (4) Holocene flooding surfaces (11-8 ka) buried at 70-30 m depth in the axial Columbia River Valley. Weathering rims and cementation are used for relative dating of incised Pleistocene gravel units. Soil development on the abandoned Missoula flood terraces is directly related to terrace deposit lithology, including thin Bw horizons in gravel, irregular podzols in sand, and multiple Bw horizons in thicker loess-capping layers. Radiocarbon dating of sand and mud alluvium in the submerged axial valley ties Holocene flooding surfaces to a local sea level curve and establishes Holocene sedimentation rates of 1.5 cm year- 1 during 11-9 ka and 0.3 cm year- 1 during 9-0 ka. The sequences of Pleistocene gravel aggradation, river valley incision, cataclysmic Missoula flooding, and Holocene submergence yield complex geomorphic landscapes in the ancestral lower Columbia River Valley.

  20. 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

  1. 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

  2. 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.

  3. Crustal anisotropy in the Archean Minnesota River Valley Subprovince and its significance

    Science.gov (United States)

    Gebelin, A.; Ferre, E. C.; Teyssier, C.

    2007-12-01

    The origin and evolution of the American continental lithosphere is a key question addressed by EarthScope. The Superior Province formed as an amalgamation of Archean/ Proterozoic terranes that subsequently acted as a stabilizing nucleus. This province is characterized by a strong seismic anisotropy (SWS = 1.3 s) of unknown origin. As suggested for the Archean Kaapvaal Craton (South Africa), this could be attributed (1) to current asthenospheric flow, or (2) to fossil lithospheric anisotropy, or (3) to the role of lithospheric keels on modern asthenospheric flow. The first hypothesis is not favored because SWS data for the Superior Province do not fit global mantle flow models. The second hypothesis would be compatible with obliquity between lithospheric mantle and crustal seismic anisotropies, possibly due to oblique docking. The third hypothesis would require asthenospheric flow to be controlled by lithospheric block geometry. The origin of seismic anisotropy and its spatial variations need to be determined to test these hypotheses. The deployment of USArray in the Superior Province in FY10, along with the prospect of deployment of a Flexible Array and the GeoFrame Superior focus area should provide a wealth of seismic data. Yet, the contribution of the Archean-early Proterozoic continental crust to seismic anisotropy is unknown. This study focusses on the Minnesota River Valley (MRV) Subprovince, part of the Superior Province. The MRV Subprovince consists of four juxtaposed blocks (Benson, Montevideo, Morton and Jeffers) of amphibolite to granulite grade migmatites, tonalites, granodiorites, diorites and pelitic rocks interlayered into each other. These blocks are separated by EW-dipping shear zones broadly parallel to SWS observations. In other parts of the world, the crustal seismic anisotropy is generally considered to be modest (SWS = 0.1-0.2 s), although experiments specifically designed to constrain it are scarce. The MRV represents a 200 km-wide, tilted

  4. 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...

  5. 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.

  6. Late Pleistocene and Holocene environmental history of the Iguala Valley, Central Balsas Watershed of Mexico

    OpenAIRE

    Piperno, D. R.; Moreno, J. E.; J Iriarte; Holst, I.; Lachniet, M.; Jones, J. G.; Ranere, A. J.; Castanzo, R.

    2007-01-01

    The origin of agriculture was a signal development in human affairs and as such has occupied the attention of scholars from the natural and social sciences for well over a century. Historical studies of climate and vegetation are closely associated with crop plant evolution because they can reveal the ecological contexts of plant domestication together with the antiquity and effects of agricultural practices on the environment. In this article, we present paleoecological evidence from three l...

  7. 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.

  8. 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...

  9. 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...

  10. 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...

  11. 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

  12. 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...

  13. 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.

  14. 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.

  15. 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.)

  16. [Depth of edge influence on agriculture-forestry boundary in arid valley of upper reaches of Minjiang River, China].

    Science.gov (United States)

    Li, Liguang; He, Xingyuan; Li, Xiuzhen; Wen, Qingchun; Zhao, Yonghua; Hu, Zhibin; Chang, Yu; Zhu, Yaping

    2004-10-01

    By using moving split-window techniques (MSWT), this study estimated how far the edge effects penetrated the forest and agricultural fields in the arid valley of upper reaches of Minjiang River, southwestern China. Its aim was to provide general information on vegetation along edge to interior gradients in order to assist in interpretation and prediction of biological phenomena associated with agriculture-forestry boundary, and to improve current management practices in such areas. Three types of boundaries (10 transects) were investigated and sampled. The results showed that when the window width reached 6-10, the change of the SED curve on the graph tended to become stable, and one or two peaks occurred. The depth of edge influence was clearly different for different types of boundaries, and could be estimated within 50 m from the edge to interior. The depth of edge influence (DEI) on vegetation diversity almost varied between 12-30 m, mainly depending on the patch type, topography and microclimate, but seldom on slope orientation. Of the 6 forest transects in the three types of boundaries, the DEI was detected only in the forest part transects M2 and M6, but almost detectable in the agricultural part of all transects. MSWT was considered to be a useful tool for characterizing edge dynamics if enough data was available, and became a simple and powerful technique for analyzing the boundary. The results will provide further knowledge for understanding the interaction between forestry and agriculture in the arid valley. PMID:15624812

  17. Block and shear-zone architecture of the Minnesota River Valley subprovince: Implications for late Archean accretionary tectonics

    Science.gov (United States)

    Southwick, D.L.; Chandler, V.W.

    1996-01-01

    The Minnesota River Valley subprovince of the Superior Province is an Archean gneiss terrane composed internally of four crustal blocks bounded by three zones of east-northeast-trending linear geophysical anomalies. Two of the block-bounding zones are verified regional-scale shears. The geological nature of the third boundary has not been established. Potential-field geophysical models portray the boundary zones as moderately north-dipping surfaces or thin slabs similar in strike and dip to the Morris fault segment of the Great Lakes tectonic zone at the north margin of the subprovince. The central two blocks of the subprovince (Morton and Montevideo) are predominantly high-grade quartzofeldspathic gneiss, some as old as 3.6 Ga, and late-tectonic granite. The northern and southern blocks (Benson and Jeffers, respectively) are judged to contain less gneiss than the central blocks and a larger diversity of syntectonic and late-tectonic plutons. A belt of moderately metamorphosed mafic and ultramafic rocks having some attributes of a dismembered ophiolite is partly within the boundary zone between the Morton and Montevideo blocks. This and the other block boundaries are interpreted as late Archean structures that were reactivated in the Early Proterozoic. The Minnesota River Valley subprovince is interpreted as a late accretionary addition to the Superior Province. Because it was continental crust, it was not subductible when it impinged on the convergent southern margin of the Superior Craton in late Archean time, and it may have accommodated to convergent-margin stresses by dividing into blocks and shear zones capable of independent movement.

  18. Decrease of soil fertility and release of mercury following deforestation in the Andean Amazon, Napo River Valley, Ecuador.

    Science.gov (United States)

    Mainville, N; Webb, J; Lucotte, M; Davidson, R; Betancourt, O; Cueva, E; Mergler, D

    2006-09-01

    Soil erosion and degradation provoked by deforestation in the Amazon is a global concern, and recent studies propose a link between deforestation, soil erosion and the leaching of naturally occurring mercury (Hg). In the Ecuadorian Amazon, elevated deforestation rates and the proximity of volcanoes could play an important role in soil fertility and soil Hg levels. The goal of this study is to evaluate the impacts of deforestation on Andisol and Inceptisol fertility and Hg levels in the Napo River Valley, Ecuador. Results show a significant decrease in surface soil organic matter (-15% to -70% of C and N) and exchangeable cations (-25% to -60%) in deforested plots. Hg concentrations at the surface (0-5 cm), higher in Andisols (225 ng/g average) than in Inceptisols (95 ng/g average), show a decrease of up to 60% following deforestation. Soil erosion exposes the mineral horizon, a layer with a higher Hg burden, to the elements thus provoking and accelerating Hg leaching. These results suggest that deforestation and the associated Hg leaching could contribute to the fish Hg contamination measured in the Napo River watershed. PMID:16499953

  19. 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.

  20. 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

  1. 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.

  2. Mercury partitioning within alluvial sediments of the Carson river valley, Nevada: Implications for sampling strategies in tropical environments

    Science.gov (United States)

    Miller, Jerry R.; Lechler, Paul J.

    The Carson River system of west-central Nevada was subjected to a massive influx of mercury-enriched tailings derived from mining and milling of the Comstock Lode near the end of the 1800s. Detailed investigations have shown that these contaminated tailings were deposited along the Carson River Valley during a period of channel and floodplain aggradation. Following cessation of mining, incision re-exposed the historical sediment in banks of the modern channel. Concentrations of mercury in these deposits are commonly two to three orders of magnitude above background levels observed in other sediments and soils of the region. Most of the mercury is carried on fine-grained particles as would be expected from previous studies of trace metal partitioning in alluvial deposits. However, erosion and reworking of the historical sediment during lateral channel migration leads to a loss of fine-grained particles and a concentration of mercury-gold/silver amalgam grains in the modern channel bed. As a result, mercury is distributed in both fine- and coarse-grained sediment fractions of the channel floor. The enrichment of trace metals in fine-grained sediment of most aquatic systems has caused some investigators to argue that geographical and temporal trends in trace metal concentrations should be determined only after applying one of the several methodologies developed to correct for the effects of varying grain size. While this concept seems to apply well to the historical deposits of the Carson River, it would lead to erroneous conclusions if applied to the modern channel bed sediments. In addition, mercury, gold and silver are partitioned along the channel in to specific depositional sites, possibly in the form of amalgam grains that are concentrated as placers. It is therefore imperative that downstream trends in mercury concentrations are assessed by examining data collected from similar depositional environments.

  3. Geohydrology and simulated response to groundwater pumpage in Carson Valley, a river-dominated basin in Douglas County, Nevada, and Alpine County, California

    Science.gov (United States)

    Maurer, D.K.

    1986-01-01

    A numerical model was used to simulate the effect of development of the groundwater reservoir in Carson Valley on Carson River outflow, evapotranspiration, and groundwater levels and storage. The basin-fill groundwater reservoir consists of: (1) confined and unconfined sedimentary deposits of Quaternary age that underlie the valley floor, and (2) sedimentary deposits of Tertiary age that are exposed mainly on the east side of the valley. Water levels indicate the presence of two confined aquifer systems: one River flow, 360,000; (2) direct precipitation, 70,000; (3) runoff from perennial and ephemeral streams, 24,000: and (4) subsurface inflow, 38,000. Approximate estimates of outflow components were, in acre-ft/yr; (1) mainstem Carson River flow, 291,000; (2) potential evapotranspiration, 200,000. Both inflow and outflow totaled about 490,000 acre-ft/yr. These flow volumes show that the hydrologic regimen of the basin is dominated by surface water flow of the Carson River. Steady-state and transient calibration of the model provided an unacceptable fit of observed versus simulated groundwater level fluctuations and storage, and surface water outflow from the valley. These values provide a reasonable balance for the simulated steady-state water budget. Simulations show that surface water flow is the ultimate source of about 75% of pumped water for six scenarios of possible future ground-water development. Model simulations indicate that changes from agricultural to urban land uses could decrease the loss of Carson River outflow to pumpage when streamflow is not used for flood irrigation in that area. (Lantz-PTT)

  4. 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)

  5. 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.

  6. Early findings from artificial recharge efforts of the Mississippi River Valley Alluvial Aquifer

    Science.gov (United States)

    The long-term success and sustainability of agriculture in the Lower Mississippi River Basin will depend largely on water resources. Aquifer decline in the region has been documented since the 1980s and continues today. Artificial recharge is one possible tool that could help alleviate this declin...

  7. 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.

  8. 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

  9. Metal Transport, Heavy Metal Speciation and Microbial Fixation Through Fluvial Subenvironments, Lower Coeur D'Alene River Valley, Idaho

    Science.gov (United States)

    Hooper, R. L.; Mahoney, J. B.

    2001-12-01

    The lower Coeur d'Alene River Valley of northern Idaho is the site of extensive lead and zinc contamination resulting from both direct riverine tailings disposal and flood remobilization of contaminated sediments derived from the Coeur d'Alene mining district upstream. Variations in the hydrologic regime, redox conditions, porosity/permeability, organic content and microbial activity results in complicated metal transport pathways. Documentation of these pathways is a prerequisite to effective remediation, and requires accurate analysis of lateral and vertical variations. An analytical approach combining sequential extraction, electron microscopy, and microanalysis provides a comprehensive assessment of particulate speciation in this complex hydrologic system. Rigorously controlled sample preparation and a new sequential extraction protocol provide unprecedented insight into the role of metal sequestration in fluvial subenvironments. Four subenvironments were investigated: bedload, overbank (levee), marsh, and lacustrine. Periodic floods remobilize primary ore minerals and secondary minerals from upstream tailings (primarily oxyhydroxides, sulfides and carbonates). The bedload in the lower valley is a reducing environment and acts as a sink for detrital carbonates and sulfides moving downstream. In addition, authigenic/biogenic Fe, Pb and Zn sulfides and phosphates are common in bedload sediments near the sediment/water interface. Flood redistribution of oxide, sulfide and carbonate phases results in periodic contaminant recharge generating a complex system of metal dissolution, mobilization, migration and precipitation. In levee environments, authigenic sulfides from flood scouring are quickly oxidized resulting in development of oxide coated grain surfaces. Stability of detrital minerals on the levee is variable depending on sediment permeability, grain size and mineralogy resulting in a complex stratigraphy of oxide zones mottled with zones dominated by detrital

  10. 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

  11. 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...

  12. Flow prediction models using macroclimatic variables and multivariate statistical techniques in the Cauca River Valley

    International Nuclear Information System (INIS)

    The project this centred in the revision of the state of the art of the ocean-atmospheric phenomena that you affect the Colombian hydrology especially The Phenomenon Enos that causes a socioeconomic impact of first order in our country, it has not been sufficiently studied; therefore it is important to approach the thematic one, including the variable macroclimates associated to the Enos in the analyses of water planning. The analyses include revision of statistical techniques of analysis of consistency of hydrological data with the objective of conforming a database of monthly flow of the river reliable and homogeneous Cauca. Statistical methods are used (Analysis of data multivariante) specifically The analysis of principal components to involve them in the development of models of prediction of flows monthly means in the river Cauca involving the Lineal focus as they are the model autoregressive AR, ARX and Armax and the focus non lineal Net Artificial Network.

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

    OpenAIRE

    H. Wulf; B. Bookhagen; D. Scherler

    2012-01-01

    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 i...

  14. Development of Hydrological Model of Klang River Valley for flood forecasting

    Science.gov (United States)

    Mohammad, M.; Andras, B.

    2012-12-01

    This study is to review the impact of climate change and land used on flooding through the Klang River and to compare the changes in the existing river system in Klang River Basin with the Storm water Management and Road Tunnel (SMART) which is now already operating in the city centre of Kuala Lumpur. Klang River Basin is the most urbanized region in Malaysia. More than half of the basin has been urbanized on the land that is prone to flooding. Numerous flood mitigation projects and studies have been carried out to enhance the existing flood forecasting and mitigation project. The objective of this study is to develop a hydrological model for flood forecasting in Klang Basin Malaysia. Hydrological modelling generally requires large set of input data and this is more often a challenge for a developing country. Due to this limitation, the Tropical Rainfall Measuring Mission (TRMM) rainfall measurement, initiated by the US space agency NASA and Japanese space agency JAXA was used in this study. TRMM data was transformed and corrected by quantile to quantile transformation. However, transforming the data based on ground measurement doesn't make any significant improvement and the statistical comparison shows only 10% difference. The conceptual HYMOD model was used in this study and calibrated using ROPE algorithm. But, using the whole time series of the observation period in this area resulted in insufficient performance. The depth function which used in ROPE algorithm are then used to identified and calibrated using only unusual event to observed the improvement and efficiency of the model.

  15. 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.

  16. 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...

  17. Animal subsistence of the Yangshao period in the Wei river valley: a case-study from the site of Wayaogou in Shaanxi Province, China

    OpenAIRE

    Wang, H.

    2011-01-01

    This thesis focuses on the subsistence economy of the Yangshao period in the Wei River Valley, how it changes through time and how it relates to environmental change and changing social complexity. The research is based on faunal analysis at the Wayaogou site (6,500-6,000 BP) in Shaanxi Province, China. Pig and sika deer remains are studied in detail since they dominate the faunal assemblage. For the pig, its domesticated status is documented and its husbandry strategies are ex...

  18. Birth defects, season of conception, and sex of children born to pesticide applicators living in the Red River Valley of Minnesota, USA.

    OpenAIRE

    Garry, Vincent F; Harkins, Mary E; Erickson, Leanna L; Long-Simpson, Leslie K; Holland, Seth E; Burroughs, Barbara L

    2002-01-01

    We previously demonstrated that the frequency of birth defects among children of residents of the Red River Valley (RRV), Minnesota, USA, was significantly higher than in other major agricultural regions of the state during the years 1989-1991, with children born to male pesticide applicators having the highest risk. The present, smaller cross-sectional study of 695 families and 1,532 children, conducted during 1997-1998, provides a more detailed examination of reproductive health outcomes in...

  19. 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.

  20. 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.

  1. Formation and failure of volcanic debris dams in the Chakachatna River valley associated with eruptions of the Spurr volcanic complex, Alaska

    Science.gov (United States)

    Waythomas, C.F.

    2001-01-01

    The formation of lahars and a debris avalanche during Holocene eruptions of the Spurr volcanic complex in south-central Alaska have led to the development of volcanic debris dams in the Chakachatna River valley. Debris dams composed of lahar and debris-avalanche deposits formed at least five times in the last 8000-10,000 years and most recently during eruptions of Crater Peak vent in 1953 and 1992. Water impounded by a large debris avalanche of early Holocene (?) age may have destabilized an upstream glacier-dammed lake causing a catastrophic flood on the Chakachatna River. A large alluvial fan just downstream of the debris-avalanche deposit is strewn with boulders and blocks and is probably the deposit generated by this flood. Application of a physically based dam-break model yields estimates of peak discharge (Qp) attained during failure of the debris-avalanche dam in the range 104 eruptions in 1953, and 1992, impounded smaller lakes in the upper Chakachatna River valley and peak flows attained during failure of these volcanic debris dams were in the range 103 Volcanic debris dams have formed at other volcanoes in the Cook Inlet region, Aleutian arc, and Wrangell Mountains but apparently did not fail rapidly or result in large or catastrophic outflows. Steep valley topography and frequent eruptions at volcanoes in this region make for significant hazards associated with the formation and failure of volcanic debris dams. Published by Elsevier Science B.V.

  2. 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.

  3. 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...... 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...

  4. 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

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

    Directory of Open Access Journals (Sweden)

    H. Wulf

    2012-07-01

    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 and earthquake records, and field observations, 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 variations with respect to river discharge, 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. In future climate change scenarios, including continuous glacial retreat and

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

    Science.gov (United States)

    Wulf, H.; Bookhagen, B.; Scherler, D.

    2012-07-01

    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 and earthquake records, and field observations, 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 variations with respect to river discharge, 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. In future climate change scenarios, including continuous glacial retreat and more frequent

  7. Attempted cultivation of Jatropha curcas L. in the lower Senegal river valley: story of a failure

    OpenAIRE

    Terren, Marieke; Saverys; Jacquet de Haveskercke, Paul; Winandy, Stéphane; Mergeai, Guy

    2012-01-01

    With the objective of determining whether it would be possible to sustainably produce Jatropha curcas L. seeds on the marginal land situated close to the Senegal River, a 6-hectare pilot plantation was cultivated under drip irrigation between September 2007-November 2011, close to the village of Bokhol (Lat. 16°31’N, Long. 15°23’W). A series of tests were conducted on this plot, in order to identify the best cultivation methods for the area (date, density and method of planting, appropriat...

  8. Attempted Cultivation of Jatropha curcas L. in the Lower Senegal River Valley: Story of a Failure

    OpenAIRE

    Terren, M.; Saverys, S.; Jacquet de Haveskercke, P.; Winandy, S; Mergeai, G.

    2012-01-01

    With the objective of determining whether it would be possible to sustainably produce Jatropha curcas L. seeds on the marginal land situated close to the Senegal River, a 6-hectare pilot plantation was cultivated under drip irrigation between September 2007-November 2011, close to the village of Bokhol (Lat. 16°31'N, Long. 15°23'W). A series of tests were conducted on this plot, in order to identify the best cultivation methods for the area (date, density and method of planting, appropriate t...

  9. Geohydrology of the valley-fill aquifer in the Bath area, Lower Cohocton River, Steuben County, New York

    Science.gov (United States)

    Pagano, Timothy S.; Terry, D.B.; Shaw, M.L.; Ingram, A.W.

    1984-01-01

    The Bath valley-fill aquifer, southern New York, composed of outwash, ice-contact, and ice-disintegration sand and gravel, is highly productive and is in many areas in hydraulic contact with the Cohocton River. Potential well yields range 50 to more than 1,000 gallons per minute. Most of the aquifer is under shallow water-table conditions and vulnerable to surface contamination. Thickness ranges from 20 to 40 feet. Buried aquifers are present locally. The aquifer system underlies an area containing only a few small communities and therefore is not heavily pumped. Geohydrologic data are compiled on six maps at 1:24,000 scale and on a sheet of geologic sections. The maps depict surficial geology, soil-infiltration capacity, potentiometric surface, aquifer thickness, well yields, and land use. This map report set is one in a series of four that depict selected aquifers in Wester New York. It supplements a series that is being done by the U.S. Geological Survey in cooperation with State agencies. The maps are based largely on published reports, data filled in several State agencies, and some additional field data collection. (USGS)

  10. Geohydrology of the valley-fill aquifer in the Cohocton area, upper Cohocton River, Steuben County, New York

    Science.gov (United States)

    Terry, David B.; Pagano, Timothy S.; Shaw, Martha L.; Ingram, Arlynn W.

    1984-01-01

    The Cohocton valley-fill aquifer, composed of outwash, kame, and alluvial sand and gravel, is highly productive and is in hydraulic contact with the Cohocton River. Potential well yields range from 50 to more than 1,000 gallons per minute. Most of the aquifer is under shallow water-table conditions and vulnerable to surface contamination. Thickness ranges from 20 to 100 feet. The aquifer lies in an area containing only small communities and therefore is not heavily pumped. Geohydrologic data are compiled on six maps at 1:24,000 scale and in geologic sections. The maps depict surficial geology, soil-infiltration capacity, potentiometric surface, aquifer thickness, well yields, and land use. The maps are designed to help planners evaluate developments that may affect the aquifer, particularly potential contamination sources. This set is one in a series of four that depict selected aquifers in western New York. It supplements a series that is being done by the U.S. Geological Survey in cooperation with State agencies. The maps are based largely on published reports, file data in several State agencies, and field notes. (USGS)

  11. 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.

  12. 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.

  13. 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)

  14. 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.

  15. 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.

  16. 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.

  17. 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).

  18. Evaluation of Selected Model Constraints and Variables on Simulated Sustainable Yield from the Mississippi River Valley Alluvial Aquifer System in Arkansas

    Science.gov (United States)

    Czarnecki, John B.

    2008-01-01

    An existing conjunctive use optimization model of the Mississippi River Valley alluvial aquifer was used to evaluate the effect of selected constraints and model variables on ground-water sustainable yield. Modifications to the optimization model were made to evaluate the effects of varying (1) the upper limit of ground-water withdrawal rates, (2) the streamflow constraint associated with the White River, and (3) the specified stage of the White River. Upper limits of ground-water withdrawal rates were reduced to 75, 50, and 25 percent of the 1997 ground-water withdrawal rates. As the upper limit is reduced, the spatial distribution of sustainable pumping increases, although the total sustainable pumping from the entire model area decreases. In addition, the number of binding constraint points decreases. In a separate analysis, the streamflow constraint associated with the White River was optimized, resulting in an estimate of the maximum sustainable streamflow at DeValls Bluff, Arkansas, the site of potential surface-water withdrawals from the White River for the Grand Prairie Area Demonstration Project. The maximum sustainable streamflow, however, is less than the amount of streamflow allocated in the spring during the paddlefish spawning period. Finally, decreasing the specified stage of the White River was done to evaluate a hypothetical river stage that might result if the White River were to breach the Melinda Head Cut Structure, one of several manmade diversions that prevents the White River from permanently joining the Arkansas River. A reduction in the stage of the White River causes reductions in the sustainable yield of ground water.

  19. 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.

  20. Application of Environmental Isotopes in Hydrological Studies Along the River Nile Valley, Egypt

    International Nuclear Information System (INIS)

    This paper reviews some of the contributions of isotope techniques to better understanding hydrological problems in Egypt and the Nile basin. The stable isotope composition of precipitation shows considerable variations both in time and space since it is controlled by climatic factors. Surface waters became enriched in deuterium and oxygen-18 relative to their initial isotopic composition as losses by evaporation occur. The GNIP sampling stations at Entebbe and Addis Ababa, which are located at the source of the Nile River, present relatively depleted isotopic contents. Assuming that the central Africa runoff (White Nile downstream from Sudan) represents 30% of the natural discharge of Egypt, and the remaining 70% is derived from Ethiopia (Blue Nile), we obtain a composite depleted stable isotope composition of the river Nile reaching upper Egypt under natural conditions (before the construction of the Aswan High Dam). Stable isotopes were used to estimate the evaporation rate from Lake Nasser, based on the isotopic content of the lake water. The lake can be divided into two sectors: the first sector, with remarkable vertical gradient in O-18 and deuterium, and a second sector, characterized by a lower vertical isotopic gradient. In order to detect this effect, surface Nile water samples have been collected at Cairo after a heavy storm event covering all Egypt at the beginning of November 1994, characterized by very negative deuterium and oxygen-18 contents. The isotopic content of Nile water samples fluctuated and slightly changed with time. The variation of the bomb tritium response of the Nile has been reconstructed using a model based on the contents in the catchment areas of the Nile. Pre-bomb tritium content in the Nile was about 5 TU, reaching a maximum level during the early sixties of about 500 TU. At present the tritium level content of the Nile is about 6 TU. (author)

  1. 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

  2. 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.

  3. 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)

  4. Attempted Cultivation of Jatropha curcas L. in the Lower Senegal River Valley: Story of a Failure

    Directory of Open Access Journals (Sweden)

    Terren, M.

    2012-01-01

    Full Text Available With the objective of determining whether it would be possible to sustainably produce Jatropha curcas L. seeds on the marginal land situated close to the Senegal River, a 6-hectare pilot plantation was cultivated under drip irrigation between September 2007-November 2011, close to the village of Bokhol (Lat. 16°31'N, Long. 15°23'W. A series of tests were conducted on this plot, in order to identify the best cultivation methods for the area (date, density and method of planting, appropriate type of pruning, fertilisers to be applied, irrigation method, etc.. The average yields obtained at this site, after four years of cultivation (less than 500 kg.ha-1 of dry seed, using the best known production techniques, are significantly lower than anticipated, compared to the available figures for the irrigated cultivation of Jatropha in other parts of the world. The main causes of this failure are the plant's limited useful vegetation period of six months per year, instead of twelve, and the scale of attacks by a soilborne vascular disease, which destroyed over 60% of the plantation within four years.

  5. 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

  6. 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.

  7. 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

  8. Case studies of the expansion of Acacia dealbata in the valley of the river Miño (Galicia, Spain

    Directory of Open Access Journals (Sweden)

    Antonio Vazquez de la Cueva

    2014-04-01

    Full Text Available Aim of study: Acacia dealbata is a naturalized tree of invasive behaviour that has expanded from small plots associated with vineyards into forest ecosystems. Our main objective is to find evidence to support the notion that disturbances, particularly forest fires, are important driving factors in the current expansion of A. dealbata.Area of study: We mapped it current distribution using three study areas and assesses the temporal changes registered in forest cover in these areas of the valley of the river Miño. Material and Methods: The analyses were based on visual interpretation of aerial photographs taken in 1985 and 2003 of three 1x1 km study areas and field works.Main result: A 62.4%, 48.6% and 22.2% of the surface area was covered by A. dealbata in 2003 in pure or mixed stands. Furthermore, areas composed exclusively of A. dealbata make up 33.8%, 15.2% and 5.7% of the stands. The transition matrix analyses between the two dates support our hypothesis that the areas currently covered by A. dealbata make up a greater proportion of the forest area previously classified as unwooded or open forest than those without A. dealbata cover. Both of these surface types are the result of an important impact of fire in the region. Within each area, A. dealbata is mainly located on steeper terrain, which is more affected by fires. Research highlights: A. dealbata is becoming the dominant tree species over large areas and the invasion of this species gives rise to monospecific stands, which may have important implications for future fire regimes.Keywords: Fire regime; Mimosa; plant invasion; silver wattle.

  9. 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.

  10. Statistical analyses of soil properties on a quaternary terrace sequence in the upper sava river valley, Slovenia, Yugoslavia

    Science.gov (United States)

    Vidic, N.; Pavich, M.; Lobnik, F.

    1991-01-01

    Alpine glaciations, climatic changes and tectonic movements have created a Quaternary sequence of gravely carbonate sediments in the upper Sava River Valley, Slovenia, Yugoslavia. The names for terraces, assigned in this model, Gu??nz, Mindel, Riss and Wu??rm in order of decreasing age, are used as morphostratigraphic terms. Soil chronosequence on the terraces was examined to evaluate which soil properties are time dependent and can be used to help constrain the ages of glaciofluvial sedimentation. Soil thickness, thickness of Bt horizons, amount and continuity of clay coatings and amount of Fe and Me concretions increase with soil age. The main source of variability consists of solutions of carbonate, leaching of basic cations and acidification of soils, which are time dependent and increase with the age of soils. The second source of variability is the content of organic matter, which is less time dependent, but varies more within soil profiles. Textural changes are significant, presented by solution of carbonate pebbles and sand, and formation is silt loam matrix, which with age becomes finer, with clay loam or clayey texture. The oldest, Gu??nz, terrace shows slight deviation from general progressive trends of changes of soil properties with time. The hypothesis of single versus multiple depositional periods of deposition was tested with one-way analysis of variance (ANOVA) on a staggered, nested hierarchical sampling design on a terrace of largest extent and greatest gravel volume, the Wu??rm terrace. The variability of soil properties is generally higher within subareas than between areas of the terrace, except for the soil thickness. Observed differences in soil thickness between the areas of the terrace could be due to multiple periods of gravel deposition, or to the initial differences of texture of the deposits. ?? 1991.

  11. 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.``

  12. Water scarcity in the Jordan Valley; Impacts on Agriculture and Rural livelihoods : Threaths and opportunities to local sustainable agriculture; the case of al-Auja, Jordan River Valley

    OpenAIRE

    Dobricic, Kristina

    2013-01-01

    Palestine has during the last two decades suffered from increasing water scarcity. This is particularlyvisible in the agricultural sector and in farming communities. These are heavily dependent on water as primaryirrigation source. Lack of water and investments has resulted in the destruction of the agricultural sector inPalestine. This thesis is focused as a case study in al-Auja, Jordan Valley that was once well-known for itsagricultural productivity and abundance of water resources. The ai...

  13. 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

  14. 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.

  15. Use of environmental isotopes in the lower valley and delta area of the River Llobregat (Barcelona, Spain) to solve flow and mass transport problems in aquifers

    International Nuclear Information System (INIS)

    The aquifer system of the lower valley and delta of the River Llobregat is an important part of the water resources system of Barcelona. Its destruction would cause major problems and have costly economic consequences. For that reason, detailed studies have been performed in order to gain an adequate idea of how it functions so that well founded proposals can be made to the relevant bodies to ensure that it is protected. The chemical changes produced by the flow process and the characteristic saline contamination of the river provide chemical tools which can be used to construct qualitative and quantitative hypotheses regarding the functioning of the aquifer as a complement to the hydrodynamic studies. By using environmental isotopes, where the volume of data is smaller, and data from studies with different objectives selected in such a way as to make them comparable, it was possible to confirm these hypotheses and define them more precisely. The stable isotopes in water confirm that river water is the recharge source both currently and in the non-disturbed state, whereas the tritium confirms that there is rapid renewal in the lower valley, delayed transit to the wells in the delta lasting some ten years, as indicated also by the chemical results, and 'old' fresh water which, owing to the extractions, is moving from the coast to the wells and is being followed by sea water which is currently causing a serious salinization problem. The radiocarbon content of the dissolved inorganic carbon (DIC) indicates that the renewal times are, at most, a few hundred years under natural conditions for the water in the deep aquifer, which confirms the connection between the confined aquifer and the sea bottom. Recharge in the valley from the irrigated fields results in an increase in the DIC content which agrees with the δ13C content. This water shows a slight evaporation effect. 17 refs, 14 figs, 2 tabs

  16. Life history, population dynamics and production of eastern mosquitofish, Gambusia holbrooki (Pisces, Poeciliidae), in rice fields of the lower Mondego River Valley, western Portugal

    OpenAIRE

    Cabral, João Alexandre; Marques, João Carlos

    1999-01-01

    The introduced population of Gambusia holbrooki from the rice fields of the lower Mondego River Valley, Portugal, was studied for 15 months, relating their life cycle and population dynamics with its production, in order to assess the role of the species in the energy flow and secondary production in this type of agro-ecosystem. Two main annual cohorts (1995 and 1996 cohorts) were identified. The females outnumbered males and the average female/male-ratio was 4. The inspection of ovary develo...

  17. 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.

  18. 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

  19. 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

  20. 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.

  1. 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

  2. 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

  3. 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.

  4. 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)

  5. 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

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

    OpenAIRE

    Anastacio Espejel-García; Jorge Romero-Domínguez; Ariadna Isabel Barrera-Rodríguez; Benjamín Torres-Espejel; Jesús Félix-Crescencio

    2015-01-01

    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 fo...

  7. 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.

  8. 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

  9. 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.)

  10. 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

  11. 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

  12. 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)

  13. 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...

  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. Current tufa sedimentation in a changing-slope valley: The River Añamaza (Iberian Range, NE Spain)

    Science.gov (United States)

    Auqué, L.; Arenas, C.; Osácar, C.; Pardo, G.; Sancho, C.; Vázquez-Urbez, M.

    2014-04-01

    A three-year study of modern carbonate sedimentation was conducted through analysis of sedimentological and hydrochemical parameters measured every six months at 10 sites along a high-slope river in northeastern Spain (River Añamaza). Three stretches of the river were characterised. The dominant water inputs from the upstream karstic springs, primarily from the Jurassic rock aquifer, determined the SO4-HCO3-Ca composition of the river water. From this area, decreasing trends in alkalinity, calcium and total dissolved inorganic carbon occurred downstream in both the warm and cool periods as a result of calcite precipitation. Tufa thickness variations were consistent with such hydrochemical evolution. Deposition rates increased downstream, primarily where the gradient is steeper (middle stretch), and subsequently decreased at the downstream gently sloped stretch. Therefore, the slope along the river and the distance from the main upstream springs conditioned the spatial distribution of tufa deposits by determining the chemical characteristics of the water.

  16. 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.

  17. Study of chemical composition of precipitation at an alpine site and a rural site in the Urumqi River Valley, Eastern Tien Shan, China

    Energy Technology Data Exchange (ETDEWEB)

    Zhao, Z.P.; Tian, L.; Fischer, E.; Li, Z.Q.; Jiao, K.Q. [Chinese Academy of Sciences, Beijing (China)

    2008-12-15

    We report on a 1-year continuous precipitation sampling record from an alpine site and a rural site in the Urumqi River Valley, East Tien Shan, China. The 128 samples, collected from April 2003 to February 2004, at two sites were analyzed for the major inorganic ions, pH, electrical conductivity and insoluble microparticles. The precipitation was typically alkaline with a volume-weighted mean pH of 6.99 and 7.27 at the alpine site and the rural site, respectively. Ca{sup 2+} was the dominant cation, and SO{sub 4}{sup 2-} was the dominant anion. The precipitation chemistry in this region was mainly controlled by regional Asian dust storms, local dust and anthropogenic activities. The relative impact of anthropogenic activities, specifically uncontrolled coal combustion, was larger at the rural site compared to the alpine monitoring site.

  18. 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.

  19. 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.

  20. 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.

  1. 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.

  2. THE FEASIBILITY OF WETLAND RESTORATION TO REDUCE FLOODING IN THE RED RIVER VALLEY: A CASE STUDY OF THE MAPLE RIVER WATERSHED, NORTH DAKOTA

    OpenAIRE

    Shultz, Steven D.; Leitch, Jay A.

    2001-01-01

    The economic feasibility of alternative wetland restoration activities to store water and reduce flood damage was evaluated in the Maple River Watershed, North Dakota, a sub-watershed of the Red River of the North Watershed. The evaluation was based on recent hydrologic modeling and wetland restoration studies, the National Wetland Inventory, local land rental values, and site-specific historical flood damage. With benefit-cost ratios ranging from 0.08 to 0.13, neither simple wetland restorat...

  3. 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 ...

  4. 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...

  5. 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.

  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. 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.

  8. A Debris Flow Chronology and Analysis of Controls on Debris Flow Occurrence in the Upper Colorado River Valley, Rocky Mountain National Park, CO

    Science.gov (United States)

    Grimsley, K. J.; Rathburn, S. L.; Grosicki, G.

    2011-12-01

    In high gradient environments, debris flows are commonly a dominant source of sediment transport and erosion. The importance of debris flows along the Upper Colorado was recently highlighted when the Grand Ditch, a 19th century water-conveyance ditch, overtopped from snowmelt and triggered a large debris flow along Lulu Creek, a tributary of the Upper Colorado River. Earlier research suggests that multiple debris flows have been triggered from the Grand Ditch over the last century, with higher magnitude and frequency than naturally occurring debris flows. To thoroughly test this hypothesis, debris flows are being mapped, dated using dendrogeomorphic evidence from tree cores and tree scars, and analyzed for relative magnitude. A total of approximately 15-20 mappable debris flows along the Upper Colorado have been located and sampled using a combination of historic aerial photos and field exploration in the basin. Berms observed along these debris flows are up to 1.5 meters high and frequently extend to the Colorado River valley bottom. Where even-aged stands are observed as a result of simultaneous stand germination after a debris flow, tree cores are collected from the oldest trees in the stand to estimate the age of the debris flow. Species of sampled trees include Lodgepole pine, Douglas fir, and Engelmann spruce. Initial core dates from a debris flow that extends along the Colorado River to just north of the Lulu wetland range from 29 to 37 years. Sampling of scarred survivor trees from debris flow berms provides an even better indicator of age because the warped tree rings can be counted to precisely date scarring events. Thus far 40 tree scars have been wedged and will be processed and dated during Fall 2011. Relative flow magnitudes will be compared using the heights of tree scars above the channel thalweg. Debris flow occurrence is related to the distribution of hydrothermally altered rocks in addition to other factors such as the aspect and gradient of the

  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. Influencia de las coberturas de sombreo suspendidas instaladas en balsas de riego sobre los requerimientos de filtrado

    OpenAIRE

    Maestre Valero, José Francisco; Martínez Álvarez, Víctoriano

    2013-01-01

    Este estudio presenta el análisis del efecto de la instalación de coberturas de sombreo suspendidas sobre los requerimientos de lavado de filtros de un sistema de riego. Se evaluó el filtrado en 10 balsas, 2 de ellas cubiertas con una cobertura de sombreo suspendida. Un equipo de riego portátil dotado con dos manómetros analógicos y uno digital registro el aumento progresivo de las pérdidas de carga en filtro (indicador de retención de partículas). Adicionalmente, una sonda OTT-DS5 determinó ...

  11. 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%...

  12. Effect of activities at the Idaho National Engineering and Environmental Laboratory on the water quality of the Snake River Plain aquifer in the Magic Valley study

    Science.gov (United States)

    Bartholomay, Roy C.

    1998-01-01

    Radiochemical and chemical constituents in wastewater generated at facilities of the Idaho National Engineering and Environmental Laboratory (INEEL) (figure 1) have been discharged to waste-disposal ponds and wells since the early 1950 s. Public concern has been expressed that some of these constituents could migrate through the Snake River Plain aquifer to the Snake River in the Twin Falls-Hagerman area Because of these concerns the U.S. Department of Energy (DOE) requested that the U.S. Geological Survey (USGS) conduct three studies to gain a greater understanding of the chemical quality of water in the aquifer. One study described a one-time sampling effort for radionuclides, trace elements, and organic compounds in the eastern part of the A&B Irrigation District in Minidoka County (Mann and Knobel, 1990). Another ongoing study involves sampling for tritium from 19 springs on the north side of the Snake River in the Twin Falls-Hagerman area (Mann, 1989; Mann and Low, 1994). A third study an ongoing annual sampling effort in the area between the southern boundary of the INEEL and Hagerman (figure 1) (hereafter referred to as the Magic Valley study area), is being conducted with the Idaho Department of Water Resources in cooperation with the DOE. Data for a variety of radiochemical and chemical constituents from this study have been published by Wegner and Campbell (1991); Bartholomay, Edwards, and Campbell (1992, 1993, 1994a, 1994b); and Bartholomay, Williams, and Campbell (1995, 1996, 1997b). Data discussed in this fact sheet were taken from these reports. An evaluation of data collected during the first four years of this study (Bartholomay Williams, and Campbell, 1997a) showed no pattern of water-quality change for radionuclide data as concentrations randomly increased or decreased. The inorganic constituent data showed no statistical change between sample rounds.

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

    Science.gov (United States)

    Sharma, Shubhra; Bartarya, S. K.; Marh, B. S.

    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 during the 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 declining ISM. 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.

  14. 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.

  15. 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

  16. Field measurements of incision rates following bedrock exposure: Implications for process controls on the long profiles of valleys cut by rivers and debris flows

    Science.gov (United States)

    Stock, Jonathan D.; Montgomery, David R.; Collins, Brian D.; Dietrich, William E.; Sklar, Leonard

    2005-01-01

    Until recently, published rates of incision of bedrock valleys came from indirect dating of incised surfaces. A small but growing literature based on direct measurement reports short-term bedrock lowering at geologically unsustainable rates. We report observations of bedrock lowering from erosion pins monitored over 1–7 yr in 10 valleys that cut indurated volcanic and sedimentary rocks in Washington, Oregon, California, and Taiwan. Most of these channels have historically been stripped of sediment. Their bedrock is exposed to bed-load abrasion, plucking, and seasonal wetting and drying that comminutes hard, intact rock into plates or equant fragments that are removed by higher flows. Consequent incision rates are proportional to the square of rock tensile strength, in agreement with experimental results of others. Measured rates up to centimeters per year far exceed regional long-term erosion-rate estimates, even for apparently minor sediment-transport rates. Cultural artifacts on adjoining strath terraces in Washington and Taiwan indicate at least several decades of lowering at these extreme rates. Lacking sediment cover, lithologies at these sites lower at rates that far exceed long-term rock-uplift rates. This rate disparity makes it unlikely that the long profiles of these rivers are directly adjusted to either bedrock hardness or rock-uplift rate in the manner predicted by the stream power law, despite the observation that their profiles are well fit by power-law plots of drainage area vs. slope. We hypothesize that the threshold of motion of a thin sediment mantle, rather than bedrock hardness or rock-uplift rate, controls channel slope in weak bedrock lithologies with tensile strengths below ∼3–5 MPa. To illustrate this hypothesis and to provide an alternative interpretation for power-law plots of area vs. slope, we combine Shields' threshold transport concept with measured hydraulic relationships and downstream fining rates. In contrast to fluvial

  17. 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...

  18. 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.

  19. Geochronology of cave deposits at Liang Bua and of adjacent river terraces in the Wae Racang valley, western Flores, Indonesia: a synthesis of age estimates for the type locality of Homo floresiensis.

    Science.gov (United States)

    Roberts, R G; Westaway, K E; Zhao, J-x; Turney, C S M; Bird, M I; Rink, W J; Fifield, L K

    2009-11-01

    A robust timeframe for the extant cave deposits at Liang Bua, and for the river terraces in the adjoining Wae Racang valley, is essential to constrain the period of existence and time of extinction of Homo floresiensis and other biota that have been excavated at this hominin type locality. Reliable age control is also required for the variety of artifacts excavated from these deposits, and to assist in environmental reconstructions for this river valley and for the region more broadly. In this paper, we summarize the available geochronological information for Liang Bua and its immediate environs, obtained using seven numerical-age methods: radiocarbon, thermoluminescence, optically- and infrared-stimulated luminescence (collectively known as optical dating), uranium-series, electron spin resonance, and coupled electron spin resonance/uranium-series. We synthesize the large number of numerical age determinations reported previously and present additional age estimates germane to questions of hominin evolution and extinction. PMID:19254806

  20. 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

  1. 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...

  2. Historical development and politico-geographical characteristics of the border and borderland between the Republic of Croatia and Republic of Slovenia on Žumberak and in the Rivers Kupa and Čabranka Valley

    OpenAIRE

    Helena Ilona Bognar; Andrija Bognar

    2010-01-01

    Although natural basis cannot be a decisive criterion in defining borders, historical and politico-geographic development of the researched area reveals that natural bounds have been considerably used in the boundary demarcation between the Republic of Croatia and Republic of Slovenia. This can be also concluded for the analyzed sectors which are tied with the Žumberak Mountain and the Kupa and Čabranka River valleys. Besides natural favours (the boundary line runs over the top ridges of the ...

  3. 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

  4. 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

  5. Simulation of the effects of management alternatives on the stream-aquifer system, South Fork Solomon River Valley between Webster Reservoir and Waconda Lake, north-central Kansas

    Science.gov (United States)

    Burnett, R.D.; Reed, T.B.

    1985-01-01

    With extensive irrigation use of both surface water and groundwater in the South Fork Solomon River valley shortages of these water supplies have been created. A two-dimensional digital model of transient groundwater flow was applied to investigate the potential effects on the stream aquifer system of seven management alternatives. These alternatives included proposals to conserve surface water supplies by lining the Osborne Irrigation Canal with clay, replacing the lateral canals with pipe, removing phreatophytes, decreasing surface water use by 75%, 50%, or 25% and replacing it with groundwater sources, and continuing 1978 groundwater use and 1970-78 average surface water use until the end of the 20th century. Results were assessed by comparison of drawdowns of hydraulic head in the alluvial aquifer and base flow for each simulation. As listed in order of the smallest to the greatest potential effects on the system relative to drawdown and base flow the alternatives are: (1) removal of one-half of the phreatophytes; (2) continuation of 1978 groundwater withdrawals and average 1970-78 surface water supply; (3) replacement of the lateral canals with pipe; (4) lining the Osborne Irrigation Canal with clay; (5) decrease of surface water use by 25% and replacement of it with groundwater; (6) decrease of surface water use by 50% and replacement of it with groundwater; and (7) decrease of surface water use by 75% and replacement of it with groundwater. The removal of one-half of the phreatophytes would result in a decrease in average drawdown in the alluvial aquifer to about 1.74 ft and an increase in base flow of the Solomon River to about 12.3 cu ft/sec. The decrease of surface water supply by 75 % and a corresponding increase in groundwater withdrawal would result in an increase in drawdown in the aquifer to about 2.5 ft and a decrease in base flow to about 6.8 cu ft/sec. (Lantz-PTT)

  6. 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

  7. 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.

  8. Carbon dioxide emissions as affected by alternative long-term irrigation and tillage management practices in the lower Mississippi River Valley.

    Science.gov (United States)

    Smith, S F; Brye, K R

    2014-01-01

    Ensuring the sustainability of cultivated soils is an ever-increasing priority for producers in the Lower Mississippi River Valley (LMRV). As groundwater sources become depleted and environmental regulations become more strict, producers will look to alternative management practices that will ensure the sustainability and cost-effectiveness of their production systems. This study was conducted to assess the long-term (>7 years) effects of irrigation (i.e., irrigated and dryland production) and tillage (conventional and no-tillage) on estimated carbon dioxide (CO2) emissions from soil respiration during two soybean (Glycine max L.) growing seasons from a wheat- (Triticum aestivum L.-) soybean, double-cropped production system in the LMRV region of eastern Arkansas. Soil surface CO2 fluxes were measured approximately every two weeks during two soybean growing seasons. Estimated season-long CO2 emissions were unaffected by irrigation in 2011 (P > 0.05); however, during the unusually dry 2012 growing season, season-long CO2 emissions were 87.6% greater (P = 0.044) under irrigated (21.9 Mg CO2 ha(-1)) than under dryland management (11.7 Mg CO2 ha(-1)). Contrary to what was expected, there was no interactive effect of irrigation and tillage on estimated season-long CO2 emissions. Understanding how long-term agricultural management practices affect soil respiration can help improve policies for soil and environmental sustainability. PMID:25371912

  9. A regional model simulation of the 1991 severe precipitation event over the Yangtze-Huai River Valley. Part 2: Model bias

    Energy Technology Data Exchange (ETDEWEB)

    Gong, W.; Wang, W.C.

    2000-01-01

    This is the second part of a study investigating the 1991 severe precipitation event over the Uangtze-Huai River valley (YHRV) in China using both observations and regional model simulations. While Part 1 reported on the Mei-yu front and its association with large-scale circulation, this study documents the biases associated with the treatment of the lateral boundary in the regional model. Two aspects of the biases were studied: the driving field, which provides large-scale boundary forcing, and the coupling scheme, which specified how the forcing is adopted by the model. The former bias is defined as model uncertainty because it is not related to the model itself, while the latter bias (as well as those biases attributed to other sources) is referred to as model error. These two aspects were examined by analyzing the regional model simulations of the 1991 summer severe precipitation event over YHRV using different driving fields (ECMWF-TOGA objective analysis, ECMWF reanalysis, and NCEP-NCAR reanalysis) and coupling scheme (distribution function of the nudging coefficient and width of the buffer zone). Spectral analysis was also used to study the frequency distribution of the bias.

  10. 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. PMID:24530858

  11. Ethnobotany of food plants in the high river Ter valley (Pyrenees, Catalonia, Iberian Peninsula): non-crop food vascular plants and crop food plants with medicinal properties.

    Science.gov (United States)

    Rigat, Montse; Bonet, Maria Àngels; Garcia, Sònia; Garnatje, Teresa; Vallès, Joan

    2009-01-01

    The present study reports a part of the findings of an ethnobotanical research project conducted in the Catalan region of the high river Ter valley (Iberian Peninsula), concerning the use of wild vascular plants as food and the medicinal uses of both wild and cultivated food plants. We have detected 100 species which are or have been consumed in this region, 83 of which are treated here (the remaining are the cultivated food plants without additional medicinal uses). Some of them, such as Achillea ptarmica subsp. pyrenaica, Convolvulus arvensis, Leontodon hispidus, Molopospermum peloponnesiacum and Taraxacum dissectum, have not been previously reported, or have only very rarely been cited or indicated as plant foods in very restricted geographical areas. Several of these edible wild plants have a therapeutic use attributed to them by local people, making them a kind of functional food. They are usually eaten raw, dressed in salads or cooked; the elaboration of products from these species such as liquors or marmalades is a common practice in the region. The consumption of these resources is still fairly alive in popular practice, as is the existence of homegardens, where many of these plants are cultivated for private consumption. PMID:21883071

  12. 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.

  13. 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.

  14. 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.

  15. 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.

  16. 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...

  17. 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

  18. 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...... answer two fundamental questions: How has anthropogenic disturbance of rivers changed the fundamental form and physical processes in river valleys? Can we use our understanding of fl uvial patterns to restore the dynamic nature of channelised rivers and drained fl oodplains in river valleys?...

  19. 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

  20. 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

  1. 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

  2. Ground-water quality in the West Salt River Valley, Arizona, 1996-98: relations to hydrogeology, water use, and land use

    Science.gov (United States)

    Edmonds, Robert J.; Gellenbeck, Dorinda J.

    2002-01-01

    The U.S. Geological Survey collected and analyzed ground-water samples in the West Salt River Valley from 64 existing wells selected by a stratified-random procedure. Samples from an areally distributed group of 35 of these wells were used to characterize overall ground-water quality in the basin-fill aquifer. Analytes included the principal inorganic constituents, trace constituents, pesticides, and volatile organic compounds. Additional analytes were tritium, radon, and stable isotopes of hydrogen and oxygen. Analyses of replicate samples and blank samples provided evidence that the analyses of the ground-water samples were adequate for interpretation. The median concentration of dissolved solids in samples from the 35 wells was 560 milligrams per liter, which exceeded the U.S. Environmental Protection Agency Secondary Maximum Contaminant Level for drinking water. Eleven of the 35 samples had a nitrate concentration (as nitrogen) that exceeded the U.S. Environmental Protection Agency Maximum Contaminant Level for drinking water of 10 milligrams per liter. Pesticides were detected in eight samples; concentrations were below the Maximum Contaminant Levels. Deethylatrazine was most commonly detected. The pesticides were detected in samples from wells in agricultural or urban areas that have been irrigated. Concentrations of all trace constituents, except arsenic, were less than the Maximum Contaminant Levels. The concentration of arsenic exceeded the Maximum Contaminant Level of 50 micrograms per liter in two samples. Nine monitoring wells were constructed in an area near Buckeye to assess the effects of agricultural land use on shallow ground water. The median concentration of dissolved solids was 3,340 milligrams per liter in samples collected from these wells in August 1997. The nitrate concentration (as nitrogen) exceeded the Maximum Contaminant Level (10 milligrams per liter) in samples from eight of the nine monitoring wells in August 1997 and again in

  3. 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

  4. A new age within MIS 7 for the Homo neanderthalensis of Saccopastore in the glacio-eustatically forced sedimentary successions of the Aniene River Valley, Rome

    Science.gov (United States)

    Marra, Fabrizio; Ceruleo, Piero; Jicha, Brian; Pandolfi, Luca; Petronio, Carmelo; Salari, Leonardo

    2015-12-01

    Field observations as well as borehole, sedimentological and geochronologic data allow us to reconstruct the geologic setting of the Aniene River Valley in northern Rome, framing it within the recently recognized picture of temporally constrained, glacio-eustatically forced aggradational successions of this region. The sedimentary successions cropping out in this area include those described in the literature of the early 20th century in Saccopastore, where two skulls of Homo neanderthalensis were recovered. Based on the geometry, elevation and sedimentologic features of the investigated sedimentary deposits, the stratigraphic record of Saccopastore is correlated with the aggradational succession deposited in response to sea-level rise during glacial termination III at the onset of MIS 7 (i.e. ˜250 ka), corresponding to the local Vitinia Formation, as opposed to previous correlation with the MIS 5 interglacial and a locally defined "Tyrrhenian" stage (˜130 ka). This previous attribution was based on the interpretation of the sedimentary succession of Saccopastore, occurring between 15 and 21 m a.s.l., as a fluvial terrace formed around 130 ka during the Riss-Würm interglacial, ca. 6 m above the present-day alluvial plain of the Aniene River. In contrast to this interpretation, a 40Ar/39Ar age of 129 ± 2 ka determined for this study on a pyroclastic-flow deposit intercalated in a fluvial-lacustrine sequence forming a terrace ˜37 m a.s.l. near the coast of Rome constrains the aggradational succession in this area to MIS 5, precluding the occurrence of an equivalent fluvial terrace at lower elevation in the inland sector of Saccopastore. We therefore interpret the stratigraphic record of Saccopastore as the basal portion of the aggradational succession deposited in response to sea-level rise during MIS 7, whose equivalent fluvial terrace occurs around 55 m a.s.l. in this region. We also review the published paleontological and paleoethnological records recovered

  5. 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.

  6. 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.

  7. An Economic Valuation Of The Water Footprint: A Case Study Of The Citrus Sector In The Lower Sundays River Valley, Eastern Cape, South Africa.

    Science.gov (United States)

    Munro, S. A.; Fraser, G. C. G.; Snowball, J. D.

    2014-12-01

    With the implementation of the South African National Water Act (NWA) currently underway, water intensive sectors, such as the irrigated agriculture sector, can expect reduced water allocations and an increase in water prices. Water footprints (WFs) are increasingly being recognised as a meaningful way by which to represent human appropriation of water resources. This study examines the green and blue WFs of a variety of citrus cultivars in the lower Sundays River Valley, Eastern Cape, South Africa. WFs were calculated across dry, humid and long-term average climates and comparisons were made to available global average benchmark WFs. An number of indicators were also explored including; water productivity (ton/m3), economic land productivity (R/ha) and economic water productivity (R/m3) across all three climatic years. Most applications of WF sustainability assessments have focused on examining physical water scarcity as a measure for determining environmental hotspots. This study, therefore, also calculates the marginal product value for the irrigation water using a non-parametric linear programming approach. Marginal product value of irrigation water is not only useful in assisting with water-allocation decision making, but also useful in demonstrating the effects of resource depletion and degradation, and is therefore a useful measure for determining economic water scarcity. The study highlights that both farmers and governments could reduce blue WF's through adopting measures to increase water efficiency and considering economic water and land productivity. It also demonstrates the importance of including both environmental and economic scarcity indicators into water management and planning strategies, and the importance of conducting WF assessments using more accurate, site specific data.

  8. Life history, population dynamics and production of eastern mosquitofish, Gambusia holbrooki (Pisces, Poeciliidae), in rice fields of the lower Mondego River Valley, western Portugal

    Science.gov (United States)

    Cabral, João Alexandre; Marques, João Carlos

    1999-11-01

    The introduced population of Gambusia holbrooki from the rice fields of the lower Mondego River Valley, Portugal, was studied for 15 months, relating their life cycle and population dynamics with its production, in order to assess the role of the species in the energy flow and secondary production in this type of agro-ecosystem. Two main annual cohorts (1995 and 1996 cohorts) were identified. The females outnumbered males and the average female/male-ratio was 4. The inspection of ovary developmental stages of this viviparous fish, revealed that the most important reproductive period was between April and August. The first recruits were recorded in June and were present thereafter until October. Males from the parental cohort died before August, whereas parental females could survive until October. Mean adjusted fecundity (number of embryos divided by female standard length) peaked in July 1996 (0.95) and in June 1997 (1.05). Females reached greater sizes, had a higher growth rate and lived longer than males. Annual production was estimated at 3.101 g.m -2.year -1 (ash-free dry weight, AFDW), the average biomass at 2.896 g.m -2 (AFDW), and the P/B ratio was 1.071. A conjugation of life history, population dynamics, production and ecological traits (e.g. fast growth, reduced longevity, viviparity, high productivity, an intermediate position in food chain, and no special habitat requirements for reproduction) clearly show that the populations of G. holbrooki, introduced into rice fields all over the world, may play an important role in the structure and functioning of the biological communities of these important agro-ecosystems.

  9. 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.

  10. A regional model simulation of the 1991 severe precipitation event over the Yangtze-Huai River Valley. Part 1: Precipitation and circulation statistics

    Energy Technology Data Exchange (ETDEWEB)

    Wang, W.C.; Gong, W.; Wei, H.

    2000-01-01

    The summer Mei-yu event over eastern China, which is strongly influenced by large-scale circulation, is an important aspect of East Asian climate; for example, the Mei-yu frequently brings heavy precipitation to the Yangtze-Huai River valley (YHRV). Both observations and a regional model were used to study the Mei-yu front and its relation to large-scale circulation during the summer of 1991 when severe floods occurred over YHRV. This study has two parts: the first part, presented here, analyzes the association between heavy Mei-yu precipitation and relevant large-scale circulation, while the second part, documented by W. Gong and W.C. Wang, examines the model biases associated with the treatment of lateral boundary conditions (the objective analyses and coupling schemes) used as the driving fields for the regional model. Observations indicate that the Mei-yu season in 1991 spans 18 May--14 July, making it the longest Mei-yu period during the last 40 yr. The heavy precipitation over YHRV is found to be intimately related to the western Pacific subtropical high, upper-tropospheric westerly jet at midlatitudes, and lower-tropospheric southwest wind and moisture flux. The regional model simulates reasonably well the regional mean surface air temperature and precipitation, in particular the precipitation evolution and its association with the large-scale circulation throughout the Mei-yu season. However, the model simulates smaller precipitation intensity, which is due partly to the colder and drier model atmosphere resulting from excessive low-level clouds and the simplified land surface process scheme used in the present study.

  11. 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.

  12. Physicochemical and macroinvertebrate community trends in manmade ponds constructed in reclaimed opencast coal mines = Tendencias en la fisicoquímica y la comunidad de macroinvertebrados en balsas de nueva creación en minas de carbón a cielo abierto recuperadas

    OpenAIRE

    Miguel Chinchilla, Leticia

    2013-01-01

    En las últimas décadas el número de balsas construidas por el hombre ha crecido considerablemente. Sin embargo, el aumento en el número de balsas artificiales no ha sido acompañado por estudios científicos de carácter ecológico acerca de sus características y su funcionamiento a lo largo del tiempo. De hecho, el conocimiento que se tiene sobre la evolución a largo plazo en balsas artificiales es todavía escaso desde los puntos de vista fisicoquímico y biológico. Las balsas artificiales se con...

  13. 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.

  14. 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

  15. 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.

  16. 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.

  17. 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

  18. 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

  19. 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

  20. 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)

  1. 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

  2. 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

  3. Incidence of the phenomena El Nino and The Nina, on the climatic conditions in the valley of the River Cauca. Part I - climatological Analysis

    International Nuclear Information System (INIS)

    The influence of the phenomena known as El Nino and La Nina on the climatic conditions in the Cauca Valley (South-western Colombia) was studied by means of the analysis of climatic variability caused by these phenomena. Data were analysed from three weather stations located in the sugarcane area of influence, recorded during the 1972-1998 period. It was found that when these events are present in the Tropical Pacific Ocean, the behaviour of some climatic variables in the Cauca Valley is altered. These anomalies, which are of different magnitude for the different climatic variables, tend to be opposite in nature. The incidence of these phenomena on the Cauca Valley climate is noticeable in certain seasons and months

  4. 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

  5. Co-creating Understanding in Water Use & Agricultural Resilience in a Multi-scale Natural-human System: Sacramento River Valley--California's Water Heartland in Transition

    Science.gov (United States)

    Fairbanks, D. H.; Brimlowe, J.; Chaudry, A.; Gray, K.; Greene, T.; Guzley, R.; Hatfield, C.; Houk, E.; Le Page, C.

    2012-12-01

    The Sacramento River Valley (SRV), valued for its $2.5 billion agricultural production and its biodiversity, is the main supplier of California's water, servicing 25 million people. . Despite rapid changes to the region, little is known about the collective motivations and consequences of land and water use decisions, or the social and environmental vulnerability and resilience of the SRV. The overarching research goal is to examine whether the SRV can continue to supply clean water for California and accommodate agricultural production and biodiversity while coping with climate change and population growth. Without understanding these issues, the resources of the SRV face an uncertain future. The defining goal is to construct a framework that integrates cross-disciplinary and diverse stakeholder perspectives in order to develop a comprehensive understanding of how SRV stakeholders make land and water use decisions. Traditional approaches for modeling have failed to take into consideration multi-scale stakeholder input. Currently there is no effective method to facilitate producers and government agencies in developing a shared representation to address the issues that face the region. To address this gap, researchers and stakeholders are working together to collect and consolidate disconnected knowledge held by stakeholder groups (agencies, irrigation districts, and producers) into a holistic conceptual model of how stakeholders view and make decisions with land and water use under various management systems. Our approach integrates a top-down approach (agency stakeholders) for larger scale management decisions with a conceptual co-creation and data gathering bottom-up approach with local agricultural producer stakeholders for input water and landuse decisions. Land use change models that combine a top-down approach with a bottom-up stakeholder approach are rare and yet essential to understanding how the social process of land use change and ecosystem function are

  6. 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 ...

  7. 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 ...

  8. Historical development and politico-geographical characteristics of the border and borderland between the Republic of Croatia and Republic of Slovenia on Žumberak and in the Rivers Kupa and Čabranka Valley

    Directory of Open Access Journals (Sweden)

    Helena Ilona Bognar

    2010-06-01

    Full Text Available Although natural basis cannot be a decisive criterion in defining borders, historical and politico-geographic development of the researched area reveals that natural bounds have been considerably used in the boundary demarcation between the Republic of Croatia and Republic of Slovenia. This can be also concluded for the analyzed sectors which are tied with the Žumberak Mountain and the Kupa and Čabranka River valleys. Besides natural favours (the boundary line runs over the top ridges of the mountain massif of Žumberak/Gorjanci, as well as along the river flows, one must point out the fact that it is adapted to spatial organization of the borderland. Therefore, the boundary line is subsequent and co-operative here. Evolutionally, the border and borderland developed from terra nullius, frontier, and, finally, since the 16th century, have become a boundary line on the rivers Kupa and Čabranka, and since 1816, on Žumberak. Consequently, in spite of disputes in particular historical periods about the researched area's state and property appurtenance, the border has a centuries-old continuity. This can explain that nowadays the quoted sectors are least disputable in the boundary demarcation of the two sovereignties.

  9. 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

  10. 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

  11. Incidence of the phenomena El Nino and The Nina, on the climatic conditions in the valley of the River Cauca. Part II - Analysis of correlations

    International Nuclear Information System (INIS)

    In this research we seeked to evaluate the influence of the phenomena El Nino and La Nina on the climate regime in the Cauca Valley (south-western Colombia). Correlation analysis between climatic variables and ENSO external parameters was used. 11 climate variables of three weather stations and 14 external parameters, recorded during the 1972 -1998 period, were used in this investigation. The highest correlations were found using statistical artifices. These correlations show a strong dependence of the climatic variables during El Nino and La Nina events. In order to determine the seasons more affected, lineal correlations were calculated, particularly on a decadal, monthly and seasonal basis. These analyses show that the incidence of these phenomena on the Cauca Valley climate is very noticeable particularly in certain seasons, months and decades

  12. 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...

  13. 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 Redshouldered Hawks Buteo lineatus in a total of 32 of the 51 areas searched. We...

  14. Probability of Unmixed Young Groundwater (defined using chlorofluorocarbon-11 concentrations and tritium activities) in the Eagle River Watershed Valley-Fill Aquifer, Eagle County, North-Central Colorado, 2006-2007

    Science.gov (United States)

    Rupert, Michael G.; Plummer, L. Niel

    2009-01-01

    This raster data set delineates the predicted probability of unmixed young groundwater (defined using chlorofluorocarbon-11 concentrations and tritium activities) in groundwater in the Eagle River watershed valley-fill aquifer, Eagle County, North-Central Colorado, 2006-2007. This data set was developed by a cooperative project between the U.S. Geological Survey, Eagle County, the Eagle River Water and Sanitation District, the Town of Eagle, the Town of Gypsum, and the Upper Eagle Regional Water Authority. This project was designed to evaluate potential land-development effects on groundwater and surface-water resources so that informed land-use and water management decisions can be made. This groundwater probability map and its associated probability maps were developed as follows: (1) A point data set of wells with groundwater quality and groundwater age data was overlaid with thematic layers of anthropogenic (related to human activities) and hydrogeologic data by using a geographic information system to assign each well values for depth to groundwater, distance to major streams and canals, distance to gypsum beds, precipitation, soils, and well depth. These data then were downloaded to a statistical software package for analysis by logistic regression. (2) Statistical models predicting the probability of elevated nitrate concentrations, the probability of unmixed young water (using chlorofluorocarbon-11 concentrations and tritium activities), and the probability of elevated volatile organic compound concentrations were developed using logistic regression techniques. (3) The statistical models were entered into a GIS and the probability map was constructed.

  15. 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.

  16. 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...

  17. 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.

  18. Boron and strontium isotopes in studying the high boron content of the alluvial aquifer of the Cecina River valley, Central Italy

    International Nuclear Information System (INIS)

    The Cecina River basin extends over 900 km2 in Western Tuscany and includes the Northern part of the Larderello geothermal field. In this work the isotopic composition and concentration of boron and strontium dissolved in ground water, in surface waters, and in bottom sediments were analysed

  19. 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

  20. 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.

  1. 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.

  2. Overbank flooding and human occupation of the Shalongka site in the Upper Yellow River Valley, northeast Tibet Plateau in relation to climate change since the last deglaciation

    Science.gov (United States)

    Li, Guoqiang; Dong, Guanghui; Wen, Lijuan; Chen, Fahu

    2014-09-01

    Increased flooding caused by global warming threatens the safety of coastal and river basin dwellers, but the relationship of flooding frequency, human settlement and climate change at long time scales remains unclear. Paleolithic, Neolithic and Bronze Age cultural deposits interbedded with flood sediments were found at the Shalongka site near the north bank of the upper Yellow River, northeastern Tibetan Plateau. We reconstruct the history of overbank flooding and human occupation at the Shalongka site by application of optically stimulated luminescence and radiocarbon dating, grain size, magnetic susceptibility and color reflectance analysis of overbank sediment and paleosols. The reliability of OSL dating has been confirmed by internal checks and comparing with independent 14C ages; alluvial OSL ages have shown a systematic overestimation due to poor bleaching. Our results indicate that the Yellow River episodically overflowed and reached the Shalongka site from at least ~ 16 ka and lasting until ~ 3 ka. Soil development and reduced flooding occurred at ~ 15, ~ 8.3-5.4, and after ~ 3 ka, and prehistoric populations spread to the Shalongka site area at ~ 8.3, ~ 5.4, and ~ 3 ka. We suggest that climate change influenced the overbank flooding frequency and then affected prehistoric human occupation of the Shalongka site.

  3. A seringueira (Hevea brasiliensisMuell.-Arg. no Vale do Rio Paraíba The rubber plant in the Valley of the Paraiba river

    Directory of Open Access Journals (Sweden)

    João Ferreira da Cunha

    1966-01-01

    Full Text Available Foi feito um estudo sôbre o cultivo de seringueira (Hevea brasiliensisMuell. - Arg. no vale do rio Paraíba, no Estado de São Paulo, onde se fêz pela primeira vez o plantio com a finalidade de pesquisar a adaptação dessa espécie vegetal ao ambiente e as possibilidades da exploração comercial na região. O seringal foi plantado em terreno terciário, da série Guatemala, próximo de baixada, na Estação Experimental de Pindamonhangaba, localizada mais ou menos no centro do referido vale, a 22°55' de latitude sul, 45°25' de longitude e à altitude de 570 metros. O desenvolvimento das plantas foi normal. Ao completar sete anos de idade, havia 70% das plantas com as dimensões convencionais para início de exploração do seringal. A produção obtida de borracha foi de cêrca de 460 quilogramas por hectare no primeiro ano de colheita, 620 no segundo e 835 no terceiro. O aparecimento da moléstia das fôlhas, causada por Dothidella ulei,nos dois últimos anos de colheita, parece não ter tido influência apreciável na produção, que continuou aumentando. Os exames tecnológicos efetuados na borracha obtida revelaram características de fina qualidade.A study was made about the culture of the rubber plant (Hevea brasiliensisMuell.-Arg. in the Paraíba Valley of the State of São Paulo, in a region where this planting was done for the first time, with a view to investigate about the adaptability of its culture to this habitat and the possibility of its exploitation on this land. The rubber culure was established in the lowlands of the valley on tertiary soil that belongs to the Guatemala series, at the Pindamonhangaba Experiment station, located practically in the center of the valley, at 22°55' S. and 45°22' W., 570 m above sea level. The development of the plants was normal. After 7 years, when these plants had been settled, 70% were found to have the conventional dimensions for starting their exploitation. Rubber production was

  4. Uranium favorability of tertiary sedimentary rocks of the western Okanogan highlands and of the upper Columbia River valley, Washington. [Measurement and sampling of surface sections, collection of samples from isolated outcrops, and chemical and mineralogical analyses of samples; no known uranium deposits

    Energy Technology Data Exchange (ETDEWEB)

    Marjaniemi, D.K.; Robins, J.W.

    1975-08-01

    Tertiary sedimentary rocks in the northern portions of the western Okanogan highlands and in the upper Columbia River valley were investigated during a regional study to determine the favorability for potential uranium resources of the Tertiary sedimentary rocks of northeastern Washington. This project involved measurement and sampling of surface sections, collection of samples from isolated outcrops, and chemical and mineralogical analyses of samples. No portion of the project area of this report is rated of high or of medium favorability for potential uranium resources. Low favorability ratings are given to Oroville, Tonasket, and Pine Creek areas of the Okanogan River valley; to the Republic graben; and to the William Lakes, Colville, and Sheep Creek areas of the upper Columbia River valley. All these areas contain some fluvial, poorly sorted feldspathic or arkosic sandstones and conglomerates. These rocks are characterized by very low permeability and a consistently high siliceous matrix suggesting very low initial permeability. There are no known uranium deposits in any of these areas, and low level uranium anomalies are rare.

  5. 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

  6. 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.

  7. 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

  8. 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.

  9. 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

  10. 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.

  11. Production technology and provenance study of archaeological ceramics from relevant sites in the Alcantara River Valley (North-eastern Sicily, Italy)

    International Nuclear Information System (INIS)

    In this paper, volcanic-rich ceramic remains from the archaeological sites of Francavilla, Naxos and Taormina (Province of Messina, North-eastern Sicily) were studied by using inclusions as main provenance marker. Technological features, such as temper choice, vitrification degree and firing temperatures, were investigated by polarizing microscopy, X-ray diffractometry (XRD) and scanning electron microscopy (SEM). Information on the production centres was obtained through the identification of the source area of raw materials used as temper. Indeed, petrochemical analysis of the volcanic inclusions within the examined ceramics displayed strong affinities with structures/textures and compositions of the locally outcropping mugearitic products, probably ascribed to the eruptive activity of an eccentric vent of Mt. Etna (Mt. Mojo). A local production for the studied pottery samples has been therefore advanced, assuming that the used volcanic temper was easily available from the alluvial deposits along the Alcantara River stream, which is connected to the lava flow of Mt. Mojo.

  12. 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.

  13. 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.

  14. 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.

  15. 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。

  16. 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)

  17. 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

  18. 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

  19. 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.

  20. Perspectives for Very High-Resolution Climate Simulations with Nested Models: Illustration of Potential in Simulating St. Lawrence River Valley Channelling Winds with the Fifth-Generation Canadian Regional Climate Model

    Directory of Open Access Journals (Sweden)

    Mélissa Cholette

    2015-04-01

    Full Text Available With the refinement of grid meshes in regional climate models permitted by the increase in computing power, the grid telescoping or cascade method, already used in numerical weather prediction, can be applied to achieve very high-resolution climate simulations. The purpose of this study is two-fold: (1 to illustrate the perspectives offered by climate simulations on kilometer-scale grid meshes using the wind characteristics in the St. Lawrence River Valley (SLRV as the test-bench; and (2 to establish some constraints to be satisfied for the physical realism and the computational affordability of these simulations. The cascade method is illustrated using a suite of five one-way nested, time-slice simulations carried out with the fifth-generation Canadian Regional Climate Model, with grid meshes varying from roughly 81 km, successively to 27, 9, 3 and finally 1 km, over domains centered on the SLRV. The results show the added value afforded by very high-resolution meshes for a realistic simulation of the SLRV winds. Kinetic energy spectra are used to document the spin-up time and the effective resolution of the simulations as a function of their grid meshes. A pragmatic consideration is developed arguing that kilometer-scale simulations could be achieved at a reasonable computational cost with time-slice simulations of high impact climate events. This study lends confidence to the idea that climate simulations and projections at kilometer-scale could soon become operationally feasible, thus offering interesting perspectives for resolving features that are currently out of reach with coarser-mesh models.

  1. 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...

  2. 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

  3. 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

  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. A 1-D morphodynamic model of postglacial valley incision

    Science.gov (United States)

    Tunnicliffe, Jon F.; Church, Michael

    2015-11-01

    Chilliwack River is typical of many Cordilleran valley river systems that have undergone dramatic Holocene degradation of valley fills that built up over the course of Pleistocene glaciation. Downstream controls on base level, mainly blockage of valleys by glaciers, led to aggradation of significant glaciofluvial and glaciolacustrine valley fills and fan deposits, subsequently incised by fluvial action. Models of such large-scale, long-term degradation present a number of important challenges since the evolution of model parameters, such as the rate of bedload transport and grain size characteristics, are governed by the nature of the deposit. Sediment sampling in the Chilliwack Valley reveals a complex sequence of very coarse to fine textural modes. We present a 1-D numerical morphodynamic model for the river-floodplain system tailored to conditions in the valley. The model is adapted to dynamically adjust channel width to optimize sediment transporting capacity and to integrate relict valley fill material as the channel incises through valley deposits. Sensitivity to model parameters is studied using four principal criteria: profile concavity, rate of downstream grain size fining, bed surface sand content, and the timescale to equilibrium. Model results indicate that rates of abrasion and coarsening of the grain size distributions exert the strongest controls on all of the interrelated model performance criteria. While there are a number of difficulties in satisfying all model criteria simultaneously, results indicate that 1-D models of valley bottom sedimentary systems can provide a suitable framework for integrating results from sediment budget studies and chronologies of sediment evacuation established from dating.

  6. 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.

  7. 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

  8. Valley polarization in bismuth

    Science.gov (United States)

    Fauque, Benoit

    2013-03-01

    The electronic structure of certain crystal lattices can contain multiple degenerate valleys for their charge carriers to occupy. The principal challenge in the development of valleytronics is to lift the valley degeneracy of charge carriers in a controlled way. In bulk semi-metallic bismuth, the Fermi surface includes three cigar-shaped electron valleys lying almost perpendicular to the high symmetry axis known as the trigonal axis. The in-plane mass anisotropy of each valley exceeds 200 as a consequence of Dirac dispersion, which drastically reduces the effective mass along two out of the three orientations. According to our recent study of angle-dependent magnetoresistance in bismuth, a flow of Dirac electrons along the trigonal axis is extremely sensitive to the orientation of in-plane magnetic field. Thus, a rotatable magnetic field can be used as a valley valve to tune the contribution of each valley to the total conductivity. As a consequence of a unique combination of high mobility and extreme mass anisotropy in bismuth, the effect is visible even at room temperature in a magnetic field of 1 T. Thus, a modest magnetic field can be used as a valley valve in bismuth. The results of our recent investigation of angle-dependent magnetoresistance in other semi-metals and doped semiconductors suggest that a rotating magnetic field can behave as a valley valve in a multi-valley system with sizeable mass anisotropy.

  9. 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。

  10. 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

  11. The carbon stable isotope biogeochemistry of streams, Taylor Valley, Antarctica

    International Nuclear Information System (INIS)

    Highlights: ► δ13C-DIC reported from McMurdo Dry Valleys, Antarctica, streams. ► Stream water δ13CPDB values range −9.4‰ to +5.1‰, largely inorganic in character. ► Atmospheric exchange is the dominant control on δ13C-DIC. - Abstract: The McMurdo Dry Valleys region of Antarctica is the largest ice-free region on the continent. This study reports the first C stable isotope measurements for dissolved inorganic C present in ephemeral streams in four dry valleys that flow for four to twelve weeks during the austral summer. One of these valleys, Taylor Valley, has been the focus of the McMurdo Dry Valleys Long-Term Ecological Research (MCM-LTER) program since 1993. Within Taylor Valley, numerous ephemeral streams deliver water to three perennially ice-covered, closed-basin lakes: Lake Fryxell, Lake Hoare, and Lake Bonney. The Onyx River in the Wright Valley, the longest river in Antarctica, flows for 40 km from the Wright Lower Glacier and Lake Brownworth at the foot of the glacier to Lake Vanda. Streamflow in the McMurdo Dry Valley streams is produced primarily from glacial melt, as there is no overland flow. However, hyporheic zone exchange can be a major hydrogeochemical process in these streams. Depending on landscape position, these streams vary in gradient, channel substrate, biomass abundance, and hyporheic zone extent. This study sampled streams from Taylor, Wright, Garwood, and Miers Valleys and conducted diurnal sampling of two streams of different character in Taylor Valley. In addition, transect sampling was undertaken of the Onyx River in Wright Valley. The δ13CPDB values from these streams span a range of greater than 14‰, from −9.4‰ to +5.1‰, with the majority of samples falling between −3‰ and +2‰, suggesting that the C stable isotope composition of dissolved C in McMurdo Dry Valley streams is largely inorganic in character. Because there are no vascular plants on this landscape and no groundwater input to these streams

  12. 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

  13. 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.

  14. 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...

  15. 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.

  16. 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...

  17. 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.

  18. 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...

  19. 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,...

  20. 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

  1. 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

  2. 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.

  3. 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

  4. 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

  5. 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

  6. 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

  7. Erosion of steepland valleys by debris flows

    Science.gov (United States)

    Stock, J.D.; Dietrich, W.E.

    2006-01-01

    Episodic debris flows scour the rock beds of many steepland valleys. Along recent debris-flow runout paths in the western United States, we have observed evidence for bedrock lowering, primarily by the impact of large particles entrained in debris flows. This evidence may persist to the point at which debris-flow deposition occurs, commonly at slopes of less than ???0.03-0.10. We find that debris-flow-scoured valleys have a topographic signature that is fundamentally different from that predicted by bedrock river-incision models. Much of this difference results from the fact that local valley slope shows a tendency to decrease abruptly downstream of tributaries that contribute throughgoing debris flows. The degree of weathering of valley floor bedrock may also decrease abruptly downstream of such junctions. On the basis of these observations, we hypothesize that valley slope is adjusted to the long-term frequency of debris flows, and that valleys scoured by debris flows should not be modeled using conventional bedrock river-incision laws. We use field observations to justify one possible debris-flow incision model, whose lowering rate is proportional to the integral of solid inertial normal stresses from particle impacts along the flow and the number of upvalley debris-flow sources. The model predicts that increases in incision rate caused by increases in flow event frequency and length (as flows gain material) downvalley are balanced by rate reductions from reduced inertial normal stress at lower slopes, and stronger, less weathered bedrock. These adjustments lead to a spatially uniform lowering rate. Although the proposed expression leads to equilibrium long-profiles with the correct topographic signature, the crudeness with which the debris-flow dynamics are parameterized reveals that we are far from a validated debris-flow incision law. However, the vast extent of steepland valley networks above slopes of ???0.03-0.10 illustrates the need to understand debris

  8. 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...

  9. 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.

  10. 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。

  11. 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...

  12. 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...

  13. 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.

  14. Lista de espécies de borboletas (Lepidoptera, Papilionoidea e Hesperioidea da região do vale do rio Maquiné, Rio Grande do Sul, Brasil Butterfly species list (Lepidoptera, Papilionoidea and Hesperioidea in a region at valley of Maquiné river, Rio Grande do Sul State, Brazil

    Directory of Open Access Journals (Sweden)

    Cristiano Agra Iserhard

    2004-09-01

    Full Text Available Procurando contribuir para o levantamento sistemático e o conhecimento das borboletas da Mata Atlântica do Rio Grande do Sul, foram realizadas saídas bimestrais em quatro localidades no vale do rio Maquiné, entre junho de 2001 e agosto de 2002. Foi elaborada uma listagem com 292 espécies de borboletas, sendo destas 42 registros novos para o Rio Grande do Sul e sete espécies raras e/ou indicadoras de ambiente preservado.To add to the knowledge on the diversity of the butterflies from Atlantic Rainforest of Rio Grande do Sul State, a systematic survey was carried out at the valley of Maquiné river, from june 2001 to august 2002, in four sampling localities. A list resulted with 292 butterfly species, with 42 new registers for Rio Grande do Sul and seven rare and/or environmental quality indicator butterfly species.

  15. 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.

  16. 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.

  17. 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 (Canavalia ensiformis, submetidas a dois manejos (subtratamentos: (a ceifada e deixada na superfície do terreno e (b ceifada e incorporada ao solo, havendo ainda uma testemunha sem leguminosa. O segundo experimento, que se iniciou com o quinto ciclo de produção de uva, abrangeu três tratamentos: (1 testemunha; (2 crotalária júncea e (3 feijão-de-porco, combinados com dois subtratamentos: (1 100 % da adubação recomendada pela análise de solo e (2 50 % dessa adubação. Ao todo, houve onze ciclos de leguminosas e nove safras de uva. A produção de biomassa das leguminosas decresceu ao longo do tempo. A adubação verde proporcionou uma melhoria nas características químicas do solo, aumentando os teores da MO e do Ca trocável e o valor da CTC na camada de 0-10 cm de profundidade. Não houve um efeito consistente da adubação verde na produtividade e qualidade da uva.The soils of the Submiddle São Francisco River Valley are generally sandy, with low nutrient retention capacity. Since they are

  18. ¿Héroe cultural o víctima expiatoria? innovaciones técnicas y transgresión social entre los nahuas del alto balsas (México)1

    OpenAIRE

    Hémond, Aline

    2013-01-01

    Note portant sur l’auteur Introducción Desde los años 60, la región nahua de la cuenca alta del río Balsas vive al ritmo de la producción artesanal turística. Actualmente, más de 12 000 personas, distribuidas en siete comunidades y organizadas en talleres familiares y escuelas artísticas, pintan sobre papel amate, cerámica y peces de madera. La “epopeya” artesanal de aquella región se inició en la década de los años 50 con una sola familia en el pueblo de Ameyaltepec, la cual empezó a dibujar...

  19. 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). ...

  20. The geochemistry of groundwater resources in the Jordan Valley: The impact of the Rift Valley brines

    International Nuclear Information System (INIS)

    The chemical composition of groundwater in the Jordan Valley, along the section between the Sea of Galilee and the Dead Sea, is investigated in order to evaluate the origin of the groundwater resources and, in particular, to elucidate the role of deep brines on the chemical composition of the regional groundwater resources in the Jordan Valley. Samples were collected from shallow groundwater in research boreholes on two sites in the northern and southern parts of the Jordan Valley, adjacent to the Jordan River. Data is also compiled from previous published studies. Geochemical data (e.g., Br/Cl, Na/Cl and SO4/Cl ratios) and B, O, Sr and S isotopic compositions are used to define groundwater groups, to map their distribution in the Jordan valley, and to evaluate their origin. The combined geochemical tools enabled the delineation of three major sources of solutes that differentially affect the quality of groundwater in the Jordan Valley: (1) flow and mixing with hypersaline brines with high Br/Cl (>2 x 10-3) and low Na/Cl (-3); and (3) recharge of anthropogenic effluents, primarily derived from evaporated agricultural return flow that has interacted (e.g., base-exchange reactions) with the overlying soil. It is shown that shallow saline groundwaters influenced by brine mixing exhibit a north-south variation in their Br/Cl and Na/Cl ratios. This chemical trend was observed also in hypersaline brines in the Jordan valley, which suggests a local mixing process between the water bodies

  1. Glacial geology of the upper Wairau Valley, Marlborough, New Zealand

    International Nuclear Information System (INIS)

    Late Pleistocene glaciers in the upper Wairau Valley deposited four groups of moraines inferred to represent one Waimean ice advance, two Otiran ice advances, and an advance of early Aranuian age. The Waimean and early Otiran glaciers advanced into Tarndale Valley, deposited terminal moraines, and shed outwash down both the Alma River and Travellers Valley. The middle Otiran glacier terminated in northern Tarndale Valley and shed outwash from the southern part of its terminus down the Alma River. The north side of the terminus abutted a large ice-dammed lake in the Wairau Gorge, and fan-deltas graded to an old shore level at an elevation of 1040 m. Well-preserved moraines at the mouths of four glaciated tributaries may be middle Otiran recessional, or late Otiran terminal moraines. The latest ice advance extended 11 km down the upper Wairau Valley and deposited a subdued moraine at Island Gully. The composite chronology of the latest glacial advance based on 10 radiocarbon ages suggests it occurred between about 9.5 and 10.2 ka. This age span is similar to that of early Aranuian glacial advances dated by other workers in the Southern Alps, and may reflect Younger Dryas cooling. (author). 22 refs., 10 figs., 3 tabs

  2. BIRDS SEASONAL FLUCTIATIONS IN SMALL RIVERS’ VALLEYS OF THE SOUTHERN PART OF ZAPOROZHSKAYA REGION

    Directory of Open Access Journals (Sweden)

    Matruhan T.I.

    2011-10-01

    Full Text Available Role of river valleys in the existence of a large number of bird species is greater than in the breeding period andduring seasonal migrations and movements. Total during the year they recorded 102 bird species, including 62 speciesof breeding period. Feature of the habitat of the valleys of small rivers is the combination in small areas of differenthabitats. This increases the patchiness of zonal steppe landscape, which allows the expansion of areas along the riverbeds of individual species. Flood regime of rivers is the determining factor for the birds: The most diverse speciescomposition and abundance of avifauna of individual species in the high-water seasons.

  3. Breathing Valley Fever

    Centers for Disease Control (CDC) Podcasts

    2014-02-04

    Dr. Duc Vugia, chief of the Infectious Diseases Branch in the California Department of Public Health, discusses Valley Fever.  Created: 2/4/2014 by National Center for Emerging and Zoonotic Infectious Diseases (NCEZID).   Date Released: 2/5/2014.

  4. Silicon Valley's Turnaround

    Institute of Scientific and Technical Information of China (English)

    Joseph Leu

    2006-01-01

    @@ During Silicon Valley's dramatic economic growth fueled by the Internet boom and business investment in information technology, employment in the region's high-tech sec tor tripled between 1995 and 2000. The economic boom gave rise to many new firms,drawing em ployees into high-tech jobs from other regions and other industries.

  5. Silicon Valley Policy

    Institute of Scientific and Technical Information of China (English)

    2006-01-01

    @@ Silicon Valley is home to the most dynamic industries in the California economy. These industries--the high-tech sector--are driven by innovation, and each new wave of innovation is usually led by creative entrepreneurs starting new firms.

  6. Metal and organic residues in addled eggs of least terns and piping plovers in the Platte Valley of Nebraska

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The concentration of most residues detected in eggs of least terns and piping plovers nesting in the Platte River valley are not a cause for alarm. However,...

  7. Water power small scale hydro. Elan Valley

    International Nuclear Information System (INIS)

    The Elan Valley small-scale hydro project, which is owned and operated by Hyder Industrial Ltd, is located on the Elan Valley estate in the Cambrian Mountains in mid-Wales. Five reservoirs and four impounding dams were built in the Elan and Claerwen river valleys during the first half of the 20th century to supply water to Birmingham. Following the award of a contract under the Government's third non-Fossil Fuel Obligation Order (NFFO-3) to supply 4.2 MW of electricity to the National Grid during the 1990s, Hyder refurbished the original turbines at one location and built new units at four others. The existing water infrastructure was utilised. The total cost of the scheme, which generated some 35,700 MWh of electricity between May 1997 and March 1999, was 5.2 million pounds sterling. Details of the power generation units at the five hydro power stations, the power output, power transmission, planning requirements, measures taken by Hyder to minimise the scheme's environmental impact and the scheme's benefits are given

  8. 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

  9. Landslide Buries Valley of the Geysers

    Science.gov (United States)

    2007-01-01

    Geysers are a rare natural phenomena found only in a few places, such as New Zealand, Iceland, the United States (Yellowstone National Park), and on Russia's far eastern Kamchatka Peninsula. On June 3, 2007, one of these rare geyser fields was severely damaged when a landslide rolled through Russia's Valley of the Geysers. The landslide--a mix of mud, melting snow, trees, and boulders--tore a scar on the land and buried a number of geysers, thermal pools, and waterfalls in the valley. It also blocked the Geyser River, causing a new thermal lake to pool upstream. The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA's Terra satellite captured this infrared-enhanced image on June 11, 2007, a week after the slide. The image shows the valley, the landslide, and the new thermal lake. Even in mid-June, just days from the start of summer, the landscape is generally covered in snow, though the geologically heated valley is relatively snow free. The tree-covered hills are red (the color of vegetation in this false-color treatment), providing a strong contrast to the aquamarine water and the gray-brown slide. According to the Russian News and Information Agency (RIA) [English language], the slide left a path roughly a kilometer and a half (one mile) long and 200 meters (600 feet) wide. Within hours of the landslide, the water in the new lake inundated a number of additional geysers. The geysers directly buried under the landslide now lie under as much as 60 meters (180 feet) of material, according to RIA reports. It is unlikely that the geysers will be able to force a new opening through this thick layer, adds RIA. Among those directly buried is Pervenets (Firstborn), the first geyser found in the valley, in 1941. Other geysers, such as the Bolshoi (Greater) and Maly (Lesser) Geysers, were silenced when buried by water building up behind the new natural dam. According to Vladimir and Andrei Leonov of the Russian Federation Institute of

  10. Modern Pollen Study in Lake Qinghai Valley

    Science.gov (United States)

    Shang, X.; Li, X.; An, Z.; Ji, M.; Zhang, H.

    2008-12-01

    This study shows results of modern pollen in Lake Qinghai valley in the northeastern Tibetan Plateau. The records suggest that most pollen assemblages are dominated by shrub and herb pollen (mostly>84%). Seventeen taxa of indicator pollen are significantly correlated with the vegetation types of this area. In the pollen spectra, Artemisia is over-represented, while Poaceae, Cyperaceae and Polygonaceae are low- represented. Artermisia/Chenopodiaceae (A/C) radios with the regional vegetation characteristic can be used as a proper index to reconstruct the history of vegetation and climate in Lake Qinghai valley. Modern pollen in the lake mainly comes from the nearby vegetation. The pollen spectra is controlled by the directions and velocity of the wind and influenced by rivers. The distribution of modern pollen in Lake Qinghai tends to be similar in most part of the lake. The difference of pollen sedimentation process in the lake can be potentially influenced by the focusing function of the lake, river streams, and lake current.

  11. Evolution of collapse valleys in karst - examples from the Carpatho-Balkanides of Serbia

    Science.gov (United States)

    Petrović, Aleksandar S.; Ćalić, Jelena; Spalević, Aleksandra; Pantić, Marko

    2016-04-01

    Development of valleys in karst is an issue which has not been sufficiently studied in karst surface morphology. THESE valleys are long linear forms whose orthogonal projections resemble normal valleys, but most of their characteristics are strongly influenced by karst process. In largest number of relevant references, this subject is either only briefly mentioned or completely lacking. This paper presents the examples of a particular type of valley in karst formed by cave ceiling collapse close to the topographical surface. Karst of the Carpatho-Balkanides in eastern Serbia is characterized by uneven spatial distribution in several large massifs, but also in a large number of relatively small outcrops (patches and belts), which enable the development of contact karst and fluviokarst. Many morphological elements are of fluvial origin, subsequently modified by karst process. Collapse valleys occur mostly at the downstream contacts (where a seasonal watercourse leaves limestones) or in karst/limestone belts. In the first phase, which is visible on the example of the Radovanska Reka, the river course sinks to the swallets in the riverbed and forms a blind valley. After sinking, the water flows through the tunnel cave, while largest part of the valley remains above the cave. The bottom of the dry valley is dissected by deep dolines, reaching almost to the cave roof. In this part of the study, the area was scanned by a multistation Leica Nova MS 50 (resolution 20 cm @ 10 m). In the second phase, the doline bottoms reach the cave ceilings which develop holes at certain points, as it is case at the Zamna River valley. These hollows tend to enlarge with time, and the surface of the cave ceiling is reduced. The third, final phase is characterised by collapse of larger segments of cave ceilings. Only the natural bridges remain, as the remnants of former caves (e.g. in the Vratna River valley, Ravna Reka valley). These parts of valleys in karst are usually narrow, steep

  12. 汶川地震中国道 G213左侧某典型高山河谷场地地震滑坡响应分析%ANALYSIS OF LANDSLIDE RESPONSES OF A TYPICAL HIGH HILL-RIVER VALLEY FIELD NEAR NATIONAL ROAD G213 DURING WENCHUAN EARTHQUAKE

    Institute of Scientific and Technical Information of China (English)

    杨长卫; 张建经

    2013-01-01

      以国道 G213左侧一处包含河谷地形的高陡边坡为原型,采用新型离散元计算方法——基于连续模型的离散元方法(CDEM),对高烈度地震作用下高陡边坡上的堆积体滑坡由变形累计到破坏滑动的全过程进行模拟,并结合振动台试验结果,对该高陡边坡上堆积体的地震滑坡响应进行研究。研究结果表明,在地震力和重力作用下,堆积体顶部先出现应力集中,造成堆积体沿基岩–堆积体结构面后缘产生变形,进而造成该处出现拉伸、剪切破坏点,之后随着地震动的持续,基岩–堆积体结构面上的剪切破坏点逐渐向堆积体中前部的锁固段扩展,同时伴随着堆积体表面拉伸破坏点的增加,最终造成锁固段发生渐进性破坏,堆积体从剪出口滑出形成滑坡。滑塌发生的时间与地震动峰值加速度到达的时间同步或稍微有所滞后。在高陡边坡地形中,以输入地震波为基准,不论是坡面还是坡体内,不同位置的峰值加速度沿坡高均有所放大,表现为竖向峰值加速度的放大效应>水平峰值加速度的放大效应,坡面峰值加速度的放大效应>坡体内峰值加速度的放大效应。在河谷地形中,以输入波为基准,不论是河床还是河岸两侧的斜坡,不同位置的峰值加速度沿高程均具有不同程度的放大;河谷对加速度放大效应的影响具有一定范围,且在该范围内水平加速度的放大效应>竖向加速度的放大效应,与坡面处加速度的放大效应刚好相反;加速度的放大效应具有一定的方向性,且该方向性与河岸两侧斜坡的坡度有关;加速度放大效应在河谷底部的分布具有不均匀性,距离河岸越近,加速度放大效应越强烈。%  A high steep hill with river valley near National Road G213 is used as a prototype. A full process from initial deformation to sliding of the

  13. Where rivers and oceans collide

    Science.gov (United States)

    Crockett, J. S.; Nittrouer, C. A.; Ogston, A. S.; Sternberg, R. W.; Driscoll, N. W.; Babcock, J.; Milliman, J. D.; Slingerland, R.; Naar, D. F.; Donahue, B.; Walsh, J. P.; Dietrich, W.; Parker, G.; Bera, M.; Davies, H.; Harris, P.; Goni, M.; Aller, R.; Aller, J.

    Fluvial sediment fills the coastal ocean, and sea level rise floods river valleys. This epic battle of terrestrial and marine processes occurs along all shorelines, and the complexities are especially well revealed in the Gulf of Papua, a foreland basin on the southern coast of New Guinea. Two hundred to four hundred million tons of sediment are supplied each year by the Fly and other rivers to a continental shelf that has been dissected by ancestors of these same rivers. The new sediment builds a large depositional feature known as a clinoform, which grows seaward and buries the record of earlier environments.

  14. THE BIOLOGY AND BEHAVIOUR OF JAPANESE ENCEPHALITIS VECTORS IN THE HUMAN HOUSES IN THE UPPER VALLEY OF THE MEKONG RIVER IN YUNNAN, P.R. CHINA%中国云南湄公河上游乙型脑炎传播媒介生物学及行为的研究

    Institute of Scientific and Technical Information of China (English)

    周红宁; 李春富; 吴超; 张再兴; 王丕玉; Nigel Hill

    2005-01-01

    Objective To study the seasonal abundance, host preference and patterns of biting activity in houses, and larval biology of Japanese Encephalitis(JE) vectors, so as to develop effective control measures. Methods From June to December 2001, choosing one plantation in the upper valley of the Mekong River in the south of Yunnan, Centres for Disease Control (CDC) light-trap and human landing methods were used to capture mosquitoes, blood meal samples were tested by the precipitin method and biologic habits of immature stages were investigated for their breeding sites. Results A total of 5 726 JE vector mosquitoes of 11 species of 5 genera were collected from a plantation in the upper valley of the Mekong River. Peaks in the population densities of Culex tritaeniorhynchus, Cx. pseudovishnui, Cx. fuscocephala and Anopheles sinensis were in the rainy season from June to August, by both light-trap and human landing catches. Biting activity of these three Culex mosquitoes, both in and outside plantation, began after sunset and maintained through the night. But the An. sinensis biting peak was before 21:00 hours. Comparison of the efficacy of mosquito collection by light trap in houses with that out of doors by human landing catches, showed that the indoor catches of JE vectors were higher than that out of doors. Analysis of mosquito blood meals showed that their human blood indices were high. Larvae had characteristic distributions in relation to the plantation. Conclusion All of these finds suggested that in the upper valley of Mekong River, Cx. tritaeniorhynchus, Cx. pseudovishnui, Cx. fuscocephala and An. sinensis are different on the biologics and behaviours in comparison with those of previous studies in animal sheds.%目的探讨乙型脑炎病毒媒介在人房的季节消长、嗜血习性和叮人行为,以及其幼虫相关的生物学习性, 从而制定出有效的媒介控制措施. 方法 2001年6~12月,在云南南部湄公河上游,选

  15. Green valley galaxies

    Directory of Open Access Journals (Sweden)

    Salim S.

    2014-01-01

    Full Text Available The “green valley” is a wide region separating the blue and the red peaks in the ultraviolet-optical color magnitude diagram, first revealed using GALEX UV photometry. The term was coined by Christopher Martin (Caltech, in 2005. Green valley highlights the discriminating power of UV to very low relative levels of ongoing star formation, to which the optical colors, including u−r, are insensitive. It corresponds to massive galaxies below the star-forming, “main” sequence, and therefore represents a critical tool for the study of the quenching of star formation and its possible resurgence in otherwise quiescent galaxies. This article reviews the results pertaining to (predominantly disk morphology, structure, environment, dust content and gas properties of green valley galaxies in the local universe. Their relationship to AGN is also discussed. Attention is given to biases emerging from defining the “green valley” using optical colors. We review various evolutionary scenarios and we present evidence for a new one, the quasi-static view of the green valley, in which the majority (but not all of galaxies currently in the green valley were only partially quenched in the distant past and now participate in a slow cosmic decline of star formation, which also drives down the activity on the main sequence, presumably as a result of the dwindling accretion/cooling onto galaxy disks. This emerging synthetic picture is based on the findings from Fang et al. (2012, Salim et al. (2012 and Martin et al. (2007, as well as other results.

  16. Revitalizing the Mahoning Valley

    OpenAIRE

    T F Buss; Vaughan, R J

    1987-01-01

    For nearly a decade, since the closing of its steel mills, the Mahoning Valley in northeast Ohio has pursued a traditional development strategy, based upon large capital subsidies, to attract new or support existing businesses. These policies have failed. As a result, local business leaders have questioned the foundations of traditional policy and have developed an alternative strategy that involves a far broader set of state and local programs in the development process. The new strategy aim...

  17. Estudo genético de bacia orgânica do Vale do Paraíba Genetic study of the organic basin of the Paraiba River Valley

    Directory of Open Access Journals (Sweden)

    Francisco da Costa Verdade

    1966-01-01

    Full Text Available Através de sondagens, fotointerpretação do relêvo e altimetria, foi estudada a formação duma bacia orgânica situada entre São José dos Campos e Caçapava. Esta bacia teve sua origem provável em um lento abatimento por acomodação de camadas no substrato terciário da planície aluvial. Êste fenômeno propiciou o acúmulo orgânico abaixo do nível atual do rio. A preservação da bacia, situada ao sul do rio, sem destruição pela oscilação meândrica, deve-se à tendência do leito em se deslocar para o norte, conforme comprovam os terraços. Estas condições devem prevalecer em outras áreas do mesmo rio e que possuam espêssas camadas orgânicas.With the help of probing, relief photointerpretation and altimetry, the formation of an organic basin located between São José dos Campos and Caçapava was studied. This basin probably was originated by slow settlement through accomodation of layers on the tertiary substract below alluvial plains. This phenomenon favored the organic accumulation under the present level of the river. The preservation of the southern basin of the river without being destroyed by meandric oscillation, is due to the tendency of the river-bed to dislocate toward the north, as can be proved by the terraces. These conditions should prevail in other areas of the same river and which may have deep organic layers.

  18. Quantifying flooding regime in floodplain forests to guide river restoration

    OpenAIRE

    Christian O. Marks; Keith H Nislow; Magilligan, Francis J.

    2014-01-01

    Abstract Determining the flooding regime needed to support distinctive floodplain forests is essential for effective river conservation under the ubiquitous human alteration of river flows characteristic of the Anthropocene Era. At over 100 sites throughout the Connecticut River basin, the largest river system in New England, we characterized species composition, valley and channel morphology, and hydrologic regime to define conditions promoting distinct floodplain forest assemblages. Species...

  19. Just Water? Social Disparities and Drinking Water Quality in California's San Joaquin Valley

    OpenAIRE

    Balazs, Carolina Laurie

    2011-01-01

    California's San Joaquin Valley is one of the world's richest agricultural regions yet it is also home to some of the greatest environmental problems, including drinking water contamination. After decades of intensive agriculture in the San Joaquin Valley (SJV), the region's aquifers and rivers are some of the most contaminated in the nation. This creates a notoriously difficult environmental problem to regulate, and related public health and environmental justice issues. Ninety-five perce...

  20. Ethno-Botanical Study of Medicinal Plants of Paddar Valley of Jammu and Kashmir, India

    OpenAIRE

    Gupta, Sushil Kumar; Sharma, Om Prakash; Raina, Narinder Singh; Sehgal, Sandeep

    2013-01-01

    The Paddar Valley, historically known as Sapphire Valley situated in Kishtwar district, is a prime landmark in the Jammu region of J&K state and is known for its rich cultural and plant diversity because of diverse habitats such as rivers, streams, meadows and steep mountain slopes. The area is located in the dry temperate region comprising typical vegetation which disappears completely on the eastern slopes, dominated by a variety of economical species which play an important role in the rur...

  1. Community Irrigation Supplies and Regional Water Transfers in the Colca Valley, Peru

    OpenAIRE

    Vera Delgado, J.R.; Vincent, L.F.

    2013-01-01

    Water governance of Andean river valleys that are the site of large-scale water transfers and the home to highland communities with their own irrigation practices has been the subject of research and debate since the large water transfers began. In Peru, local and regional water governance has been shaped by changing national water laws that remain controversial regarding their effects on highland water users. This article presents findings from the Colca Valley, where water has been transfer...

  2. Social Networks in Silicon Valley

    Institute of Scientific and Technical Information of China (English)

    Joseph Leu

    2006-01-01

    @@ Social network is a dominant, distinguishing characteristic of Silicon Valley. Because innovation entails coping with a high degree of uncertainty,such innovation is particularly dependent on networks.

  3. Session: Long Valley Exploratory Well

    Energy Technology Data Exchange (ETDEWEB)

    Tennyson, George P. Jr.; Finger, John T.; Eichelberger, John C.; Hickox, Charles E.

    1992-01-01

    This session at the Geothermal Energy Program Review X: Geothermal Energy and the Utility Market consisted of four presentations: ''Long Valley Exploratory Well - Summary'' by George P. Tennyson, Jr.; ''The Long Valley Well - Phase II Operations'' by John T. Finger; ''Geologic results from the Long Valley Exploratory Well'' by John C. Eichelberger; and ''A Model for Large-Scale Thermal Convection in the Long Valley Geothermal Region'' by Charles E. Hickox.

  4. Geohydrology of the Unconsolidated Valley-Fill Aquifer in the Meads Creek Valley, Schuyler and Steuben Counties, New York

    Science.gov (United States)

    Miller, Todd S.; Bugliosi, Edward F.; Reddy, James E.

    2008-01-01

    The Meads Creek valley encompasses 70 square miles of predominantly forested uplands in the upper Susquehanna River drainage basin. The valley, which was listed as a Priority Waterbody by the New York State Department of Environmental Conservation in 2004, is prone to periodic flooding, mostly in its downstream end, where development is occurring most rapidly. Hydraulic characteristics of the unconsolidated valley-fill aquifer were evaluated, and seepage rates in losing and gaining tributaries were calculated or estimated, in an effort to delineate the aquifer geometry and identify the factors that contribute to flooding. Results indicated that (1) Meads Creek gained about 61 cubic feet of flow per second (about 6.0 cubic feet per second per mile of stream channel) from ground-water discharge and inflow from tributaries in its 10.2-mile reach between the northernmost and southernmost measurement sites; (2) major tributaries in the northern part of the valley are not significant sources of recharge to the aquifer; and (3) major tributaries in the central and southern part of the valley provide recharge to the aquifer. The ground-water portion of streamflow in Meads Creek (excluding tributary inflow) was 11.3 cubic feet per second (ft3/s) in the central part of the valley and 17.2 ft3/s in the southern part - a total of 28.5 ft3/s. Ground-water levels were measured in 29 wells finished in unconfined deposits for construction of a potentiometric-surface map to depict directions of ground-water flow within the valley. In general, ground water flows from the edges of the valley toward Meads Creek and ultimately discharges to it. The horizontal hydraulic gradient for the entire 12-mile-long aquifer averages about 30 feet per mile, whereas the gradient in the southern fourth of the valley averages about half that - about 17 feet per mile. A water budget for the aquifer indicated that 28 percent of recharge was derived from precipitation that falls on the aquifer, 32

  5. Silicon Valley Lifestyle

    Institute of Scientific and Technical Information of China (English)

    Joseph Leu

    2005-01-01

    @@ As we embrace the rapid developments of the new media age,competitiveness in the field of internet and computer technology is an increasingly crucial factor in stimulating new business,jobs and new industry in the region.Accelerating advancements in new media,internet,software and computer technologies offer new commercial opportunities and sources of economic revenue. Silicon Valley has been a model of the new age since its existence.While the dream place not only has a unique business model,but also has a very special lifestyle.

  6. 萨拉乌苏河流域高分辨率的沙丘砂常量元素分布指示的全新世寒冷事件%Cold events of Holocene indicated by primary elements distribution of the high-resolution sand dunes in the Salawusu River Valley

    Institute of Scientific and Technical Information of China (English)

    牛东风; 李保生; 杜恕环; 温小浩; 邱世藩; 欧先交; 杨艺

    2008-01-01

    The components of the primary elements in the dune sands for the MGS1 subsection of the Milanggouwan section in the Salawusu River valley, compared with those of modern dune sands, show that they were caused by East Asian winter monsoon in the Mu Us desert during Holocene. The examined ages for the 11 layers of dune sands, based on the average sedimentary rate, are: 0 to 960, 1350-2240, 2470 to 3530, 4000 to 4180, 4290 to 4350, 4380 to 4760, 5040 to 5920, 6570 to 8270, 9020 to 9700, 9880 to 10160 and 10580 to 11080 a BP, respectively. The climatic events indicated by these dune sands are consistent with those records in the Huguangyan volcanic lake, Zoige peat bog, Hulu cave and Dunde ice core, particularly with the climatic fluctuations of the North Atlantic since 11 000 a BP.Among them, patterns from BO to B8 correspond to the peak values of 0MD, 2D, 4D,6D+8D+10D, 12D, 14D, 16D, 18D and 20D respectively. It might be caused by the North Atlantic ice age induced by the heat circulation, which strengthened the polar high pressure and Siberian-Mongolian high pressure and further led to the dominance of the winter monsoon over China's desert area.

  7. Late Pleistocene and Holocene-Age Columbia River Sediments and Bedforms: Hanford Reach Area, Washington - Part 2

    Energy Technology Data Exchange (ETDEWEB)

    K.R. Fecht, T.E. Marceau

    2006-03-28

    This report presents the results of a geologic study conducted on the lower slopes of the Columbia River Valley in south-central Washington. The study was designed to investigate glaciofluvial and fluvial sediments and bedforms that are present in the river valley and formed subsequent to Pleistocene large-scale cataclysmic flooding of the region.

  8. Glacier Geosite of Tale-Tange Valley

    Directory of Open Access Journals (Sweden)

    Kamran Rezaeizadeh Mahabadi

    2014-08-01

    Full Text Available Geological sites or geosites are the key evidence or specific periods of geological history which are very important in public education of earth sciences and environmental implications. They are also non-renewable parts of the earth as a tool for sustainable development. By its diverse geology, climate, geological features and unique nature, Iran can use geological phenomenon (geotope across the country, such as caves, canyons, valleys, fossil sites, geological formations, mud volcanoes, types of minerals, mountain glaciers, and Kaluts As a geological heritage in the form of multiple potential geosites following the provision of tourism infrastructure, as a useful tool for geotourism development and establishment of geoparks. Tale-Tange valley is located in northern Jajrud Basin in the southern highlands of central Alborz. Several geomorphological phenomena such Cirque glaciers, moraines, waterfalls, River terraces, wandering rocks in the area can be a geotourist factor to attract tourists to this region. Hence, the area can be considered as a paleoclimatic site or geosite.

  9. Soil transfers from valley oak (Quercus lobata Nee) stands increase ectomycorrhizal diversity and alter root and shoot growth on valley oak seedlings.

    Science.gov (United States)

    Berman, J T; Bledsoe, C S

    1998-02-01

    Soils from valley oak (Quercus lobata Nee) riparian areas of the Cosumnes River Nature Conservancy Preserve near Sacramento, California were added to growth medium of valley oak seedlings grown in a greenhouse or in agricultural fields at Cosumnes which probably once supported valley oak trees and are now replanted with native riparian vegetation or allowed to revegetate naturally. Agricultural field soil from the Cosumnes River Preserve was presumed to be low or lacking in ectomycorrhizal inoculum. The study was designed to (1) determine whether valley oak stand soil transfer could cause mycorrhizal infection on valley oak seedlings in an agricultural field and in a greenhouse, (2) describe ectomycorrhizal morphological types formed on valley oak seedlings, and (3) determine whether seedling growth is enhanced more by transfer of natural valley oak stand soil than agricultural field soil. In the field study, transfer of forest soil increased average ectomycorrhizal diversity (2.4 types) more than transfer of agricultural field soil (1.2 types). Valley oak seedlings were responsive to ectomycorrhizal infection in the field study. With increase in mycorrhizal infection there was an increase in shoot growth at the expense of root growth. In the greenhouse study, both percent mycorrhizal infection and mycorrhizal diversity were increased more by transfer of oak forest and woodland soils than agricultural field soil. Eight morphotypes occurred on seedlings in forest and woodland soils but only three morphotypes in agricultural soil. This result strongly suggests that the agricultural field also harbors ectomycorrhizal propagules but forest and woodland soils support a more abundant and diverse ectomycorrhizal flora. PMID:24578047

  10. Assessment of ecological concerns with alternative water sources used for wetland maintenance at Mason Valley Wildlife Management Area, Lyon County, Nevada

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Mason Valley Wildlife Management Area in Lyon County, Nevada, obtains water from the Walker River, groundwater via fish hatchery effluent and power plant cooling...

  11. Comparative analysis on influencing factors of cultivated land use intensity in valley and middle mountain area of upper Dadu River watershed%大渡河上游河谷与半山区耕地利用集约度及影响因素的对比分析

    Institute of Scientific and Technical Information of China (English)

    花晓波; 阎建忠; 王琦; 张叶生

    2013-01-01

    集约度变化是土地利用变化研究的核心问题,而目前对西部地区耕地利用集约度特征及原因解释的研究较少。该文采取参与式农村评估法(participatory rural appraisal,PRA),以大渡河上游典型河谷与半山区为例,共调查农户357户,通过Tobit和OLS估计方法,定量对比分析了河谷与半山区耕地利用集约度及其影响因素。研究表明:河谷区和半山区在耕地利用集约度上存在显著差异。无论是资本集约度还是劳动集约度,河谷区均高于半山区。影响河谷与半山区耕地利用集约度差异的因素有承包耕地面积、人均实际耕地面积、家庭固定资产、离集镇的距离、二三产业收入、农业劳动力、年需换工数量、人情往来支出等。耕地资源禀赋和农业劳动力数量是导致集约度差异的关键因素,农业生产条件或环境和家庭收入水平对其有重要影响。%Changes in land use intensity are core academic issues in land-use change research. At present, empirical studies on features and driving forces on cultivated land use intensity in Western China are scarce. Besides, how to apply quantitative analysis methods to analyze the influencing factors on the cultivated land use intensity in depth also lack in the research. This paper analyzes differences of cultivated land use intensity based on the field surveys of 357 households in five villages from valley to the middle mountain area of Jinchuan County in the upper Dadu River watershed, by adopting the methods of participatory rural appraisal (PRA). This paper also qualitatively and quantitatively analyzes the factors influencing on the differences using Tobit model and Ordinary Least Squares (OLS) estimation method. The results show that:1) There are statistically significant differences in cultivated land use intensity between the valley and the middle mountain area. Both capital intensity and labor intensity in valley

  12. The impact of 90 years of drainage works on some chemical properties of raised peat bog organic soils - case study from valley of the Upper San river in Polish Bieszczady Mts. (Eastern Carpathians).

    Science.gov (United States)

    Stolarczyk, Mateusz

    2016-04-01

    Wetland ecosystems, including raised peat bogs are characterized by a specific water conditions and unique vegetation, which makes peatland highly important habitats due to protection of biodiversity. Transformation of peat bog areas is particularly related to changes in the environment e.g. according to reclamation works. Drainage of peatlands is directly associated to the decrease of groundwater levels and lead to a number of changes in the chemical and physical properties of peat material, included contents of exchangeable cations in the surface layers of peat soils in the decession phase of peat development and release above compounds from the soil to ground or surface waters. The aim of the research was to determine the impact of extended drainage works on chemical composition of sorption complex of raised peat bog organic soils and identification the potential environmental effects of alkaline cations leaching to the surface waters. Research was carried out on the peat bogs located in the Upper San valley in Polish Bieszczady Mts. (Eastern Carpathians). Soil samples used in this study were collected from 3 soil profiles in 10 or 20 cm intervals to the approximately 130 cm depth. Laboratory analyses included determination of basic properties of organic material such as the degree of peat decomposition, ash content, soil pH and carbon, hydrogen, nitrogen concentrations. Additionally the amount of alkaline cations, exchangeable and extractable acidity was determined. Furthermore, the degree of saturation of the sorption complex with alkaline cations (V) and cation exchange capacity (CEC) are calculated. In order to evaluate the impact of the examined peat bog to the environment, also water samples were collected and ions composition was measured. The obtained results show that studied organic soils are oligotrophic and strongly acidic. In the case of organic material related to decession phase of peat development, as a result of the lengthy drainage works

  13. Creating a catchment perspective for river restoration

    Directory of Open Access Journals (Sweden)

    L. Benda

    2011-03-01

    Full Text Available 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 tributary-confluence dynamics can be obscured, and information to develop appropriate and cost effective river restoration strategies can be unavailable. This is the case in the Pas River catchment in northern Spain (650 km2, in which land use and development have obscured the natural fluvial landscape in many parts of the basin. To address this issue we coupled general principles of hydro-geomorphic processes with computer tools to characterize the fluvial landscape. Using a 5-m digital elevation model, valley-floor surfaces were mapped according to elevation above the channel and proximity to key geomorphic processes. The predicted fluvial landscape is patchily distributed according to topography, valley morphology, river network structure, and fan and terrace landforms. The vast majority of the fluvial landscape in the main segments of the Pas River catchment is presently masked by human infrastructure, with only 15% not impacted by river control structures and development. The reconstructed fluvial landscape provides a catchment scale context to support restoration planning, in which areas of potential ecological productivity and diversity could be targeted for in-channel, floodplain and riparian restoration projects.

  14. The Cheonggyechon River Restoration of Seoul

    OpenAIRE

    PARK, Chanpil

    2013-01-01

    Korea is a large peninsula where 70 percent of the land is mountainous. Traditionally, cities were built on the riversand coastline. These harbor and river valley cities that still stand today have transformed themselves over thegenerations. The river city of Seoul is one such city, with over 600 years of history it has seen some sudden changein recent times. The Cheonggyecheon project attracted public support for several reasons. There was hope that Seoulwould see environmental improvement a...

  15. Geotourism and water quality of river Hornad (E. Slovakia)

    International Nuclear Information System (INIS)

    The paper deals with some issues concerning geotourism and the environmental problems of the Horna river valley (E. Slovakia). The data given below were obtained within the 'RECENT', 'Caring after my river Hornad' projects as well as from the Watershed management company (PBaH) databank. The paper gives some basic data on the river valley, and of the main contaminating agents. Then their significance from the point of view of environmental quality of the studied region and its impact on geotourism is analysed. The impact of water quality on trekking, water sports and fishing are considered, together with the aesthetic problems posed by waste dumping. (authors)

  16. Irrigation channels of the Upper Rhone valley (Switzerland). Geomorphological analysis of a cultural heritage

    Science.gov (United States)

    Reynard, Emmanuel

    2016-04-01

    The Upper Rhone valley (Canton of Valais, Switzerland) is characterised by dry climatic conditions that explain the presence of an important network (about 800 km) of irrigation channels - called Bisses in the French-speaking part of the canton or Suonen in the German-speaking area - dating back to the Middle Ages. This network constitutes a cultural heritage and during the last 30 years these agricultural infrastructures have sparked a renewed interest for tourist and cultural reasons. Indeed, the paths along the channels are used as tourist trails and several abandoned channels have been renovated for tourist use. Based on an inventory of the Bisses/Suonen of Valais, the proposed communication has three aims: (1) to analyse the geomorphological context (morphometric analysis, structural geomorphology, main processes) of various types of channels and to show the impact of the geomorphological context on the building techniques; (2) to identify particularly active processes along the channels; (3) to classify the Bisses/Suonen according to their geomorphological value and to their geomorphological sensitivity, and to propose managing measures. Structural and climatic conditions influence the geomorphological context of the channels. In a structural point of view, irrigation channels are developed in three main contexts: (1) in the Aar Massif crystalline basement; (2) in the limestone and marl cover nappes of the Helvetic Alps; (3) in the metamorphic cover nappes of the Penninic domain. The Rhone River valley is boarded by two high mountain ranges: the Penninic Alps in the South and the Bernese Alps in the North. Because of rain shadow effects, the climate is relatively dry and, between Brig and Martigny, annual rainfall is not more than 600 mm at 500 m ASL and 800 mm at 1600 m ASL. Nevertheless, due to important vertical precipitation gradients annual rainfall totals are high at high altitudes. On the southern facing tributary valleys, the dry climatic conditions

  17. 27 CFR 9.58 - Carmel Valley.

    Science.gov (United States)

    2010-04-01

    ... 27 Alcohol, Tobacco Products and Firearms 1 2010-04-01 2010-04-01 false Carmel Valley. 9.58... Carmel Valley. (a) Name. The name of the viticultural area described in this section is “Carmel Valley.” (b) Approved maps. The approved maps for determining the boundary of the Carmel Valley...

  18. Alluvium of antiquity: Polycyclic terraces in a confined bedrock valley

    Science.gov (United States)

    Kermode, S. J.; Cohen, T. J.; Reinfelds, I. V.; Nanson, G. C.; Pietsch, T. J.

    2012-02-01

    Confined river valleys are not the localities where long term preservation of alluvium would be expected. The 25 km long low gradient (0.0014 m.m - 1 ) confined valley setting of the Shoalhaven River has archived alluvium of middle Pleistocene age to maintain a relatively uniform channel as an efficient conduit for a wide range of flows in a confined bedrock valley of variable morphology. Single-grain optically stimulated luminescence (OSL) dating has identified polycyclic terraces up to 193 ka in age (marine isotope stage [MIS] 7) with lower terrace remnants dating from 173-140 ka (MIS 6) and 106 ka (MIS 5). Holocene alluvium 2-3.5 ka in age caps these old Pleistocene units and a well-constrained combination of one-dimensional and two-dimensional hydraulic modelling demonstrates that these polycyclic terraces are clearly within reach of the modern hydrological regime. The 106 ka terrace at 17 m above low flow is inundated by floods recurring on average every ~ 20 years, and the 140-193 ka terraces at 20-22 m are overtopped every 50-100 years. These ancient diachronous landforms exhibit complex depositional histories and are on-lapped by longitudinal benches of modern sand and gravel. Their polycyclic nature appears to be a response to flow reduction, using alluvium to adjust the boundary of the otherwise inflexible morphology of a bedrock gorge.

  19. Agronomic and molecular traits of the 'Italia Muscat' clone in Sao Francisco River Valley Caracterização agronômica e molecular do clone Itália Muscat no submédio do Vale do São Francisco

    Directory of Open Access Journals (Sweden)

    Patrícia Coelho de Souza Leão

    2011-03-01

    Full Text Available The objective of this study was to evaluate agronomic and molecular traits of the 'Italia Muscat' clone and compare it with the cv. 'Italia', providing information to support the cultivation of 'Italia Muscat' this cultivar in the São Francisco River Valley. Agronomic characteristics of both clones were evaluated for two seasons in 2004. The characteristics were phenology, bud break (%, bud fertility (%, yield (kg mass of bunches (g, length and width of bunches (cm, mass of berries (g, length and diameter of berries (mm, TSS (ºBrix, ATT (% titratable acidity and TSS/TTA. Molecular analysis of seven SSR markers were carried out. The clone 'Italia Muscat' showed larger berries, mass of bunches and better TSS/TA ratio than 'Italia'. The molecular analysis resulted in the same allelic profile in both clones, highlighting the need to use a larger number of microsatellite markers or other molecular technique to allow their discrimination. Based on their morpho-agronomic characteristics, 'Italia Muscat' seems to be a good table grape cultivar alternative for grape growers of São Francisco River Valley.O objetivo deste trabalho foi avaliar características agronômicas e moleculares do clone 'Itália Muscat' e compará-lo à 'Itália', disponibilizando informações para subsidiar o cultivo da cultivar Itália Muscat no Submédio do Vale do São Francisco. Foram avaliadas durante dois ciclos, no ano de 2004, as características agronômicas nos dois clones, tais como, fenologia, brotação (%, fertilidade de gemas (%, produção (kg, massa de cachos (g, comprimento e largura de cachos (cm, massa de bagas (g, comprimento e diâmetro de bagas (mm, SST (Brix, ATT (% ácido tartárico e relação SST/ATT. Realizou-se a análise molecular com sete marcadores moleculares SSR. O clone 'Itália Muscat' apresentou maior tamanho de bagas, peso de cachos e melhor relação SST/ATT que a 'Itália'. O mesmo perfil alélico foi observado nos dois clones, o que

  20. A didactical geological path in Val Rosandra valley (Trieste - Italy)

    Science.gov (United States)

    Godini, E.

    2012-04-01

    Introduction: the presented field work is aimed to involve a group of 15-17 years old students in building a simplified geomorphological and geological model of Val Rosandra valley, by means of guided observations and data collection. The didactical path may be changed according to age, skills or particular needs of students and meteorological conditions; at best, 4-5 hours are needed for the complete field trip. Some ideas about sedimentary rocks, folding and faulting, and the principle of superposition could be useful as pre-concepts, but "could" also be learnt during the experience. Organization: students will be divided into small groups (3-4 students each), possibly with different roles within the group (topographer, photographer, draftsman, geologist, geomorphologist,…). Needed materials for each group: notebook, paper, pencil, rubber, photo camera, ruler, compass, scale 10.000 topographic map, stratigraphic chart, altimeter, diluted hydrochloric acid. Observation points: 1. Bagnoli spring, marl outcrop 2. Bagnoli village, towards the "heart-shaped quarry" 3. By the river, in the lower part of the valley 4. Moccò lookout 5. Marl outcrop, from Moccò to the old railway 6. From the old railway, above the valley 7. By the river, in the upper part of the valley The field work: at first, students will be guided to observe and take notes of the main morphological characteristics, so that the different "observation points" will be drawn on the map, with the help of compass. An easily recognizable system of faults cuts the valley; a "V" profile is visible in the lower part of the valley (a small amount of sediment is present), while a calcareous gorge is evident in the upper valley, where there are no sediments (observation points 3, 4, 6 and 7). The morphology is asymmetric, due to the different arrangement of strata in the left and right side of the valley: right side shows big "steps" (horizontal arrangement of strata), left side is rich in slopes (tilted

  1. Accelerating optimization by tracing valley

    Science.gov (United States)

    Li, Qing-Xiao; He, Rong-Qiang; Lu, Zhong-Yi

    2016-06-01

    We propose an algorithm to accelerate optimization when an objective function locally resembles a long narrow valley. In such a case, a conventional optimization algorithm usually wanders with too many tiny steps in the valley. The new algorithm approximates the valley bottom locally by a parabola that is obtained by fitting a set of successive points generated recently by a conventional optimization method. Then large steps are taken along the parabola, accompanied by fine adjustment to trace the valley bottom. The effectiveness of the new algorithm has been demonstrated by accelerating the Newton trust-region minimization method and the Levenberg-Marquardt method on the nonlinear fitting problem in exact diagonalization dynamical mean-field theory and on the classic minimization problem of the Rosenbrock's function. Many times speedup has been achieved for both problems, showing the high efficiency of the new algorithm.

  2. The History of Silicon Valley

    Institute of Scientific and Technical Information of China (English)

    Joseph Leu

    2005-01-01

    @@ Just as Manchester was once the center for indus trial progress, the microelectronics industry also has a heartland. Silicon Valley is located in a thirty by ten miles strip between San Francisco and San Jose,California.

  3. Social Networks in Silicon Valley

    Institute of Scientific and Technical Information of China (English)

    Joseph; Leu

    2006-01-01

      Social network is a dominant, distinguishing characteristic of Silicon Valley. Because innovation entails coping with a high degree of uncertainty,such innovation is particularly dependent on networks.……

  4. The Drentsche Aa valley system

    International Nuclear Information System (INIS)

    This thesis is composed of five papers concerned with Late Quaternary geology and geomorphology of the Aa valley system. The correlation and chronostratigraphic position of the layers have been established by radiocarbon dating. (Auth.)

  5. RailroadValleySpringfish_CH

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — These data identify the areas where final critical habitat for the Railroad Valley springfish (Crenichthys nevadae) occur. The irrigation ditch that is on the north...

  6. Análisis estadístico probabilístico de las variables que condicionan la inestabilidad de las laderas en los valles de los ríos Las Cuevas y Mendoza Probabilistic analysis of the variables that impose conditions to the slope instability in the Las Cuevas and Mendoza river valleys

    Directory of Open Access Journals (Sweden)

    Stella Maris Moreiras

    2009-12-01

    Full Text Available Se analizaron las variables que condicionan la inestabilidad de las laderas en los valles de los ríos Las Cuevas y Mendoza mediante la aplicación de un modelo probabilístico. Para ello, se superpusieron en el entorno de un SIG el mapa inventario de los procesos de remoción en masa y diferentes mapas temáticos de las principales variables condicionantes de la inestabilidad. De esta manera se calculó el valor de favorabilidad y el factor de incertidumbre de cada clase de las variables. Las variables que mejor predicen el comportamiento de las laderas a escala regional son la litología, la pendiente y la altura. Un mayor número de variables no incrementa significativamente la calidad predictiva del modelo aplicado. Más aún, la incorporación de ciertas variables disminuye su calidad. La identificación de las variables con mayor capacidad predictiva de la inestabilidad per-mite un fácil reconocimiento de los sectores más vulnerables a colapsar en este sector de los Andes Centrales.Using a probabilistic model, parameters conditioning the slope instability were analysed along the valleys of Las Cuevas and Mendoza rivers. For that, the landslide inventory map and thematic maps of several parameters were crossed in a GIS allowing to calculate the favourability value and the certainly factor for classes of each variable considered in the model. Better variables predicting slope instability are the lithology, the slope range, and the elevation. Incorporation of more variables does not increase significantly prediction of the applied model. Moreover, certain variables reduce the quality of the model. The identification of those variables with greater predictive capacity lets to approach the behaviour of the slope in this portion of Central Andes.

  7. VEGETATION INVENTORY OF BALABANDERE VALLEY

    OpenAIRE

    Erol, Ulvi Erhan

    2009-01-01

    Balabandere Valley where Belgrad forest and Bosphorus meet in the easterly orientation of the forest has a very important ecological wealth within the greater Istanbul manucipality. The area, in which this study was conducted, has a potantial to become an outdoor recreation laboratory in and around Istanbul city. Balabandere valley and its vicinity can as well be described as a conservation zone with its cultural and ecological landscaoe history. It harbors a very crucial watershed for the ci...

  8. River engineering

    NARCIS (Netherlands)

    De Vries, M.

    1993-01-01

    One dimension models - basic eauations, analytical models, numberical models. One dimensional models -suspended load, roughness and resistance of river beds. Solving river problems - tools, flood mitigation, bank protection.

  9. The palaeochannel record in the Trent Valley UK: contributions towards cultural heritage management

    Directory of Open Access Journals (Sweden)

    Steve Baker

    2007-04-01

    Full Text Available The Trent Valley is one of Britain's major river systems, and the dynamic history of the river has produced a rich and varied palaeochannel record. This paper reports on a catchment-scale survey of surface-visible palaeochannels within the Holocene floodplain of the Trent, using aerial photographs as a primary data source. This is an important contribution towards comprehensive geomorphological mapping of the Trent floodplain. In addition, the GIS database produced by the survey has enabled a significant part of the palaeoenvironmental resource in the valley to be located within the archaeological cultural resource management framework for the first time. The catchment scale of the survey has allowed analysis of changing geomorphology and land-use along the course of the valley, and the implications of these factors for the preservation and visibility of palaeochannels in different zones. This article has been published with financial assistance from the English Heritage Aggregates Levy Sustainability Fund (ALSF.

  10. Francisella philomiragia, bacteria asociada con altas mortalidades en salmones del Atlántico (Salmo salar) cultivados en balsas-jaulas en el lago Llanquihue Francisella philomiragia, a bacteria associated with high mortalities in Atlantic salmon (Salmo salar) cage-farmed in Llanquihue lake

    OpenAIRE

    H Bohle; Tapia, E.; A Martínez; M Rozas; Figueroa, A.; Bustos, P.

    2009-01-01

    Francisella philomiragia fue aislada de salmón del Atlántico cultivado en balsas-jaulas en el lago Llanquihue con brotes de una enfermedad granulomatosa con altas tasas de morbilidad y mortalidad acumuladas entre 5% a 20%. Los aislados bacterianos tienen 100% similitud con F. philomiragia ssp noatunensis o F. piscicida aislado de bacalao en Noruega, 99% de similitud con Francisella sp. detectado en tilapia en Asia y Centroamérica y 99% de similitud con la especie tipo F. philomiragia por anál...

  11. Site records of softshell turtles (Chelonia: Trionychidae from Barak Valley, Assam, northeastern India

    Directory of Open Access Journals (Sweden)

    K.C. Das

    2011-04-01

    Full Text Available We report for the first time the occurrence of four species of Trionychid turtles Nilssonia gangetica, N. hurum, Chitra indica and Lissemys punctata andersonii from 57 sites in the Barak Valley region of Assam, northeastern India. Sites of occurrence include rivers, small streams, floodplain lakes and ox-bows.

  12. 77 FR 64544 - Central Valley Project Improvement Act, Water Management Plans

    Science.gov (United States)

    2012-10-22

    ... Dorado Irrigation District Lower Tule River Irrigation District City of Roseville East Bay Municipal... Irrigation District Porterville Irrigation District To meet the requirements of the Central Valley Project... available cost-effective technology and best management practices.'' These criteria state that all...

  13. Hydrological connectivity of alluvial Andean valleys: a groundwater/surface-water interaction case study in Ecuador

    Science.gov (United States)

    Guzmán, Pablo; Anibas, Christian; Batelaan, Okke; Huysmans, Marijke; Wyseure, Guido

    2016-06-01

    The Andean region is characterized by important intramontane alluvial and glacial valleys; a typical example is the Tarqui alluvial plain, Ecuador. Such valley plains are densely populated and/or very attractive for urban and infrastructural development. Their aquifers offer opportunities for the required water resources. Groundwater/surface-water (GW-SW) interaction generally entails recharge to or discharge from the aquifer, dependent on the hydraulic connection between surface water and groundwater. Since GW-SW interaction in Andean catchments has hardly been addressed, the objectives of this study are to investigate GW-SW interaction in the Tarqui alluvial plain and to understand the role of the morphology of the alluvial valley in the hydrological response and in the hydrological connection between hillslopes and the aquifers in the valley floor. This study is based on extensive field measurements, groundwater-flow modelling and the application of temperature as a groundwater tracer. Results show that the morphological conditions of a valley influence GW-SW interaction. Gaining and losing river sections are observed in narrow and wide alluvial valley sections, respectively. Modelling shows a strong hydrological connectivity between the hillslopes and the alluvial valley; up to 92 % of recharge of the alluvial deposits originates from lateral flow from the hillslopes. The alluvial plain forms a buffer or transition zone for the river as it sustains a gradual flow from the hills to the river. Future land-use planning and development should include concepts discussed in this study, such as hydrological connectivity, in order to better evaluate impact assessments on water resources and aquatic ecosystems.

  14. Age, distribution, and formation of late cenozoic paleovalleys of the lower Colorado River and their relation to river aggradation and degradation

    Science.gov (United States)

    Howard, K.A.; Lundstrom, S.C.; Malmon, D.V.; Hook, S.J.

    2008-01-01

    Distinctive far-traveled fluvial sediment of the lower Colorado River fills 20 paleo-valleys now stranded by the river downstream of Grand Canyon as it crosses the Basin and Range Province. These sediments resulted from two or more aggradational epi sodes in Pliocene and Pleistocene times following initial incision during the early Pliocene. A review of the stratigraphic evidence of major swings in river elevation over the last 5 m.y. from alternating degradation and aggradation episodes establishes a framework for understanding the incision and filling of the paleovalleys. The paleo-valleys are found mostly along narrow bedrock canyon reaches of the river, where divides of bedrock or old deposits separate them from the modern river. The paleo-valleys are interpreted to have stemmed from periods of aggradation that filled and broadened the river valley, burying low uplands in the canyon reaches into which later channel positions were entrenched during subsequent degradation episodes. The aggradation-degradation cycles resulted in the stranding of incised river valleys that range in elevation from near the modern river to 350 m above it. ?? 2008 The Geological Society of America.

  15. Alligator Rivers Region

    International Nuclear Information System (INIS)

    An introduction to the Alligator Rivers Region is presented. It contains general information regarding the physiography, climate, hydrology and mining of the region. The Alligator Rivers Region is within an ancient basin, the Pine Creek Geosyncline, which has an area of approximately 66000 km2. The Geosyncline has a history of mineral exploitation dating back to 1865, during which time 16 metals have been extracted (silver, arsenic, gold, bismuth, cadmium, cobalt, copper, iron, manganese, molybdenum, lead, tin, tantalum, uranium, tungsten, zinc). Uranium exploration in the Pine Creek Geosyncline was stimulated by the discovery in 1949 of secondary uranium mineralisation near Rum June, 70 km south-east of Darwin. This was followed by a decade of intense exploration activity resulting in the discoveries of economic uranium ore bodies at Rum Jungle and in the upper reaches of the South Alligator River Valley. All the known major uranium deposits of the East Alligator River uranium field have been discovered since 1969. The present known resources of the Geosyncline are approximately 360 000 tonnes of contained U3O8. 2 refs., 2 figs., 1 tab

  16. Mitochondrial DNA Variability of Domestic River Buffalo (Bubalus bubalis) Populations: Genetic Evidence for Domestication of River Buffalo in Indian Subcontinent

    OpenAIRE

    Nagarajan, Muniyandi; Nimisha, Koodali; Kumar, Satish

    2015-01-01

    River buffalo, Bubalus bubalis is a large bovine species frequently used livestock in southern Asia. It is believed that the river buffalo was domesticated from Bubalus arnee, the wild buffalo of mainland Asia, a few thousand years ago, probably during the period of Indus Valley civilization. However, the domestication history of the river buffalo has been the subject of debate for many decades mainly due to the lack of clear archeological evidence and the divisive conclusions of the genetic ...

  17. 四川宜宾金沙江河谷区地热资源成藏条件分析%Analysis of Geothermal Resources Formation Conditions in the Jinsha River Valley of the Yibin Area,Sichuan Province

    Institute of Scientific and Technical Information of China (English)

    闫秋实; 高志友; 尹观

    2012-01-01

    Taking the Yibin section of the Jinsha River as an example,this paper studied its geothermal resources and potential from geological background,hydrogeology,tectonics and heat-storage conditions.It is indicated that the paleo-geographic environment is favorable for migration and cycling of underground thermal water as well as exchanging heat with the deep heat-storage reservoir.This helps to form relatively closed thermal structures,making the deep thermal water be in pressurized situation.The cap rocks can increase thermal insulation and control thermal diffusion,and prevent the surface water from migrating downward.And this region is located at the junction of several faults which provide conduits for the thermal water convection at depth.The water precipitated downwards from higher places in this area,passing over a long distance and to a big depth.Extensive thermal exchange with hot wall-rocks occurred when the water was resorted at depth for a long time.The geothermal resources in this area have a big economic potential.%本文从地热地质背景、水文地质条件、构造条件、热储条件等几方面对金沙江宜宾段河谷区的地热成藏条件及开发潜力进行了较为深入的论述。研究表明:该区的古地理环境有利于地表水向深部补给、运移、往更纵深循环以及形成与深部热储充分进行热交换,有利于形成保持相对封闭的热水构造,使深部地热水处于承压状态;热储层盖层对地下热水具有良好的保温防热扩散作用,且阻隔浅层地表水向下运移;东西向断裂与南北向断裂或与NE、NW向断裂的多方向构造的交切复合部位为深部地热水向上运移排泄的极为有利构造部位;区内地下热水其热源主要是地热增温,大气降水经由深循环加热,与深部热储层岩石进行充分的热交换,温泉水以补给地高、运移途径长、循环深、滞留时间长为特征。

  18. El saber de la partera tradicional del valle del río Cimitarra: cuidando la vida Traditional midwifery knowledge in the Cimitarra River Valley. Taking Care of life O saber da parteira tradicional do vale do Rio Cimitarra: cuidando a vida

    Directory of Open Access Journals (Sweden)

    RUIZ DE CÁRDENAS CARMEN HELENA

    2009-12-01

    Full Text Available Para la recolección y análisis de la información se utilizaron la Etnografía focalizada y la técnica de Spradley y la teoría de la diversidad y la universalidad de los cuidados culturales de Leininger se tomó como referente teórico. Su objetivo fue describir los cuidados que brindaban las parteras tradicionales a partir de creencias y prácticas en las mujeres durante el parto en la zona rural de la región del valle del río Cimitarra, Magdalena Medio. El estudio se desarrolló en el valle del río Cimitarra y la ciudad de Barrancabermeja. Participaron siete parteras tradicionales y se recolectaron los datos mediante entrevista etnográfica y observación participante entre los años 2007 y 2008. El tema central es “El saber de la partera tradicional del valle del río Cimitarra: cuidando la vida” y cinco dominios culturales: alistarse para la atención del mismo, identificar el momento del parto, ayudar a la mujer a parir, proteger al bebé después del nacimiento y proteger a la mujer después del nacimiento. Cuidar la vida se relaciona con la necesidad de “sobrevivir” a pesar de la guerra, la violencia y el abandono estatal. Las acciones de cuidado se fundan en creencias culturales, la cotidianidad del trabajo del campo, la tradición oral y la invocación divina en medio del complejo contexto ambiental, la incertidumbre del conocimiento y el miedo a problemas legales.Focalized ethnography and Spradley’s technique were used to collect and analyze information. Diversity and universality stated in Leninger’s study of culture were regarded as a theoretical reference. The objective was to describe care given by traditional midwives, using their traditional beliefs and practices, on women during delivery in the rural area of the Cimitarra river valley, Mid Magdalena river basin. It took place in the Cimitarra River and in the town Barrancabermeja, where seven traditional midwives participated. Data was collected using

  19. El saber de la partera tradicional del valle del río Cimitarra: cuidando la vida O saber da parteira tradicional do vale do Rio Cimitarra: cuidando a vida Traditional midwifery knowledge in the Cimitarra River Valley: Taking Care of life

    Directory of Open Access Journals (Sweden)

    CELMIRA LAZA VÁSQUEZ

    sete parteiras tradicionais. A compilação dos dados foi realizada através de entrevistas etnográficas e de observação participante entre os anos 2007 e 2008. Para analisar a informação, utilizou-se a técnica de Spradley. Emerge como tema central " O saber da parteira tradicional do vale do Rio Cimitarra: cuidando a vida" e cinco domínios culturais: preparação para a atenção do parto, identificação do momento do parto, ajudar à mulher no parto, cuidado do bebê depois do nascimento e cuidado da mulher depois do nascimento. O cuidado da vida está relacionado com a necessidade de " sobreviver" apesar da guerra, a violência e o abandono estatal. As ações de cuidado se suportam nas crenças culturais, a cotidianidade do trabalho de campo, a tradição oral e a invocação divina em médio do complexo contexto ambiental, a incerteza do conhecimento e o medo a problemas legais.Focalized ethnography and Spradley's technique were used to collect and analyze information. Diversity and universality stated in Leninger's study of culture were regarded as a theoretical reference. The objective was to describe care given by traditional midwives, using their traditional beliefs and practices, on women during delivery in the rural area of the Cimitarra river valley, Mid Magdalena river basin. It took place in the Cimitarra River and in the town Barrancabermeja, where seven traditional midwives participated. Data was collected using ethnographic interview and participative observation during 2007 and 2008. Spradley's technique was used for the analysis of the information. " Traditional midwifery knowledge in the Cimitarra River Valley. Taking care of life" emerges as a core subject, plus it contains five separate cultural domains: preparation for birth, identify the moment of birth, assist the woman during delivery, the health of the mother and child after delivery. General health care is connected to the need to " survive" despite war, violence and state

  20. Geochemical evidence for seasonal controls on the transportation of Holocene loess, Matanuska Valley, southern Alaska, USA

    Science.gov (United States)

    Muhs, Daniel R.; Budahn, James R.; Skipp, Gary L.; McGeehin, John P.

    2016-06-01

    Loess is a widespread Quaternary deposit in Alaska and loess accretion occurs today in some regions, such as the Matanuska Valley. The source of loess in the Matanuska Valley has been debated for more than seven decades, with the Knik River and the Matanuska River, both to the east, being the leading candidates and the Susitna River, to the west, as a less favorable source. We report here new stratigraphic, mineralogic, and geochemical data that test the competing hypotheses of these river sources. Loess thickness data are consistent with previous studies that show that a source or sources lay to the east, which rules out the Susitna River as a source. Knik and Matanuska River silts can be distinguished using Sc-Th-La, LaN/YbN vs. Eu/Eu∗, Cr/Sc, and As/Sb. Matanuska Valley loess falls clearly within the range of values for these ratios found in Matanuska River silt. Dust storms from the Matanuska River are most common in autumn, when river discharge is at a minimum and silt-rich point bars are exposed, wind speed from the north is beginning to increase after a low-velocity period in summer, snow depth is still minimal, and soil temperatures are still above freezing. Thus, seasonal changes in climate and hydrology emerge as critical factors in the timing of aeolian silt transport in southern Alaska. These findings could be applicable to understanding seasonal controls on Pleistocene loess accretion in Europe, New Zealand, South America, and elsewhere in North America.

  1. Seismic response of the geologic structure underlying the Roman Colosseum and a 2-D resonance of a sediment valley

    Directory of Open Access Journals (Sweden)

    P. Labak

    1995-06-01

    Full Text Available The seismic response of the geologic structure beneath the Colosseum is investigated using a two-dimensional modeling for a vertically incident plane SH wave. Computations indicate that the southern part of the Colosseum may be exposed to a seismic ground motion with significantly larger amplitudes, differential motion and longer duration than the northern part. because the southern part of the Colosseum is underlain by a sedimentfilled valley created by sedimentary filling of the former tributary of the River Tiber. A 2-D resonance may develop in the valley. Unlike the previous theoretical studies on 2-D resonance in sediment-filled valleys, an effect of heterogeneous valley surroundings on the resonance is partly investigated. A very small sensitivity of the maximum spectral amplifications connected with the fundamental and first higher modes to the presence of a horizontal surface layer (with an intermediate velocity in the valley surroundings is observed in the studied models.

  2. Glacial meltwater impounding: Evidence from the late Quaternary glaciogenic sediments in the Sangla valley, district Kinnaur, Himachal Pradesh, India

    Indian Academy of Sciences (India)

    R K Ganjoo; M N Koul

    2005-08-01

    Sangla valley is situated at an altitude of ∼3500m above mean sea level and lies in the Kinnaur district of Himachal Pradesh. It is fed by river Baspa, a tributary of river Sutlej, that entrenches through the Quaternary glaciogenic deposits before emerging out of the valley and joining the river Sutlej at Karcham. The unstratified to stratified glaciogenic deposits consist of large boulders to fine silt and are classified into four major depositional facies on the basis of sedimentary texture and depositional environment. The facies — basal conglomerates, debris flow, water/sheet flow and laminites — represents the change in the environment of deposition from glaciofluvial to lacustrine and also the extent of the glacier to the valley floor during late Quaternary.

  3. 2012 Puget Sound LiDAR Consortium (PSLC) Topographic LiDAR: Upper Naches River, Washington

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Watershed Sciences, Inc. (WSI) collected Light Detection and Ranging (LiDAR) data of the Upper Naches River Valley and Nile Slide area of interest on September...

  4. Examining the evolution of an ancient irrigation system: the Middle Gila River Canals

    Science.gov (United States)

    Zhu, Tianduowa; Ertsen, Maurits

    2014-05-01

    Studying ancient irrigation systems reinforces to understand the co-evolution process between the society and water systems. In the prehistoric Southwest of America, the irrigation has been a crucial feature of human adaptation to the dry environment. The influences of social arrangements on irrigation managements, and implications of the irrigation organization in social developments are main issues that researchers have been exploring for a long time. The analysis of ceramics pattern and distribution has assisted to the reconstruction of prehistoric social networks. The existing study shows that, a few pottery fragments specially produced by the materials of the middle Gila River valley, were found in the Salt River valley; however, very few specialized ceramics of the Salt River valley occurred in the middle Gila River valley. It might indicate that there were trades or exchanges of potteries or raw materials from the middle Gila River valley to the Salt River valley. The most popular hypothesis of trading for the potteries is crop production. Based on this hypothesis, the ceramics trade was highly tied to the irrigation system change. Therefore, examining the changing relationship among the ceramics distribution along the middle Gila River, canals flow capacity, and available streamflows, can provide an insight into the evolutionary path among the social economy, irrigation and water environment. In this study, we reconstruct the flow capacity of canals along the middle Gila River valley. In combination with available streamflow from the middle Gila River, we can simulate how much water could be delivered to the main canals and lateral canals. Based on the variation and chronology of potteries distribution, we may identify that, the drama of the middle Gila River receiving insufficient flows for crop irrigation caused the development of ceramics exchange; or the rising of potteries exchange triggers the decline of irrigation in the study area.

  5. A method for distinguishing different water sources during flood events in river floodplains, northern Poland

    NARCIS (Netherlands)

    Chormanski, J.; Karalevich, J.; Kardel, I.; Okruszko, T.; Wassen, M.J.

    2010-01-01

    The Biebrza wetlands are located in an ice-marginal valley in northeastern Poland and cover some 195 000 hectares. The Biebrza river is not regulated, the valley is not reclaimed and still has marsh, fen and grassland vegetation whereas large scale human interventions in hydrology are absent. The mo

  6. The Wichita Valley irrigation project: Joseph Kemp, boosterism, and conservation in northwest Texas, 1886-1939.

    Science.gov (United States)

    Anderson, Jahue

    2011-01-01

    This is the story of failure: in this case, an irrigation project that never met its boosters' expectations. Between 1880 and 1930, Wichita Falls entrepreneur Joseph Kemp dreamed of an agrarian Eden on the Texas rolling plains. Kemp promoted reclamation and conservation and envisioned the Big Wichita River Valley as the "Irrigated Valley." But the process of bringing dams and irrigation ditches to the Big Wichita River ignored knowledge of the river and local environment, which ultimately was key to making these complex systems work. The boosters faced serious ecological limitations and political obstacles in their efforts to conquer water, accomplishing only parts of the grandiose vision. Ultimately, salty waters and poor drainage doomed the project. While the livestock industry survived and the oil business thrived in the subsequent decades, the dream of idyllic irrigated farmsteads slowly disappeared. PMID:22180941

  7. A method for distinguishing different water sources during flood events in river floodplains, northern Poland

    OpenAIRE

    Chormanski, J; Karalevich, J.; Kardel, I.; T. Okruszko; M. J. Wassen

    2010-01-01

    The Biebrza wetlands are located in an ice-marginal valley in northeastern Poland and cover some 195 000 hectares. The Biebrza river is not regulated, the valley is not reclaimed and still has marsh, fen and grassland vegetation whereas large scale human interventions in hydrology are absent. The most characteristic feature of the Biebrza river is flooding, which occurs almost every year during the spring thaw. During these floods the inundated wetlands covers many km2. This water may in prin...

  8. Modelling photochemistry in alpine valleys

    Directory of Open Access Journals (Sweden)

    G. Brulfert

    2005-01-01

    Full Text Available Road traffic is a serious problem in the Chamonix Valley, France: traffic, noise and above all air pollution worry the inhabitants. The big fire in the Mont-Blanc tunnel made it possible, in the framework of the POVA project (POllution in Alpine Valleys, to undertake measurement campaigns with and without heavy-vehicle traffic through the Chamonix and Maurienne valleys, towards Italy (before and after the tunnel re-opening. Modelling is one of the aspects of POVA and should make it possible to explain the processes leading to episodes of atmospheric pollution, both in summer and in winter. Atmospheric prediction model ARPS 4.5.2 (Advanced Regional Prediction System, developed at the CAPS (Center for Analysis and Prediction of Storms of the University of Oklahoma, enables to resolve the dynamics above a complex terrain. This model is coupled to the TAPOM 1.5.2 atmospheric chemistry (Transport and Air POllution Model code developed at the Air and Soil Pollution Laboratory of the Ecole Polytechnique Fédérale de Lausanne. The numerical codes MM5 and CHIMERE are used to compute large scale boundary forcing. This paper focuses on modelling Chamonix valley using 300-m grid cells to calculate the dynamics and the reactive chemistry which makes possible to accurately represent the dynamics in the Chamonix valley (slope and valley winds and to process chemistry at fine scale. The summer 2003 intensive campaign was used to validate the model and to study chemistry. NOy according to O3 reduction demonstrates a VOC controlled regime, different from the NOx controlled regime expected and observed in the nearby city of Grenoble.

  9. Modelling photochemistry in alpine valleys

    Directory of Open Access Journals (Sweden)

    G. Brulfert

    2005-03-01

    Full Text Available Road traffic is a serious problem in the Chamonix Valley, France: traffic, noise and above all air pollution worry the inhabitants. The big fire in the Mont-Blanc tunnel made it possible, in the framework of the POVA project (POllution in Alpine Valleys, to undertake measurement campaigns with and without heavy-vehicle traffic through the valley, towards Italy (before and after the tunnel re-opening. Modelling in POVA should make it possible to explain the processes leading to episodes of atmospheric pollution, both in summer and in winter.

    Atmospheric prediction model ARPS 4.5.2 (Advanced Regional Prediction System, developed at the CAPS (Center for Analysis and Prediction of Storms of the University of Oklahoma, enables to resolve the dynamics above a complex terrain.

    This model is coupled to the TAPOM 1.5.2 atmospheric chemistry (Transport and Air POllution Model code developed at the Air and Soil Pollution Laboratory of the Ecole Polytechnique Fédérale de Lausanne.

    The numerical codes MM5 and CHIMERE are used to compute large scale boundary forcing.

    Using 300-m grid cells to calculate the dynamics and the reactive chemistry makes possible to accurately represent the dynamics in the valley (slope and valley winds and to process chemistry at fine scale.

    Validation of campaign days allows to study chemistry indicators in the valley. NOy according to O3 reduction demonstrates a VOC controlled regime, different from the NOx controlled regime expected and observed in the nearby city of Grenoble.

  10. Surface Water and Ground Water Interactions in an Irrigated Valley in Northern New Mexico

    Science.gov (United States)

    Ochoa, C.; Fernald, A.; Guldan, S.; Tidwell, V.; King, P.; Cevik, Y.; Cusack, C.

    2008-12-01

    Interactions between surface water and ground water can provide many benefits like terrestrial and aquatic species habitat, aquifer recharge, and shallow ground water return flow. In northern New Mexico, the use of traditional irrigation systems has effectively expanded riparian functions to encompass full irrigated valley width. The objective of this study was to characterize the surface water and ground water interactions occurring in an irrigated valley along the Rio Grande in northern New Mexico. We used a combination of field measurements and modeling for determining different components of the water budget. Our results show that on average ditch flow is 0.9 cms, ditch seepage is 10%, irrigated field deep percolation is 30%, and ground water level rise is 0.4 m over the entire valley after the irrigation season started. We calculated that on average, 50% of the water diverted into the main irrigation ditch returns back to the river as surface return flow and about 10% of the total ditch inflow returns as groundwater flow. Results from this study show that a significant amount of water being diverted into the valley returns back to the river after completing its task of supporting important production and ecological functions in this expanded riverine valley.

  11. HACIA EL COMPORTAMIENTO HUMANO MODERNO. NUEVAS APORTACIONES AL PALEOLÍTICO MEDIO FINAL EN EL VALLE DEL RÍO ARLANZA (HORTIGÜELA, BURGOS, ESPAÑA (Understanding modern human behavior. New contributions from the later Middle Paleolithic in the Arlanza river valley

    Directory of Open Access Journals (Sweden)

    Marta Navazo

    2010-12-01

    Full Text Available En el valle medio del Arlanza (Hortigüela, Burgos se conocen dos asentamientos musterienses ya clásicos en la bibliografía: Millán y La Ermita. En este trabajo se incorporan estudios que permiten un mejor y actualizado conocimiento de los mismos en base al análisis de uno de los niveles de Millán, la caracterización geoquímica de los afloramientos de sílex de la zona, y del material arqueológico, para conocer las fuentes de aprovisionamiento; y los sistemas de explotación y configuración de ambas cavidades. El estudio derivado del valle medio del Arlanza, a partir de sus características tecnológicas y cronología (Paleolítico medio final, da pie para abordar un interesante debate abierto sobre el surgimiento del comportamiento humano moderno, reflexionando sobre si las características que han servido para definir dicha conducta son exclusivas del Homo sapiens o si, por el contrario, esos procesos de cambio ya estaban presentes al final del Paleolítico medio. ENGLISH: In the middle valley of the Arlanza river (Hortigüela, Burgos, two classic Mousterian sites, Millán and La Ermita, have been documented. This paper enhances and updates the previously known information about these sites. The study includes the analysis of one of the Millán levels, geochemical characterization of the flint outcrops in the zone and artifacts found in the archaeological record, with a view to ascertaining lithic material sources, and the exploitation systems characterizing both sites. The chronological position of these late Middle Paleolithic settlements facilitates a discussion about whether the characteristics that have served to define modern human behavior are exclusive to Homo sapiens or if, on the contrary, the markers of change were already present at the end of the Middle Paleolithic.

  12. Implications of Historic River Channel Modifications on Contemporary Restoration Opportunities

    Science.gov (United States)

    Hanrahan, T. P.

    2013-12-01

    Identifying contemporary river management and restoration opportunities relies on understanding how river ecosystems respond to historic forcing from natural events and human impacts. Over the past 70 years, the Big Wood River in central Idaho, USA, has experienced significant engineered channel modifications and realignment, as well as natural changes in channel location and riverbank instability. Understanding the effects of these historic conditions on contemporary river characteristics and processes was needed to inform river management and restoration planning. A geomorphic assessment along 16 km of the Big Wood River was completed in order to understand the physical characteristics and processes upstream, within, and downstream of a 3 km long project reach. This evaluation included analysis of the longitudinal profile, planform pattern, cross-section dimensions, cross-section hydraulics, riverbed and riverbank materials, sediment transport conditions, and large roughness elements such as boulders and large wood material. As a result of residential and highway encroachment along the river corridor, river channel modifications (bank revetments, grade-control drop structures, training channels, sediment traps) have been implemented in attempts to limit the vertical and lateral channel adjustments that would negatively affect infrastructure along the river corridor. These river channel modifications have interrupted the geomorphic processes of the Big Wood River, and have initiated the need for ongoing maintenance of in-channel structures and new efforts at river restoration. Future river ecosystem response along this reach of the Big Wood River will be constrained as a result of river channel and floodplain modifications throughout the valley.

  13. A stable isotope reconnaissance of groundwater resources in the Kathmandu Valley, Nepal

    International Nuclear Information System (INIS)

    Groundwater, surface water, spring water, and precipitation obtained during the monsoon season in the Kathmandu Valley of central Nepal were analysed for the stable environmental isotopes oxygen-18 (18O) and deuterium (2H). The distributions of the isotopes in the hydrologic cycle suggest that valley groundwaters have different origins. The Kathmandu Valley is a tectonic basin in the middle hill region of Nepal, 80 km south of the crest of the Himalayan Mountains. The 600 km2 bowl-like valley contains more than 400 m of lacustrine and fluvial sediments. The elevation of the relatively flat valley floor is roughly 1300 m. Steep hills surrounding the valley rise generally to 1600 m, and to a maximum of 2760 m. The small mountain reservoirs that supplied 80% of the drinking water for the city of Kathmandu (population exceeds 200 000) no longer meet demand during the dry season. New production wells show high levels of dissolved iron (> 2 mg/L) and high acidity (pH 18O and δ2H. The isotopically lightest sample was -10.4 and -74, and the heaviest was -6.9 and -55. Light surface waters originating in northern and southern uplands plot near the world meteoric water line. Waters with intermediate values, groundwater in the northern area of the valley and several small rivers, plot along a possible evaporation or mixing line. The heaviest waters, collected from a small river flowing from the east, groundwater in the centre of the valley, and deep groundwater containing natural gas in the southwestern area of the valley, all have signatures similar to those reported from the first range of the Himalayan uplift, roughly 1000 m lower in elevation. A volume weighted composite sample of rain water collected in the city of Kathmandu from August 22 to September 12, 1986 had values of -8.0 and -58. One overnight storm produced more than 10 cm of rain with values of -1.8 and -6. It is assumed that large variations between individual precipitation events are naturally averaged to

  14. Karst Springs in the Upper Soča Valley

    Directory of Open Access Journals (Sweden)

    Jože Janež

    2002-12-01

    Full Text Available Alpine karst springs in the Soča river basin (The karst springs of the alpine rivers Soča, Krajcarca, Lepena, Vrsnica, Koritnica, Možnica, Tolminka, Zadlaščica and Kneža and karst springs Šumnik in Bavščica Valley, Kršovec, Glijun, Boka and Podlaznica arepresented in this article. Due to high discharges and good quality they represent very important reserves of drinking water. Their importance will be shown especially in the future. Because of increasing exploitation of the alpine environment and water in this area, the latter has to be studied thoroughly and protected constantly.

  15. 27 CFR 9.154 - Chiles Valley.

    Science.gov (United States)

    2010-04-01

    ... 27 Alcohol, Tobacco Products and Firearms 1 2010-04-01 2010-04-01 false Chiles Valley. 9.154... Chiles Valley. (a) Name. The name of the viticultural area described in this section is “Chiles Valley.” (b) Approved maps. The appropriate maps for determining the boundary of the Chiles...

  16. Constraining Subsurface Structure and Composition Using Seismic Refraction Surveys of Proglacial Valleys in the Cordillera Blanca, Peru

    Science.gov (United States)

    Glas, R. L.; Lautz, L.; McKenzie, J. M.; Mark, B. G.; Baker, E. A.; Aubry-Wake, C.; Somers, L. D.; Wigmore, O.

    2015-12-01

    As tropical glaciers rapidly recede in response to climate change, the storage and discharge of groundwater will play an increasing role in regulating river baseflow, particularly during the dry season, when stream flow is currently sustained predominantly by glacial melt. Little is understood regarding the hydrogeologic processes controlling base flow characteristics of low-gradient proglacial valleys of the Cordillera Blanca in Northwestern Peru, which has the world's highest density of tropical glaciers. To better understand the processes of groundwater storage and discharge in proglacial meadows, we completed seismic refraction surveys in three representative valleys of the Cordillera Blanca range: the Quilcayhuanca, Yanamarey, and Pachacoto valleys. The locations of survey transects were chosen based on locations of previous sediment core sampling, GPR lines, and quantification of groundwater-surface water interaction derived from dye and temperature tracing experiments. The seismic surveys consisted of 48 vertical component geophones with 2.5 m spacing. Across the three representative valleys a total of 15 surveys were conducted, covering a distance of 1800 m in cross, down, and oblique-valley directions. Preliminary interpretation of the seismic refraction data indicates a maximum imaging depth of 16 m below land surface, and a transition from glacio-lacustrine sediments to buried saturated talus at a depth of 6 m in the Quilcayhuanca valley. The organic-rich glacio-lacustrine sediments in the Yanamarey valley have seismic velocities ranging from 300 to 800 m/s and are >16 m in thickness at mid- valley. Weathered metasedimentary bedrock in the Pachacoto valley was imaged at ~5 m below the valley surface, exhibiting a p-wave velocity of 3400 m/s. The knowledge of hydrogeologic structure derived from seismic refraction surveys will provide crucial boundary conditions for future groundwater models of the valleys of the Cordillera Blanca.

  17. The Aterno valley strong-motion array: seismiccharacterization and determination of subsoil model

    OpenAIRE

    Lanzo, G.; Dipartimento di Ingegneria Strutturale e Geotecnica, Università di Roma “La Sapienza”, Roma, Italia; Tallini, M.; Dipartimento di Ingegneria delle Strutture, delle Acque e del Terreno, Università dell’Aquila,L’Aquila, Italy; Milana, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italia; Di Capua, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italia; Del Monaco, F.; Dipartimento di Ingegneria delle Strutture, delle Acque e del Terreno, Università dell’Aquila,L’Aquila, Italy; Pagliaroli, A.; CNR-IGAG, Rome, Italy; Peppoloni, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italia

    2011-01-01

    The paper focuses on the strong motion array deployed in the upper Aterno River Valley, in the immediate outskirts north-west of the town of L’Aquila, which is part of the Italian Strong Motion Network operated by the Department of Civil Protection. The array is composed of six accelerometric stations located along a cross section of the valley. The importance of this array relies on the fact that a large amount of high-quality records were obtained during the 2009 L’Aquila seismic sequenc...

  18. 印度纳尔玛达地区发现的粗壮智人化石及其与亚洲直立人的连续性%Discovery of a Robust Fossil Homo sapiens in India (Orsang River Valley, Lower Narmada Basin, Gujarat): Possible Continuity with Asian Homo erectus

    Institute of Scientific and Technical Information of China (English)

    LS Chamyal; A Dambricourt Malassé; DM Maurya; Rachna Raj; N Juyal; S Bhandari; RK Pant; C Gaillard; 崔娅铭

    2011-01-01

    1999年,在印度西部的纳尔玛达(Narmada)河的一条支流--奥尔桑(Orsang)河谷发现了一具孤立的智人头骨,这对于了解印度人类进化历史和南亚直立人与最古老的亚洲智人(或AMH,解剖学上现代的人)之间的联系有着重要的意义.化石是在古老的河流沉积物中发现的.对主体沉积和颅内沉积物的红外光释光(IRSL)测年结果显示,其年代为3-5万年.然而,对化石的直接测年(放射性碳加速器质谱测年AMS)结果表明,其年代最小为4981-5579年前.头骨被归类为圆颅型智人.头骨上最引人注意的特征是颅外有亚洲直立人头后部很发达的角圆枕.头骨最宽处在下部(颞骨)如直立人,这样的情况从来不见于智人.这可能是由于乳突的气窦化而形成的.乳突上脊发育,从破损的眉间区(20mm)可以看到很宽的额窦.所有这些粗壮的特征都表明Orsang头骨和晚期亚洲直立人之间具有遗传连续性.%The discovery in 1999 of an isolated skull of Homo sapiens in the Orsang River valley,a tributary of the Narmada River in western India, is significant for understanding human evolution in India and the links between South Asian Homo erectus and the oldest Asian Homo sapiens (or AMH, anatomically modern human). The fossil was found in an old fluvial deposit.Infrared stimulated luminescence (IRSL) dating of the host sediments and of those within the endocranium provided an age ranging from 50 to 30 ka. However, direct dating (AMS radiocarbon) of the bone gave a minimum age of 4981-5579 cai BP. The skull is found to refer to a brachycranial Homo sapiens. and The most interesting features observed are the exocranial, a well developed torus angularis in the posterior part of the Asian Homo erectus, the greatest width in the lower part of the cranium (temporal) as in Homo erectus, which may be due to pneumatization of the mastoid process. The supramastoid crest is developed and very broad frontal sinuses are

  19. The Future of Silicon Valley

    Institute of Scientific and Technical Information of China (English)

    Joseph Leu

    2006-01-01

    @@ By the end of 1984, Silicon Valley was going through the down cycle fol lowing the PC boom. A hundred PC companies wanted just 10 percent of the market, wanting to strike it rich, as rich as the Apple IPO (Initial Public Of fering) -the Google celebrity IPO of its day.

  20. Climate change impact on future water resources availability for a semi-arid area (Ferghana Valley, Central Asia)

    Science.gov (United States)

    Radchenko, Iuliia; Breuer, Lutz; Mannig, Birgit; Frede, Hans-Georg

    2014-05-01

    Considering increasing temperatures and glacier recession during the last decades, it is of high interest to study the climate change impact on water resources availability in semi-arid regions of Central Asia. The Ferghana Valley is surrounded by the Tien-Shan and Pamiro-Alay mountain systems that store big amounts of water in snowpacks and glaciers. In the valley the agricultural activity of local people strongly depends on available water from the Syrdarya River. The river is formed by the confluence of the Naryn and Karadarya Rivers, which are mainly fed by the glacier and snow melt from the Akshiirak and Ferghana ridges of the aforementioned mountain systems. The small upper river basins of the valley also contribute with runoff (~34 %) to the Syrdarya River. These small rivers are mainly fed by precipitation and seasonal snow melt. Thus, because of climate change and glacier decline, it is necessary to investigate the comparative contribution of the small catchments versus two big river basins to the Syrdarya River system, as these small upper catchments could become more important for future water consumption. In this study the conceptual hydrological HBV-light model has been calibrated and validated for the period 1980-1985 over 18 upper catchments that feed the Syrdarya River from the surrounding mountain ridges. Dynamically downscaled climate change scenarios were then applied up to the year 2100 for these basins. The scenarios were generated by means of Global Circulation Model (ECHAM5) and Regional Climate Model (REMO) with a baseline period from 1971 till 2000. We will present modelling results of water resources, the contribution of small rivers to the Syrdarya River and to what extent this contribution is likely to change in the future. Moreover, the results of simulated potential runoff will be used to develop future climate change adaptation strategies regarding socio-economic and environmental sustainable water use.

  1. Salmon River Habitat Enhancement, 1989 Annual Report.

    Energy Technology Data Exchange (ETDEWEB)

    Rowe, Mike

    1989-04-01

    This project was funded by the Bonneville Power Administration (BPA). The annual report contains three individual subproject papers detailing tribal fisheries work completed during the summer and fall of 1989. Subproject 1 contains summaries of evaluation/monitoring efforts associated with the Bear Valley Creek, Idaho enhancement project. Subproject 2 contains an evaluation of the Yankee Fork of the Salmon River habitat enhancement project. This report has been sub-divided into two parts: Part 1; stream evaluation and Part 2; pond series evaluation. Subproject 3 concerns the East Fork of the Salmon River, Idaho. This report summarizes the evaluation of the project to date including the 1989 pre-construction evaluation conducted within the East Fork drainage. Dredge mining has degraded spawning and rearing habitat for chinook salmon and steelhead trout in the Yankee Fork drainage of the Salmon River and in Bear Valley Creek. Mining, agricultural, and grazing practices degraded habitat in the East Fork of the Salmon River. Biological monitoring of the success of habitat enhancement for Bear Valley Creek and Yankee Fork are presented in this report. Physical and biological inventories prior to habitat enhancement in East Fork were also conducted. Four series of off-channel ponds of the Yankee Fork are shown to provide effective rearing habitat for chinook salmon. 45 refs., 49 figs., 24 tabs.

  2. The root of branching river networks.

    Science.gov (United States)

    Perron, J Taylor; Richardson, Paul W; Ferrier, Ken L; Lapôtre, Mathieu

    2012-12-01

    Branching river networks are one of the most widespread and recognizable features of Earth's landscapes and have also been discovered elsewhere in the Solar System. But the mechanisms that create these patterns and control their spatial scales are poorly understood. Theories based on probability or optimality have proven useful, but do not explain how river networks develop over time through erosion and sediment transport. Here we show that branching at the uppermost reaches of river networks is rooted in two coupled instabilities: first, valleys widen at the expense of their smaller neighbours, and second, side slopes of the widening valleys become susceptible to channel incision. Each instability occurs at a critical ratio of the characteristic timescales for soil transport and channel incision. Measurements from two field sites demonstrate that our theory correctly predicts the size of the smallest valleys with tributaries. We also show that the dominant control on the scale of landscape dissection in these sites is the strength of channel incision, which correlates with aridity and rock weakness, rather than the strength of soil transport. These results imply that the fine-scale structure of branching river networks is an organized signature of erosional mechanics, not a consequence of random topology. PMID:23222614

  3. Update of the Accounting Surface Along the Lower Colorado River

    Science.gov (United States)

    Wiele, Stephen M.; Leake, Stanley A.; Owen-Joyce, Sandra J.; McGuire, Emmet H.

    2008-01-01

    The accounting-surface method was developed in the 1990s by the U.S. Geological Survey, in cooperation with the Bureau of Reclamation, to identify wells outside the flood plain of the lower Colorado River that yield water that will be replaced by water from the river. This method was needed to identify which wells require an entitlement for diversion of water from the Colorado River and need to be included in accounting for consumptive use of Colorado River water as outlined in the Consolidated Decree of the United States Supreme Court in Arizona v. California. The method is based on the concept of a river aquifer and an accounting surface within the river aquifer. The study area includes the valley adjacent to the lower Colorado River and parts of some adjacent valleys in Arizona, California, Nevada, and Utah and extends from the east end of Lake Mead south to the southerly international boundary with Mexico. Contours for the original accounting surface were hand drawn based on the shape of the aquifer, water-surface elevations in the Colorado River and drainage ditches, and hydrologic judgment. This report documents an update of the original accounting surface based on updated water-surface elevations in the Colorado River and drainage ditches and the use of simple, physically based ground-water flow models to calculate the accounting surface in four areas adjacent to the free-flowing river.

  4. Topological spin and valley pumping in silicene.

    Science.gov (United States)

    Luo, Wei; Sheng, L; Wang, B G; Xing, D Y

    2016-01-01

    We propose to realize adiabatic topological spin and valley pumping by using silicene, subject to the modulation of an in-plane ac electric field with amplitude Ey and a vertical electric field consisting of an electrostatic component and an ac component with amplitudes and . By tuning and , topological valley pumping or spin-valley pumping can be achieved. The low-noise valley and spin currents generated can be useful in valleytronic and spintronic applications. Our work also demonstrates that bulk topological spin or valley pumping is a general characteristic effect of two-dimensional topological insulators, irrelevant to the edge state physics. PMID:27507592

  5. Soil formation in the Tsauchab Valley, Namibia

    Science.gov (United States)

    Eden, Marie; Bens, Oliver; Ramisch, Arne; Schwindt, Daniel; Völkel, Jörg

    2016-04-01

    The BMBF-funded project GeoArchives (Spaces) investigates soils and sediments in Southern Africa. A focus area lies on the Tsauchab Valley (Namibia), South of the Naukluft mountain range (24°26'40'' S, 16°10'40'' E). On a gently sloping alluvial fan facing East towards the river, the surface is characterized by a desert pavement covering soils used as farmland. The landscape units were mapped and the area at the lower slope of a hill was divided into three units: a rinsing surface and a gravel plain, separated by a channel. On these surfaces soil profiles were excavated. Profile description followed the German system (Bodenkundliche Kartieranleitung KA 5) and disturbed samples were taken at various depths and analysed in the lab. Undisturbed soil cores with a volume of 100 cm³ were taken just below the surface at a depth of ~1-6 cm. Lab analyses included texture and gravel content, colour, pH, electrical conductivity, carbonates, CNS, cation exchange capacity, pedogenic oxides, main and trace elements (XRF), and clay mineral distribution (XRD). Undisturbed samples were used to determine soil water retention curve, air permeability and bulk density. The profiles revealed moderately developed cambic soils rich in clay minerals and with total carbon contents ranging up to 1.8 %, bearing shrubs and after episodic rainfall a dense grass vegetation. Their genesis is discussed and interpreted in the context of the landscape and climate history of this semi-desert environment.

  6. Tennessee Valley Region: a year 2000 profile

    Energy Technology Data Exchange (ETDEWEB)

    None

    1978-06-01

    A study was undertaken to determine the potential radiological implications of nuclear facilities in the combined watersheds of the Tennessee and Cumberland rivers, an area covering portions of 7 states of varied topography. The regional population in 1970 was about 4.6 million and is expected to increase to about 7 million by the year 2000. A 1973 projection estimated the installed electric generating capacity of the region to increase from a 1970 value of 45,000 megawatts to a total of 222,000 megawatts by the year 2000. In that year, about 144,000 megawatts were projected to be nuclear plants. The profile of the Tennessee Valley Region in the year 2000, as drawn from this report, contains the essential data for calculation of the radiological dose from operation of nuclear facilities in that year. Those calculations are reported in the companion document, DOE/ET-0064/2. Specifically, Volume I establishes the parameters describing where the people live, what they eat, the activities in which they engage, and the environmental surroundings that enable an evaluation of the potential radiation dose to the population. Airborne radionuclides from nuclear facilities in this zone may enter the study area and be deposited on the ground, on growing food, and on water surfaces. Consideration was not given to waterborne radionuclides external to the study region. 17 references. (MCW)

  7. Tennessee Valley Region: a year 2000 profile

    International Nuclear Information System (INIS)

    A study was undertaken to determine the potential radiological implications of nuclear facilities in the combined watersheds of the Tennessee and Cumberland rivers, an area covering portions of 7 states of varied topography. The regional population in 1970 was about 4.6 million and is expected to increase to about 7 million by the year 2000. A 1973 projection estimated the installed electric generating capacity of the region to increase from a 1970 value of 45,000 megawatts to a total of 222,000 megawatts by the year 2000. In that year, about 144,000 megawatts were projected to be nuclear plants. The profile of the Tennessee Valley Region in the year 2000, as drawn from this report, contains the essential data for calculation of the radiological dose from operation of nuclear facilities in that year. Those calculations are reported in the companion document, DOE/ET-0064/2. Specifically, Volume I establishes the parameters describing where the people live, what they eat, the activities in which they engage, and the environmental surroundings that enable an evaluation of the potential radiation dose to the population. Airborne radionuclides from nuclear facilities in this zone may enter the study area and be deposited on the ground, on growing food, and on water surfaces. Consideration was not given to waterborne radionuclides external to the study region. 17 references

  8. Transportation Plan Rappahannock River Valley National Wildlife Refuge 2010

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This study is intended to present a plan to identify transportation enhancements that will provide efficient mobility for visitors and staff to and within the...

  9. New River Valley among America's Super Cities of the Future

    OpenAIRE

    Harris, Sally L.

    2005-01-01

    The Blacksburg/Christiansburg/Radford area is among the communities cited in Expansion Management magazine's third annual "Knowledge Worker Quotient," a designation that "identifies metro areas that are exceptionally well placed to attract and nurture high-tech companies and entrepreneurs because of their concentration of extremely well-educated workers."

  10. The Road Inventory of Rappahannock River Valley National Wildlife Refuge

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — To determine the relative needs of the U.S. Fish and Wildlife Service, the Federal Highway Administration FHWA was asked to inventory all public access and...

  11. Hydromorphological and landscape valorization of the Poprad river valley

    Directory of Open Access Journals (Sweden)

    Nawieśniak Maria

    2015-12-01

    Full Text Available Hydromorfologiczna i krajobrazowa waloryzacja doliny rzeki Poprad. Artykuł przedstawia wyniki hydromorfologicznej oraz krajobrazowej oceny doliny rzeki Poprad, na odcinku od Piwnicznej-Zdrój do miejscowości Rytro (województwo małopolskie. Waloryzację hydromorfologiczną przeprowadzono metodą oceny hydromorfologicznej jakości rzeki, a waloryzację krajobrazową wykonano metodą ECOVAST. Na podstawie przeprowadzonych badań stwierdzono, że obszar badawczy charakteryzuje się znaczną zmiennością hydromorfologiczną, w szczególności w odniesieniu do teras zalewowych i ich łączności z korytem głównym cieku. Jednocześnie dolina rzeki Poprad charakteryzuje się krajobrazem o znaczeniu regionalnym, z bardzo dużym potencjałem turystycznym.

  12. Tipping Points in Texas Rivers

    Science.gov (United States)

    Phillips, Jonathan

    2016-04-01

    Anticipating geomorphic tipping points requires that we learn from the past. Major geomorphic changes in coastal plain rivers of Texas resulting in river metamorphosis or regime shifts were identified, and the major driving factors determined. Nine fluvial tipping points were identified from contemporary observations, historical records, and Quaternary reconstructions. Two of the tipping points (between general aggrading and degrading valley states) are associated with reversals in a fundamental system control (sea-level). One (stable or aggrading vs. degrading channels) is associated with an abrupt change in sediment supply due to dam construction, and two others (changes from meandering to anastomosing channel patterns, and different anastomosis styles) are similarly related to changes in sediment supply and/or transport capacity, but with additional elements of historical contingency. Three tipping points are related to avulsions. One, from a regime dominated to reoccupation of former channels to one dominated by progradation into flood basins, is driven by progressive long term filling of incised valleys. Another, nodal avulsions, are driven by disturbances associated with tectonics or listric faults. The third, avulsions and related valley metamorphosis in unfilled incised valleys, is due to fundamental dynamical instabilities within the fluvial system. This synthesis and analysis suggests that geomorphic tipping points are sometimes associated with general extrinsic or intrinsic (to the fluvial system) environmental change, independent of any disturbances or instabilities. Others are associated with natural (e.g., tectonic) or human (dams) disturbances, and still others with intrinsic geomorphic instabilities. This suggests that future tipping points will be equally diverse with respect to their drivers.

  13. Geomorphologic characteristics and origin of the valley bottom troughs at the site of Three Gorges Dam

    Institute of Scientific and Technical Information of China (English)

    LIXusheng; YANGDayuang; KEXiankun; ZHOULufu; CHENDeji

    2003-01-01

    This paper describes valley bottom troughs of the Changjiang River and infers the geomorphologic development of troughs. Based on the morphology of the troughs, the following conclusions are drawn. (1) The deep troughs on the Three Gorges valley bottom are formed by river downcutting along the structural zones on the background of regional tectonic uplift at about 40-30 ka BP. (2) When river downcutting occurred in the river bed of Changjiang, the jets current (particularly eddy current) with a large number of pebbles ground and eroded the valley bottom, resulting in trough formation and deepening. Meanwhile, water currents with gravels and pebbles eroded the bank and the left wall of No.76 trough as well as the right wall of No.77 trough by striking, scouring, horizontal and vertical grinding. (3) The depth of the trough is mainly determined by the intensity of the water current and the consistency of bedrock against erosion, and is not controlled hv the altihlde of the sea level as the base level of erosion.

  14. River Styles, a Geomorphic Approach to Catchment Characterization: Implications for River Rehabilitation in Bega Catchment, New South Wales, Australia.

    Science.gov (United States)

    Brierley; Fryirs

    2000-06-01

    / Geomorphologically derived river styles provide an integrative framework for examining the interactions of biophysical processes in rivers throughout a drainage basin. Nine styles of river character and behavior are identified in Bega catchment, on the south coast of New South Wales, Australia. Headwater streams above the escarpment drain into gorges in the escarpment zone. In different subcatchments at the base of the escarpment, there are three different river styles, namely cut-and-fill, vertically accreted floodplains, and fans. Downstream of these river styles, in the rounded foothills of the catchment, throughput and transfer river styles convey sediments to the lowland plain. In one mid-catchment setting, a floodout traps sediment. Finally, along the lowland plain of Bega River, there is a floodplain accumulation river style. Downstream patterns of river styles in differing subcatchments of the Bega River basin are differentiated into three types, reflecting river adjustments to valley width, slope, and responses to human disturbance. Analysis of the character and condition of each river style in Bega catchment, and their downstream patterns, are used to provide a biophysical basis to prioritorize river management strategies. These reach-scale strategies are prioritorized within an integrative catchment framework. Conserving near-intact sections of the catchment is the first priority. Second, those parts of the catchment that have natural recovery potential are targeted. Finally, rehabilitation priorities are considered for highly degraded reaches. At these sites, erosion and sedimentation problems may reflect irreversible changes to river structure. PMID:10790530

  15. Southwestern Alaska archeological survey, Kagati Lake, Kisarilik-Kwethluk Rivers: A final research report to the National Geographic Society

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Discusses archeological survey of the east of Kagati Lake to Nenevok Lake, north to Trail Creek and Kwethluk River valleys, west along the Kwethluk and Kisaralik...

  16. CRYOGENESIS AND GEODYNAMICS OF ICING VALLEYS

    Directory of Open Access Journals (Sweden)

    V. R. Alekseyev

    2015-09-01

    Full Text Available Due to local groundwater seeping and freezing in layers that accumulate over each other and create large ice clusters on the ground surface, specific conditions of energy and mass transfer are created in the atmosphere–soil–lithosphere system. In winter, the vertical temperature distribution curve is significantly deformed due to heat emission from the water layer above the ice cover during its freezing, and a thermocline is thus formed. Deformation of the temperature curve is gradually decreasing in size downward the profile and decays at the interface of frozen and thaw rocks. Values and numbers of temperature deviations from a 'normal' value depend on heat reserves of aufeis water and the number of water seeps/discharges at a given location. The production of the thermocline alters freezing conditions for underlying ground layers and changes the mechanism of ice saturation, thus leading to formation of two-layer ice-ground complexes (IGC. IGCs are drastically different from cryogenic formations in the neighbouring sections of the river valley. Based on genetic characteristics and the ratios of components in the surface and subsurface layers, seven types of aufeis IGCs are distinguished: massive-segregation, cement-basal, layered-segregation, basal-segregation, vacuum-filtration, pressure-injection, and fissure-vein. Annual processes of surface and subsurface icing and ice ablation are accompanied by highly hazardous geodynamic phenomena, such as winter flooding, layered water freezing, soil heaving/pingo, thermokarst and thermal erosion. Combined, these processes lead to rapid and often incidental reconfigurations of the surface and subsurface runoff channels, abrupt uplifting and subsiding of the ground surface, decompaction and 'shaking-up' of seasonally freezing/thawing rocks, thereby producing exceptionally unfavourable conditions for construction and operation of engineering structures.Formation and development of river networks are

  17. Ambiguities of resistance and collaboration on the Eastern Cape frontier : the Kat River settlement 1829-1856

    NARCIS (Netherlands)

    Ross, R.; Abbink, J.; Bruijn, de M.E.; Walraven, van K.

    2003-01-01

    This chapter unravels the complexities of resistance to, and collaboration with, the British colonizers of the Eastern Cape, South Africa, by the inhabitants of the Upper Kat River Valley. Since the Khoikhoi landholders of the valley had received their land as a result of British action against the

  18. The Owens Valley solar array

    International Nuclear Information System (INIS)

    Solar microwave emission contains essential information for the study of the coronal magnetic structure of active regions and of thermal and nonthermal flare electrons. To exploit this potential requires BOTH imaging and spectroscopy with sufficient resolution to resolve spatial and spectral features. The VLA provides excellent solar imaging (when in the C and D configurations) but inadequate spectral coverage. The existing Owens Valley system has excellent spectral coverage but imaging that is adequate only for very simple sources. The Owens Valley system is currently undergoing an expansion, which when completed in October 1990 will provide a SOLAR-DEDICATED 5 antenna array (10 baselines). By using frequency-synthesis, this will provide a significant imaging capability in addition to its current spectral coverage

  19. Beaver Valley Power Station and Shippingport Atomic Power Station. 1984 Annual environmental report, radiological. Volume 2

    International Nuclear Information System (INIS)

    This report describes the Radiological Environmental Monitoring Program conducted during 1984 in the vicinity of the Beaver Valley Power Station and the Shippingport Atomic Power Station. The Radiological Environmental Program consists of on-site sampling of water and gaseous effluents and off-site monitoring of water, air, river sediments, soils, food pathway samples, and radiation levels in the vicinity of the site. This report discusses the results of this monitoring during 1984. The environmental program outlined in the Beaver Valley Power Station Technical Specifications was followed throughout 1984. The results of this environmental monitoring program show that Shippingport Atomic Power Station and Beaver Valley Power Station operations have not adversely affected the surrounding environment. 23 figs., 18 tabs

  20. Exchange between a river and groundwater, assessed with hydrochemical data

    Directory of Open Access Journals (Sweden)

    E. Hoehn

    2010-11-01

    Full Text Available We describe the chemical composition of groundwater from an alluvial granular aquifer in a valley fill flood plain (River Thur Valley. The aim of this work is to investigate the chemical processes, which are necessary to manage groundwater quality during river restorations. The river flows along this valley and is mostly downwelling on its way, indirectly through an unsaturated zone in the upstream part, and directly through the water-saturated bed in the downstream part. River Thur has been channelized with barriers for more than a century. Since 1992, the authorities started to restore sections of River Thur with river-bed enlargements. Several wells near the river draw groundwater, which is partly to mainly recharged by bank filtration. Many alpine and perialpine rivers have a total mineralization in the order of 200–400 mg L−1 and the chemical composition of the main constituents is of a Ca-Mg-HCO3-(NO3 type. The groundwater composition changes with increasing distance from the downwelling river and with increasing depth in the aquifer. The groundwater body consists of a mixture of groundwater from the seepage of precipitation and from river-bank filtration. The main difference between river water and groundwater results from the microbial activity in river-bed and bank materials. This activity leads to a consumption of O2 and to a higher partial pressure in CO2 in the groundwater. A spatial distribution of different groundwater types was established with geochemical mapping of concentration data, and with fluid logging. Criteria for the distinction of different groundwater compositions are the distance of a well from the river and the subsurface residence time of the groundwater to reach this well. Some of the groundwater has a very short residence time in the subsurface of days to weeks, and some of months to years. Groundwater in the River Thur valley aquifer is not