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Sample records for sw poland peridotite

  1. Origin and evolution of rare amphibole-bearing mantle peridotites from Wilcza Góra (SW Poland), Central Europe

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    Matusiak-Małek, Magdalena; Puziewicz, Jacek; Ntaflos, Theodoros; Grégoire, Michel; Kukuła, Anna; Wojtulek, Piotr Marian

    2017-08-01

    Mantle xenoliths in the 20 Ma Wilcza Góra basanite (Lower Silesia, NE Bohemian Massif) are mostly harzburgites, some with amphibole which is exceptional in the region. Forsterite content in olivine defines two Groups of peridotites: Group A (Fo89.1-91.5) and Group B (Fo84.2-89.2). Hornblende-clinopyroxenite, websterite and one composite xenolith consisting of dunite, olivine-hornblendite and pyroxene-hornblende-peridotite contain olivine with Fo77.3-82.5 and are classified as Group C. Group A xenoliths contain Al-poor orthopyroxene and some contain LREE-enriched clinopyroxene with negative Ti, Zr-Hf and Nb-Ta anomalies. Spinel (Cr# 0.57-0.68) is scarce in Group A, and Cr-rich pargasite occurs in only two xenoliths. Group B xenoliths contain less magnesian orthopyroxene and clinopyroxene. The REE patterns of Group B clinopyroxene are convex downward, less enriched in LREE and have smaller negative Ti, Zr-Hf and Nb-Ta anomalies than those in Group A. The Cr# in Group B spinel is 0.26-0.56, while pargasite is Ti-rich and Cr-poor. Clinopyroxene from Group C is low magnesian, slightly enriched in LREE and has no negative Ti, Zr-Hf and Nb-Ta anomalies. Group C pargasite is rich in Ti and poor in Cr. Equilibration temperatures recorded in all groups vary within the range of 905-970 °C. Xenoliths from Wilcza Góra record a polyphase lithospheric mantle evolution, starting with melting which extracted ca. 30% melt from the protolith and left a harzburgite residuum depleted in Al, lacking clinopyroxene and containing rare Cr-rich spinel. This residuum was later overprinted by chromatographic metasomatism by carbonated hydrous silicate melt related to Cenozoic volcanism. The metasomatic agent was locally hydrous enough to enable amphibole to crystallize. The Group C pyroxenites formed directly from the metasomatic melt or during peridotite-melt reactions at high melt-rock ratio. The melt is inferred to have percolated through the wall-rock peridotite, decreasing its amount

  2. Thermal and metasomatic rejuvenation and dunitization in lithospheric mantle beneath Central Europe - The Grodziec (SW Poland) case study

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    Matusiak-Małek, Magdalena; Ćwiek, Mateusz; Puziewicz, Jacek; Ntaflos, Theodoros

    2017-04-01

    The 32 Ma Grodziec nephelinite (Lower Silesia, SW Poland) contains xenolith of peridotite (mostly lherzolite) and clinopyroxenite/olivine clinopyroxenite composition. The forsterite content in olivine classifies these rocks into three groups: groups A and B consist of peridotites, while group C xenoliths are pyroxenitic cumulates. Group A xenoliths contain olivine Fo 87.90-91.8% and pyroxenes with high Mg# ( 0.91-0.92); clinopyroxene is strongly LREE-enriched (LaN/LuN = 2.19-17.74) and strongly impoverished in Zr, Hf and Ti relative to primitive mantle. The group B xenoliths (dunites and wehrlite) are orthopyroxene-free, olivine and clinopyroxene are less magnesian than those in the A group (Fo = 85.2-87.2%, Mg# = 0.86-0.88), clinopyroxene is less LREE-enriched (LaN/LuN = 4.07-4.15) and only slightly impoverished in Zr, Hf and Ti. Group C xenoliths contain olivine with forsterite content from 78.6 to 86.6% and clinopyroxene of Mg# from 0.84 to 0.85, with LREE/trace element characteristics similar to those of B group (LaN/LuN = 1.96-3.10). Group A xenoliths from Grodziec record migration of mixed carbonatite-alkaline silicate melts through the subcontinental lithospheric mantle beneath Lower Silesia, which preceded the migration of melts similar to the Grodziec nephelinite. The peridotitic protoliths were dunitized at the direct contacts with the migrating nephelinite melt and are now represented by group B. Group C pyroxenites originated in mantle conditions by crystal settling in places of transient nephelinite melt stagnation. The mantle section beneath Grodziec was reheated to ca 1000-1100 °C. The Grodziec scenario is similar to that of Księginki (northern extension of Eger Rift, SW Poland), which shares a similar age of xenolith entrainment. Both sites show that the processes of mantle metasomatism and thermal rejuvenation of subcontinental lithospheric mantle were more intense during the Lower Oligocene volcanic climax compared to those recorded in younger

  3. Metals in Racomitrium lanuginosum from Arctic (SW Spitsbergen, Svalbard archipelago) and alpine (Karkonosze, SW Poland) tundra.

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    Wojtuń, Bronisław; Samecka-Cymerman, Aleksandra; Kolon, Krzysztof; Kempers, Alexander J

    2018-02-19

    Arctic-alpine tundra habitats are very vulnerable to the input of relatively small amounts of xenobiotics, and thus their level in such areas must be carefully controlled. Therefore, we collected the terrestrial widespread moss Racomitrium lanuginosum (Hedw.) Brid. in Spitsbergen in the Arctic moss lichen tundra and, for comparison, in the Arctic-alpine tundra in the Karkonosze (SW Poland). Concentrations of the elements Cd, Co, Cr, Cu, Fe, Hg, Li, Mn, Mo, Na, Ni, Pb, V, and Zn in this species and in the parent rock material were measured. We tested the following hypothesis: R. lanuginosum from Spitsbergen contains lower metal levels than the species from the Karkonosze collected at altitudes influenced by long-range transport from former Black Triangle industry. Principal component and classification analysis (PCCA) ordination revealed that mosses of Spitsbergen were distinguished by a significantly higher Na concentration of marine spray origin and mosses of Karkonosze were distinguished by significantly higher concentrations of Cd, Cr, Cu, Fe, Hg, Li, Mn, Pb, V, and Zn probably from long-range atmospheric transport. The influence of the polar station with a waste incinerator resulted in significantly higher Co, Li, and Ni concentrations in neighbouring mosses in comparison with this species from other sites. This investigation contributes to the use of R. lanuginosum as a bioindicator for metal contamination in Arctic and alpine tundra regions characterised by severe climate habitats with a restricted number of species. This moss enables the control of pollution usually brought solely by long-range atmospheric transport in high mountains as well as in Arctic areas.

  4. Lithospheric mantle beneath NE part of Bohemian Massif and its relation to overlying crust: new insights from Pilchowice xenolith suite, Sudetes, SW Poland

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    Ćwiek, Mateusz; Matusiak-Małek, Magdalena; Puziewicz, Jacek; Ntaflos, Theodoros

    2017-12-01

    The Oligocene/Miocene basanite from Pilchowice (Sudetes Mts., SW Poland) carries numerous small xenoliths of mantle peridotite, mostly harzburgite. The Pilchowice xenolith suite is dominated by harzburgites and dunites containing olivine Fo 90.2-91.5 (group A). The peridotites of group B (olivine Fo 88.6-89.4), and C (olivine Fo 83.2-86.5) are subordinate. The peridotites suffered from significant melt extraction (20-30%) and were subsequently subjected to metasomatism. Three different trace element compositional patterns of group A clinopyroxene occur, which are typical of silicate melt, carbonatite melt and silicate-carbonatite melt metasomatism, whereas groups B and C were affected by silicate melt metasomatism only. The Pilchowice basanite occurs at the contact of Karkonosze-Izera Block and Kaczawa Complex, two major geological units of Sudetes. The Pilchowice xenolith suite documents underlying lithospheric mantle of composition and depletion degree similar to those described in the whole Lower Silesian mantle domain, which forms NE termination of Saxo-Thuringian zone of the European Variscan orogen. The crustal structure of the orogen is, therefore, not mirrored in the mantellic root.

  5. Lithological indicators of loess sedimentation of SW Poland

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    Krawczyk, Marcin; Ryzner, Kamila; Skurzyński, Jacek; Jary, Zdzisław

    2017-12-01

    High-resolution grain-size investigations were carried out in two SW Polish loess sections: Biały Kościół (Niemcza-Strzelin Hills) and Zaprężyn (Trzebnica Hills). Each sequence was sampled by using the same methodology and samples were taken at 5 centimeters intervals. The particle size distribution was obtained with a Mastersizer 2000 laser, used for diffraction methods. From the obtained results the basic parameters and grain size indicators were calculated: Mz, Grain Size Index ratio, U-ratio and the percentage content of clay ( 63 μm). Both loess-soil sequences are composed of interfluve and slope loess facies and consist of five litho-pedostratigraphic units developed during the Late Pleistocene and Holocene: two loess units L1LL1, L1LL2 and three polygenetic fossil soils sets S0, S1 and L1SS1. The distance between these two profiles is about 60 km. Zaprężyn, as a section located more to the north, has almost no lower younger loess and higher level of weathering which could be related to proximity of this site to the Ice Sheet margin. The climate here was more extreme and harsh. What is more, the difference in development of soil L1SS1 can be observed: while in Biały Kościół pedogenesis process was slower and less disturbed than in Zaprężyn. The upper part of L1SS1 in Biały Kościół was deformed by gelifluction, frost heave and other periglacial processes. Mz indicator by the grain-size distribution in these sediments reflects subtle variations in the climatic system. Moreover, in Zaprężyn the content of sand fraction is higher than in Biały Kościół what can be the evidence of short episodes of strong winds during cold period of sedimentation. The aim of this paper is to compare two loess profiles by their stratigraphical and lithological similarities which are result of climate conditions and features of surrounding environment.

  6. Distribution of Ag in Cu-sulfides in Kupferschiefer deposit, SW Poland

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    Kozub, Gabriela A.

    2014-05-01

    The Cu-Ag Kupferschiefer deposit located at the Fore-Sudetic Monocline (SW Poland) is a world class deposit of stratabound type. The Cu-Ag mineralization in the deposit occurs in the Permian sedimentary rocks (Rotliegend and Zechstein) in three lithological types of ore: the dolomite, the black shale and the sandstone. Silver, next to copper, is the most important element in the Kupferschiefer deposit (Salamon 1979; Piestrzyński 2007; Pieczonka 2011). Although occurrence of the Ag-minerals such as native silver, silver amalgams, stromeyerite, jalpaite and mckinstryite, silver is mainly present in the deposit due to isomorphic substitutions in Cu-minerals such as chalcocite, bornite, tennantite, covellite and chalcopyrite. The aim of the study was to define distribution of silver in Cu-minerals and correlate occurrence of Ag-enriched Cu-sulfides with native silver and silver amalgams. Identification of minerals and textural observation were performed using field emission scanning electron microscope. Analyzes of chemical composition of Cu-sulfides were performed utilizing electron microprobe. Silver concentration in Cu sulfides ranges from 0.1 to 10.4 wt.% in chalcocite, 0.2-15.8 wt.% in bornite, 0.1-2.9 wt.% in tennantite, 0.05-0.3 wt.% in chalcopyrite and ca. 0.4 wt.% in covellite. In general, distribution of silver in Cu-minerals is irregular, as indicated by high variations of Ag concentration in each mineral. Content of Ag in Cu-sulphides, in samples where native silver and silver amalgams are not found, is lower than in samples, where native silver and silver amalgams are noted. The chemical analyzes of Ag-bearing Cu-minerals indicate decrease of Cu content in minerals with high Ag concentration. In such case, decrease of Fe content is also noted in bornite. Lack of micro-inclusions of the native silver or silver amalgams in the Cu-minerals indicates that presence of Ag is mainly related to the isomorphic substitutions. This is in agreement with previous

  7. The Anita Peridotite, New Zealand

    DEFF Research Database (Denmark)

    Czertowicz, Tom; Scott, James; Waight, Tod Earle

    2016-01-01

    The orogenic Anita Peridotite in Fiordland, SW New Zealand, provides an opportunity to examine the composition of a large block of upper mantle exhumed from beneath a Cretaceous arc. This Little studied 1km2 km massif is dominated by spinel-facies harzburgite and dunite. Olivine Mg# of 92...

  8. Chromites from the Gogoł;ów-Jordanów Serpentinite Massif (SW Poland) - evidence of the arc setting magmatism

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    Wojtulek, Piotr; Puziewicz, Jacek; Ntaflos, Theodoros; Bukała, Michał

    2014-05-01

    The Gogołów-Jordanów Serpentinite Massif (GJSM) is a peridotitic member of the Variscan Ślęża Ophiolite (SW Poland). Chromitite veinlets and pockets occur in the central part of the massif in the Czernica Hill area within completely serpentinized rocks. Chromitites consist of rounded chromite grains up to 4 cm and chlorite filling the interstices. The veins are embedded in serpentine-olivine-chlorite aggregates. Chemical composition of chromite occurring in chromitites defines two varieties. Chromite I (Cr# = 0.49 - 0.58) contains 23.32 - 28.36 wt.% Al2O3, 40.29 - 48.10 wt.% Cr2O3, 15.10 - 15.50 wt.% FeO, 14.50 - 15.50 wt.% MgO and ~0.1 wt.% TiO2. Chromite II (Cr# = 0.71 - 0.73) contains 13.83 - 15.24 wt.% Al2O3, 54.85 - 56.65 wt.% Cr2O3, 16.71 - 18.04 wt.% FeO, 10.62 - 11.59 wt.% MgO and 0.1 wt.% TiO2. Chromite grains are composed mostly of chromite I. Chromite II forms irregular spongy domains up to 150 µm, located at fissures or forming grain rims. The bulk chromitite composition of the massive ores reveals Rb, Ba, Pb and Sb enrichment relative to primitive mantle; Pt and Pd (up to 36 ppb) are also enriched relative to primitive mantle. Other phases coexisting with chromite are chlorite and olivine. Chlorite (Fe# = 0.02) contains 17.5 - 23.0 wt.% Al2O3, 0.6 - 1.8 wt.% Cr2O3 and 31.8 - 34.2 wt.% MgO. Olivine (Fo93.5-96.2) contains 0.44- 0.51 wt.% NiO. Olivine grains are zoned - the low-forsteritic cores are surrounded by high-forsteritic domain. Chromite II and chlorite are secondary phases and were probably formed due to greenschist facies metamorphism. Chromitites are cumuletes of melt blocked during its flow through peridotitic host. Low TiO2 content and moderate chromian number of the GJSM chromitites is typical for chromian spinels originated from melt derived from back arc depleted source (cf. Python et al., 2008, Gonzalez-Jimenez, 2011). The GJSM chromitites are rich in Al and poor in Pt and Pd what is typical for chromitites occurring in the

  9. New records of rare lichenicolous and lichen-forming fungi from volcanic rocks in SW Poland

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    Katarzyna Szczepańska

    2015-08-01

    Full Text Available Records of two lichenicolous and nine lichen-forming fungi found in the southwestern part of Poland are presented. All of the reported species are very rare and they have only a few scattered localities in the country. One of them, Lecanora pannonica, is reported for the second time from Poland. Additionally, the new, contemporary records of Cercidospora macrospora, Rhizocarpon disporum, R. viridiatrum and Stereocaulon pileatum in Lower Silesia were noted. These species were known only from historical collections in the study area. Furthermore, Lecidea fuscoatra has been found a new host for Sagediopsis barbara. All of the localities of recorded species were found on natural outcrops of basalt rocks.

  10. Decreasing concentrations of metals in Sphagnum mosses in ombrotrophic mires of the Sudety mountains (SW Poland) since late 1980s.

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    Wojtuń, Bronisław; Samecka-Cymerman, Aleksandra; Kolon, Krzysztof; Kempers, Alexander J

    2013-06-01

    In this investigation we focus on the evaluation of changes in metal pollution between 1986 until 2011 by Sphagnum species as bioindicators in 100 km part of the Sudety mountains influenced by the former Black Triangle Region. Concentrations of Cd, Co, Cr, Cu, Fe, Mn, Ni, Pb and Zn were measured in various Sphagnum species all from ombrotrophic bogs in the Sudety mountains (SW Poland). The tested hypothesis was that overall improvements in pollution control in the former Black Triangle Region between 1986 until recent reduced the amount of metals deposited and accumulated by these plants. Concentrations of Cd, Cr, Cu, Fe, Pb and Zn in Sphagnum species were very high in 1986 indicating a heavy pollution of the examined bogs in this period, and significantly higher than in samples collected in 2011. The PCCA ordination showed the similar pattern in all bogs. In 2011 concentration of the Co was significantly higher in hollow species and concentration of Mn was significantly higher in those from hummocks. Differences between hollow/hummock sites were more important than species-specific abilities of Sphagnum mosses to accumulate metals. Species from hollows were better bioindicators of Co and those from hummocks were better bioindicators of Mn pollution. Copyright © 2012 Elsevier Ltd. All rights reserved.

  11. Recent advances in geomorphological mapping in the Sudetes Mountains, SW Poland

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    Kasprzak, Marek; Traczyk, Andrzej; Migoń, Piotr

    2013-04-01

    The Sudetes - a medium-altitude mountain range in Central Europe - have a long history of mapping geomorphic features. Past approaches relied heavily on ground registration of specific landforms and interpretation of topographic maps at the scale of 1:25,000 and 1:10,000, although both tended to underestimate roughness of local hillslope topography. Aerial photography, in turn, proved of limited usefulness in the densely forested terrain. An increasing availability of LiDAR-derived digital elevation models provides new opportunities for geomorphological mapping and allows to verify previous views, whereas portable tools help to map subtle geomorphic features if LiDAR is not available. Selected results of recent mapping exercises will be presented, based on three case study areas: Karkonosze Mountains, Stołowe ('Table') Mountains and Kamienne Mountains. In the Karkonosze, the highest mountain range within the Sudetes, elevated above the timberline in its axial part, a complete multi-layered geomorphological map based on LiDAR data with 0.6 x 0.6 m resolution and ortophomap interpretation has been prepared in the GIS-Environment (Global Mapper, QGIS). DEM was used to establish geomorphometric parameters of relief, mainly slope, and to track boundaries between different landforms, whereas aerial photographs helped mainly to map the extent of specific cold-climate relief features above the timberline. The map consists of 46 thematic SHP layers, showing landforms of different origin. The value of the map is twofold. First, this is the first complete digital geomorphological map for a mountainous area in Poland. Second, since it is based on high-resolution altimetric data, it allowed to verify previous views on the extent and style of mountain glaciation, distribution of mid-slope benches, characteristics of channel pattern etc. The Stołowe Mountains are an example of nearly completely forested tableland morphology, difficult to perform ground mapping, especially along

  12. Subduction-related prograde metamorphism of the ultramafic members of the Central-Sudetic Ophiolite (SW Poland)

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    Wojtulek, Piotr; Puziewicz, Jacek; Ntaflos, Theodoros

    2016-04-01

    The Central-Sudetic Ophiolite (CSO) consists of Ślęża (SM), Braszowice-Brzeźnica (BBM), Szklary (SZM) and Nowa Ruda massifs. Ultramafic rocks occurring in ŚM, BBM and SM have MgO/SiO2 (0.82-1.20) and Al2O3/SiO2 (~0.01) ratios typical for serpentinized mantle peridotites. They are enriched in Cs, Pb and Sb and depleted in Rb, Ba, Nb, La, Ce, Sr, Zr, Er and Y relative to primitive mantle. The serpentinites are antigorite ones, pseudomorphic chrysotile varieties occur sparsely. Serpentinites from each massif contain specific non-serpentine phases. Ślęża serpentinites contain primary olivine-chromite aggregates, olivine and clinopyroxene aggregates interpreted as basaltic melt percolation phases, secondary olivine with magnetite inclusions (locally with cleavage) and secondary microcrystalline olivine-clinopyroxene-magnetite aggregates ("brownish aggregates") with bastite and mesh textures. The BBM serpentinites contain primary olivine-chromite aggregates, primary diopside grains, secondary magnetite-bearing olivine and tremolite. The SZM serpentinites contain olivine, tremolite and enstatite grains. Enstatite (Mg# = 92.8-93.0) contains >0.2 wt.% Cr2O3 and >0.7 Al2O3. All secondary non-serpentine phases are intergrown by antigorite. Very low overall trace element contents, Cs and high Pb-Sb anomalies of the CSO serpentinites are similar to subduction zone related serpentinites not affected by later fluid refertilization. Mineral assemblages shows prograde alteration of the rocks: (1) low-T serpentinization I forming pseudomorphic lizardite-chrysotile serpentinites; (2) antigorite recrystallization; (3) deserpentinization forming secondary olivine with magnetite inclusions, "brownish structures", tremolite and/or enstatite; (4) high-T serpentinization II forming antigorite intergrowths. Alteration degree is different in each massif: rocks from the SM are the most altered, they contain antigorite-olivine-enstatite-tremolite assemblage typical for temperatures

  13. Poland

    OpenAIRE

    Kus, Michal

    2011-01-01

    The concept of media accountability is a relatively new issue in Poland, both for Polish media researchers and journalists (media professionals), as well as for media users. Traditional institutions and instruments of media accountability are not very well developed (see Głowacki & Urbaniak, 2010). In this context, possible development of media accountability innovations online creates significant opportunities for fulfilling existing gaps in this area. A desk study and interviews conducted w...

  14. UAV and SfM in Detailed Geomorphological Mapping of Granite Tors: An Example of Starościńskie Skały (Sudetes, SW Poland)

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    Kasprzak, Marek; Jancewicz, Kacper; Michniewicz, Aleksandra

    2017-11-01

    The paper presents an example of using photographs taken by unmanned aerial vehicles (UAV) and processed using the structure from motion (SfM) procedure in a geomorphological study of rock relief. Subject to analysis is a small rock city in the West Sudetes (SW Poland), known as Starościńskie Skały and developed in coarse granite bedrock. The aims of this paper were, first, to compare UAV/SfM-derived data with the cartographical image based on the traditional geomorphological field-mapping methods and the digital elevation model derived from airborne laser scanning (ALS). Second, to test if the proposed combination of UAV and SfM methods may be helpful in recognizing the detailed structure of granite tors. As a result of conducted UAV flights and digital image post-processing in AgiSoft software, it was possible to obtain datasets (dense point cloud, texture model, orthophotomap, bare-ground-type digital terrain model—DTM) which allowed to visualize in detail the surface of the study area. In consequence, it was possible to distinguish even the very small forms of rock surface microrelief: joints, aplite veins, rills and karren, weathering pits, etc., otherwise difficult to map and measure. The study includes also valorization of particular datasets concerning microtopography and allows to discuss indisputable advantages of using the UAV/SfM-based DTM in geomorphic studies of tors and rock cities, even those located within forest as in the presented case study.

  15. Post-glacial acidification of two alpine lakes (Sudetes Mts., SW Poland, as inferred from diatom analyses

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    Sienkiewicz Elwira

    2016-06-01

    Full Text Available Past environmental changes in mountain lakes can be reconstructed with the use of subfossil diatoms from post-glacial sediments. This study applied such an analysis to two mountain lakes in the Sudetes Mts. in Poland: Mały Staw (MS and Wielki Staw (WS. Cores 882 cm long (MS and 1100 cm long (WS taken from the centre of each lake in 1982 were used to study the long-term acidification history of these lakes. Changes in vegetation indicate that the initial phase of MS started at the end of the Pleistocene. WS sediments began to accumulate shortly after that, at the beginning of the Holocene. The majority of the diatom assemblages are typical of oligotrophic acidic lakes located in alpine and arctic regions. A pH reconstruction based on diatoms (DI-pH showed long-term acidification dating to almost the beginning of the lakes’ existence. Natural acidification began after the deglaciation, and the most intensive acidification continued to the end of the mid-Holocene. Through the whole period studied, pH decreased by 1.4 in MS and 0.9 in WS. After a period of relatively stable lake water pH, it decreased rapidly during the last few decades of the 20th century, due to anthropogenic pollution: pH declined by 0.7 in MS and 0.3 in WS. Mały Staw, being shallower, smaller, and with a larger drainage basin than Wielki Staw, is more sensitive to acid deposition; this accounts for the difference in pH.

  16. Holocen history of vegetation at “Uroczysko Mokradła” (SW Poland – paleobotanical research

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    Klara Tomaszewska

    2016-09-01

    Full Text Available Two peat bogs were studied in the Bory Dolnośląskie, the forest complex in Lower Silesia (Poland. An Instorf drill was used to collect two peat profiles from the deepest places. The macroremains analysis showed that after the initiation of peat-forming processes phytocoenoses responsible for the deposition of transition sphagnum peat were developed at both locations. Later on, the development of both peat bogs differed. The smaller peat bog continued to develop, whereas the big bog was shifted to ombrotrophic water regime. Therefore, phytocoenoses accumulated 1.3 m of Sphagnum peat. The peat-forming process was initiated at different times in both sites. For the smaller peat bog, it took place during the Atlantic period, while in the case of the larger peat bog – several thousand years later. The first identified forest phytocoenoses in the Atlantic period are mesophilic multi-species deciduous forests. Dry coniferous forests and mixed birch-pine forests grew in dry habitats. Riparian forests occupied lower grounds. In the Subboreal period, the oak–hazel communities initially developed and mixed coniferous forests were partially replaced by light oak forests. The encroachment of spruce, fir, hornbeam, and beech resulted in the development of dry ground forests, including beech–fir woods. The importance of riparian forests increased, whereas in dry grounds pine and mixed coniferous forests continued to occur. In the Subatlantic period, the transformations in forest communities were associated with the spread of hornbeam, beech, and fir and thereby vast fertile habitats were colonized by dry ground communities and beech woods. Pine and mixed forests as well as riparian forests were of lesser importance. Pollen records from the last 500 years showed the clear presence of humans. It was evident from the presence of cereal and weed pollen and from the disturbances in the pollen records caused by peat extraction in the Middle Ages.

  17. Mycorrhizal status of plants in two successional stages on spoil heaps from fireloam mining in Lower Silesia (SW Poland

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    Dorota Kasowska

    2014-01-01

    Full Text Available The mycorrhizal status of two plant communities representing an initial stage (1-2 year-old and a 8-9-year-old stage of succession on spoil heaps from fireloam mining in Lower Silesia, Poland, was determined. In the initial stage, the mycorrhizal structures were not observed in 39% of the investigated species; they were members of the Polygonaceae, Chenopodiaceae and Poaceae families. The relative cover of non-mycorrhizal plants exceeded 50% and the major role was played by the Polygonum aviculare population, which predominated the whole community. Mycorrhizal species (arbuscular mycorrhizae contributed to 61 % of the composition of the initial phyto-coenosis. The most numerous taxa were those with 20-40% of the root length colonized, with a small number of arbuscules (0.2-3.1% of the root length containig arbuscules and no vesicles. In the advanced stage of succession, mycorrhizal plants definitely dominated and the major role was played by the Tussilago farfara population. Compared with the initial stage, the later one also harboured more plants with mycorrhizas occupied >40% of the root length, as well as containing numerous arbuscules (>20% of the root length and vesicles. The non-mycorrhizal species, i.e., Equisetum arvense and Poa compressa, represented 11 % o': the community composition and their relative cover amounted to 3%. Despite the relatively frequent occurrence of the arbuscular mycorrhizae in the initial stage of succession, the qualitative properties of the colonization indicated a low effectiveness of symbiosis. This could be caused by the lack of adaptation of the fungal symbiont to the edaphic conditions which were changed after disturbance.

  18. Using soil properties as a tool to differentiate landslide generations and constrain their ages - Rogowiec landslide, Sudetes (SW Poland)

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    Kacprzak, Andrzej; Migoń, Piotr

    2013-04-01

    The Sudetes, at the border of Poland and the Czech Republic, are generally considered as a mountain range where landslides play a marginal geomorphic role. Only a few larger landslides have been recorded during historical times, mainly on steep valley sides undercut by rivers. Forested slopes, which dominate in the Sudetes, are usually inferred to be stable, except for near-surface bioturbation and localized accelerated surface erosion at sites subject to strong human impact. Large, apparently relict landslides in the Kamienne Mountains, Middle Sudetes, pose a considerable challenge to this view and two interpretations are possible. First, they may be indeed relict, pre-Holocene features that formed under different environmental conditions and have been completely stabilized since the origin. Second, they may be rare components of the contemporary (Holocene) geomorphic system but their frequency of occurrence is low and this is why none has been reported in written or oral records. If the second scenario captures the reality adequately, this would have significant implications for hazard and risk assessment. To address this issue, an extensive soil survey was carried out on the large landslide of Rogowiec, likely of complex flow nature as suggested by landform mapping. The rationale of the study involved an assumption that soil formation time in the area is limited to the Holocene, since harsh periglacial conditions typified the late Pleistocene. 15 soil pits were excavated within landslide terrain and on adjacent reference slopes which do not bear any evident traces of significant displacements. Despite the small area under investigation, the soil profiles are very diverse in terms of depth, horizonation, organic matter content, development of soil structure, as well as the content and lithology of coarse fragments. A great deal of this diversity can be explained by different duration of pedogenesis controlled by geomorphic processes. Very weakly developed soil

  19. The role of landslides in downslope transport of caprock-derived boulders in sedimentary tablelands, Stołowe Mts, SW Poland

    Science.gov (United States)

    Duszyński, Filip; Jancewicz, Kacper; Kasprzak, Marek; Migoń, Piotr

    2017-10-01

    Escarpment slopes in sedimentary tablelands are often mantled by extensive boulder blankets. While lithology shows beyond doubt that caprock is the source of boulders, the processes involved in boulder movement and their distribution patterns are rarely examined. In this paper we investigate the role of landslides initiated within middle and lower escarpment slopes in redistributing boulder covers, on the example of the Stołowe Mountains in SW Poland. Quartz sandstones form caprock and give rise to precipitous, albeit rather low (30 m high at most, typically 10-15 m) uppermost slope sections, and are the source of boulders which occur at distances even 1 km away from the caprock, on the nearly flat footslope. Sedimentary series beneath caprock include fine-grained rocks such as mudstones, claystone and calcareous sandstones. Geomorphological mapping and geomorphometric analysis of a high-resolution DEM allowed us to identify landform patterns interpreted as resulting from landslides, both rotational and translational. The latter produced distinctive tread-and-riser topography, with risers up to 10 m high. Results of geophysical prospecting using Electrical Resistivity Tomography (ERT) confirm the presence of allochthonous, sandstone-derived upper layer that wedges out downslope and indicate resistivity contrasts at depth of 5-15 m, interpreted as basal boundaries of landslide material. Sandstone boulders rafted on top of slid masses and reached very distant footslope settings. The primary role of landsliding consists of transporting allochthonous boulders further than would be possible otherwise and accumulating boulders in clusters and linear belts across the slope, notably on risers.

  20. Breeding avifauna of Niemodlin countryside (SW Poland during the years 2002-2007, and its changes over the last 56 years (1962-2007

    Directory of Open Access Journals (Sweden)

    Kopij Grzegorz

    2016-09-01

    Full Text Available Niemodlin countryside (c. 300 km2 is situated in the south-western part of Opole Silesia, SW Poland. Forests occupy c. 40%, arable grounds – 1/3, and meadows and pastures – 7%. There are 31 fish-ponds with a total diked surface of 663 ha. The paper presents results of field investigations carried out during the years 2002-2007 and an analysis of changes in the breeding avifauna over the last 56 years. During the years 2002-2007, 123 breeding and 11 probably breeding bird species were recorded in this area. During the years 1962-2007 151 species were recorded as breeding residents; and additional five species – as probably breeding resident. The following species were recorded as breeding for the first time in 1962-2007: Haliaeetus albicilla, Larus canus, Motacilla cinerea, Saxicola torquata, Locustella luscinioides, Ficedula albicollis, Corvus corax and Carpodacus erythrinus. In the same period the following species became extinct: Podiceps nigricollis, Anas clypeata, Milvus milvus, and Tringa glareola. The following species increaed in numbers in 1962-2007: Coturnix coturnix, Grus grus, Columba oenas, Apus apus, Dryocopus martius, Dendrocopos medius, Motacilla cinerea, Saxicola torquata and Corvus corax. In the same period, Tachybaptus ruficollis, Podiceps cristatus, Podiceps grisegena, Ciconia ciconia, Aythya nyroca, Perdix perdix, Gallinago gallinago, Larus ridibundus, Tyto alba, Alcedo atthis, Picus viridis, Riparia riparia and Corvus cornix decreased in numbers. The areas with the highest concentration of rare and endangered species are postulated to be protected as nature reserves, landscape parks and other spatial forms of nature conservation.

  1. Multi-seasonal pattern in 5-year record of stable H, O and S isotope compositions of precipitation (Wrocław, SW Poland)

    Science.gov (United States)

    Górka, Maciej; Skrzypek, Grzegorz; Hałas, Stanisław; Jędrysek, Mariusz-Orion; Strąpoć, Dariusz

    2017-06-01

    Sulphur dioxide is still a major industrial pollutant in the atmosphere. However, its origin is not always easily traceable, particularly at regional scale where numerous sulphur sources coexist. Geochemical tracers, such as the stable sulphur (δ34S) and oxygen (δ18O) isotopic compositions of sulphates in precipitation, have been successfully applied for estimation of the S-contribution from multiple sources to the atmosphere. However, the majority of previous studies conducted over relatively short time spans have revealed a short-term seasonal trends only and were unable to capture multi seasonal systematics. Here, we present results from a five-year monitoring program conducted in Wrocław (SW Poland). We have determined the Local Meteoric Water Line of δ2H= (6.91 ± 0.25) × δ18O + (2.39 ± 2.43) and sulphates stable sulphur (δ34S(SO4) 0.3-5.4‰) and oxygen (δ18O(SO4) 4.7-19.1‰) isotope composition in precipitation. The stable sulphur isotope results confirm that sulphates in precipitation primarily originate from high temperature (minimum mean over sampling period 680 °C) combustion of fuels with δ34S signatures ≤4.4‰. The stable oxygen isotope composition of sulphates and precipitation water indicates that the primary sulphate (generated directly by industrial processes) contribution was <49% during the whole study period, with a mean of ∼20% during the non-heating and ∼40% during the heating periods. The δ34S(SO4) value for precipitation displays multi-seasonal oscillations with an amplitude of about 2‰, which has not been previously reported. The mechanism driving the oscillation needs further investigation in order to reveal possible associations between this phenomenon and climatic patterns or changes in fossil fuel use. This new evidence from 5-year-long records needs to be taken into consideration when analysing trends from shorter-term observations.

  2. Carbonatisation of Weathered Peridotites in Laboratory Experiments

    Science.gov (United States)

    Hövelmann, J.; Austrheim, H.; Beinlich, A.; Munz, I. A.

    2010-12-01

    Enhanced in-situ carbonatisation of ultramafic rocks has been proposed as a strategy for a permanent and safe storage of CO2 in order to reduce anthropogenic greenhouse gas emissions (e.g., Kelemen and Matter 2008). This idea emerged from studies of natural examples demonstrating that ultramafic rocks react extensively with CO2 to form ophicarbonates. However, despite their Mg-rich nature, ultramafic rocks are often associated with calcite (CaCO3) rather than magnesite (MgCO3) and dolomite (CaMg(CO3)2). Whether these so-called ophicalcites represent sedimentary or tectonic breccias or are produced during hydrothermal alteration of ultramafic rocks, has been discussed for many years (e.g., Folk and McBride 1976). The view that reactions between hydrothermal fluids and ultramafic rocks can result in the formation of ophicalcite was recently supported by Beinlich et al. (2010), who documented Ca- and CO2-metasomatism and extreme Mg depletion in serpentinised and weathered peridotite clasts from the conglomerates of the Solund basin (SW Norway). This study also suggests that weathering is an important factor for the carbonatisation of ultramafic rocks. We have performed hydrothermal experiments on weathered peridotites in order to better constrain the mechanisms and conditions that trigger Mg-loss from ultramafic rocks and subsequent calcite precipitation. Un-crushed, partly serpentinised and weathered peridotite samples were allowed to react in a Ca-bearing saline solution under CO2 pressure (PCO2: 130-160 bar) at 200°C. We were able to illustrate the textural and chemical evolution during the reaction through a detailed comparison of the solid and fluid samples before and after the experiments. The initial samples showed a typical mesh texture with veins of serpentine surrounding meshes filled either with fresh or weathered olivine. The experimentally treated samples reveal a strongly reacted rim, predominantly composed of calcite, but still showing ghosts of the

  3. The role of domestic dogs and cats in the zoonotic cycles of ticks and pathogens. Preliminary studies in the Wrocław Agglomeration (SW Poland).

    Science.gov (United States)

    Król, Nina; Kiewra, Dorota; Szymanowski, Mariusz; Lonc, Elżbieta

    2015-11-30

    The collection of 729 tick specimens (Ixodes ricinus, 88.6%; Ixodes hexagonus, 9.2%; Dermacentor reticulatus, 2.2%) removed from 373 dogs and 78 cats, along with 201 ticks from vegetation (I. ricinus, 75.6%; D. reticulatus, 24.4%), allows one to say that pets play an important role in maintaining tick life cycles in different urban area. It shows the lack of statistical differences between tick intensity in high-impact anthropogenic areas (HIAA), low-impact anthropogenic areas (LIAA) and mixed areas designed, in an objective way, by GIS techniques. The comparable (statistically insignificant) level of infection with Borrelia spp. of I. ricinus from pets (22.5%) and vegetation (24.8%), shows that dogs and cats do not have zooprophylactic competence for Borrelia spp. in different urban areas. Moreover, Borrelia spp. was detected in I. hexagonues (1.5%) collected from pets, and in D. reticulatus (2%) obtained from vegetation. The presence of D. reticulatus in the Wrocław Agglomeration confirms its expansion and the distribution range in Poland. Copyright © 2015 Elsevier B.V. All rights reserved.

  4. The effect of long-term forestry drainage on the current state of peatland soils: A case study from the Central Sudetes, SW Poland

    Directory of Open Access Journals (Sweden)

    B. Glina

    2016-10-01

    Full Text Available One important need in the context of peatland restoration is to gain knowledge of soil organic matter quality and current soil-forming process in degraded peatlands. The aim of this study was to evaluate the impact of long-term drainage on soil transformation processes. In autumn 2012, soil survey and sampling was carried out on five shallow peatlands in the Central Sudeten Mountains (Poland which had been drained for forestry use in the late 1800s or early 1900s. Four organic soils (Histosols and one organo-mineral soil (Histic Gleysol were studied. The surface soil horizons were mainly transformed due to long-term forestry drainage. Increased aeration of these layers had enhanced their content of labile forms of carbon and they were undergoing secondary transformation. Soil transformation was more advanced in fen peatlands than in transitional mire or raised bogs. Only the fens exhibited characteristic evidence of the moorsh-forming process. Further drying of these soils will negatively affect their rewetting potential and significantly reduce the effective application of restoration treatments. In order to reduce organic matter transformation and loss from the investigated peatland areas, their drainage ditches should be blocked. Additionally, some trees should be removed from their central areas to reduce evapotranspiration.

  5. Short-term radon activity concentration changes along the Underground Educational Tourist Route in the Old Uranium Mine in Kletno (Sudety Mts., SW Poland).

    Science.gov (United States)

    Fijałkowska-Lichwa, Lidia

    2014-09-01

    Short-term (222)Rn activity concentration changes along the Underground Educational Tourist Route in the Old Uranium Mine in Kletno were studied, based on continuous measurements conducted between 16 May 2008 and 15 May 2010. The results were analysed in the context of numbers of visitors arriving at the facility in particular seasons and the time per day spent inside by staff and visitors. This choice was based on partially published earlier findings (Fijałkowska-Lichwa and Przylibski, 2011). Results for the year 2009 were analysed in depth, because it is the only period of observation covering a full calendar year. The year 2009 was also chosen for detailed analysis of short-term radon concentration changes, because in each period of this year (hour, month, season) fluctuations of noted values were the most visible. Attention has been paid to three crucial issues linked to the occurrence and behaviour of radon and to the radiological protection of workers and visitors at the tourist route in Kletno. The object of study is a complex of workings in a former uranium mine situated within a metamorphic rock complex in the most radon-prone area in Poland. The facility has been equipped with a mechanical ventilation system, which is turned on after the closing time and at the end of the working day for the visitor service staff, i.e. after 6 p.m. Short-term radon activity concentration changes along the Underground Educational Tourist Route in the Old Uranium Mine in Kletno are related to the activity of the facility's mechanical ventilation. Its inactivity in the daytime results in the fact that the highest values of (222)Rn activity concentration are observed at the time when the facility is open to visitors, i.e. between 10 a.m. and 6 p.m. The improper usage of the mechanical ventilation system is responsible for the extremely unfavourable working conditions, which persist in the facility for practically all year. The absence of appropriate radiological protection

  6. SHRIMP U-Pb zircon dating for granitoids from the Strzegom-Sobótka Massif, SW Poland: Constraints on the initial time of Permo-Mesozoic lithosphere thinning beneath Central Europe

    Science.gov (United States)

    Turniak, Krzysztof; Mazur, Stanisław; Domańska-Siuda, Justyna; Szuszkiewicz, Adam

    2014-11-01

    New SHRIMP II data from the Strzegom-Sobótka composite granitoid intrusion show a successive emplacement of four magma batches with different modal compositions over the period of c. 10-15 m.y. The first emplaced was the two-mica granite that crystallised at 304.8 ± 2.7 Ma. This was followed by the biotite granodiorite the three samples of which were dated at 301.9 ± 3.6, 299.3 ± 2.4, and 297.9 ± 3.7 Ma, respectively. The biotite and hornblende-biotite granites yielded practically an identical age, 301.1 ± 2.7 Ma, 297.7 ± 2.2 Ma, and 297.1 ± 3.0 Ma, but are considered slightly younger based on the field cross-cutting relationships. The final rock type is the Łażany granodiorite dated at 294.4 ± 2.7 Ma. The temperature estimates along with the zircon crystal morphology show the gradual but significant rise of magma temperature with the decreasing age of intrusion. The temperature increased from c. 720 °C in the two-mica granite to 740-780 °C in the biotite granodiorite and 800-860 °C in the biotite-hornblende granites and Łażany granodiorite. Based on the ages obtained, the emplacement of the Strzegom-Sobótka granitoids immediately followed the cessation of compression in the Variscan externides of SW Poland. Moreover, the intrusion was synchronous with rapid uplift of the Variscides and abundant bimodal volcanism in the nearby intramontane troughs. Consequently, the gradual heating of the crust, as recorded by the data acquired, must have been caused by thermal influx into the lower crust related to the ascent of basaltic magmas. Since the latter were probably formed during the decompressional melting of lithospheric mantle, the emplacement of Strzegom-Sobótka granitoids, along with bimodal volcanism, signalled the commencement of lithospheric thinning beneath Central Europe.

  7. The Sidi Mohamed peridotites (Edough Massif, NE Algeria ...

    Indian Academy of Sciences (India)

    The Hercynian Edough massif is the easternmost crystalline massif of the Algerian coast. It consists of two tectonically superposed units composed of micaschists, gneisses, and peridotite. This study concentrates on the small and isolated Sidi Mohamed peridotite outcrop area (0.03 km2). The Sidi Mohamed peridotite.

  8. The Sidi Mohamed peridotites (Edough Massif, NE Algeria ...

    Indian Academy of Sciences (India)

    The Hercynian Edough massif is the easternmost crystalline massif of the Algerian coast. It consists of two tectonically superposed units composed of micaschists, gneisses, and peridotite. This study concentrates on the small and isolated Sidi Mohamed peridotite outcrop area (0.03 km2). The Sidi Mohamed peridotite is ...

  9. Ultrabasic Spring Geomicrobiology of the Cedars Peridotite

    Science.gov (United States)

    Johnson, O. J.; Morrill, P.; Muyzer, G.; Kuenen, J. G.; Nealson, K. H.

    2006-12-01

    Peridotite hosted aquifers are becoming well-known as a modern analog for both extraterrestrial and early- Earth habitats despite relatively few studies on microbes in ultramafic systems. To investigate the microbiology associated with aquifers of the actively serpentinizing Cedars Peridotite in coastal Northern California an interdisciplinary approach involving molecular phylogenetics, organic and inorganic geochemistry, as well as culture-based ecophysiological methods are being utilized. Based on our findings, Cedars spring microorganisms endure one of the harshest low-temperature aqueous environments on Earth with pH greater than 11.8, Eh less than -600 mV, undetectable dissolved CO2 and O2 and a lack of other obvious e- acceptors. Despite these conditions, life inhabits solid substrate surfaces within the springs to a concentration of 10E6-10E7 cells/sq. cm, but planktonic cell densities are extremely low (much less than 10E3/ml). Preliminary 16S data of 3 ultrabasic fluids reveals a community comprised primarily of bacteria that appears to be of low-diversity. Methanogens are strongly suggested to be present based on the isotopic composition of methane bubbling from the springs, but have not yet been identified via molecular techniques. Community level metagenomic sequencing of the ultrabasic spring microorganisms sampled from peridotite-associated mineral surfaces and glass slides incubated in specially designed flow- through chambers are currently in-progress and are likely to reveal several novel metabolic pathways.

  10. The SW Sex enigma

    OpenAIRE

    Dhillon, V. S.; Smith, D. A.; Marsh, T. R.

    2012-01-01

    The SW Sex stars are a class of cataclysmic variables, originally identified because they shared a number of enigmatic properties – most notably, single-peaked emission lines instead of the double-peaked lines one would expect from their high-inclination accretion discs. We present high-time-resolution spectrophotometry of the eclipsing nova-like variables SW Sex and DW UMa, two of the founding members of the SW Sex class. Both systems show single-peaked Balmer and He II λ4686 Å emission line...

  11. Structural petrology of the garnet-peridotite of Alpe Arami (Ticino, Switzerland)

    NARCIS (Netherlands)

    Möckel, J.R.

    1969-01-01

    The decomposition of pyrope-rich garnet into spinel-amphibole symplektite and the alteration of the latter into chlorite indicate the presence of three successive mineral parageneses in the peridotite of Alpe Arami: a garnet-peridotite, a spinelamphibole-peridotite, and a chlorite-peridotite

  12. Constraints on the depth and thermal history of cratonic lithosphere from peridotite xenoliths, xenocrysts and seismology

    Science.gov (United States)

    Mather, Kathy A.; Pearson, D. Graham; McKenzie, Dan; Kjarsgaard, Bruce A.; Priestley, Keith

    2011-07-01

    Despite the relatively long-standing availability of numerical approaches for estimating palaeogeotherms using peridotite xenolith Pressure-Temperature (P-T) data, the practise of fitting xenolith P-T arrays to simple models of lithospheric heat generation, in a non-quantitative manner, remains widespread. The lack of quantification in both the magnitude and uncertainty of heat flow and lithosphere thickness estimates leads to difficulty in evaluating proposed models for lithosphere evolution on a local and regional scale. Here, we explore the advantages of using a numerical approach to palaeogeotherm fitting, in terms of the ability to make objective comparisons of the effect that differing thermobarometer combinations and varying states of mineral and textural equilibrium have on the shape of the palaeogeotherm, and the resulting estimates of lithospheric thickness and heat flow. We also make quantitative comparisons between lithospheric mantle properties estimated using peridotite xenoliths versus single mineral xenocrysts. Using two reference peridotite xenolith databases from Bultfontein (S. Africa) and Somerset Island (Canada) we show that the same lithospheric mantle properties are predicted using harzburgite versus lherzolite thermobarometry methods. Filtering mineral data for the effects of inter-mineral disequilibrium does not produce significantly different palaeogeotherms but does increase the quality of fit of the palaeogeotherm to the P-T data, allowing more confidence to be placed in comparisons between locations. Palaeogeotherms calculated using xenocryst data, screened for peridotitic affinities, show misfits that are 2-3 times greater than those obtained using xenoliths. Lithospheric properties calculated from the Somerset Island xenocryst-based geotherm yield results that are within error of the xenolith estimate. A mutually consistent and quantitative palaeogeotherm fitting approach is used to evaluate existing hypotheses for the evolution of

  13. Natural Carbonation of Peridotite and Applications for Carbon Storage

    Science.gov (United States)

    Streit, E.; Kelemen, P.; Matter, J.

    2009-05-01

    Natural carbonation of peridotite in the Samail Ophiolite of Oman is surprisingly rapid and could be further enhanced to provide a safe, permanent method of CO2 storage through in situ formation of carbonate minerals. Carbonate veins form by low-temperature reaction between peridotite and groundwater in a shallow weathering horizon. Reaction with peridotite drives up the pH of the water, and extensive travertine terraces form where this groundwater emerges at the surface in alkaline springs. The potential sink for CO2 in peridotite is enormous: adding 1wt% CO2 to the peridotite in Oman could consume 1/4 of all atmospheric carbon, and several peridotite bodies of comparable size exist throughout the world. Thus carbonation rate and cost, not reservoir size, are the limiting factors on the usefulness of in situ mineral carbonation of peridotite for carbon storage. The carbonate veins in Oman are much younger than previously believed, yielding average 14C ages of 28,000 years. Age data plus estimated volumes of carbonate veins and terraces suggest 10,000 to 100,000 tons per year of CO2 are consumed by these peridotite weathering reactions in Oman. This rate can be enhanced by drilling, hydraulic fracture, injecting CO2-rich fluid, and increasing reaction temperature. Drilling and hydraulic fracture can increase volume of peridotite available for reaction. Additional fracture may occur due to the solid volume increase of the carbonation reaction, and field observations suggest that such reaction-assisted fracture may be responsible for hierarchical carbonate vein networks in peridotite. Natural carbonation of peridotite in Oman occurs at low pCO2, resulting in partial carbonation of peridotite, forming magnesite and serpentine. Raising pCO2 increases carbonation efficiency, forming of magnesite + talc, or at complete carbonation, magnesite + quartz, allowing ˜30wt% CO2 to be added to the peridotite. Increasing the temperature to 185°C can improve the reaction rate by

  14. Garnet peridotites from Pohorje: Petrography, geothermobarometry and metamorphic evolution

    Directory of Open Access Journals (Sweden)

    Mirijam Vrabec

    2010-06-01

    Full Text Available Ultrahigh-pressure (UHP metamorphism has been recorded in Eo-Alpine garnet peridotites from the PohorjeMts., Slovenia, belonging to the Eastern Alps. The garnet peridotite bodies are found within serpentinized metaultrabasitesin the SE edge of Pohorje and are closely associated with UHP kyanite eclogites. These rocks belongto the Lower Central Austroalpine basement unit of the Eastern Alps, exposed in the proximity of the Periadriaticfault system.Garnet peridotites show signs of a complex four-stage metamorphic history. The protolith stage is represented bya low-P high-T assemblage of olivine + Al-rich orthopyroxene + Al-rich clinopyroxene + Cr-spinel. Due to metamorphism,primary clinopyroxene shows exsolutions of garnet, orthopyroxene, amphibole, Cr-spinel and ilmenite. TheUHP metamorphic stage is defined by the assemblage garnet + olivine + Al-poor orthopyroxene + clinopyroxene +Cr-spinel. Subsequent decompression and final retrogression stage resulted in formation of kelyphitic rims aroundgarnet and crystallization of tremolite, chlorite, serpentine and talc.Pressure and temperature estimates indicate that garnet peridotites reached the peak of metamorphism at 4 GPaand 900 °C, that is well within the UHP stability field. Garnet peridotites in the Pohorje Mountains experiencedUHP metamorphism during the Cretaceous orogeny and thus record the highest-pressure conditions of all Eo-Alpinemetamorphism in the Alps.

  15. The SW Sex enigma

    Science.gov (United States)

    Dhillon, V. S.; Smith, D. A.; Marsh, T. R.

    2013-02-01

    The SW Sex stars are a class of cataclysmic variables, originally identified because they shared a number of enigmatic properties - most notably, single-peaked emission lines instead of the double-peaked lines one would expect from their high-inclination accretion discs. We present high-time-resolution spectrophotometry of the eclipsing nova-like variables SW Sex and DW UMa, two of the founding members of the SW Sex class. Both systems show single-peaked Balmer and He ii λ4686 Å emission lines that appear to originate from a region in the disc that lies close to, but downstream of, the bright spot. The emission-line light curves are consistent with the finding from X-ray and ultraviolet observations that we predominantly see the flared disc rim and the unobscured back portion of the disc in these systems. In DW UMa, the He ii λ4686 Å emission line originates from close to the white dwarf and exhibits flaring. Such flares have been used to argue for magnetically channelled accretion, as in the intermediate polars, but the lack of a clear periodicity in the flares argues for a simpler model in which we are viewing the central regions of the disc through the non-uniform upper edge of a flared disc rim. We also observe narrow, blueshifted, transient absorption features in the Balmer lines of DW UMa, which we attribute to blobs of material ejected from the system, possibly by a magnetic propeller, that happen to be passing between us and the binary. Our results suggest that the solution to the SW Sex enigma is a combination of dominant bright-spot emission and a self-occulting disc. We also propose a simplified classification scheme for nova-like variables.

  16. SW21 Summary Report

    Energy Technology Data Exchange (ETDEWEB)

    Juarez, A. [Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)

    2016-02-10

    Los Alamos and Lawrence Livermore National Laboratories hosted the tenth annual Strategic Weapons in the 21st Century Conference (SW21) on 21 January 2016 to reinforce the national commitment to leadership and institutional excellence for nuclear deterrence. The event has been successful over the years in drawing together a diverse, high-level group of policy makers and experts from multiple disciplines to engage in informed dialogue on topics related to strategic weapons in national and international security.

  17. Geochemistry of abyssal peridotites from the super slow-spreading ...

    Indian Academy of Sciences (India)

    (2006) proposed an avolcanic, or nearly avolcanic mode of seafloor spreading which may be analogous to processes at the ocean-continent transition of continental margins. (Whitmarsh et al. 2001), and which appears to have created nearly half of the oceanic crust in the. SWIR. Abyssal peridotite compositions can provide ...

  18. Crustal Signatures in Mantle Peridotites From Yakutian Kimberlites

    Science.gov (United States)

    Taylor, L. A.; Spetsius, Z.; Wiesli, R.; Anand, M.; Valley, J.

    2002-12-01

    Peridotites and eclogites are considered as the original hosts for diamonds in the mantle. However, it is now generally agreed that these "mantle" eclogites from kimberlites had their origin in the subduction of oceanic crust beneath the major cratons of the world. One of the first indications for such crustal protoliths was from studies of oxygen and carbon isotopes (e.g., Peter Deines and colleagues, Ian McGregor, as well as our group). Indeed, subsequent studies of such rocks have revealed several additional crustal signatures. A possible scenario involves the subduction of an ophiolite sequence, whereby the basaltic and lower mafic components were metamorphosed, devolatilized/partially melted, and otherwise transformed into eclogites. Being within the diamond-stability field, they later experience metasomatic diamond formation. Surprisingly, the closely associated diamondiferous peridotites are considered to be of original mantle origin. We pose the query: What became of the ultramafic portion at the bottom of the crustal sequence? Could this be the origin of at least some of the mantle peridotites? The restricted δ13C values for P-type (peridotitic) diamonds is commonly used as evidence for the mantle origin of peridotites. However, a compilation of δ13C data, published by Peter Deines and our group, for P-type diamonds, mainly from numerous south African pipes, also shows a significant number of values that are well below the mantle field (to -20 \\permil). Fresh, clean garnets were carefully selected from over a hundred peridotites collected from several Yakutian kimberlites. These were subjected to oxygen-isotope analyses by laser-fluorination at the University of Wisconsin. The majority of the δ18O values plot within the accepted mantle value of 5.5+/-0.4 \\permil (Mattey et al., 1994). However, a significant number (~20%) lies outside this window, both above and below. These values are interpreted to represent the effects of both high- and low

  19. Carbon Dioxide Removal from Air using Seafloor Peridotite

    Science.gov (United States)

    Kelemen, P. B.; Brandt, A. R.; Benson, S. M.

    2016-12-01

    We describe a method for Carbon Dioxide Removal from Air (CDR) using CO2 uptake via mineral carbonation, about half the cost of that proposed by Kelemen & Matter [1,2]. Reaction of CO2-bearing fluids and gases with peridotite rapidly forms inert, non-toxic carbonate minerals. In proposed methods for combined capture and storage of ambient CO2 via reaction of seawater or ground water with peridotite [1-5], return of depleted water to the surface draws down CO2 from air. Because they use available chemical and thermal energy that drive spontaneous natural reactions, they may be the least expensive methods for capture of CO2 from air. We focus on subsurface CO2 uptake during flow of surface water through fractured peridotite. Previously [1-3], we envisioned a design similar to enhanced geothermal systems (EGS), involving two large diameter boreholes, subject to the challenges of achieving rapid, efficient return flow that limit the success of EGS. Recent discussions yielded a less expensive, more robust design: A single well produces ambient, CO2-depleted pore water from seafloor peridotite. Such water has low carbon and high pH [6,7,8]. Where such waters are delivered to the surface, observations reveal rapid CO2 uptake from air [1,3,8-10]. Delivery to the sea surface would also reduce local acidification. Thermal buoyancy and pumps powered by wave and tidal energy would bring warm formation water from wells to the surface through conduits surrounded by colder seawater. Recharge would be via flow in natural or enhanced fracture networks in unconfined submarine aquifers. This method could be tested and scaled-up in coastal, sub-seafloor peridotite with onshore drilling off Oman, New Caledonia and Papua New Guinea, Spain, Morocco, USA, etc. It is possible to achieve much larger scale. Giant volumes of peridotite are exposed on the seafloor along slow-spreading mid-ocean ridges [3]. Robotic drills could install wells that deliver CO2-depleted water through fabric tubes

  20. Petrofabrics, microtextures and dislocation substructures of olivine in a peridotite mylonite (Alpe Arami, Switzerland)

    NARCIS (Netherlands)

    Buiskool Toxopeus, J.M.A.

    1978-01-01

    The development of preferred crystallographic orientation and dimensional fabric of olivine in relation to deformation were investigated in a thin, continuous chlorite peridotite mylonite rim around the garnet peridotite body of Alpe Arami, Ticino, Switzerland. The mylonite is a foliated rock

  1. Mantle depletion and metasomatism recorded in orthopyroxene in highly depleted peridotites

    DEFF Research Database (Denmark)

    Scott, James; Liu, Jingao; Pearson, D. Graham

    2016-01-01

    Although trace element concentrations in clinopyroxene serve as a useful tool for assessing the depletion and enrichment history of mantle peridotites, this is not applicable for peridotites in which the clinopyroxene component has been consumed (~ 25% partial melting). Orthopyroxene persists in ...

  2. Serpentinization: Getting water into a low permeability peridotite

    Science.gov (United States)

    Ulven, Ole Ivar

    2017-04-01

    Fluid consuming rock transformation processes occur in a variety of settings in the Earth's crust. One such process is serpentinization, which involves hydration of ultramafic rock to form serpentine. With peridotite being one of the dominating rocks in the oceanic crust, this process changes physical and chemical properties of the crust at a large scale, increases the amount of water that enters subduction zones, and might even affect plate tectonics te{jamtveit}. A significant number of papers have studied serpentinization in different settings, from reaction fronts progressing over hundreds of meters te{rudge} to the interface scale fracture initiation te{pluemper}. However, the process represents a complicated multi-physics problem which couples external stress, mechanical deformation, volume change, fracture formation, fluid transport, the chemical reaction, heat production and heat flow. Even though it has been argued that fracture formation caused by the volume expansion allows fluid infiltration into the peridotite te{rudge}, it remains unclear how sufficient water can enter the initially low permeability peridotite to pervasively serpentinize the rock at kilometre scale. In this work, we study serpentinization numerically utilizing a thermo-hydro-mechanical model extended with a fluid consuming chemical reaction that increases the rock volume, reduces its density and strength, changes the permeability of the rock, and potentially induces fracture formation. The two-way coupled hydromechanical model is based on a discrete element model (DEM) previously used to study a volume expanding process te{ulven_1,ulven_2} combined with a fluid transport model based on poroelasticity te{ulven_sun}, which is here extended to include fluid unsaturated conditions. Finally, a new model for reactive heat production and heat flow is introduced, to make this probably the first ever fully coupled chemo-thermo-hydromechanical model describing serpentinization. With this model

  3. Homogeneous Solution for SW Lacertae

    Directory of Open Access Journals (Sweden)

    Kyungjoo Kim

    1996-06-01

    Full Text Available We have analyzed collected photoelectric light curves for light variations of SW Lac. The method of Fourier analysis was adopted to quantify the light variation from season to season. We found the linear relation between the Fourier coefficient, B1 and the magnitude difference between two maxima. The total light of the system has been decreased as much as 0m.04 during approximately 20 years time interval. Photoelectric parameters including spot parameters for all light curves were obtained by the method of the Wilson and Devinney differential correction in order to secure the variations of parameters from season to season. SW Lac, not like RS CVn type stars, required to adjust all parameters as well as spot parameters for a reasonable fit to the observations of each epoch. A surface temperature of cooler star is one of the most sensitive parameters to affect a shape of light curve of SW Lac. We conclude that the shape of light curve of SW Lac varies even during one season as well as season to season. The light curve is mainly caused by inhomogeneous surface temperature due to strong chromospheric activity of the system.

  4. New field evidence for the emplacement of the Ronda peridotite

    Science.gov (United States)

    Bessière, Eloïse; Romagny, Adrien; Jolivet, Laurent; Augier, Romain; Savastano, Lucia

    2017-04-01

    The Betic-Rif orogen forms the westernmost part of the Alpine orogenic system and results from the closure of the Tethys Ocean between Africa and the Iberian Peninsula. Subduction and crustal thickening leading to the formation of high-pressure and low-temperature (HP/LT) metamorphic complexes were followed by a late-orogenic extension stage in an overall convergent setting. Plate kinematic reconstructions indeed reveal a continuous convergence between Africa and Eurasia from Late Cretaceous times currently characterized by slow convergence rates that add in complex ways with body forces stored during crustal thickening stages and subsequently released during crustal thinning. If this large-scale scenario is now broadly admitted, some first order questions remain opened. Among these questions, the timing and kinematics of the emplacement of the Ronda or Beni Bousera peridotite massifs remain particularly unclear. Due to the numerous published early Miocene ages, the emplacement of the Ronda or the Beni Bousera massifs is classically considered a very fast event before the high-temperature event. In this scenario, peridotite bodies are emplaced by overthrusting onto the continental crust within a compressional context. Based on new detailed field observations along the contact between the Ronda peridotites and the high-temperature continental basement and high-temperature marbles of the Dorsale Unit, as well as a metamorphic petrology approach, we reconsider this interpretation. We argue that this contact could instead be an early detachment, possibly active during the Mesozoic or before. A few old ages found in the western part of the chain could indeed be linked with such an episode of extreme thinning. This event is consistent with the opening of the Tethyan Ocean and associated with oceanization in the eastern part of the chain. In this work, we will argue for an emplacement as old as the Triassic, at least, thus much older than the Miocene thrusting event. This

  5. To understand Poland / Joanna Bar

    Index Scriptorium Estoniae

    Bar, Joanna

    2003-01-01

    Uurimustest Poola igapäevaelu kohta Nõukogude perioodil : Wedel, Janine. The private Poland : an anthropologist look at everyday life ; Dziğiel, Leszek. Paradise in a concrete cage : daily life in communist Poland. Krak̤w, 1998

  6. Systematics of melt stagnation in peridotites from the Godzilla Megamullion

    Science.gov (United States)

    Loocke, M.; Snow, J. E.; Ohara, Y.

    2010-12-01

    The Godzilla Megamullion (GM) Massif is the largest known example of an Oceanic Core Complex (OCC) or the exhumed footwall of a low angle-large offset oceanic detachment fault. It lies on the extinct Parece Vela Rift spreading center within the Parece Vela Back-arc Basin of the Philippine Sea. This has thus allowed for sampling of a young back-arc mantle section. Sampling of the massif has returned a dominantly ultramafic lithology, divided petrographically into depleted, fertile, and melt-percolated groups (1). Petrographic analysis of the extant peridotite thin section collection found that 44% of all GM peridotites (71 out of 161) exhibit evidence of plagioclase impregnation compared to the worldwide abyssal peridotite average of ~20% (2). The mullion is divided up into three regions, the proximal region ( closest to termination of spreading), the medial region, and the distal region (furthest from the termination of spreading)(3).Observations by region provide that 53% ( 62 out of 116 samples) in the proximal region (15 dredges), 12% ( 2 out of 17 samples) in the medial mullion (3 dredges), and 25% (7 out of 28) in the distal mullion (5 dredges) show of evidence of plagioclase impregnation (4). Major element analyses of spinels were completed using the Cameca SX-50 Electron Microprobe facility at the University of Houston. The Cr# [100 x Cr/(Cr + Al)] ranges from 10 to 65 with TiO2 concentrations ranging from less than 0.01 up to 1.6 wt%. When the Cr#s of the samples are plotted along the massif, a pattern of melt depletion exists that is consistent with the degree of plagioclase impregnation. In the distal region, Cr#s start at around an average of 35 and range up to 65 for melt percolated samples. In the medial region, a drop off in Cr# of about 1 Cr# per kilometer is observed with the trend bottoming out at around a Cr# of 10. In the proximal region, Cr#s closer to the medial region are observed as having more fertile values of around 20 but are found

  7. Rates of mineral dissolution and carbonation in peridotite and basalt

    Science.gov (United States)

    Kelemen, P. B.; Matter, J. M.

    2009-12-01

    We study natural rates and processes of mineral carbonation in peridotite (olivine-rich rock) in mantle rocks exposed to weathering in northern Oman to learn effective mechanisms from natural processes, and seek ways to accelerate them to achieve significant CO2 capture and storage via mineral carbonation at the lowest possible cost. In our first paper (1), we fit data on mantle olivine carbonation from the DOE Albany Research Center (2,3, ARC). These data, and data from Arizona State University (4, ASU) suggest that a peridotite rock volume heated to 185°C and infused with H2O+CO2 at PCO2 > 75 bars could consume ~ 1 ton CO2 per cubic meter of rock per year. Because it is more abundant than peridotite, other workers focus on carbonation of the most common type of lava on Earth, basalt, whose main mineral constituent is generally labradorite, part of the plagioclase feldspar solid solution series. Our intuition is that labradorite carbonation is much slower than mantle olivine carbonation. To quantify this, we compiled data on dissolution of mantle olivine, labradorite, crystalline basalt, and basaltic glass in aqueous fluids, as well as data on mantle olivine carbonation. The dissolution data are calibrated as a function of surface area (i.e., grain size and shape) and pH, as well as temperature, whereas most of the ARC and ASU experiments were done at a single pH and grain size. Thus, for comparison, we calculated dissolution rates for 70 micron spheres at pH 8, close to the ARC and ASU experimental conditions. At these conditions, olivine carbonation observed by ARC and ASU is 100 to 1000 times faster than labradorite and crystalline basalt, and faster than conventionally measured olivine dissolution rates. The ARC and ASU experiments were different from conventional dissolution experiments in several ways that could lead to an enhancement in olivine reaction rates: (a) they may have lower a(Mg) in fluid due to solid MgCO3 (magnesite) precipitation, (b) they

  8. Poland- Ukraine Relations

    Directory of Open Access Journals (Sweden)

    Andrzej Szeptycki

    2016-01-01

    Full Text Available Poland and Ukraine are the two biggest and most populated countries of Central and Eastern Europe. Because of their size, neighbourhood and position in the region the two countries have often been compared to France and Germany. Both countries are deeply interested in their mutual cooperation. Such situation steams from five factors: direct neighbourhood, common (albeit difficult history, attractiveness of the Polish labour market for the Ukrainians, membership of Poland in the Western structures, and last but not least, the Russian threat. Despite complimentary interests, both countries have difficulty to effectively develop their mutual relations and turn them into a real “strategic partnership”. These problems are due to the internal political and economic situation in Ukraine, limits imposed by the membership of Poland in the EU, Russian policy aiming at keeping Ukraine within its zone of influence and, finally, the EU reluctance to effectively engage in Ukraine.

  9. Shrub expansion in SW Greenland

    DEFF Research Database (Denmark)

    Jørgensen, Rasmus Halfdan

    of firewood collection. A delayed reaction to the ending of the little ice age cannot be excluded, but seems rather unlikely considering other studies from Greenland. Effects of global warming in SW Greenland must be studied over even longer time periods than the 120 years of the current study. To answer......, and has a range of ecosystem effects where it occurs. Shrub expansion has to a large extend been attributed to increasing temperatures over the past century, while grazing and human disturbance have received less attention. Alnus viridis ssp. crispa is a common arctic species that contributes...... by factors like grazing and human disturbance; II. which climatic factors control shrub growth in SW Greenland and whether these have improved sufficiently over the past century to allow shrub expansion; III. whether growth of A. viridis is promoted by experimental warming; IV. and whether plant genotypes...

  10. Water Management in Poland

    Directory of Open Access Journals (Sweden)

    Wojciech Majewski

    2015-03-01

    Full Text Available This paper presents the current situation in Polish water resources management. Discussed here are measures taken by the Ministry of Environment to introduce a new water law, as well as reforms of water management in Poland. The state of water resources in Poland are described, and the actions needed to improve this situation, taking into account possible climate changes and their impact on the use of water resources. Critically referred to is the introduction by the Ministry of Environment of charges for water abstraction by hydro power plants, and adverse effects for the energy and water management sectors are discussed.

  11. [Rural migration in Poland].

    Science.gov (United States)

    Rakowski, W

    1985-01-01

    Migration of the rural population in Poland from 1946 to 1983 is analyzed, with a focus on rural-urban migration. Consideration is given to regional variations in migration patterns, the causes of migration, and the impact of migration on areas of origin.

  12. South Africa and Poland

    African Journals Online (AJOL)

    kirstam

    The typology of countries, namely those with innovation-driven, efficiency-driven and factor-/resource-driven ... Switzerland, Norway, Australia, Japan, Singapore, Taiwan, Qatar, Puerto Rico,. Tobago and Trinidad ... of the cultures and values of two countries, namely South Africa and Poland, on entrepreneurial intentions ...

  13. Seawater-derived rare earth element addition to abyssal peridotites during serpentinization

    Science.gov (United States)

    Frisby, Carl; Bizimis, Michael; Mallick, Soumen

    2016-04-01

    Serpentinized abyssal peridotites are evidence for active communication between the Earth's hydrosphere and the upper mantle, where exchange and retention of both major and trace elements occur. Bulk rock Nd isotopes in serpentinized abyssal peridotites imply interaction of seawater with the peridotite. In contrast, the Nd isotopes of clinopyroxenes from serpentinized abyssal peridotites retain their primary magmatic signature. It is currently unclear if, how and where seawater-derived Nd and other REE are being added or exchanged with the mantle peridotite minerals during serpentinization. To remedy this knowledge gap, we present in situ trace and major element concentrations, bulk rock and sequential leaching experiment trace element concentrations as well as Nd, Sr isotope data on refertilized and depleted serpentinized abyssal peridotites from the Southwest Indian Ridge. The secondary serpentine matrix and magnetite veins in these peridotites have elevated LREE concentrations, with variable negative Ce anomalies and large Rb, Sr, Pb and U enrichments that resemble seawater trace element patterns. The LREE concentrations in the serpentine phase are higher than those expected for the primary mantle mineralogy (olivine, orthopyroxene) based on data from relic clinopyroxenes and equilibrium partition coefficients. These data are consistent with seawater-derived REE addition to the peridotite during serpentinization. The bulk rocks have more radiogenic Sr and more unradiogenic Nd isotopes than their clinopyroxene (up to 8 εNd units lower than clinopyroxene). Sequential leaching experiments designed to mobilize secondary carbonates and Fe-oxides show even more unradiogenic Nd isotope ratios in the leachates than the bulk rock and clinopyroxene, approaching seawater compositions (up to 15 εNd units lower than clinopyroxene). Mass balance calculations using trace elements or Nd isotopes suggest that up to 30% of the bulk peridotite Nd budget is of seawater origin and

  14. POLAND AT CERN

    CERN Multimedia

    2000-01-01

    17 to 20 October 2000 Administration Building Bldg 60 - 1st floor 09h00 - 17h30 (Friday 09h00-12h00) POLAND AT CERN Twenty companies will present their latest technology at the «Poland at CERN» exhibition. The Polish industries will exhibit products and technologies, which are specifically related to the field of particle physics. The main subjects are: cryogenics and vacuum technologies, electric power and power electronics, heavy mechanical components, small and precision machined mechanical components, instrumentation, electrical and mechanical, electronics and software, power-control and fibre optic cables. The exhibition is being organised by the Technology Transfer Agency, Techtra Ltd under the auspices of the National Atomic Energy Agency, the State Committee for Scientific Research and the Ministry of the Economy. There follows: - the list of exhibitors. A detailed programme will be available in due course at: - your Divisional Secretariat, - the Reception information desk, buildin...

  15. Poland syndrome with absent ribs

    Directory of Open Access Journals (Sweden)

    Rupam Kumar Ta

    2014-01-01

    Full Text Available Poland syndrome is a rare congenital disorder characterized by ipsilateral absence of pectoralis major muscle. This syndrome is associated with various anomalies such as ipsilateral syndactyly, brachidactyly, dextrocardia, herniation of lung, underdevelopment of upper ribs, aplasia or hypoplasia of breast, etc. Only few cases had been reported with absent ribs in Poland syndrome. We report a rare case of Poland syndrome presented to us with mal-development of his right hemithorax and weakness of right hand.

  16. Soybean diseases in Poland

    Directory of Open Access Journals (Sweden)

    J. Marcinkowska

    2013-12-01

    Full Text Available Field observations on the occurrence of soybean diseases were undertaken in the southern and central regions of Poland in the period 1976-1980. Most prevalent were foliage diseases caused by Peronospora manshurica, Pseudomonas syrinqae pv. glycinea and soybean mosaic virus (SMV. Sclerotinia sclerotiorum and Ascochyta sojaecola were reported as pathogens of local importance. The following pathogenic fungi: Botrytis cinerea, Fusarium culmorum, F. oxysporum and Rhizoctonia solani were also isolated from soybean.

  17. [Migrant vaccinations in Poland].

    Science.gov (United States)

    Sakowski, Piotr

    2012-01-01

    After the European Union accession in 2004, Poland has been perceived by foreigners as an attractive destination of their migration, and also as a popular transit country for people going further to the Western Europe countries. The Nofer Institute of Occupational Medicine is involved in the implementation of the international project PROMOVAX (Promote Vaccinations among Migrant Populations in Europe). The objective of the project is to promote immunizations among migrant populations in Europe. This article presents the up-to-date legal regulations that are effective in Poland, taking into account their relevance to the issue of vaccinations in migrant population. The analysis of the Polish legislation concerning this problem shows that there are no specific regulations addressed to migrant population staying in our country. This issue seems to be popular in the European Union, where immunization of migrants is given high priority. From the point of view of health care professionals it is important to be aware of the fact that EU open borders favor the increased flow of people between countries. The scale of migration from outside the EU to its member states also contributes to the increase in potential contacts between health care workers and migrants working in Poland.

  18. Shrub expansion in SW Greenland

    DEFF Research Database (Denmark)

    Jørgensen, Rasmus Halfdan

    , and has a range of ecosystem effects where it occurs. Shrub expansion has to a large extend been attributed to increasing temperatures over the past century, while grazing and human disturbance have received less attention. Alnus viridis ssp. crispa is a common arctic species that contributes...... including only undisturbed sites. Shrub cover increased most on E and SE facing slopes, in sites with stable substrate, in areas characterised by human disturbance and in areas without muskoxen grazing. Aspect and human disturbances had the strongest effect on shrub expansion, followed by muskoxen...... locations. A. viridis represents an interesting case to study these effects. SW Greenland is a subarctic to low-arctic region with only limited increases in temperatures during the past decades, and observed climate trends being largely dependent on the observation period. In this region there is limited...

  19. The aluminum-in-olivine thermometer for mantle peridotites - Experimental versus empirical calibration and potential applications

    Science.gov (United States)

    Bussweiler, Y.; Brey, G. P.; Pearson, D. G.; Stachel, T.; Stern, R. A.; Hardman, M. F.; Kjarsgaard, B. A.; Jackson, S. E.

    2017-02-01

    This study provides an experimental calibration of the empirical Al-in-olivine thermometer for mantle peridotites proposed by De Hoog et al. (2010). We report Al concentrations measured by secondary ion mass spectrometry (SIMS) in olivines produced in the original high-pressure, high-temperature, four-phase lherzolite experiments by Brey et al. (1990). These reversed experiments were used for the calibration of the two-pyroxene thermometer and Al-in-orthopyroxene barometer by Brey and Köhler (1990). The experimental conditions of the runs investigated here range from 28 to 60 kbar and 1000 to 1300 °C. Olivine compositions from this range of experiments have Al concentrations that are consistent, within analytical uncertainties, with those predicted by the empirical calibration of the Al-in-olivine thermometer for mantle peridotites. Fitting the experimental data to a thermometer equation, using the least squares method, results in the expression: This version of the Al-in-olivine thermometer appears to be applicable to garnet peridotites (lherzolites and harzburgites) well outside the range of experimental conditions investigated here. However, the thermometer is not applicable to spinel-bearing peridotites. We provide new trace element criteria to distinguish between olivine from garnet-, garnet-spinel-, and spinel-facies peridotites. The estimated accuracy of the thermometer is ± 20 °C. Thus, the thermometer could serve as a useful tool in settings where two-pyroxene thermometry cannot be applied, such as garnet harzburgites and single inclusions in diamond.

  20. GEOTHERMAL WATERS IN POLAND

    OpenAIRE

    Chrzan, T.

    2006-01-01

    This study presents the role of the geothermal waters mainly for the municipal heating, greenhouses, swimming pools, etc. Presently, two types of geothermal waters are used in the world. Waters of the temperatures higher than 130oC (steam) used mostly to drive turbines in geothermal power plants. Waters of low temperatures (20oC to 100oC) are used as a direct energy carrier for the municipal heating systems. The geothermal waters in Poland are presented in this paper.

  1. Electrical conductivity of mantle peridotite at the uppermost lower mantle condition

    Energy Technology Data Exchange (ETDEWEB)

    Yoshino, T; Katsura, T; Yamazaki, D; Ito, E, E-mail: tyoshino@misasa.okayama-u.ac.j [Institute for Study of the Earth' s Interior, Okayama University, 827 Yamada, Misasa, Tottori 682-1093 (Japan)

    2010-03-01

    Electrical conductivity of mantle peridotite was measured at 25 GPa and temperature up to 1800 K in a Kawai-type multi-anvil apparatus. The starting material was gel with a composition of fertile spinel lherzolite (KLB1). After the conductivity measurement, mineral phases of run products are composed of magnesium silicate perovskite, ferro-periclase and Ca perovskite. The conductivity value of the peridotite is distinctly higher than those of post-spinel and magnesian silicate perovskite with a composition of (Mg{sub 0.9},Fe{sub 0.1})SiO{sub 3}, but lower than that of ferro-periclase. Both absolute values and change in activation enthalpy for the conductivity of the mantle peridotite are similar to those for the silicate perovskite. A presence of aluminous perovskite with substantial amount of ferric iron in crystal structure would enhance bulk conductivity of the lower mantle.

  2. Geochronological Constraints on the Exhumation and Emplacement of Subcontinental Lithospheric Mantle Peridotites in the Westernmost Mediterranean

    Science.gov (United States)

    Garrido, Carlos J.; Hidas, Károly; Marchesi, Claudio; Varas-Reus, María Isabel; Booth-Rea, Guillermo

    2017-04-01

    Exhumation of subcontinental mantle peridotite in the Western Mediterranean has been attributed to different tectonic processes including pure extension, transpression, or alternating contractive and extensional processes related with continental subduction followed by extension, before final their contractive intracrustal emplacement. Any model trying to explain the exhumation and emplacement of subcontinental lithospheric mantle peridotites in the westernmost Mediterranean should take into account the available geochronological constraints, as well as the petrological and geochemical processes that lead to internal tectono-magmatic zoning so characteristic of the Betic and Rif orogenic peridotites. Different studies have suggested a Hercynian, Cenozoic-Mesozoic or an Alpine age for the late tectono-magmatic evolution and intra-crustal emplacement of Betic-Rif peridotites. The pervasive presence of Mesozoic U-Pb zircon ages in Ronda UHP and HP garnet pyroxenites does not support a Hercynian age for the intracrustal emplacement of the peridotite. A hyper-extended margin setting for is in good agreement with the Jurassic extensional event that pervasively affected ALKAPECA terrains (i.e. the Alboran, Kabylides, Peloritani, and Calabria domains) in the western Mediterranean due to the opening of the Piemonte-Ligurian Ocean. However, a Jurassic age and a passive margin tectonic setting do not account, among other observations, for the late Miocene thermochronological ages recorded in zircons rims (U-Pb) and garnets (Lu-Hf) in garnet pyroxenites from the Betic-Rif peridotites, the pervasive Miocene resetting of U-Pb zircon and monazite ages in the overlying Jubrique crustal section, the supra-subduction radiogenic signature of late pyroxenite intrusive dikes in the Ronda peridotite, and the arc tholeiitic affinity of late mantle-derived, gabbroic dykes intruding in the Ronda and Ojen plagioclase lherzolites. These data are more consistent with a supra

  3. Mantle peridotite in newly discovered far-inland subduction complex, southwest Arizona: Initial report

    Science.gov (United States)

    Haxel, Gordon B.; Jacobson, Carl E.; Wittke, James H.

    2015-01-01

    The latest Cretaceous to early Palaeogene Orocopia Schist and related units are generally considered a low-angle subduction complex that underlies much of southern California and Arizona. A recently discovered exposure of Orocopia Schist at Cemetery Ridge west of Phoenix, Arizona, lies exceptionally far inland from the continental margin. Unexpectedly, this body of Orocopia Schist contains numerous blocks, as large as ~300 m, of variably serpentinized mantle peridotite. These are unique; elsewhere in the Orocopia and related schists, peridotite is rare and completely serpentinized. Peridotite and metaperidotite at Cemetery Ridge are of three principal types: (1) serpentinite and tremolite serpentinite, derived from dunite; (2) partially serpentinized harzburgite and olivine orthopyroxenite (collectively, harzburgite); and (3) granoblastic or schistose metasomatic rocks, derived from serpentinite, made largely of actinolite, calcic plagioclase, hercynite, and chlorite. In the serpentinite, paucity of relict olivine, relatively abundant magnetite (5%), and elevated Fe3+/Fe indicate advanced serpentinization. Harzburgite contains abundant orthopyroxene, only slightly serpentinized, and minor to moderate (1–15%) relict olivine. Mantle tectonite fabric is locally preserved. Several petrographic and geochemical characteristics of the peridotite at Cemetery Ridge are ambiguously similar to either abyssal or mantle-wedge (suprasubduction) peridotites and serpentinites. Least ambiguous are orthopyroxene compositions. Orthopyroxene is distinctively depleted in Al2O3, Cr2O3, and CaO, indicating mantle-wedge affinities. Initial interpretation of field and petrologic data suggests that the peridotite blocks in the Orocopia Schist subduction complex at Cemetery Ridge may be derived from the leading corner or edge of a mantle wedge, presumably in (pre-San Andreas fault) southwest California. However, derivation from a subducting plate is not precluded.

  4. Mantle-derived peridotites in southwestern Oregon: relation to plate tectonics.

    Science.gov (United States)

    Medaris, L G; Dott, R H

    1970-09-04

    A group of peridotites in southwestern Oregon contains high-pressure mineral assemblages reflecting recrystallization at high temperatures (1100 degrees to 1200 degrees C) over a range of pressure decreasing from 19 to 5 kilobars. It is proposed that the peridotites represent upper-mantle material brought from depth along the ancestral Gorda-Juan de Fuca ridge system, transported eastward by the spreading Gorda lithosphere plate, and then emplaced by thrust-faulting in the western margin of the Cordillera during late Mesozoic time.

  5. The upper mantle can be fractured: Cataclasitic peridotite xenolith from Ichinomegata crater, the Northeast Japan arc

    Science.gov (United States)

    Takeuchi, Miyuki; Arai, Shoji

    2013-04-01

    A peculiar peridotite xenolith with cataclastic texture was found from Ichinomegata crater, Megata volcano, the Northeast Japan arc, one of the most famous mantle peridotite xenolith localities (e.g., Kuno, 1967; Takahashi, 1978). The peridotite xenoliths that show strong deformation textures, well-known as "sheared lherzolites", have been reported from kimberlite xenoliths. Mylonitic peridotites have been documented in several localities (e.g., Basu, 1977; Kaeser et al., 2006), and some of them are interpreted to have been derived from ductile shear zones in the upper mantle (e.g., Xu et al., 1993). The texture of the Ichinomegata peridotite discussed here is totally different from these deformed xenoiths. Coarse mineral grains are angular and rarely kinked, but never elongated. Some of coarse olivine grains are split and displaced. Fragmented grains of pyroxenes and chromian spinel are elongated to form thin streaks. It has the same mineral assemblage as ordinary peridotite xenoliths from Ichinomegata, and is totally free of serpentine and other low-temperature alteration minerals. Coarse minerals are equivalent in mineral chemistry to weakly hydrated lherzolites reported from Ichinomegata (Abe et al., 1992). Fo (100 Mg/(Mg + Fe)) of olivine is around 90, and chromian spinel shows a low Cr/(Cr + Al) ratio, around 0.2. Estimated temperaturesfrom coarse pyroxene grains are in the range of 910-1000°C (Wells, 1977; Witt-Eickschen & Seck, 1991), which are the same as in ordinary Ichinomegata peridotites. On the other hand, some of fine-grained minerals (less than 50 μm) have different chemical characteristics from ordinary xenoliths. Fine-grained olivine show relatively high Fo (91 - 93) and CaO content (0.1 - 0.3 wt%). Pyroxenes show a wide range of the Mg/(Mg + Fe) ratio and Al2O3 content. Especially the CaO content of pyroxenes is higher in orthopyroxene, lower in clinopyroxene than in coarse grained pyroxenes, indicating some higher temperatures. From the

  6. Poland and Global Threats

    Science.gov (United States)

    Kleer, Jerzy

    2016-01-01

    This essay seeks to present the specifics of global threats, as well as the reasons for them being universal in nature, and for their persistence. A certain classification of the threats is also engaged in. At the same time, an attempt is made to show the specific threats present - irrespective of their global counterparts - in different regions, and even in different states. The genesis and nature of the latter are demonstrated in a somewhat ad hoc manner by reference to the threats considered to face Poland. If the global threats are truly universal, and arise out of the changes taking place around the world in the last half-century (primarily around the twin phenomena of globalisation and the information revolution), a specific reverse kind of situation applies to decolonisation, plus the collapse of the communist system and the transformation into market economies that apply to formerly communist countries. Equally, some at least of the threats facing Poland may have even a longer history, given that they are very much influenced by past economic and political development, as well as the dominant cultural system.

  7. Liandratite from Karkonosze pegmatites, Sudetes, Southwestern Poland

    Science.gov (United States)

    Matyszczak, Witold

    2017-11-01

    The chemical composition of liandratite, U6+(Nb,Ta)2O8, was determined from material collected in Niobium, Yttrium, Fluorine type (NYF) pegmatites of the Karkonosze intrusion (Sudetes, SW Poland). Liandratite occurs mainly as rims, up to 40 µm thick, and fracture infillings in fergusonite-(Y) and other Nb-Ta-Ti minerals. Its formation was related to the fluid-driven alteration of primary minerals by three potential mechanisms: (i) direct replacement of a primary mineral by liandratite; (ii) breakdown of the primary mineral to liandratite and a product with the composition of minerals of the pyrochlore group; (iii) multistage alteration, which involved: removal of A-site cations (mostly Y + REE with the exception of U4+) and formation of phases with the composition of pyrochlore group minerals; then crystallization of U-, Bi-, Pb-rich pyrochlores and their replacement by liandratite. The chemical compositions of liandratite formed by the breakdown of different primary minerals are also different, mainly in their U, Ti and Nb contents. Excess Ti, relative to the U6+Nb2O8 end-member, is incorporated into the structure together with additional U. The Ti content of liandratite, and partially through this the U content, are dependent on the nature of the precursor mineral.

  8. Carbonatite melt-peridotite interaction at 5.5-7.0 GPa: Implications for metasomatism in lithospheric mantle

    Science.gov (United States)

    Sokol, Alexander G.; Kruk, Alexey N.; Chebotarev, Dimity A.; Palyanov, Yury N.

    2016-04-01

    Interaction between carbonatite melt and peridotite is studied experimentally by melting samples of interlayered peridotite-carbonatite-peridotite in graphite containers at 1200-1350 °C and 5.5-7.0 GPa in a split-sphere multianvil apparatus. Starting compositions are lherzolite and harzburgite, as well as carbonatite which may form in the upper part of a slab or in a plume-related source. Most experimental runs were of 150 h duration in order for equilibrium to be achieved. The interaction produced carbonatitic melts with low SiO2 (≤ 7 wt.%) and high alkalis. At 1200 °C, melt-peridotite interaction occurs through Mg-Ca exchange, resulting in elimination of orthopyroxene and crystallization of magnesite and clinopyroxene. At 1350 °C hybridization of the carbonatite and magnesite-bearing peridotite melts occurred with consumption of clinopyroxene and magnesite, and crystallization of orthopyroxene at MgO/CaO ≥ 4.3. The resulting peridotite-saturated melt has Ca# (37-50) depending on primary carbonatite composition. Compositions of silicate phases are similar to those of high-temperature peridotite but are different from megacrysts in kimberlites. CaO and Cr2O3 changes in garnet produced from the melt-harzburgite interaction at 1200 and 1350 °C perfectly match the observed trend in garnet from metasomatized peridotite of the Siberian subcontinental lithospheric mantle. K-rich carbonatite melts equilibrated with peridotite at 5.5-7.0 GPa and 1200-1350 °C correspond to high-Mg inclusions in fibrous diamond. Carbonatite melt is a weak solvent of entrained xenoliths and therefore cannot produce kimberlitic magma if temperatures are ~ 1350 °C on separation from the lithospheric peridotite source and ~ 1000 °C on eruption.

  9. Hazardous Waste Test Methods / SW-846

    Science.gov (United States)

    The Resource Conservation and Recovery Act Test Methods for Evaluating Solid Waste: Physical/Chemical Methods (SW-846) provide guidance to analytical scientists, enforcement officers and method developers across a variety of sectors.

  10. Laboratory Characterization of Solid Grade SW Brick

    National Research Council Canada - National Science Library

    Williams, Erin M; Akers, Stephen A; Reed, Paul A

    2007-01-01

    Personnel of the Geotechnical and Structures Laboratory, U.S. Army Engineer Research and Development Center, conducted a laboratory investigation to characterize the strength and constitutive property behavior of solid Grade SW brick...

  11. POLAND AT CERN

    CERN Multimedia

    2000-01-01

    17 to 20 October 2000 Administration Building Bldg 60 - 1st floor 09h00 - 17h30 (Friday 09h00-12h00) OPENING CEREMONY 10h00 - 17 October Nineteen companies will present their latest technology at the “Poland at CERN” exhibition. The Polish industries will exhibit products and technologies, which are specifically related to the field of particle physics. The main subjects are: cryogenics and vacuum technologies, electric power and power electronics, heavy mechanical components, small and precision machined mechanical components, instrumentation, electrical and mechanical, electronics and software, power-control and fibre optic cables. The exhibition is being organised by the Technology Transfer Agency, Techtra Ltd under the auspices of the National Atomic Energy Agency, the State Committee for Scientific Research and the Ministry of the Economy. There follows: the list of exhibitors. A detailed programme will be available in due course at: your Divisional Secretariat, the Reception information desk, b...

  12. POLAND AT CERN

    CERN Multimedia

    2000-01-01

    17 to 20 October 2000 Administration Building Bldg 60 - 1st floor 09h00 - 17h30 (Friday 09h00-12h00) OPENING CEREMONY 10h00 - 17 October Nineteen companies will present their latest technology at the “Poland at CERN” exhibition. The Polish industries will exhibit products and technologies, which are specifically related to the field of particle physics. The main subjects are: cryogenics and vacuum technologies, electric power and power electronics, heavy mechanical components, small and precision machined mechanical components, instrumentation, electrical and mechanical, electronics and software, power-control and fibre optic cables. The exhibition is being organised by the Technology Transfer Agency, Techtra Ltd under the auspices of the National Atomic Energy Agency, the State Committee for Scientific Research and the Ministry of the Economy. There follows: the list of exhibitors. A detailed programme will be available in due course at: your Divisional Secretariat, the Reception information desk, bu...

  13. POLAND AT CERN

    CERN Multimedia

    2000-01-01

    17 to 20 October 2000 Administration Building Bldg 60 - 1st floor 09h00 - 17h30 (Friday 09h00-12h00) Twenty companies will present their latest technology at the ´Poland at CERNª exhibition. The Polish industries will exhibit products and technologies, which are specifically related to the field of particle physics. The main subjects are: cryogenics and vacuum technologies, electric power and power electronics, heavy mechanical components, small and precision machined mechanical components, instrumentation, electrical and mechanical, electronics and software, power-control and fibre optic cables. The exhibition is being organised by the Technology Transfer Agency, Techtra Ltd under the auspices of the National Atomic Energy Agency, the State Committee for Scientific Research and the Ministry of the Economy. There follows: - the list of exhibitors. A detailed programme will be available in due course at: - your Divisional Secretariat, - the Reception information desk, building 33, - the exhi...

  14. [Emigration from Poland].

    Science.gov (United States)

    Fassmann, H

    1998-01-01

    "Apart from Ireland and Italy Poland belongs to the ¿classical' emigration countries of the 19th and 20th century. Due to economical and political factors a considerable number of Poles left their country.... Spread over many countries on several continents the emigrants established a Polish diaspora and developed a national feeling that is...[connected] with the Polish culture and the Polish ¿community'. The existence of ethnic networks structures characterized the Polish emigration also after 1989/90. Political and ethnic factors become thereby less important in comparison with economical push- and pull-factors. This leads to an emigration of qualified people who get jobs in the urban labour markets of Western Europe in private households, and in the building trade, sometimes under precarious circumstances." (EXCERPT)

  15. Melt-peridotite reactions in upwelling EM1-type eclogite bodies

    DEFF Research Database (Denmark)

    Søager, Nina; Holm, Paul Martin

    2013-01-01

    the Payenia volcanic province (34–38 °S) in Argentina, for which Sr, Nd and double-spike Pb isotope ratios are presented, and from other north Patagonian volcanic fields may provide details of the eclogite melt–peridotite reactions taking place in the melting column of an upwelling OIB-type mantle...

  16. The force of crystallization and fracture propagation during in-situ carbonation of peridotite

    NARCIS (Netherlands)

    van Noort, Reinier; Wolterbeek, Timotheus K.T.; Drury, Martyn R.; Kandianis, Michael T.; Spiers, Christopher J.

    2017-01-01

    Subsurface mineralization of CO2 by injection into (hydro-)fractured peridotites has been proposed as a carbon sequestration method. It is envisaged that the expansion in solid volume associated with the mineralization reaction leads to a build-up of stress, resulting in the opening of further

  17. Origin of garnet and clinopyroxene in Kaapvaal low-T peridotite xenoliths

    NARCIS (Netherlands)

    Simon, N.S.C.; Irvine, G.J.; Davies, G.R.; Pearson, D.G.; Carlson, R.W.

    2003-01-01

    A detailed petrographic, major and trace element and isotope (Re-Os) study is presented on 18 xenoliths from Northern Lesotho kimberlites. The samples represent typical coarse, low-temperature garnet and spinel peridotites and span a P-T range from ∼60 to 150 km depth. With the exception of one

  18. Genetics Home Reference: Poland syndrome

    Science.gov (United States)

    ... located in the right side of the chest (dextrocardia). Rarely, chest and hand abnormalities resembling those of ... NH, Keum DY, Kim YH. Rare combination of dextrocardia with right-sided Poland syndrome. Ann Thorac Surg. ...

  19. Probing Upper Mantle Heterogeneity: Os and Pb Isotopic Compositions of Individual Sulfide Grains in Abyssal Peridotites

    Science.gov (United States)

    Warren, J. M.; Shirey, S. B.

    2008-12-01

    Abyssal peridotites from mid-ocean ridges are unique samples of the depleted upper mantle that can be used to understand a variety of processes from melting and melt extraction to the compositional evolution of the interior of the earth. Traditional work on abyssal peridotites has focused on either bulk rock compositions or on the compositions of clinopyroxenes, which are the main repository of trace elements in these rocks. However, recent (e.g., Alard et al., 2000; Luguet et al., 2003; Harvey et al., 2006) and previous (Meijer, 1980; Morgan, 1985) works on peridotites have indicated that Fe-Ni-Cu sulfides, present at trace levels in abyssal peridotites, may contain a significant proportion of both the Pb and Os budget of the upper mantle. As the isotopic compositions of Pb and Os provide important information about the long term evolution of the mantle, analysis of single sulfide grains can provide unique information not available from basalt or whole-rock peridotite studies: the spatial scale is small compared to basaltic melt sampling, adjacent silicate mineralogy can be evaluated, and secondary sulfide and alteration minerals can be avoided. Thus, while sulfides represent chalcopyrite. We have adapted single grain sulfide techniques from studies of sulfide inclusions in diamonds, to allow us to extract Os, Pb and transition metals from sulfides down to 5 μg. Os concentrations in pentlandites are ~0.4-5 ppm, 2-3 orders of magnitude higher than bulk rock abyssal peridotite concentrations. In contrast, chalcopyrites, associated with veins in the peridotites, do not contain measurable quantities of Os. Preliminary Pb data indicates that pentlanditic sulfides have Pb concentrations close to ~9 ppm. 187Os/188Os isotopic compositions range from 0.1209 to 0.1278 in sulfides away from hotspots, typical of depleted mantle and in agreement with the depleted Sr and Nd isotopic composition of clinopyroxenes from the same samples. To date, we have not found any anomalously

  20. Negative CO2 emissions via subsurface mineral carbonation in fractured peridotite

    Science.gov (United States)

    Kelemen, P. B.; Matter, J.

    2014-12-01

    Uptake of CO2 from surface water via mineral carbonation in peridotite can be engineered to achieve negative CO2 emissions. Reaction with peridotite, e.g., CO2 + olivine (A), serpentine (B) and brucite (C), forms inert, non-toxic, solid carbonates such as magnesite. Experimental studies show that A can be 80% complete in a few hours with 30 micron powders and elevated P(CO2) [1,2,3]. B is slower, but in natural systems the rate of B+C is significant [4]. Methods for capture of dilute CO2 via mineral carbonation [4,5,6,7] are not well known, though CO2 storage via mineral carbonation has been discussed for decades [8,9]. Where crushed peridotite is available, as in mine tailings, increased air or water flow could enhance CO2 uptake at a reasonable cost [4,5]. Here we focus on enhancing subsurface CO2 uptake from surface water flowing in fractured peridotite, in systems driven by thermal convection such as geothermal power plants. Return of depleted water to the surface would draw down CO2 from the air [6,7]. CO2 uptake from water, rate limited by flow in input and output wells, could exceed 1000 tons CO2/yr [7]. If well costs minus power sales were 0.1M to 1M and each system lasts 10 years this costs oil industry. Uptake of 1 Gt CO2/yr at 1000 t/well/yr requires 1M wells, comparable to the number of producing oil and gas wells in the USA. Subsurface CO2 uptake could first be applied in coastal, sub-seafloor peridotite with onshore drilling. Sub-seafloor peridotite is extensive off Oman, New Caledonia and Papua New Guinea, with smaller amounts off Spain, Morocco, USA, etc. This would be a regional contribution, used in parallel with other methods elsewhere. To achieve larger scale is conceivable. There is a giant mass of seafloor peridotite along slow-spreading mid-ocean ridges. Could robotic drills enhance CO2 uptake at a reasonable cost, while fabric chimneys transport CO2-depleted water to the sea surface? Does anyone know James Cameron's phone number? [1] O

  1. Symphytocarpus trechisporus (Myxogastrea in Poland

    Directory of Open Access Journals (Sweden)

    Salamaga Agnieszka

    2014-12-01

    Full Text Available Symphytocarpus trechisporus (Berk. ex Torrend Nann.-Bremek. is rare in Poland, known previously from only one locality. Sixty years after the original report, this paper presents two new localities of it in separate regions of Poland. Although S. trechisporus is recorded mostly on Sphagnum sp., the taxon does not seem to be attached to a specific substrate; rather it is associated with acidic habitats.

  2. Paragenesis of Diamond and Minerals of Peridotites and Carbonatites in the Mantle Magma Chambers Based on Experiments Data

    Science.gov (United States)

    Kuzyura, Anastasia; Simonova, Dariya; Litvin, Yury

    2014-05-01

    It is considered that role of carbonate melts is important in processes of mantle metasomatism; according to other representations, it is also assumed that they could be formed at partial melting of carbonated peridotite. Dissolving of peridotite minerals and carbon in carbonate melts are responsible for formation of completely miscible carbonate-silicate-carbon magmas parental for diamonds. It can be expected that such carbonate magmas are capable to assimilate an form parental magama "chambers" within the hosting mantle peridotite. While natural cooling of the chambers dissolved in carbonate melts components of the peridotite crystallize forming minerals similar to these of the host mantle peridotite. The recrystallized peridotite minerals are fragmentarily included hermetically within growing diamonds and occur as syngenetic inclusions in them. Therefore experimental modeling of origin of the upper mantle carbonate-silicate diamond-forming melts, their consolidations in the magmatic chambers and evolutions at conditions of equilibrium and fractional crystallization are especially significant for understanding of processes of deep magmatic petrology and genetic mineralogy, including genesis of diamond. In the study at 6 GPa model approximations of mineral phases, significant in compositions of probable metasomatic agents, the upper mantle peridotites, and also syngenetic inclusions in diamonds were used: starting mixtures were model peridotite with composition Ol48Opx16Cpx16Grt20, close to model compositions of the primitive mantle and real mantle xenolithes, as well as multicomponent carbonate (CaCO3)20(Na2CO3)20(FeCO3)20(Na2CO3)20(K2CO3)20 modeling carbonatite inclusions in natural diamonds. Spectral pure graphite was used as a source of carbon in the system. Pressure and temperature were reached using apparatus of toroidal type 'anvil-with-hole'. Electron microprobe and SEM researches were carried out on the polished surfaces with carbon covering at IEM RAS

  3. Abiotic Methane in Land-Based Serpentinized Peridotites: New Discoveries and Isotope Surprises

    Science.gov (United States)

    Whiticar, M. J.; Etiope, G.

    2014-12-01

    Until 2008, abiotic methane in land-based serpentinized ultramafic rocks was documented (including gas and C- and H- isotope compositions) only at sites in Oman, Philippines, New Zealand and Turkey. Methane emanates from seeps and/or hyperalkaline water springs along faults and is associated with molecular hydrogen. These were considered to be very unusual and rare occurrences of gas. Now, methane is documented for peridotite-based springs or seeps (in ophiolites, orogenic massifs or intrusions) in US, Canada, Costa Rica, Greece, Italy, Japan, New Caledonia, Portugal, Spain and United Arab Emirates. Gas flux measurements are indicating that methane can also flux as invisible microseepages from the ground, through fractured peridotites, even far removed from seeps and springs. Methane C-isotope ratios range from -6 to -37 permil (VPDB) for dominantly abiotic methane. The more 13-C depleted values, e.g., California, are likely mixed with biotic gas (microbial and thermogenic gas). Methane H-isotope ratios cover a wide range from -118 to -333 permil (VSMOW). The combination of C- and H-isotopes clearly distinguish biotic from abiotic methane. Radiocarbon (14-C) analysis from bubbling seeps in Italian peridotites indicate that the methane is fossil (pMC <0.2), i.e., older than 50,000 years, similar to the Chimaera seeps in Turkey. So, methane observed in the hyperalkaline waters cannot be produced in the same waters because these are only a few thousands years old. The low temperatures of land-based peridotites (generally <100 °C at depths of 3-4 km) also constrain methane production. We discuss some hypotheses concerning gas generation in water vs. dry systems, i.e., in deeper, older, waters or in unsaturated rocks). We also discuss low vs. high temperatures, i.e., at the present-day low T conditions or at higher temperatures eventually occurring in the early stages of peridotite emplacement on land.

  4. The roles of pyroxenite and peridotite in the mantle sources of oceanic basalts

    Science.gov (United States)

    Matzen, Andrew K.; Wood, Bernard J.; Baker, Michael B.; Stolper, Edward M.

    2017-07-01

    Subduction of oceanic crust generates chemical and lithological heterogeneities in the mantle. An outstanding question is the extent to which these heterogeneities contribute to subsequent magmas generated by mantle melting, but the answer differs depending on the geochemical behaviour of the elements under investigation: analyses of incompatible elements (those that preferentially concentrate into silicate melts) suggest that recycled oceanic crust is an important contributor, whereas analyses of compatible elements (those that concentrate in crystalline residues) generally suggest it is not. Recently, however, the concentrations of Mn and Ni--two elements of varying compatibility--in early-crystallizing olivines, have been used to infer that erupted magmas are mixtures of partial melts of olivine-rich mantle rocks (that is, peridotite) and of metasomatic pyroxene-rich mantle rocks (that is, pyroxenite) formed by interaction between partial melts of recycled oceanic crust and peridotite. Here, we test whether melting of peridotite alone can explain the observed trend in olivine compositions by combining new experimental data on the partitioning of Mn between olivine and silicate melt under conditions relevant to basalt petrogenesis with earlier results on Ni partitioning. We show that the observed olivine compositions are consistent with melts of fertile peridotite at various pressures--importantly, melts from metasomatic pyroxenites are not required. Thus, although recycled materials may well be present in the mantle source regions of some basalts, the Mn and Ni data can be explained without such a contribution. Furthermore, the success of modelling the Mn-Ni contents of olivine phenocrysts as low-pressure crystallization products of partial melts of peridotite over a range of pressures implies a simple new approach for constraining depths of mantle melting.

  5. Shaping drug policy in Poland.

    Science.gov (United States)

    Malinowska-Sempruch, Kasia

    2016-05-01

    Poland, a post-socialist democracy with a high interest in successful integration with the European Union and a strong catholic tradition, currently has some of the most restrictive anti-drug laws in Europe. Structural violence towards drug users has intensified as a result of decades of shifting drug policies and, surprisingly, the more recent process of political and economic liberalization. This commentary considers the contextual and historical dynamics of drug policy-making in Poland. It traces transitions in Poland's drug control policy, throughout Poland's history as a soviet satellite state, under martial law, and in the democracy that it is today. This case study draws on an analysis of interviews with key actors and participant observations in combination with documents and archival records. This paper follows the changes in Poland's drug control policy, throughout Poland's history as a soviet satellite state, under martial law, and in the democracy that it is today. Factors contributing to the enactment of restrictive drug laws have occurred in a highly politicized context during a series of dramatic political transitions. Current drug policies are woefully inadequate for treating those in need of drug treatment and care as well as for preventing HIV and other harms linked to drug injecting. Copyright © 2016 Elsevier B.V. All rights reserved.

  6. Plagioclase-peridotites recording the incipient stage of oceanic basin formation: new constraints from the Nain ophiolites (central Iran)

    Science.gov (United States)

    Pirnia Naeini, Tahmineh; Arai, Shoji; Saccani, Emilio

    2016-04-01

    Pargasite-bearing plagioclase peridotites of Nain have recorded a complex tectono-magmatic and -metamorphic history. Based on texture, as well as mineral major and trace element chemistry, two stages of facies exchange have been documented in the peridotites, namely, from plagioclase to spinel and vice versa. The earliest event that influenced the peridotites was a low degree of flux melting (crystallized in-situ in the peridotites in form of plagioclase. After the melting stage, cooling caused the peridotites to recrystallize in spinel facies. Recrystallization obliterated all textural features associated with formation of magmatic plagioclase in the peridotites. However, lines of evidence are documented by the chemistry of the spinel-facies mineral assemblage, which strongly suggest the pre-existence of plagioclases. This evidence includes a positive Eu anomaly in pargasites and pyroxenes, as well as a Zr negative anomaly in orthopyroxenes. The spinel-facies assemblage subsequently recrystallized in the plagioclase stability field. Recrystallization occurred in various degrees. Strong recrystallization resulted in the formation of modally typical, but atypically enriched, harzburgite from the lherzolite. Remarkable textural characteristics of peridotites that indicate subsolidus origin for plagioclases include: (1) plagioclase heterogeneous distribution, (2) plagioclase exclusive concurrence with spinel and, (3) plagioclase modal positive correlation with olivine but negative correlation with pyroxenes and pargasite. The transition from spinel to plagioclase-facies was associated with the following compositional variations in the peridotite minerals: (1) Al, Mg, Ni decrease and Cr, Ti, Fe increase in spinel; (2) Al, Ca decrease and Cr, Ti increase in pyroxenes and pargasite; (3) slight overall increase in the concentration of rare earth elements and most trace elements in pyroxenes and pargasite, except for Eu and Sr for which a slight decrease is observed. The

  7. Records of upper mantle oxygen fugacity gleaned from high-density sampling of basalts and peridotites at ultraslow ridges

    Science.gov (United States)

    Birner, S.; Cottrell, E.; Warren, J. M.; Kelley, K. A.; Davis, F. A.

    2016-12-01

    Mantle oxygen fugacity (fO2) controls volatile speciation, phase stability, and the depth of the peridotite solidus, and is thus critical to our understanding of melt production at mid-ocean ridges. Both basalts [1] and peridotites [2] have been used as proxies for calculating upper mantle fO2 beneath ridges. Though the global peridotite dataset for fO2 is limited and does not overlap geographically with samples from the more comprehensive global basalt dataset, the average fO2 recorded by peridotites is lower than that recorded by basalts. Ultraslow spreading ridges such as the Southwest Indian Ridge (SWIR) and Gakkel Ridge have limited magma production due to thick conductive cooling lids at the ridge axis, and thus offer a unique opportunity to compare geographically overlapping suites of basalt and peridotite. In this study, we determined the oxygen fugacity of 41 peridotite samples from the Oblique Segment of SWIR and 10 peridotite samples from Gakkel - more than doubling the number of fO2 estimates for ridge peridotites globally. Our results for SWIR show that peridotite fO2 is highly variable on the dredge to sub-segment scale, ranging from 1.7 log units below the quartz-fayalite-magnetite buffer (QFM) to 1 log unit above QFM, with an average of QFM+0.2 (±0.6). We also calculated fO2 for 25 basalt glasses from the Oblique Segment, which have an average fO2 of QFM+0.3 (±0.1). Importantly, on average, we find no offset between mantle fO2 as recorded by basalts versus peridotites. However, fO2 recorded by basalts is significantly more homogenous than by peridotites, consistent with the idea of aggregate melts recording homogenization of a heterogeneous mantle. The most reduced peridotites at both ridges are generally highly refractory samples at high spinel Cr# (Cr# = Cr/(Cr+Al)) and low modal cpx. This suggests that the process of melt extraction may leave behind a reduced residue. Alternatively, if these highly refractory lithologies are residues from

  8. Poland health system review.

    Science.gov (United States)

    Sagan, Anna; Panteli, Dimitra; Borkowski, W; Dmowski, M; Domanski, F; Czyzewski, M; Gorynski, Pawel; Karpacka, Dorota; Kiersztyn, E; Kowalska, Iwona; Ksiezak, Malgorzata; Kuszewski, K; Lesniewska, A; Lipska, I; Maciag, R; Madowicz, Jaroslaw; Madra, Anna; Marek, M; Mokrzycka, A; Poznanski, Darius; Sobczak, Alicja; Sowada, Christoph; Swiderek, Maria; Terka, A; Trzeciak, Patrycja; Wiktorzak, Katarzyna; Wlodarczyk, Cezary; Wojtyniak, B; Wrzesniewska-Wal, Iwona; Zelwianska, Dobrawa; Busse, Reinhard

    2011-01-01

    Since the successful transition to a freely elected parliament and a market economy after 1989, Poland is now a stable democracy and is well represented within political and economic organizations in Europe and worldwide. The strongly centralized health system based on the Semashko model was replaced with a decentralized system of mandatory health insurance, complemented with financing from state and territorial self-government budgets. There is a clear separation of health care financing and provision: the National Health Fund (NFZ) the sole payer in the system is in charge of health care financing and contracts with public and non-public health care providers. The Ministry of Health is the key policy-maker and regulator in the system and is supported by a number of advisory bodies, some of them recently established. Health insurance contributions, borne entirely by employees, are collected by intermediary institutions and are pooled by the NFZ and distributed between the 16 regional NFZ branches. In 2009, Poland spent 7.4% of its gross domestic product (GDP) on health. Around 70% of health expenditure came from public sources and over 83.5% of this expenditure can be attributed to the (near) universal health insurance. The relatively high share of private expenditure is mostly represented by out-of-pocket (OOP) payments, mainly in the form of co-payments and informal payments. Voluntary health insurance (VHI) does not play an important role and is largely limited to medical subscription packages offered by employers. Compulsory health insurance covers 98% of the population and guarantees access to a broad range of health services. However, the limited financial resources of the NFZ mean that broad entitlements guaranteed on paper are not always available. Health care financing is overall at most proportional: while financing from health care contributions is proportional and budgetary subsidies to system funding are progressive, high OOP expenditures

  9. Mumps in Poland in 2012.

    Science.gov (United States)

    Rogalska, Justyna; Paradowska-Stankiewicz, Iwona

    2014-01-01

    Vaccination against mumps, introduced initially as recommended, from 2003 is mandatory in Poland and given as two dose scheme with MMR vaccine (mumps, measles, and rubella). Despite observed decline in mumps incidence for over a decade which is a result of conducted vaccinations, mumps is still a common childhood disease in Poland. To assess epidemiological situation of mumps in Poland in 2012, including vaccination coverage in Polish population, in comparison to previous years. The descriptive analysis was based on data retrieved from routine mandatory surveillance system and published in the annual bulletins "Infectious diseases and poisonings in Poland in 2012" and "Vaccinations in Poland in 2012" (Czarkowski MP i in., Warszawa 2013, NIZP-PZH i GIS). Mumps cases were classified according to the criteria of surveillance case definition implemented in the European Union (Commission Decision of 28 April 2008 amending Decision 2002/253/EC). National Immunisation Programme for year 2012 was also used. In total, there were 2779 mumps cases registered in Poland in 2012. Incidence of mumps was 7.2 per 100 000 and it was higher by 7.5% in comparison with 2011 and lower by 19.4% in comparison to median for the years 2006-2010. The highest incidence rate was observed among children aged 5 years (71.8 per 100 000). Incidence in women (5.9) was lower than in men (8.6). In 2012, 25 people were hospitalized due to mumps. Vaccination coverage of children aged 3 years in Poland in 2012 was 97.9%. Systematic execution of mumps vaccination in accordance with the National Immunisation Programme resulted in a significant decrease in the number of registered cases. Due to the high vaccination coverage further decline in the number of cases is expected.

  10. Nurse prescribing in Poland

    Science.gov (United States)

    Binkowska-Bury, Monika; Więch, Paweł; Bazaliński, Dariusz; Marć, Małgorzata; Bartosiewicz, Anna; Januszewicz, Paweł

    2016-01-01

    Abstract The aim of this study was to identify and examine the differences in opinions held by health care professionals and the general public concerning the right to administer and prescribe medication which has been awarded to nurses and midwives in Poland. The study was conducted from December 1, 2014 to July 1, 2015, in randomly selected primary health care clinics, among 2227 individuals, including 849 subjects representing medical personnel of primary health care and 1378 patients receiving primary care services. The study used 2 versions of a questionnaire. The relationships were examined with χ2 test for independence and Kruskal–Wallis test. Health professionals do not believe the new rights awarded to nurses and midwives will reduce the waiting time for medical consultations (P Nurses’ qualifications for the new tasks were most highly rated by patients, whereas the least favorable opinion was expressed by doctors (P nurse prescribing it is necessary to develop a suitable strategy enabling implementation of the government's initiative and facilitating the process of taking up the new task by nurses. PMID:27537573

  11. Orthodox Education in Poland

    Directory of Open Access Journals (Sweden)

    Antoni Mironowicz

    2016-12-01

    Full Text Available The Orthodox educational system has been meeting important tasks, which is raising a general mental level of clergy and faithful. Its foundation was driven by needs of the Orthodox Church. Educating a young generation in the spirit of the Orthodoxy happened to be the main task of the enlightened class. Brotherhood, monastery and parish school were to be part of this program. The Orthodox education shaped religious life, helped preserve the religious and national identity of the believers. An evidence of that is the fact, that only those localities preserved “the Greek faith “, in which next to the monasteries were schools. Higher education, and especially Mohyla Academy, shaped by the then elite, played a vital role in the history of Orthodox Church in the Republic and neighboring countries. A similar role had to play in the interwar period College of Orthodox Theology at the University of Warsaw and in post-war Orthodox Section of the Christian Academy of Theology Presented here outline of history of Orthodox education in Poland indicates to the, appreciated by clergy and hierarchy, need of development of theological schools. Theological schools played and still play important role in shaping the attitudes of clergy and faithful. Schools provide necessary pastoral resources, shape Orthodox cultural and scientific environment. Theological education has remained an essential element for the proper functioning of Orthodox Church in the Polish Republic.

  12. Implications of spinel compositions for the petrotectonic history of abyssal peridotite from Southwest Indian Ridge (SWIR)

    Science.gov (United States)

    Chen, T.; Jin, Z.; Wang, Y.; Tao, C.

    2012-12-01

    Abyssal peridotites generate at mid-ocean ridges. Lherzolite and harzburgite are the main rock types of peridotites in the uppermost mantle. The lherzolite subtype, less depleted and less common in ophiolites, characterizes mantle diapirs and slow-spreading ridges. Along the Earth's mid-ocean ridges, abyssal peridotites undergo hydration reactions to become serpentinite minerals, especially in slow to ultraslow spreading mid-ocean ridges. Spinel is common in small quantities in peridotites, and its compositions have often been used as petrogenetic indicators [1]. The Southwest Indian Ridge (SWIR) is one of the two ultraslow spreading ridges in the world. The studied serpentinized peridotite sample was collected by the 21st Voyage of the Chinese oceanic research ship Dayang Yihao (aka Ocean No. 1) from a hydrothermal field (63.5°E, 28.0°S, and 3660 m deep) in SWIR. The studied spinels in serpentinized lherzolite have four zones with different compositions: relic, unaltered core is magmatic Al-spinels; micro- to nano- sized ferrichromite zoned particles; narrow and discontinuous magnetite rim; and chlorite aureoles. The values Cr# of the primary Al-spinels indicate the range of melting for abyssal peridotites from SWIR extends from ~4% to ~7% [2]. The alteration rims of ferrichromite have a chemical composition characterized by Fe enrichment and Cr# increase indicating chromite altered under greenschist-amphibolite facies. Magnetites formed in syn- and post- serpentinization. Chlorite (clinochlore) formed at the boundary and crack of spinel indicating it had undergone with low-temperature MgO- and SiO2-rich hydrothermal fluids [3]. It suggests that serpentinized lherzolite from SWIR had undergone poly-stage hydration reactions with a wide range of temperature. Acknowledgments: EMPA experiment was carried out by Xihao Zhu and Shu Zheng in The Second Institute of Oceanography and China University of Geosciences, respectively. The work was supported by NSFC

  13. Variations in Oxygen Fugacity among Forearc Peridotites from the Tonga Trench

    Science.gov (United States)

    Birner, S.; Warren, J. M.; Cottrell, E.; Lopez, O. G.; Davis, F. A.; Falloon, T.

    2013-12-01

    The Tonga subduction zone is an extension-dominated, non-accreting convergent plate margin in the South Pacific, characterized by rapid slab rollback [1]. It is unusual among subduction zones in that forearc peridotites, thought to be pieces of lithospheric mantle originating from the overriding plate, have been dredged from the trench. These spinel peridotites appear in dredges along almost 1000 km of the trench's length, from near the Samoa hotspot in the north to the Louisville seamounts in the south, and have been dredged from 4-9 km depth. The samples are very depleted, consisting entirely of dunites and harzburgites, with no observed lherzolites. Low modal abundances of orthopyroxene and high spinel Cr# (Cr/(Cr+Al)) also indicate large degrees of melt extraction. While some samples have been variably altered by hydrothermal processes, a large fraction of them are remarkably unaltered, making them ideal targets for geochemical investigation. Oxygen fugacity is an important geochemical control on phase stability, the composition of volatiles, and the position of the mantle solidus, thus rendering it critical to the understanding of mantle processes. Previous studies have suggested that subduction zone processes result in arc magmas with increased oxygen fugacity (fO2) relative to ridge magmas [2], but few direct observations of mantle wedge fO2 are available. In order to investigate the oxygen fugacity of the Tonga peridotites, mineral major element compositions were determined via electron microprobe. Fe3+/ΣFe ratios were calculated for the spinel phase, calibrated with spinel standards of known Fe3+/ΣFe ratio provided by B.J. Wood to the Smithsonian following the procedure of Lopez et al [3]. Oxygen fugacity was calculated according to the olivine-orthopyroxene-spinel oxybarometer method of Wood et al. [4]. Results from five dredges along approximately 600 km of trench showed oxygen fugacity values of 1 log unit above the QFM buffer, compared to the global

  14. Geostatistical analysis of morphometric features in the selected parts of the Sudetes (SW Poland)

    Science.gov (United States)

    Pawlowski, Lukasz; Szymanowski, Mariusz; Migon, Piotr

    2017-04-01

    Recent years have brought rapid development of quantitative techniques that are successfully applied in geomorphology. They open up new interpretation possibilities, even in seemingly very well recognized areas. In particular, we are talking about the geomorphometric and geostatistical techniques whose integration in Geographic Information Systems allows to look at the spatial pattern of landforms and process signatures from a new perspective. The morphology of the Sudetes, as of other mountain ranges in central Europe, is the result of protracted interaction of tectonic and surface processes, passive geological factors such as lithology and structure, and passage of time. This raises the question whether, and to which extent, these different controls and signals have resulted in similarities or differences in the morphometric structure of different parts within the same mountain range. In this paper we assume that geomorphic signals of various origins are expressed by a set of primary and secondary topographic attributes, which can be further analyzed as regional variables and modelled using geostatistical methods. Special attention is paid to variogram modelling. This method allows the identification of the spatial structure of the morphometric characteristics, its spatial scale and direction reflected in quantitative parameters of variograms (model functions, range, sill, nugget, anisotropy). This parameters for various areas are compared to find (dis-)similarities between different parts of the Sudetes. Thus, the main goals of the paper are: 1. To evaluate the usefulness of topographic attributes' variogram modelling for quantification of the spatial morphometric structure of mountain areas, on the example of medium-altitude, non-glaciated mountain terrain. 2. To compare different parts of the Sudetes to find similarities and differences between them and to interpret the findings through the examination of geology and geomorphology of the region. The analysis includes four test areas of contrasting relief: elevated surfaces of low relief, inselbergs, cuestas and tablelands for which the set of primary (e.g. absolute and relative height, slope inclination, curvature) and secondary (e.g. topographic wetness (TWI), ruggedness (TRI) and position indices (TPI)) attributes is derived from a 10-m resolution DEM.

  15. Remote Sensing Data in Wind Velocity Field Modelling: a Case Study from the Sudetes (SW Poland)

    Science.gov (United States)

    Jancewicz, Kacper

    2014-06-01

    The phenomena of wind-field deformation above complex (mountainous) terrain is a popular subject of research related to numerical modelling using GIS techniques. This type of modelling requires, as input data, information on terrain roughness and a digital terrain/elevation model. This information may be provided by remote sensing data. Consequently, its accuracy and spatial resolution may affect the results of modelling. This paper represents an attempt to conduct wind-field modelling in the area of the Śnieżnik Massif (Eastern Sudetes). The modelling process was conducted in WindStation 2.0.10 software (using the computable fluid dynamics solver Canyon). Two different elevation models were used: the Global Land Survey Digital Elevation Model (GLS DEM) and Digital Terrain Elevation Data (DTED) Level 2. The terrain roughness raster was generated on the basis of Corine Land Cover 2006 (CLC 2006) data. The output data were post-processed in ArcInfo 9.3.1 software to achieve a high-quality cartographic presentation. Experimental modelling was conducted for situations from 26 November 2011, 25 May 2012, and 26 May 2012, based on a limited number of field measurements and using parameters of the atmosphere boundary layer derived from the aerological surveys provided by the closest meteorological stations. The model was run in a 100-m and 250-m spatial resolution. In order to verify the model's performance, leave-one-out cross-validation was used. The calculated indices allowed for a comparison with results of former studies pertaining to WindStation's performance. The experiment demonstrated very subtle differences between results in using DTED or GLS DEM elevation data. Additionally, CLC 2006 roughness data provided more noticeable improvements in the model's performance, but only in the resolution corresponding to the original roughness data. The best input data configuration resulted in the following mean values of error measure: root mean squared error of velocity = 1.0 m/s and mean absolute error of direction = 30°. The author concludes that, within specific meteorological conditions (relatively strong and constant synoptic forcing) and using the aforementioned input data, the Canyon model provides fairly acceptable results. Similarly, the quality of the presented remote sensing data is suitable for wind velocity modelling in the proposed resolution. However, CLC 2006 land use data should be first verified with a higher-resolution satellite or aerial imagery.

  16. Rare and threatened pondweed communities in anthropogenic water bodies of Opole Silesia (SW Poland

    Directory of Open Access Journals (Sweden)

    Arkadiusz Nowak

    2011-01-01

    Full Text Available The paper presents results of geobotanic studies conducted in anthropogenic water bodies like excavation ponds, fish culture ponds, other ponds, dam reservoirs, ditches, channels and recreational pools incl. watering places in Opole Silesia and surroundings in the years 2002-2005. The research focused on occurrence of threatened and rare pondweed communities. As the result of the investigations of several dozen of water bodies, 28 localities of rare pondweed communities were documented by 75 phytosociological relevés. Associations of Potametum trichoidis J. et R Tx. in R. Tx. 1965, Potametum praelongi Sauer 1937, P. alpini Br.-Bl. 1949, P. acutifolii Segal 1961, P. obtusifolii (Carst. 1954 Segal 1965 and P. perfoliati W. Koch 1926 em. Pass. 1964 were found as well as communities formed by Potamogeton berchtoldii, P. nodosus and P. pusillus. The study confirms that anthropogenic reservoirs could serve as last refugees for many threatened pondweed communities, which decline or even extinct in their natural habitats. The results indicate that man-made habitats could shift the range limits of threatened species and support their dispersal. The authors conclude that habitats strongly transformed by man are important factors in the natural syntaxonomical diversity protection and should not be omitted in strategies of nature conservation.

  17. Is Poland still attractive for foreign investments?

    OpenAIRE

    Magdalena Jasiniak

    2016-01-01

    Since the economic transition Poland has faced many changes. Accession to the European Union improved the Polish economy and made it more attractive for foreign investments. Since 2004 Poland has been one of the major destinations of FDI in East and Central Europe Countries. Also during the global economic crisis Poland was a good location for foreign capital. The main aim of this article is an attempt to assess whether Poland is still attractive for the location of foreign direct investment....

  18. Rubella in Poland in 2014

    Science.gov (United States)

    Paradowska-Stankiewicz, Iwona; Rogalska, Justyna; Polkowska, Aleksandra

    2016-01-01

    In 2004, Poland has adopted the WHO goal of rubella elimination and congenital rubella syndrome prevention. The main target of the Programme is to stop transmission of the virus in the environment and prevention of congenital rubella in children. In Poland participation in the rubella elimination program requires clinical diagnosis of rubella cases and their confirmation with laboratory tests. Vaccination against rubella was introduced in 1987, initially only in 13 - year-old girls. Since 2003, single jab vaccination against rubella, measles and mumps is used (MMR vaccine for all children: primary vaccination at the age 13-15 months and a booster vaccination at the age of 10). To assess epidemiological situation of rubella in Poland in 2014, including vaccination coverage in Polish population. The descriptive analysis was based on data retrieved from routine mandatory surveillance system and published in the annual bulletins “Infectious diseases and poisonings in Poland in 2014” and “Vaccinations in Poland in 2014” (MP. Czarkowski, Warszawa 2014, NIZP-PZH, GIS). In 2014, there was a significant decrease in the number of rubella cases - with registered 5891 cases (in 2013 - 38 548 cases) - and a decline in incidence (from 101.1 per 100 000 to 15.3). The highest incidence, regardless of gender and the environment was observed in the age group 5-6 years (respectively 93.8 and 109.4 per 100 000). Similarly to 2013, rubella incidence of males was higher than the incidence in girls and women (20.0 versus 10.9). In 2014, no cases of congenital rubella syndrome were registered. The proportion of laboratory tests confirming/excluding rubella infection is still very low in Poland. In 2014, only 0.6% of rubella cases were laboratory confirmed.

  19. Mumps in Poland in 2014

    Science.gov (United States)

    Korczyńska, Monika Roberta; Rogalska, Justyna

    Vaccination against mumps from 2003 is mandatory in Poland and given as two dose scheme with MMR vaccine (mumps, measles, and rubella). Earlier this vaccination was only recommended. Despite observed decline in mumps incidence for over a decade which is a result of conducted vaccinations, mumps is still a common disease among the children. To assess epidemiological situation of mumps in Poland in 2014, including vaccination coverage in Polish population, in comparison to previous years. The descriptive analysis was based on data retrieved from routine mandatory surveillance system and published in the annual bulletins “Infectious diseases and poisonings in Poland in 2014” and “Vaccinations in Poland in 2014” (1). Mumps cases were classified according to the criteria of surveillance case definition implemented in the European Union (Commission Decision of 28 April 2008 amending Decision 2002/253/EC). National Immunisation Programme for year 2014 was also used. In total, there were 2 508 mumps cases registered in Poland in 2014. Incidence of mumps was 6.5 per 100,000 and it was higher by 3.1 % in comparison with 2013 and lower by 9.7 % in comparison with median for the years 2008-2012. The highest incidence rate was observed among children aged 4 years (61.3 per 100,000). Incidence in men (7.8 per 100,000) was higher than in women (5.3). In 2014, 31 people were hospitalized due to mumps. Vaccination coverage of children aged 3 years in Poland in 2013 was 97.0% and it was lower by 0.5 % in comparison with year 2013 (97.5 %). Systematic execution of mumps vaccination in accordance with the National Immunisation Programme resulted in a significant decrease in the number of registered cases. Due to the high vaccination coverage further decline in the number of cases is expected.

  20. Mumps in Poland in 2013.

    Science.gov (United States)

    Korczyńska, Monika Roberta; Rogalska, Justyna

    2015-01-01

    Vaccination against mumps from 2003 is mandatory in Poland and given as two dose scheme with MMR vaccine (mumps, measles, and rubella). Earlier this vaccination was only recommended. Despite observed decline in mumps incidence for over a decade which is a result of conducted vaccinations, mumps is still a common childhood disease. To assess epidemiological situation of mumps in Poland in 2013, including vaccination coverage in Polish population, in comparison to previous years. The descriptive analysis was based on data retrieved from routine mandatory surveillance system and published in the annual bulletins "Infectious diseases and poisonings in Poland in 2013" and "Vaccinations in Poland in 2013" (Czarkowski MP i in., Warszawa 2013, NIZP-PZH i GIS). Mumps cases were classified according to the criteria of surveillance case definition implemented in the European Union (Commission Decision of 28 April 2008 amending Decision 2002/253/EC). National Immunisation Programme for year 2013 was also used. In total, there were 2 436 mumps cases registered in Poland in 2013. Incidence of mumps was 6.3 per 100,000 and it was lower by 12.5% in comparison with 2012 and lower by 18.2% in comparison with median for the years 2007-2010. The highest incidence rate was observed among children aged 5 years (54.0 per 100,000). Incidence in men (7.5) was higher than in women (5.2). In 2013, 38 people were hospitalized due to mumps. Vaccination coverage of children aged 3 years in Poland in 2013 was 97.5% and it was lower by 0.4% in comparison with year 2012. Systematic execution of mumps vaccination in accordance with the National Immunisation Programme resulted in a significant decrease in the number of registered cases. Due to the high vaccination coverage further decline in the number of cases is expected.

  1. Organic Analysis of Peridotite Rocks from the Ashadze and Logatchev Hydrothermal Sites

    Directory of Open Access Journals (Sweden)

    Naohiko Ohkouchi

    2009-07-01

    Full Text Available This article presents an experimental analysis of the organic content of two serpentinized peridotite rocks of the terrestrial upper mantle. The samples have been dredged on the floor of the Ashadze and Logatchev hydrothermal sites on the Mid-Atlantic Ridge. In this preliminary analysis, amino acids and long chain n-alkanes are identified. They are most probably of biological/microbial origin. Some peaks remain unidentified.

  2. Melt stagnation in peridotites from the Godzilla Megamullion Oceanic Core Complex, Parece Vela Basin, Philippine Sea

    Science.gov (United States)

    Loocke, Matthew; Snow, Jonathan E.; Ohara, Yasuhiko

    2013-12-01

    The Godzilla Megamullion, located in the Parece Vela Backarc Basin of the Izu-Bonin-Mariana (IBM) system, is the largest known example of an Oceanic Core Complex (OCC). Peridotites recovered from the megamullion are divided petrographically into fertile (e.g. lherzolites), depleted (e.g. harzburgites), and plagioclase-bearing groups (Ohara et al., 2003a). A total of 151 thin sections were studied from the Kairei KR03-01, Hakuho Maru KH07-02, and Yokosuka YK09-05 cruises. Melt stagnation is studied via the incidence of plagioclase-bearing peridotites and the major element chemistry of Cr-spinels in the plag-bearing samples. A distinct trend in melt stagnation is evident along the length of the megamullion representing a secular evolution in the entrapment of melts rising through the lithosphere. The distal (furthest from the termination of spreading), depleted portion of the mullion represents a robust mantle section that was still producing abundant melt and can be compared to typical oceanic spreading with its relatively “normal” percentage of plagioclase peridotites and average spinel Cr# of 0.35. The medial, fertile portion of the mullion represents a steep falloff in melt productivity represented by fertile spinel compositions (i.e. Cr# stagnation of melt into a lithosphere that was undergoing progressive thickening. We infer that the processes of mantle evolution through melt stagnation and impregnation, as evidenced by the systematic variations in plag-peridotites along Godzilla Megamullion, represent a possibly common way in which the mantle reacts to OCC formation. In this case, Godzilla Megamullion may represent an extreme endmember in OCC formation.

  3. Local Tax Competition in Poland?

    Directory of Open Access Journals (Sweden)

    Swianiewicz Paweł

    2016-09-01

    Full Text Available The concept of tax competition has been successfully applied in an analysis conducted in several European countries, but so far it has not been systematically tested either in Poland or in other countries of Central and Eastern Europe. There are two types of competition discussed in the article: classic competition for mobile tax base and ‘yardstick competition’, in which local politicians compete for political capital being related to the comparison of tax rates with neighbouring municipalities. It is expected that in Poland the ‘yardstick competition’ is more important from the classic competition for the mobile tax base.

  4. Gypsophila perfoliata (Caryophyllaceae in Poland

    Directory of Open Access Journals (Sweden)

    Bartoszek Wacław

    2016-12-01

    Full Text Available Gypsophila perfoliata L. is a maritime sand-dune species naturally occurring in Asia and southeastern Europe. In Europe it also is found in ruderal habitats rarely, mainly along railway lines. In Poland the species was first recorded in the 1950s; it was found only at railway stations where iron ore was offloaded from the Kryvyi Rih region, Ukraine. Recently it was found in a new type of habitat: the roadside of a main road in the Carpathians. The paper characterizes the current status, distribution and habitat spectrum of this alien species in Poland.

  5. Seismic Tomography in Reykjanes , SW Iceland

    NARCIS (Netherlands)

    Jousset, Philippe; Blanck, Hanna; Franke, Steven; Metz, M.; Águstsson, K.; Verdel, Arie; Ryberg, T.; Hersir, Gylfi Páll; Weemstra, C.; Bruhn, D.F.; Flovenz, Olafur G

    2016-01-01

    We present tomographic results obtained around geothermal reservoirs using seismic data recorded both on-land Reykjanes, SW-Iceland and offshore along Reykjanes Ridge. We gathered records from a network of 83 seismic stations (including 21 Ocean Bottom Seismometers) deployed between April 2014 and

  6. Methane Seepage at Hyperalkaline Springs in the Ronda Peridotite Massif (Spain)

    Science.gov (United States)

    Etiope, G.; Vadillo, I.; Whiticar, M. J.; Marques, J. M.; Carreira, P. M.; Tiago, I.; Benavente, J.; Jimenez, P.; Urresti, B.

    2014-12-01

    Methane-rich, hyperalkaline spring waters and bubbling pools have been sampled in the Ronda peridotite massif in southern Spain. Water chemistry (T: 17.1-21.5 ºC; pH: 10.7-11.7; DO: migration pathways along faults. Similar 'dry' seepage of abiotic gas was observed in the Philippines, New Zealand, Turkey and Italy. Like other land-based serpentinization systems, the Ronda peridotite massif is characterized by low heat flow (<40 mW/m2), with temperatures <60°C at depths of 1.5 km. At these low T and high pH conditions, CO32- is the only available carbon source dissolved in the water, and unlikely contributes to catalysed Fischer-Tropsch Type reactions. Methane production from CO2 hydrogenation in a gas phase system (unsaturated fractured rocks) cannot be excluded. The presence of ruthenium-enriched chromitites in the Ronda peridotites may support the hypothesis that CH4 is produced by CO2 hydrogenation catalyzed by Ru minerals, even at temperatures below 100°C, as demonstrated in recent laboratory experiments (Etiope and Ionescu, 2014, Geofluids, in press).

  7. Richtlijnen voor het werken met gemengde teams in de SW

    NARCIS (Netherlands)

    Smit, A.; Giesen, F.; Luijters, K.

    2012-01-01

    Onderzoek naar de pilot 'Regulier en SW'. De pilot 'Regulier en SW' is uitgevoerd door de Inclusief Groep in nauwe samenwerking met TNO. Doel van deze pilot was na te gaan of en zo ja hoe, het inzetten van reguliere krachten in (delen van) de Sociale Werkplaats (SW) de ontwikkeling en eventuele

  8. Air protection strategy in Poland

    Energy Technology Data Exchange (ETDEWEB)

    Blaszczyk, B.

    1995-12-31

    Air quality is one of the basic factors determining the environmental quality and influencing the life conditions of people. There is a shortage of proper quality air in many regions of Poland. In consequence, and due to unhindered transport, air pollution is the direct cause of losses in the national economy (reduction of crops, losses in forestry, corrosion of buildings and constructions, worsening of people`s health). Poland is believed to be one of the most contaminated European countries. The reason for this, primarily, is the pollution concomitant with energy-generating fuel combustion; in our case it means the use of solid fuels: hard coal and lignite. This monocultural economy of energy generation is accompanied by low efficiency of energy use (high rates of energy loss from buildings, heat transmission pipelines, energy-consuming industrial processes). This inefficiency results in the unnecessary production of energy and pollution. Among other reasons, this results from the fact that in the past Poland did not sign any international agreements concerning the reduction of the emission of pollution. The activities aimes at air protection in Poland are conducted based on the Environmental Formation and Protection Act in effect since 1980 (with many further amendments) and the The Ecological Policy of the state (1991). The goals of the Polish air pollution reduction program for the period 1994-2000 are presented.

  9. Poland's Syndrome: A Case Report

    African Journals Online (AJOL)

    jen

    http://www.bioline.org.br/. East and Central African Journal of Surgery - Volume 14 Number 2 – July/August 2009. 112. Poland's Syndrome: A Case Report. J. Gashegu1, J.C. Byiringiro2, M. Nyundo2, A. Uwineza3, L. Mutesa3. 1Anatomy Laboratory, 2Surgery Department, 3centre for Medical genetics, Faculty of Medicine, ...

  10. Education and Work in Poland.

    Science.gov (United States)

    Kluczynski, Jan, Ed.; Sanyal, Bikas C., Ed.

    This study on the relationship between education and employment in Poland attempts to demonstrate the limitations of manpower forecasts in planning for education. Following an introduction, five sections discuss the following topics and subtopics: (1) the relation between education and employment (e.g., the instrumental view of education, the…

  11. Infusion's greenfield subsidiary in Poland

    NARCIS (Netherlands)

    Williams, C.; van Eerde, W.; The, D.

    2012-01-01

    The president of Infusion Development Corporation was reviewing the progress of the new subsidiary the company had set up 15 months earlier in Krakow, Poland. The purpose of the subsidiary was to work with other Infusion offices around the world to provide innovative software development services to

  12. Shigellosis in Poland in 2012.

    Science.gov (United States)

    Stypułkowska-Misiurewicz, Hanna; Baumann-Popczyk, Anna

    2014-01-01

    Shigellosis according to European Centre for Disease Control (ECDC) Report is registered in all countries of the European Union (EU) and of the European Free Trade Association (EFTA) with exception of Italy and Luxemburg. The incidence rate in Poland below 0.1/100 000 of population is the lowest among the EU/EFTA countries. To assess epidemiological situation of shigellosis in Poland in 2012 in comparison to preceding years. An assessment of the epidemiological situation of shigellosis was based on the results from an analysis of the yearly annual bulletins: "Infectious diseases and poisonings in Poland in 2012", reports from bacteriological laboratories and reports from individual cases and epidemiological investigations of outbreaks linked to shigellosis, sent by Sanitary-Epidemiological Stations to the Department of Epidemiology at NIZP-PZH. In 2012 the tendency that the number of registered cases of shigellosis was lower than in the former years continued - only 13 confirmed cases of shigellosis were registered (incidence rate 0.03 per 100 000 inhabitantsbut in the previous year the 18 cases ( incidence rate 0.05). Cases were registered only by 6 provinces, most of the cases by the Lodz province - 4. All together 5 persons nearly 40% were infected in travel to the foreign countries. According to data from laboratories of Sanitary-Epidemiological Stations, Shigella was detected only 4 convalescents and 2 carriers. All cases of shigellosis registered in 2012, were confirmed by a hospital laboratory or a private laboratory. In our opinion the above mentioned data concerning the cases of shigellosis in Poland in 2012 are not reflecting the true epidemiological situation of shigellosis in Poland. The sanitary situation was changing nearly every year for better than in former years but the surveillance of dysentery require more active epidemiological measures.

  13. Morphology and chemistry of Cr Spinel from the peridotites of the Spontang Ophiolite Complex, Ladakh: insights into the petrogenesis of mantle peridotites

    Science.gov (United States)

    Jonnalagadda, Mallika; Karmalkar, Nitin; Harshe, Shivani

    2017-04-01

    The Spontang Ophiolite Complex in north-western Ladakh represents a fragment of oceanic lithosphere emplaced after the closure of the Neo-Tethyan Ocean. This Ophiolite Complex, one of the more complete sequences observed lies 30 kms south of the Indus Tsangpo Suture Zone (ITSZ). It forms the highest tectonic thrust slice above the Mesozoic - Early Tertiary continental margin of the north Indian plate in the Ladakh - Zanskar Himalaya. The ophiolite complex consists of a well-preserved mantle sequence dominated by peridotites, gabbros and ultramafic cumulates along with highly tectonized sheeted dykes and pillow lavas. Based on petrographic features, the peridotite varieties in the Spontang mantle suite are represented by dunites, harzburgites and few lherzolites. Harzburgites exhibit textural transition from protogranular to porphyroclastic and consist of olivine (65-78 vol. %), orthopyroxene (11-30 vol. %), clinopyroxene (Lherzolites are porphyroclastic to equigranular in texture, contain olivine (80-85 vol. %), orthopyroxene (8- 12 vol. %), clinopyroxene (10-12 vol. %) and chromian spinel (1-3 vol. %). Dunite is coarse grained constituting ≥90% olivine accompanied by ≤5% orthopyroxene and upto 1-2% spinel. Chromian spinel is brown to reddish under the microscope and its morphology and textural relationship with coexisting silicates varies with strain, occurring as blebs and vermicular exsolutions present within orthopyroxene to spherical inclusions within olivine crystals through different transitional steps, most important of which is the characteristic elongate holly leaf shape. Cr# in chromian spinel [Cr/ (Cr + Al)] shows a restricted range from 0.20 to 0.33 in harzburgites whereas higher Cr# ranging between 0.45 and 0.53 is observed in lherzolite samples. Dunite samples contain chromian spinel with highest Cr# (0.53 - 0.57). Mg# (Mg/Mg (Mg + Fe2+) is observed to be higher in the harzburgite (0.61-0.74) samples when compared with lherzolite (0.41 -0.70) and

  14. Ocean Basalt Simulator version 1 (OBS1): Trace element mass balance in adiabatic melting of a pyroxenite-bearing peridotite

    Science.gov (United States)

    Kimura, Jun-Ichi; Kawabata, Hiroshi

    2015-01-01

    We present a new numerical trace element mass balance model for adiabatic melting of a pyroxenite-bearing peridotite for estimating mantle potential temperature, depth of melting column, and pyroxenite fraction in the source mantle for a primary ocean basalt/picrite. The Ocean Basalt Simulator version 1 (OBS1) uses a thermodynamic model of adiabatic melting of a pyroxenite-bearing peridotite with experimentally/thermodynamically parameterized liquidus-solidus intervals and source mineralogy. OBS1 can be used to calculate a sequence of adiabatic melting with two melting models, including (1) melting of peridotite and pyroxenite sources with simple mixing of their fractional melts (melt-melt mixing model), and (2) pyroxenite melting, melt metasomatism in the host peridotite, and melting of the metasomatized peridotite (source-metasomatism model). OBS1 can be used to explore (1) the fractions of peridotite and pyroxenite, (2) mantle potential temperature, (3) pressure of termination of melting, (4) degree of melting, and (5) residual mode of the sources. In order to constrain these parameters, the model calculates a mass balance for 26 incompatible trace elements in the sources and in the generated basalt/picrite. OBS1 is coded in an Excel spreadsheet and runs with VBA macros. Using OBS1, we examine the source compositions and conditions of the mid-oceanic ridge basalts, Loihi-Koolau basalts in the Hawaiian hot spot, and Jurassic Shatsky Rise and Mikabu oceanic plateau basalts and picrites. The OBS1 model shows the physical conditions, chemical mass balance, and amount of pyroxenite in the source peridotite, which are keys to global mantle recycling.

  15. A Testing Framework for Critical Space SW

    Science.gov (United States)

    Fernandez, Ignacio; Di Cerbo, Antonio; Dehnhardt, Erik; Massimo, Tipaldi; Brünjes, Bernhard

    2015-09-01

    This paper describes a testing framework for critical space SW named Technical Specification Validation Framework (TSVF). It provides a powerful and flexible means and can be used throughout the SW test activities (test case specification & implementation, test execution and test artifacts analysis). In particular, tests can be run in an automated and/or step-by-step mode. The TSVF framework is currently used for the validation of the Satellite Control Software (SCSW), which runs on the Meteosat Third Generation (MTG) satellite on-board computer. The main purpose of the SCSW is to control the spacecraft along with its various subsystems (AOCS, Payload, Electrical Power, Telemetry Tracking & Command, etc.) in a way that guarantees a high degree of flexibility and autonomy. The TSVF framework serves the challenging needs of the SCSW project, where a plan-driven approach has been combined with an agile process in order to produce preliminary SW versions (with a reduced scope of implemented functionality) in order to fulfill the stakeholders needs ([1]). The paper has been organised as follows. Section 2 gives an overview of the TSVF architecture and interfaces versus the test bench along with the technology used for its implementation. Section 3 describes the key elements of the XML based language for the test case implementation. Section 4 highlights all the benefits compared to conventional test environments requiring a manual test script development, whereas section 5 concludes the paper.

  16. Shigellosis in Poland in 2011.

    Science.gov (United States)

    Stypułkowska-Misiurewicz, Hanna; Baumann-Popczyk, Anna

    2013-01-01

    Shigellosis, also known as bacillary dysentery, is a contagious and infectious disease. In the European Union, on the basis of the Commission Decision of 2 April 2009 and the Commission Decision of 28 April 2008, a unified system for collecting epidemiological data on infectious diseases was introduced, including shigellosis. This makes it possible to compare data collected at different times and in different countries. The aim of the article is to evaluate the epidemiological situation of shigellosis in Poland in 2011. An assessment of the epidemiological situation of shigellosis was based on the results from an analysis of the yearly annual bulletins: "Infectious diseases and poisonings in Poland in 2011", reports from bacteriological laboratories and reports from individual cases and epidemiological investigations of outbreaks linked to shigellosis, sent by Sanitary Epidemiological Stations to the Department of Epidemiology at NIZP-PZH. In Poland, 17 confirmed cases of shigellosis were registered in 2011. The incidence of 0.04 per 100,000 inhabitants was lower when compared to the previous year. The number of cases is lower by 48% when compared with the median of years 2005-2009--35 cases (incidence 0.09/100,000). Most of the cases were registered in the Silesian province--7 (incidence 0.15 /100,000). According to data from 16 laboratories of Sanitary Epidemiological Stations, Shigella was not detected among the subjects. All cases of shigellosis registered in 2011, were confirmed by a hospital laboratory at or a private laboratory. In Poland, we have observed a decline in the number of cases of shigellosis and the incidence remains at a relatively steady level and constitutes less than 0.1/100,000 inhabitants. Compared to the rest of the countries belonging to the EU/EFTA, the current epidemiological situation of shigellosis in Poland is good. Poland is a country with the lowest incidence. In spite of this, the surveillance of shigellosis required more active

  17. Coupled major and trace elements as indicators of the extent of melting in mid-ocean-ridge peridotites.

    Science.gov (United States)

    Hellebrand, E; Snow, J E; Dick, H J; Hofmann, A W

    2001-04-05

    Rocks in the Earth's uppermost sub-oceanic mantle, known as abyssal peridotites, have lost variable but generally large amounts of basaltic melt, which subsequently forms the oceanic crust. This process preferentially removes from the peridotite some major constituents such as aluminium, as well as trace elements that are incompatible in mantle minerals (that is, prefer to enter the basaltic melt), such as the rare-earth elements. A quantitative understanding of this important differentiation process has been hampered by the lack of correlation generally observed between major- and trace-element depletions in such peridotites. Here we show that the heavy rare-earth elements in abyssal clinopyroxenes that are moderately incompatible are highly correlated with the Cr/(Cr + Al) ratios of coexisting spinels. This correlation deteriorates only for the most highly incompatible elements-probably owing to late metasomatic processes. Using electron- and ion-microprobe data from residual abyssal peridotites collected on the central Indian ridge, along with previously published data, we develop a quantitative melting indicator for mantle residues. This procedure should prove useful for relating partial melting in peridotites to geodynamic variables such as spreading rate and mantle temperature.

  18. Origin of the Luobusa diamond-bearing peridotites from the sub-arc mantle

    Science.gov (United States)

    Liu, Chuanzhou; Zhang, Chang; Wu, Fuyuang; Chung, Sunlin

    2016-04-01

    Ophiolites are the remnants of ancient oceanic lithosphere that were emplaced onto continental margins. Ophiolites along the E-W trending Yarlung-Tsangpo Suture (YTS), which separates the Indian plate from the Eurasian plate, have been regarded as relics of the Neo-Tethys Ocean. The Luobusa ophiolite outcrops at the eastern YTS and mainly consists of harzburgites and dunites that have been intruded by gabbroic/diabase dykes at ca 130 Ma (Zhang et al., 2015). Basaltic lavas are rarely outcropped, and volumetrically minor (< 1% by volume) chromitites are enveloped as lens and layers within dunites (Zhou et al., 1996). The Luobusa peridotites have been interpreted as mantle residues experienced melt extraction at the mid-ocean ridge and subsequently reacted with boninitic magmas in subduction zone, which gave rise to podifiorm chromitites (Zhou et al., 1996). However, such a shallow depth origin fails to explain the occurrence of diamond and other ultra-high pressure (UHP) minerals in both peridotites and chromitites (Yang et al., 2007, 2014). A mantle plume origin has been proposed for the Luobusa ophiolite to explain the UHP minerals. However, this model is not reconciled with the occurrence of low-pressure crustal minerals in both chromitites and peridotites (Robinson et al., 2015). Here we report whole-rock Re-Os isotope data, which suggest that most Luobusa peridotites have subjected to ancient melting events older than 1.9 billion years. High contents of heavy rare earth elements in clinopyroxenes support the occurrence of ancient melting in garnet stability field. Hf-Nd isotopes of clinopyroxenes, which yield young model ages as 110 Ma, with one showing the lowest ɛNd(T) value of -3, do not preserve the signatures of ancient melting but record metasomatism by subduction-related agents. Consequently, we argue that protoliths of the Luobusa peridotites originated from ancient domains in the transition zone and, together with diamond-bearing chromitites, were

  19. Modeling a CO2 mineralization experiment of fractured peridotite from the Semail ophiolite/ Oman

    Science.gov (United States)

    Muller, Nadja; Zhang, Guoxiang; van Noort, Reinier; Spiers, Chris; Ten Grotenhuis, Saskia; Hoedeman, Gerco

    2010-05-01

    Most geologic CO2 sequestration technologies focus on sedimentary rocks, where the carbon dioxide is stored in a fluid phase. A possible alternative is to trap it as a mineral in the subsurface (in-situ) in basaltic or even (ultra)mafic rocks. Carbon dioxide in aqueous solution reacts with Mg-, Ca-, and Fe-bearing silicate minerals, precipitates as (MgCa,Fe)CO3 (carbonate), and can thus be permanently sequestered. The cation donors are silicate minerals such as olivine and pyroxene which are abundant in (ultra)mafic rocks, such as peridotite. Investigations are underway to evaluate the sequestration potential of the Semail Ophiolite in Oman, utilizing the large volumes of partially serpentinized peridotite that are present. Key factors are the rate of mineralization due to dissolution of the peridotite and precipitation of carbonate, the extent of the natural and hydraulic fracture network and the accessibility of the rock to reactive fluids. To quantify the influence of dissolution rates on the overall CO2 mineralization process, small, fractured peridotite samples were exposed to supercritical CO2 and water in laboratory experiments. The samples are cored from a large rock sample in the dimension of small cylinders with 1 cm in height and diameter, with a mass of ~2g. Several experimental conditions were tested with different equipment, from large volume autoclave to small volume cold seal vessel. The 650 ml autoclave contained 400-500g of water and a sample under 10 MPa of partial CO2 pressure up to 150. The small capsules in the cold seal vessel held 1-1.5g of water and the sample under CO2 partial pressure from 15MPa to 70 MPa and temperature from 60 to 200°C. The samples remained for two weeks in the reaction vessels. In addition, bench acid bath experiments in 150 ml vials were performed open to the atmosphere at 50-80°C and pH of ~3. The main observation was that the peridotite dissolved two orders of magnitude slower in the high pressure and temperature

  20. Is Poland still attractive for foreign investments?

    Directory of Open Access Journals (Sweden)

    Magdalena Jasiniak

    2016-02-01

    Full Text Available Since the economic transition Poland has faced many changes. Accession to the European Union improved the Polish economy and made it more attractive for foreign investments. Since 2004 Poland has been one of the major destinations of FDI in East and Central Europe Countries. Also during the global economic crisis Poland was a good location for foreign capital. The main aim of this article is an attempt to assess whether Poland is still attractive for the location of foreign direct investment. This article is a preliminary study. It is based on statistical analysis describing changes in foreign capital flows in Poland and its position in relation to other European Union countries. Results show that the position of Poland on the map of foreign investment has dramatically changed.

  1. Meningitis and encephalitis in Poland in 2014

    Science.gov (United States)

    Paradowska-Stankiewicz, Iwona; Piotrowska, Anna

    The aim of this study was to assess the epidemiology of meningitis and/or encephalitis in Poland in 2014. In the last three years in Poland, about 3000 cases of meningitis and/or encephalitis of viral or bacterial etiology were recorded annually. Assessment of the epidemiological situation of meningitis and/or encephalitis in Poland in 2014, was based on the results of the analysis of epidemiological reports sent to the NIZP-PZH by the Regional Sanitary-Epidemiological Stations published in the annual bulletin “Infectious diseases and poisonings in Poland in 2014” and “Preventive immunizations in Poland in 2014”. In 2014 in Poland 3488 cases of bacterial meningitis and/or encephalitis were recorded. Almost 61.3% of these were viral infections. In 2014, in comparison to 2013, a 1.1% increase in the number of cases of meningitis and/or encephalitis was observed and 91% with viral etiology.

  2. Last Glacial Maximum in Poland

    Science.gov (United States)

    Marks, Leszek

    2002-01-01

    The Last Glacial Maximum (LGM) in Poland is represented by the Leszno Phase and occurred after 21 ka radiocarbon years. In turn the deglacial Poznań Phase is estimated at 18.4 ka, the Pomeranian Phase at 15.2 ka, the Gardno Phase at about 14.0-13.8 ka, the Słupsk Bank Phase at 13.5-13.2 ka and the Southern Middle Bank Phase at 12.7-12.5 ka BP. The ice sheet limit at LGM was not synchronous everywhere in Poland but occurred as several major and minor ice lobes that reflected a stream-like structure of the ice body that radiated southwards from the Baltic Basin. Meltwater runoff during the LGM created a complex system of sandur trains and ice-marginal spillways, with numerous intervening proglacial lakes.

  3. Poland: An energy and environmental overview

    Energy Technology Data Exchange (ETDEWEB)

    Szpunar, C.B.; Bhatti, N.; Buehring, W.A.; Streets, D.G. (Argonne National Lab., IL (USA)); Balandynowicz, H.W. (Polska Akademia Nauk, Warsaw (Poland). Inst. Podstawowych Problemow Techniki)

    1990-10-01

    Poland's reliance on coal as its primary source of energy imposes heavy environmental costs on its economy and population. Specifically, many of Poland's air and water pollution problems can be traced to the high energy intensity of Polish industrial production. This overview presents environment and energy information for Poland. Topics discussed include: energy resources, production and use; energy production, trade and use; environmental quality and impacts; and control strategies. 109 refs., 25 figs., 40 tabs.

  4. Micro-scale investigation of carbonation process in partially serpentinized peridotites

    Science.gov (United States)

    Andreani, M.; Menez, B.; Delacour, A.; Pasini, V.; Auzende, A. L.; Brunelli, D.

    2012-04-01

    The carbonation of ultramafic rocks is, theoretically, the most efficient reaction to trap CO2 irreversibly in the form of solid carbonates, as predicted by equilibrium thermodynamic calculations. However, the success of industrial or natural carbonation in large ultramafic aquifers or oceanic ultramafic exposures does not only rely on the thermodynamic conditions of chemical reactions, but also on their feedback effects on the reactive surface area and on the local porosity and permeability. In addition, side processes like serpentinization, redox reactions, abiotic catalytic effects, and biological activity, can be expected in such complex natural system. Their occurrence and implications on carbon speciation and carbon transfers during hydrothermal alteration of oceanic peridotites have not been explored yet and requires detailed study of natural and/or experimental carbonation zones. We have combined petrographic and electron microscopy with SIMS, Raman and FTIR microspectroscopy on partially serpentinized peridotites drilled during the IODP leg 304 (30°N, MAR) in order to characterize the mechanisms of peridotite carbonation at the fluid-mineral interface and identify the associated speciation of carbon (inorganic and organic carbon occurrences). We present first results on zones located close to talc-tremolite sheared veins in holes 1309B and D. Associations of carbonates, porous phyllosilicates and oxides are observed in close vicinity of relict olivines that underwent a previous stage of serpentinization. The olivine-carbonate interface is nanoporous which facilitates mass transfer between fluid and mineral. The phyllosilicate identified as saponite results from the metasomatic replacement, during the carbonation stage, of previously formed serpentine. These observations do not favour reaction-induced cracking but rather a transfer-controlled process in an open system. Among the submicrometric dark clusters widely-distributed in saponite and in serpentine

  5. Petrography and mineral chemistry of metamorphosed mantle peridotites of Nain Ophiolite (Central Iran

    Directory of Open Access Journals (Sweden)

    Nargess Shirdashtzadeh

    2017-07-01

    Full Text Available Introduction Study of the petrology of the ophiolites as the relics of ancient oceanic lithosphere, is a powerful tool to reconstruct Earth’s history. Mantle peridotites have mostly undergone alteration and serpentinization to some extent. Thus, the relics of metamorphic signatures from the upper mantle and crustal processes from most of the peridotites have been ruined. Several recent papers deal with the mantle peridotites of Nain Ophiolite (e.g. Ghazi et al., 2010. However, no scientific work has been carried out on the metamorphosed mantle peridotites. The study area of the Darreh Deh that is located in the east of the Nain Ophiolite, is composed of huge massifs of metamorphosed mantle peridotites (i.e. lherzolite, clinopyroxene-bearing harzburgite, and harzburgite, and small volumes of dunite, characterized by darker color, higher topographic relief, smaller number of basic intrusives, lower serpentinization degree, and amphibolite-facies metamorphism. In this study, the petrography and mineralogy of metamorphosed peridotites in the Darreh Deh has been considered based on geochemical data. Geological Setting The Mesozoic ophiolitic mélange of Nain is located in the west of CEIM, along the Nain-Baft fault. As a part of a metamorphosed oceanic crust, it is mainly composed of harzburgite, lherzolite, dunite and their serpentinized varieties, chromitite, pyroxenite, gabbro, diabasic dike, spilitized pillow lava, plagiogranite, amphibolite, metaperidotites, schist, skarn, marble, rodingite, metachert and listwaenite (Shirdashtzadeh et al., 2010, 2014a, 2014b. Geochemical investigations indicate a suprasubduction zone in the eastern branch of the Neo-Tethys Ocean (Ghasemi and Talbot, 2006; Shirdashtzadeh et al., 2010, 2014a, 2014b. Materials and Methods Chemical analyses of mineral compositions were carried out using a JEOL JXA8800R wavelength-dispersive electron probe micro-analyzer (accelerating voltage of 15 kV and a beam current of 15 n

  6. Highly siderophile element systematics of abyssal peridotites from intermediate and fast spreading ridges

    Science.gov (United States)

    Brown, D. B.; Day, J. M.; Waters, C. L.

    2016-12-01

    Abyssal peridotites are residues of both modern and ancient partial melt extraction at oceanic ridges and can be used to examine melting processes and mantle heterogeneity. The highly siderophile elements (HSE: Os, Ir, Ru, Pt, Pd, Re, and the 187Re-187Os system embedded within them), are useful for investigating these issues, as they are generally strongly compatible. To date, limited data on HSE and Os isotopes has been obtained on abyssal peridotites from fast spreading centers. Here, we report new HSE abundance and 187Os/188Os data for Pacific Antarctic Ridge (PAR) and East Pacific Rise (EPR) abyssal peridotites. Samples from the PAR were dredged from two separate localities along the Udintsev Fracture Zone, and EPR samples were taken from Hess Deep. The PAR full spreading rate ranges from 54-83mm/year [1,2] and is 75 mm/year [2] at the Udintsev Fracture Zone. These spreading rates characterize the PAR as an intermediate spreading ridge, whereas the fast spreading EPR has a full rate ranging from 128-157 mm/year [3]. The 187Os/188Os ratios for whole-rocks from the PAR range from 0.114 to 0.134, with Re depletion ages (TRD) varying from 1 Ga to present. Despite the large variation in 187Os/188Os, HSE patterns are primitive mantle-like [4], with Ru/Ir ratios ranging from 1.5-2.1. Depletions in Re and Pd are present, as is expected in partial melt residues, and the samples have undergone 4-15% partial melting based on the rare earth elements (REE). The EPR exhibits higher levels of melt depletion ranging from 18-24%. New results show Hess Deep samples have 187Os/188Os ratios of 0.123 and 0.125 for whole-rocks. These findings indicate that PAR and EPR Os isotopic data overlap with the global record of abyssal peridotites from slower ridges and that Os isotopic heterogeneities are preserved across a wide range of spreading rates and degrees of melt extraction. [1] Géli, L., et al. (1997), Science, 278, 1281-1284; [2] Castillo, P.R., et al. (1998) EPSL, 154

  7. Monomineral universal clinopyroxene and garnet barometers for peridotitic, eclogitic and basaltic systems

    Directory of Open Access Journals (Sweden)

    I.V. Ashchepkov

    2017-07-01

    Full Text Available New versions of the universal Jd-Di exchange clinopyroxene barometer for peridotites, pyroxenites and eclogites, and also garnet barometer for eclogites and peridotites were developed. They were checked using large experimental data sets for eclogitic (∼530 and peridotitic systems (>650. The precision of the universal Cpx barometer for peridotites based on Jd-Di exchange is close to Cr-Tschermakite method produced by Nimis and Taylor (2000. Cpx barometer was transformed by the substitution of major multiplier for KD by the equations dependent from Al-Na-Fe. Obtained equation in combination with the thermometer of Nimis and Taylor (2000 allow to reconstruct position of the magma feeder systems of the alkali basaltic magma within the mantle diapirs in modern platforms like in Vitim plateau and other Southern Siberia localities and several localities worldwide showing good agreement of pressure ranges for black and green suites. These equations allow construct PTX diagrams for the kimberlite localities in Siberia and worldwide calculating simultaneously the PT parameters for different groups of mantle rocks. They give very good results for the concentrates from kimberlite lamproites and placers with mantle minerals. They are useful for PT estimates for diamond inclusions. The positions of eclogite groups in mantle sections are similar to those determined with new Gar–Cpx barometer produced by C. Beyer et al. (2015. The Fe rich eclogites commonly trace the boundary between the lower upper parts of subcontinental lithospheric mantle (SCLM at 3–4 GPa marking pyroxenite eclogites layer. Ca-rich eclogites and especially grospydites in SCLM beneath Precambrian kimberlites occurs near pyroxenite layer but in younger mantle sections they became common in the lower parts. The diamondiferous Mg Cr-less group eclogites referring to the ancient island arc complexes are also common in the middle part of mantle sections and near 5–6 GPa. Commonly

  8. Mantle melting and melt refertilization beneath the Southwest Indian Ridge: Mineral composition of abyssal peridotites

    Science.gov (United States)

    Chen, Ling; Zhu, Jihao; Chu, Fengyou; Dong, Yan-hui; Liu, Jiqiang; Li, Zhenggang; Zhu, Zhimin; Tang, Limei

    2017-04-01

    As one of the slowest spreading ridges of the global ocean ridge system, the Southwest Indian Ridge (SWIR) is characterized by discontinued magmatism. The 53°E segment between the Gallieni fracture zone (FZ) (52°20'E) and the Gazelle FZ (53°30'E) is a typical amagmatic segment (crustal thickness flat or U-type REE patterns, thus cannot be the pure residue of mantle melting. Mineral compositions of the Group 2 peridotites are more depleted than that of peridotites sampled near the Bouvet hot spot (Johnson et al., 1990), implying that the depleted mantle beneath the 53°E segment may be the residue of ancient melting event. This hypothesis is supported by the the low Ol/Opx ratios, coarse grain sizes (>1cm) Opx, and Mg-rich mineral compositions akin to harzburgite xenoliths that sample old continental lithospheric mantle (Kelemen et al., 1998). Melt refertilization model shows that Group 2 peridotites were affected by an enriched low-degree partial melt from the garnet stability field. These results indicate that depleted mantle which experiences ancient melting event are more sensitive to melt refertilization, thus may reduce the melt flux, leading to extremely thin crust at 53°E segment. This research was granted by the National Basic Research Programme of China (973 programme) (grant No. 2013CB429705) and the Fundamental Research Funds of Second Institute of Oceanography, State Oceanic Administration (JG1603, SZ1507). References: Johnson K T M, Dick H J B, Shimizu N. Melting in the oceanic upper mantle: An ion microprobe study of diopsides in abyssal peridotites[J]. Journal of Geophysical Research, 1990, 95(B3):2661-2678. Kelemen P B, Hart S R, Bernstein S. Silica enrichment in the continental upper mantle via melt/rock reaction[J]. Earth & Planetary Science Letters, 1998, 164(1-2):387-406. Zhou H, Dick H J. Thin crust as evidence for depleted mantle supporting the Marion Rise.[J]. Nature, 2013, 494(7436):195-200.

  9. Poland syndrome with dextrocardia: case report.

    Science.gov (United States)

    Galiwango, G W; Swan, M C; Nyende, R; Hodges, A M

    2010-11-01

    Poland syndrome is a rare congenital condition presentingwith typical features including an absent costosternal head of pectoralis major andipsilateral brachysyndactyly. There are many clinical variations of the syndrome including rib defects, absence of shoulder girdle muscle and breast hypoplasia or agenesis. Dextrocardia is rarely associated with Poland Syndrome with only 22 cases being previously reported in the worldwide literature. Whereas 'classical' Poland syndrome is predominantly right sided, all cases associated with dextrocardia have been left sided. We report a further case of left sided Poland syndrome with dextrocardia which might have important implications for the understanding of the pathogenesis of this unusual condition.

  10. Peridotitic lithosphere metasomatised by volatile-bearing melts, and its association with intraplate alkaline HIMU-like magmatism

    DEFF Research Database (Denmark)

    Scott, James; Brenna, Marco; Crase, Jordan

    2016-01-01

    along grain boundaries during ascent, with the distinctive peridotite isotopic compositions having been imparted earlier by mantle metasomatism. Two mantle metasomatic styles are distinguished from pyroxene trace element concentrations (in particular, rare earth elements, Ti, Zr and Hf...... of volatile-rich melts, which probably rose from the asthenosphere. Melt modelling of representative depleted and subsequently enriched samples shows that low-degree melting of a CO2-bearing melt-metasomatized peridotite could yield a melt with a trace element composition very similar to that of the Zealandia...... with HIMU-like isotope compositions in some Zealandia basalts. The melt modelling results also imply that amphibole could buffer the trace element budgets of a low-degree melt regardless of the source peridotite composition; therefore, provided that hydrous metasomatized lithospheric mantle can be perturbed...

  11. Peridotites and mafic igneous rocks at the foot of the Galicia Margin: an oceanic or continental lithosphere? A discussion

    Energy Technology Data Exchange (ETDEWEB)

    Korprobst, J.; Chazot, G.

    2016-10-01

    An ultramafic/mafic complex is exposed on the sea floor at the foot of the Galicia Margin (Spain and Portugal). It comprises various types of peridotites and pyroxenites, as well as amphibole-diorites, gabbros, dolerites and basalts. For chronological and structural reasons (gabbros were emplaced within peridotites before the continental break-up) this unit cannot be assigned to the Atlantic oceanic crust. The compilation of all available petrological and geochemical data suggests that peridotites are derived from the sub-continental lithospheric mantle, deeply transformed during Cretaceous rifting. Thus, websterite dykes extracted from the depleted MORB mantle reservoir (DMM), were emplaced early within the lithospheric harzburgites; subsequent boudinage and tectonic dispersion of these dykes in the peridotites, during deformation stages at the beginning of rifting, resulted in the formation of fertile but isotopically depleted lherzolites. Sterile but isotopically enriched websterites, would represent melting residues in the peridotites, after significant partial melting and melt extraction related to the thermal erosion of the lithosphere. The latter melts are probably the source of brown amphibole metasomatic crystallization in some peridotites, as well as of the emplacement of amphibole-diorite dykes. Melts directly extracted from the asthenosphere were emplaced as gabbro within the sub-continental mantle. Mixing these DMM melts together with the enriched melts extracted from the lithosphere, provided the intermediate isotopic melt-compositions - in between the DMM and Oceanic Islands Basalts reservoir - observed for the dolerites and basalts, none of which are characterized by a genuine N-MORB signature. An enriched lithospheric mantle, present prior to rifting of the Galicia margin, is in good agreement with data from the Messejana dyke (Portugal) and more generally, with those of all continental tholeiites of the Central Atlantic Magmatic Province (CAMP

  12. Geochemistry and tectonic significance of the Gongzhu peridotites in the northern branch of the western Yarlung Zangbo ophiolitic belt, western Tibet

    Science.gov (United States)

    Lian, Dongyang; Yang, Jingsui; Liu, Fei; Wu, Weiwei; Zhang, Li; Zhao, Hui; Huang, Jian

    2017-10-01

    The Gongzhu ophiolite is situated in the northern branch of the western Yarlung Zangbo ophiolitic belt. This massif consists of a strongly dismembered ophiolitic sequence dominated by mantle peridotites. The peridotites comprise lherzolite with low- to moderately-depleted mineral and bulk rock compositions. The degree of partial melting deduced from Cr# values of the Gongzhu peridotites varies between 7% and 10%. The mineral and whole rock compositions of the Gongzhu peridotites are comparable to those of abyssal peridotites. The chondrite normalized REE compositions of the peridotites typically display U-shaped or spoon-shaped patterns, and primitive mantle-normalized PGEs patterns show Ir depletion relative to Os and Ru, and Pt enrichment relative to Rh and Pd. On the basis of the petrological, mineralogical and geochemical data, we concluded that the Gongzhu peridotites either formed in the back-arc setting of an intra-oceanic subduction system or the Gongzhu and Dajiweng peridotites both formed in the in the same incipient forearc/proto-forearc environment of an intra-oceanic subduction zone.

  13. [Malaria in Poland in 2010].

    Science.gov (United States)

    Stepień, Małgorzata

    2012-01-01

    The objective of this study was to describe the epidemiology of imported malaria in Poland in 2010 in comparison to previous years. The study included malaria cases that were collected and registered by the State Sanitary Inspection in 2010 in Poland. Data reported was verified, processed and published by National Institute of Public Health - National Institute of Hygiene. All cases were laboratory confirmed by blood film, polymerase chain reaction or rapid diagnostic tests outlined by the EU case definition. Differences in the distribution of demographic, parasitological and clinical characteristics, and incidence were analyzed. In 2010, a total of 35 confirmed malaria cases were notified in Poland, 13 more than 2009. All cases were imported, 49% from Africa, including 1 case with relapsing malaria caused by P. vivax and 2 cases of recrudescence falciparum malaria following failure of treatment. The number of cases acquired in Asia (37% of the total), mainly from India and Indonesia, was significantly higher than observed in previous years. Among cases with species-specific diagnosis 19 (63%) were caused by P. falciparum, 9 (30%) by P. vivax, one by P. ovale and one by P. malariae. The median age of all cases was 42 years (range 9 months to 71 years), males comprised 69% of patients, females 31%, three patients were Indian citizens temporarily in Poland. Common reasons for travel to endemic countries were tourism (57%), work-related visits (37%), one person visited family and in one case the reason for travel was unknown. Sixteen travelers took chemoprophylaxis, but only three of them appropriately (adherence to the recommended drug regimen, continuation upon return and use of appropriate medicines). In 2010, there were no deaths due to malaria and clinical course of disease was severe in 7 cases. When compared with 2009, there was a marked increase in the number of imported malaria cases in Poland, however the total number of notified cases remained low. Serious

  14. The Force of Crystallization and Fracture Propagation during In-Situ Carbonation of Peridotite

    Directory of Open Access Journals (Sweden)

    Reinier van Noort

    2017-10-01

    Full Text Available Subsurface mineralization of CO2 by injection into (hydro-fractured peridotites has been proposed as a carbon sequestration method. It is envisaged that the expansion in solid volume associated with the mineralization reaction leads to a build-up of stress, resulting in the opening of further fractures. We performed CO2-mineralization experiments on simulated fractures in peridotite materials under confined, hydrothermal conditions, to directly measure the induced stresses. Only one of these experiments resulted in the development of a stress, which was less than 5% of the theoretical maximum. We also performed one method control test in which we measured stress development during the hydration of MgO. Based on microstructural observations, as well as XRD and TGA measurements, we infer that, due to pore clogging and grain boundary healing at growing mineral interfaces, the transport of CO2, water and solutes into these sites inhibited reaction-related stress development. When grain boundary healing was impeded by the precipitation of silica, a small stress did develop. This implies that when applied to in-situ CO2-storage, the mineralization reaction will be limited by transport through clogged fractures, and proceed at a rate that is likely too slow for the process to accommodate the volumes of CO2 expected for sequestration.

  15. Subduction factory in an ampoule: Experiments on sediment-peridotite interaction under temperature gradient conditions

    Science.gov (United States)

    Woodland, A. B.; Bulatov, V. K.; Brey, G. P.; Girnis, A. V.; Höfer, H. E.; Gerdes, A.

    2018-02-01

    To better understand processes above subducted oceanic slabs, we have undertaken experiments with juxtaposed sediment and peridotite layers at pressures of 7.5 and 10.5 GPa at a controlled temperature gradient from ∼100 to ∼500 °C per a sample length of ∼3 mm. The sediment starting material contains H2O (6.9 wt%) and CO2 (5.9 wt%) and has a major-element composition similar to GLOSS (Plank and Langmuir, 1998) doped with trace elements at 10-100 ppm levels. Several experiments were conducted with ∼0.5 wt% Cl or F. The peridotite layer is composed of natural olivine (66 wt%), orthopyroxene (27 wt%) and garnet (7 wt%) mixed with ∼15 wt% graphite. Several experimental configurations were investigated, but the "basic" setup has the sediment layer at the bottom in the cold zone (400-1200 °C) overlain by peridotite at 900-1500 °C. The temperature distribution was determined by two thermocouples and orthopyroxene-garnet thermometry. Features common to many experiments are (1) the development of multiple layers of various lithologies and a pool of hydrous silicate or carbonate-silicate melt in the hottest part of the capsule; (2) replacement of olivine by orthopyroxene in the metaperidotite; (3) preservation and growth of garnet and local development of magnesite in the metaperidotite layer; (4) enrichment in garnet within the metasediment layer at the contact with the metaperidotite; (5) formation of a clinopyroxene-garnet assemblage at the bottom (the coldest part); (6) presence of K-bearing phases (phlogopite or phengite) and carbonates in the metasediment layer only at temperatures <700 °C; and (7) occurrence of accessory zircon, rutile and phosphates in the coldest regions. In terms of element redistribution, the peridotite becomes strongly enriched in SiO2 compared to the starting composition, and the sediment gains MgO, FeO and Cr2O3. Potassium is fully extracted into the melt, while Na and Ca are largely retained in the coldest part of the metasediment

  16. Water in orthopyroxene from abyssal spinel peridotites of the East Pacific Rise (ODP Leg 147: Hess Deep)

    Science.gov (United States)

    Hesse, Kirsten T.; Gose, Jürgen; Stalder, Roland; Schmädicke, Esther

    2015-09-01

    Abyssal spinel peridotites from Hess Deep, East Pacific Rise (ODP Leg 147) were investigated concerning their major, minor, and trace element mineral chemistry and the incorporation of structural water in orthopyroxene. The rocks are partially serpentinized harzburgites containing primary minerals of olivine, orthopyroxene, clinopyroxene, and spinel. Orthopyroxene is enstatitic with Mg# (Mg/(Mg + Fe)) between 0.90 and 0.92 and Al2O3 from 0.5 to 2.9 wt.%. The residual harzburgite experienced high degrees of melt removal in the spinel peridotite stability field. The average degree of partial melting was calculated to be 17.5% (range: 16.4-17.8%). Trace element data of ortho- and clinopyroxenes reflect this strong depletion, characteristic for the restitic nature of abyssal peridotites. Mantle re-equilibration temperatures around 1000 °C indicate that, after melt extraction and before exhumation to the ocean floor, the rocks experienced significant cooling in the spinel peridotite facies. Water contents of orthopyroxene range from 86 to 233 wt. ppm H2O with an average concentration of 142 wt. ppm H2O. These results represent the first data on water contents in the sub-pacific mantle obtained by direct measurements of sub-oceanic peridotite. The water contents are not related to mineral chemistry, stratigraphy, melting degree, mantle equilibrium conditions or oxidation state. Calculated post-melt peridotite water contents vary between 40 and 100 wt. ppm H2O. Compared to Mid-Atlantic Ridge peridotites, the East Pacific Rise samples of Leg 147 contain somewhat lower water concentrations than samples from Leg 153 and considerably higher contents than those of Leg 209 (Gose et al., 2009; Schmädicke et al., 2011). In Leg 147, the strongest OH absorbtion band occurs at 3420 cm- 1, wheras orthopyroxene from MAR peridotite (Legs 153 and 209) has its strongest absorbtion band at 3566 and 3522 cm- 1. The mantle equilibrium temperature of Leg 147 peridotites is lower than that

  17. Centrifuge assisted percolation of Fe-S melts in partially molten peridotite: Time constraints for planetary core formation

    Science.gov (United States)

    Bagdassarov, N.; Solferino, G.; Golabek, G. J.; Schmidt, M. W.

    2009-10-01

    The mechanism which segregates molten Fe-S into metallic cores of planetary bodies is still not fully understood. Due to the high interfacial energy and wetting angle between Fe-S melts and silicate mantle minerals, the continuous percolative flow of such melts cannot be efficient for the core segregation in planetary bodies. A series of percolation experiments has been realized on a partially molten fertile garnet peridotite, employing a centrifuging piston cylinder. A high temperature garnet peridotite with Mg# ~0.90 composed of 60 vol.% olivine, 15 vol.% orthopyroxene, 6 vol.% clinopyroxene and 19 vol.% garnet has been used as the silicate matrix. Peridotite powders with the 100-200 or 20-30 µm grain size were mixed with 5-30 vol.% Fe-S of eutectic composition Fe 70S 30. The aggregates were centrifuged at 500-700 g at temperatures below and above the melting point of the peridotite. The centrifuge experiments revealed a negligible percolation of Fe-S melts through the unmolten peridotite matrix. Only at T > 1260 °C, i.e. above the solidus of the peridotite, and starting with 5 vol.% of Fe 70S 30 the vertical melt gradient achieved 1-2 vol.%/mm. In samples with 15 vol.% Fe 70S 30 the vertical separation achieved 2-2.5 vol.%/mm after 10 h of centrifuging at 500 g. An increase in the degree of partial silicate melting in the peridotite leads to an increase of the Fe-S separation rate from the peridotite matrix. Fe-S contents >10 vol.% cause an increase of the Fe-S melt droplet size and of the effective percolation velocity of Fe-S melt. A threshold dividing fast (>10 cm per year) and slow percolations (<1 mm per year) of Fe -S melt is found around 14-15 vol.% of Fe 70S 30. The experimentally determined permeabilities of Fe-S melt in the unmolten peridotite with 7-10 vol.% of Fe 70S 30 melt are 10 - 18 -10 - 19 m 2, which is 2-3 orders of magnitude lower than the values calculated previously from static experiments. The presence of the silicate melt increases the

  18. Social Inclusion of Foreigners in Poland

    Science.gov (United States)

    Sowa-Behtane, Ewa

    2016-01-01

    Poland has a relatively short history of immigration compared to other member states of the European Union. However, in recent decades, the number of foreigners in Poland has increased significantly. Intercultural relations may take the form of hostility, conflict, antagonism, segregation, separation, neutral co-presence, partial social…

  19. Poland's syndrome: radiologic findings

    Energy Technology Data Exchange (ETDEWEB)

    Bazzi Junior, Joao Lourenco, E-mail: joaobazzijr@gmail.com [Clinica Via Imagem, Xanxere, SC (Brazil); Matta, Eduardo Simoes da [Pro Circulacao - Clinica de Angiologia, Cirurgia Vascular e Ecografia Vascular, Xanxere, SC (Brazil); De Bortoli, Luciano [Materclinica Materno Infantil, Xanxere, SC (Brazil); De Bortoli, Felipe Raasch [Universidade Catolica de Pelotas (UCPel), Pelotas, RS (Brazil). Fac. of Medicine

    2012-05-15

    Poland's syndrome is a rare non-inherited congenital anomaly. The authors describe the classic radiologic findings of Poland's syndrome by reporting the case of a male four-year old patient with asymmetry of hands and chest, illustrating the fundamental imaging criteria for a conclusive diagnosis. (author)

  20. The concentration of retail in Poland

    Directory of Open Access Journals (Sweden)

    Michał Gazdecki

    2010-01-01

    Full Text Available The article discusses the processes of concentration taking place in retail in Poland. In spite of strong concentration processes, which took place after 2000, Poland still remains a country of dispersed retail structure. In the nearest years we can expect capital concentration (mainly takeovers in modern trade and contract concentration (for example, merchants’ societies in traditional trade.

  1. Understanding the Enigmatic SW Sex Stars

    Science.gov (United States)

    Szkody, Paula

    The SW Sex stars are a subgroup of cataclysmic variables that are known for several peculiar features, including high excitation single-peaked lines in their spectra, absorption features in the low excitation lines, phase offsets between the radial velocity curves and photometric eclipse times, unusual high velocity components, and orbital periods between 3-4 hrs. The cause of these peculiarities is controversial, with possibilities ranging from mass transfer stream impact and overflow at high mass transfer rates to magnetic propellers, winds and jets. As many of these suggestions depend on the inclination of the system, we propose to confront such theories by contrasting FUSE observations of the low inclination SW Sex star LS Peg and a more typical high inclination system DW UMa. The high quality, high resolution FUSE spectra we will obtain will allow us to construct detailed models of the inner accretion disk and velocity flows of both systems. This will resolve which of the properties are geometry dependent, and thereby lead to a basic advance in our understanding of this class of objects and ultimately, of the general effects of high mass transfer in close binaries.

  2. Policy factors affecting broadband development in Poland

    DEFF Research Database (Denmark)

    Henten, Anders; Windekilde, Iwona Maria

    2014-01-01

    Poland joined the EU in 2004 and still has one of the Europe’s least developed information societies. Broadband penetration in Poland is still amongst the lowest in the EU and significantly below the EU average. Considering the present state of information technology, the key challenge for Poland...... will gradually change the previous balance of power. The specific problem of the Polish market is its very poor infrastructure development and the lack of competitors on the fixed market. This translates into limited access to services for end users particularly in the rural areas. A much lower level...... and discuss broadband access development in Poland and the policy factors influencing this development as well as to examine national strategies used to stimulate service and infrastructure competition in Poland. There are, indeed, many other factors affecting broadband development such as the income level...

  3. Malaria in Poland in 2013.

    Science.gov (United States)

    Stępień, Małgorzata

    2015-01-01

    Evaluation of the epidemiological situation of imported malaria in Poland in 2013 compared to the data from previous years. The assessment was performed based on the results of the analysis of individual reports sent to the NIPH-NIH by sanitary-epidemiological stations and aggregated data published in the annual bulletins "Infectious diseases and poisonings in Poland". Cases were registered according to the case definition criteria applicable in the EU countries. In 2013, a total of 36 imported malaria cases were registered in Poland, 15 more than in 2012. No deaths were recorded. As much as 80% of all cases were imported from African countries, of whom the majority came from Nigeria, 14% from Asia and 6% from South America. Concurrent infection with dengue virus was confirmed in one person coming back from Philippines. Plasmodium species was determined in 35 of 36 cases by blood film or PCR test. Invasion with P. falciparum and P. vivax was found in 23 (66%) and 9 (26%) cases, respectively. There was also one case of each of the following: P. ovale, P. malariae and mixed invasion. As in previous years, in most cases, the invasion was associated with tourist trips (47%) or work-related travels (36%). Immigrants or students visiting the country of origin accounted for 11% of patients, in two cases (6%) purpose of the journey was not determined. As many as 7 patients used chemoprophylaxis, including two persons who took drugs in compliance with the recommendations. Despite a significant increase in the number of cases compared to previous years, the total number of imported malaria remains low. Persistent large number of delays in the diagnosis and a high percentage of severe malaria cases indicate the need to raise doctors awareness of the possibility of malaria incidence. Travelers should be also constantly reminded of the need to inform their GPs about the stay in the malaria endemic areas in the event of fever after returning.

  4. Studying sub-crustal reflectors in SW-Spain with wide-angle profiles

    Science.gov (United States)

    Palomeras, Imma; Ayarza, Puy; Carbonell, Ramon; Afonso, JuanCarlos; Diaz, Jordi

    2017-04-01

    It is nowadays widely accepted that the mantle is highly heterogeneous and has lithologies that are capable of giving impedance enough to be observed in seismic data. Nevertheless, observing those impedance contrasts at mantle depths is a challenging problem. SW Iberia has been sampled by different deep vertical reflection and wide-angle reflection/refraction experiments ILIHA, IBERSEIS, and ALCUDIA, and hence provide a good opportunity to study seismically sub-crustal reflectors. These datasets have imaged a conspicuous sub-crustal reflector. This mantle reflector was first identified on the IBERSEIS wide angle reflection shot-gathers at large offsets (above 180 km). It was modeled as a boundary located between 61-72 km depth with a Vp increase from 8.2 km/s to 8.3 km/s. The fact that this reflector was not identified in the coincident vertical incidence dataset led us to interpret it as a gradient zone. A correlation with the 'Hales gradient zone', i.e. the boundary between spinel and garnet peridotites, was our preferred interpretation. The ALCUDIA experiment also shows prominent sub-crustal arrivals with the same characteristics as those observed in the IBERSEIS wide-angle data. However, these reflections also appear, locally and at 19 s TWT, in the vertical incidence dataset. In addition, the ALCUDIA wide-angle dataset shows a deeper reflector that maybe preliminarily associated with mantle anisotropy or even with the lithosphere-asthenosphere boundary. Both upper mantle reflectors are modeled at 65 km and 100 km depth, respectively, shallowing to the north to 55 km and 90 km depth. Integration of the information provided by the IBERSEIS and ALCUDIA datasets with older and lower resolution data from the ILIHA project, where three sub-crustal phases were identified in SW Iberia, allows us to conclude that, in this area, mantle reflectivity is outstanding. Also, modeling of all the datasets contributes to map, at a regional scale, the Hales discontinuity or

  5. Two successive crustal melting events resulting from extensional exhumation and then thrusting of the Ronda Peridotites (South Spain)

    Science.gov (United States)

    Frasca, Gianluca; Gueydan, Frédéric; Poujol, Marc; Brun, Jean-Pierre; Parat, Fleurice; Monié, Patrick; Pichat, Alexandre; Maziers, Sophie

    2017-04-01

    The Alboran Domain, situated at the western end of the Mediterranean subduction system, is characterized by the Ronda Peridotites, one of the world largest exposures of sub-continental mantle. Using U-Pb (LA-ICP-MS) and Ar-Ar dating, we precisely dated two tectonic events associated with the Tertiary exhumation of the Ronda Peridotites. First, shearing along the Crust-Mantle Extensional Shear Zone caused, at ca. 22.5 Ma, mantle exhumation, local partial melting in the deep crust and coeval cooling in the upper crust. Second, the Ronda Peridotites Thrust triggered the final crustal emplacement of the peridotites onto the continental crust at ca. 21 Ma, as testified by granitic intrusions in the thrust hanging-wall. The tectonic evolution of the western Alboran Domain is therefore characterized by a fast switch from a continental lithosphere extension in a backarc setting, with sub-continental mantle exhumation, to a rift inversion by thrusting driven by shortening of the subduction upper plate.

  6. Crystal preferred orientation in peridotite ultramylonites deformed by grain size sensitive creep, étang de Lers, Pyrenees, France

    NARCIS (Netherlands)

    Drury, M.R.; Avé Lallemant, H.G.; Pennock, G.M.; Palasse, L.N.

    2011-01-01

    In naturally deformed upper mantle rocks a strong olivine crystallographic preferred orientation (CPO) occurs in rocks with grain sizes larger than about 15 mm. Finer grained peridotites tend to have weak to random olivine CPO. The different types of olivine CPO are usually interpreted in relation

  7. Experimental calibration of Forsterite-Anorthite-Ca-Tschermak-Enstatite (FACE) geobarometer for mantle peridotites

    Science.gov (United States)

    Fumagalli, P.; Borghini, G.; Rampone, E.; Poli, S.

    2017-06-01

    The crystallization of plagioclase-bearing assemblages in mantle rocks is witness of mantle exhumation at shallow depth. Previous experimental works on peridotites have found systematic compositional variations in coexisting minerals at decreasing pressure within the plagioclase stability field. In this experimental study we present new constraints on the stability of plagioclase as a function of different Na2O/CaO bulk ratios, and we present a new geobarometer for mantle rocks. Experiments have been performed in a single-stage piston cylinder at 5-10 kbar, 1050-1150 °C at nominally anhydrous conditions using seeded gels of peridotite compositions (Na2O/CaO = 0.08-0.13; X Cr = Cr/(Cr + Al) = 0.07-0.10) as starting materials. As expected, the increase of the bulk Na2O/CaO ratio extends the plagioclase stability to higher pressure; in the studied high-Na fertile lherzolite (HNa-FLZ), the plagioclase-spinel transition occurs at 1100 °C between 9 and 10 kbar; in a fertile lherzolite (FLZ) with Na2O/CaO = 0.08, it occurs between 8 and 9 kbar at 1100 °C. This study provides, together with previous experimental results, a consistent database, covering a wide range of P- T conditions (3-9 kbar, 1000-1150 °C) and variable bulk compositions to be used to define and calibrate a geobarometer for plagioclase-bearing mantle rocks. The pressure sensitive equilibrium: Mg_{2}SiO_{4}^Ol\\limits_{Forsterite} + CaAl_{2}Si_{2}O_{8}^{Pl\\limits_{Anorthite} = CaAl_{2}SiO_{6}^{Cpx}\\limits_{Ca-Tschermak} + Mg_{2}Si_{2}O_{6}^{Opx}\\limits_{Enstatite}, has been empirically calibrated by least squares regression analysis of experimental data combined with Monte Carlo simulation. The result of the fit gives the following equation: P=7.2( ± 2.9)+0.0078( ± 0.0021)T{{ }}+0.0022( ± 0.0001)T ln K, {R^2}=0.93, where P is expressed in kbar and T in kelvin. K is the equilibrium constant K = a CaTs × a en/ a an × a fo, where a CaTs, a en, a an and a fo are the activities of Ca-Tschermak in

  8. The Os isotopic variation of abyssal peridotites revised: A study from the ultra-slow spreading Gakkel Ridge

    Science.gov (United States)

    Büchl, A.; Snow, J. E.

    2003-04-01

    It is generally thought that the Os isotopic variation of abyssal peridotites (187Os/188Os varies from 0.120 to 0.129 after [1,2,3,4]) only exceeds the chondritic value of 0.127 [5] because of secondary alteration by seawater. In contrast supra-chondritic 187Os/188Os ratios in peridotites from ophiolites [6] and xenoliths from a subduction zone setting [7] have been ascribed to exchange of Os with radiogenic melts. We analysed the Os isotopic composition of 16 peridotites from the ultra-slow spreading Gakkel Ridge. The samples are unusually fresh for abyssal peridotites. The Os isotopic composition varies from 0.1208 to 0.1344 in the spinel-lherzolites, from 0.1176 to 0.1360 in the harzburgites and from 0.1325 to 0.1400 in the dunites. The reason for the supra-chondritic Os isotopic ratios could be (a) secondary alteration by seawater, (b) radiogenic ingrowth due to the decay of Re to Os, or (c) exchange with a radiogenic magmatic component. The fact that the degree of alteration does not correlate with Os isotopic composition, together with the high Os concentration in the peridotites compared with seawater, implies that the supra-chondritic 187Os/188Os ratios cannot be explained by secondary alteration processes. The similar and low Re and high Os concentrations in all samples rule out the ingrowth of 187Os as source for the supra-chondritic values. World-wide volcanic rocks mostly have supra-chondritic 187Os/188Os ratios. In addition it was shown recently that during melt percolation the peridotites can inherit the signature of percolating melts [6]. This suggests that the supra-chondritic 187Os/188Os ratios are due to the exchange with a magmatic component. This is supported by the observation that the dunites, which are expected to have the highest melt/rock ratio of all lithologies, have the most radiogenic signatures. We therefore suggest that the 187Os/188Os variation of abyssal peridotites is much larger than previously considered. However the origin of

  9. [Malaria in Poland in 2007].

    Science.gov (United States)

    Rosińska, Magdalena

    2009-01-01

    In Poland in 2007 there were 11 malaria cases confirmed according to the European Union cases definition reported through the routine surveillance system. All of them were imported, 82% from Africa, including 2 cases of relapse. Invasion with Plasmodium falciparum was diagnosed in 7 cases, mixed invasion in 2 cases and P. vivax- in one case. The majority of cases were in the age group 35-45 (8 cases) and were males (10 cases). Common reasons for travel to endemic countries were work-related (5 cases) and tourism or family visits (4 cases). Approximately half of the cases for whom the information was available used malaria chemoprophylaxis during their travel. Clinical course was severe in one case of P. falciparum malaria and the person died of the disease. The decreasing trend in malaria incidence in Poland is likely related to incomplete reporting as tourist and professional travel to endemic areas has not decreased and there is no indication of wider use ofchemoprophylaxis.

  10. Pavement noise measurements in Poland

    Science.gov (United States)

    Zofka, Ewa; Zofka, Adam; Mechowski, Tomasz

    2017-09-01

    The objective of this study is to investigate the feasibility of the On-Board Sound Intensity (OBSI) system to measure tire-pavement noise in Poland. In general, sources of noise emitted by the modern vehicles are the propulsion noise, aerodynamic resistance and noise generated at the tire-pavement interface. In order to capture tire-pavement noise, the OBSI system uses a noise intensity probe installed in the close proximity of that interface. In this study, OBSI measurements were performed at different types of pavement surfaces such as stone mastic asphalt (SMA), regular asphalt concrete (HMA) as well as Portland cement concrete (PCC). The influence of several necessary OBSI measurement conditions were recognized as: testing speed, air temperature, tire pressure and tire type. The results of this study demonstrate that the OBSI system is a viable and robust tool that can be used for the quality evaluation of newly built asphalt pavements in Poland. It can be also applied to generate reliable input parameters for the noise propagation models that are used to assess the environmental impact of new and existing highway corridors.

  11. Tetanus in Poland in 2012.

    Science.gov (United States)

    Zieliński, Andrzej

    2014-01-01

    Despite of the small number of cases reported in Poland tetanus is a permanent risk to unvaccinated people. The severity of the disease is associated with high case fatality, especially among people in older age groups. The aim of this paper is to present the data of epidemiological surveillance of tetanus in 2012. Principal source of the data is bulletin: "Infectious diseases and poisonings in Poland in 2012, and individual reports of cases of tetanus sent to the Department of Epidemiology, NIPH -NIH. In 2012, there were reported 19 cases of tetanus. 6 cases occurred in men, and 13 women. 13 cases occurred in persons over 69 years of age and in those age groups 6 cases were fatal. The paper describes the geographical distribution and the month of infection, the nature of the wounds which were portals of infection and the duration of incubation period of the cases. Severity of tetanus, despite a small number of cases each year leads to several deaths, which could be prevented by vaccination.

  12. [Malaria in Poland in 2009].

    Science.gov (United States)

    Stepiń, Małgorzata

    2011-01-01

    In Poland in 2009 were reported 22 malaria cases confirmed according to the EU case definition for the purposes of routine surveillance system. All of them were imported, including 1 case of recrudescence, 86% from Africa. In 18 cases P falciparum etiology was confirmed and in 2--P vivax, in 1--P ovale and 1 P malariae. Most cases occurred in the age group 21-40 years, there were 21 cases in males and 1 in female. Common reasons for travel to endemic countries were work-related visits (14 cases) and tourism (6 cases), one person who visited the family and in one case unknown reason for travel. Three persons used chemoprophylaxis during their travel but only one of them appropriately, relevant information was missing in 5 cases. Clinical course was severe in 7 cases of P falciparum malaria and medium-severe in one case. In 2009, there were no malaria deaths in Poland. Education on the prevention of malaria and pretravel health advising is still greatly needed.

  13. Why Should Poland Go Nuclear?

    Energy Technology Data Exchange (ETDEWEB)

    Marecki, J.; Duda, M.; Kerner, A.

    2007-07-01

    The paper presents an outcome of the optimisation analysis to showing the advantages of nuclear power development in Poland. The arguments, justifying the necessity to start the nuclear programme in Poland, are related to the energy security, economic generation and environmental features of the nuclear option. The energy security aspect means the necessity to cover the increasing demand for electricity with increasing diversification of fuels for power plants, also in the context of the growing domination of the main supplier of natural gas to Europe. The economic aspect means the necessity to achieve a structure of the electricity sources which would assure least generation costs in the conditions of limited potential of domestic fossil fuels. The environmental aspect means not only the necessity to ensure a structure of electricity generation sources which allows for compliance with the legally binding environmental requirements, but also which allows a minimal level of the environment pollution at the given stage of the development of electricity generation technologies. Additionally, the external costs of electricity generation by different fossil-fuelled and nuclear plants, as additional arguments in favour of nuclear option, are presented. (auth)

  14. Late Palaeozoic to Triassic formations unconformably deposited over the Ronda peridotites (Betic Cordilleras): Evidence for their Variscan time of crustal emplacement

    Energy Technology Data Exchange (ETDEWEB)

    Sanz de Galdeano, C.; Ruiz Cruz, M.D.

    2016-07-01

    The age of the emplacement of the Ronda Peridotites has been widely debated during recent decades, and ages ranging from the Palaeozoic to the early Miocene have been proposed, although most of the current interpretations suggest an Oligocene-Miocene age. In this article, we describe two meta-sedimentary formations (the lower one formed by detrital sediments and the upper one by marbles) that were unconformably deposited over the Ronda peridotites and now record low-grade metamorphism. The detrital formation contains layers of acidic rocks with an age of 269±9 Ma and the overlying marbles are assumed to be Triassic. The existence of these unconformable formations over the peridotites is crucial for the dating of the exhumation of the latter. The presence of peridotite clasts in the detrital formation indicates that peridotites were exposed during the Permian and other data suggest that peridotites were exhumed during the late Carboniferous. During the Alpine cycle, the peridotites operated as an element situated at the bottom of the tectonically higher Alpujarride/Sebtide unit (the Jubrique unit) and forming part of it, then being incorporated to the Alpine thrusts of this unit. (Author)

  15. Serpentinization of abyssal peridotites from the MARK area, Mid-Atlantic Ridge: Sulfur geochemistry and reaction modeling

    Science.gov (United States)

    Alt, J.C.; Shanks, Wayne C.

    2003-01-01

    The opaque mineralogy and the contents and isotope compositions of sulfur in serpentinized peridotites from the MARK (Mid-Atlantic Ridge, Kane Fracture Zone) area were examined to understand the conditions of serpentinization and evaluate this process as a sink for seawater sulfur. The serpentinites contain a sulfur-rich secondary mineral assemblage and have high sulfur contents (up to 1 wt.%) and elevated ??34Ssulfide (3.7 to 12.7???). Geochemical reaction modeling indicates that seawater-peridotite interaction at 300 to 400??C alone cannot account for both the high sulfur contents and high ??34Ssulfide. These require a multistage reaction with leaching of sulfide from subjacent gabbro during higher temperature (???400??C) reactions with seawater and subsequent deposition of sulfide during serpentinization of peridotite at ???300??C. Serpentinization produces highly reducing conditions and significant amounts of H2 and results in the partial reduction of seawater carbonate to methane. The latter is documented by formation of carbonate veins enriched in 13C (up to 4.5???) at temperatures above 250??C. Although different processes produce variable sulfur isotope effects in other oceanic serpentinites, sulfur is consistently added to abyssal peridotites during serpentinization. Data for serpentinites drilled and dredged from oceanic crust and from ophiolites indicate that oceanic peridotites are a sink for up to 0.4 to 6.0 ?? 1012 g seawater S yr-1. This is comparable to sulfur exchange that occurs in hydrothermal systems in mafic oceanic crust at midocean ridges and on ridge flanks and amounts to 2 to 30% of the riverine sulfate source and sedimentary sulfide sink in the oceans. The high concentrations and modified isotope compositions of sulfur in serpentinites could be important for mantle metasomatism during subduction of crust generated at slow spreading rates. ?? 2003 Elsevier Science Ltd.

  16. [Trichinellosis in Poland in 2010].

    Science.gov (United States)

    Sadkowska-Todys, Małgorzata; Gołab, Elzbieta

    2012-01-01

    Trichinellosis is still an epidemiological problem in Poland as well as in other countries in the European Union (EU). Across the EU, reporting cases oftrichinellosis is mandatory. In Poland, tirchinellosis is an endemic disease, occurring mainly in territories where it is customary to eat raw meat products prepared from pigs and wild boars. The aim of this work is to evaluate the epidemiological situation of trichinellosis in Poland in the year 2010 in comparison to previous years. Cases of trichinellosis infections were classified according to criteria contained in the definition approved by the European Committee on 28th April 2008 amending the decision 2002/253/EC, and was introduced in Poland in 2009. Case definitions used in are available at http://www.pzh. gov.pl/oldpage/epimeld/inne/Def_PL2_Rob1 h.pdf. An infection was classified and reported as Trichinella spp. if the genus of Trichinella that caused the infection was not specified using molecular examination. In 2010 the number of registered human trichinellosis cases was similar to the average number of cases from the last several years, and it did not exceed 55 (the exceptions were in 2004 and 2007, when larger outbreaks occurred). In 2010, 51 Trichinella infections were registered, yielding an infection rate of 0.13 per 100 000 inhabitants. The infections occurred in 5 voivodeships (table 1). Using the criteria from the definitions, 41 cases were classified as probable and 10 were confirmed cases. Trichinella infections diagnoses were based on the presence of clinical symptoms and an epidemiological link. Serological diagnostic tests confirming the presence of Trichinella antibodies was performed in approximately 20% of the cases. Four individual cases were reported, along with 4 outbreaks in which a total of 47 people were infected? The infections were generally mild. Twenty-two infected persons were hospitalised (43%). Just like in previous years, no trichinellosis-related deaths were reported. The

  17. The production of iron oxide during peridotite serpentinization: Influence of pyroxene

    Directory of Open Access Journals (Sweden)

    Ruifang Huang

    2017-11-01

    Full Text Available Serpentinization produces molecular hydrogen (H2 that can support communities of microorganisms in hydrothermal fields; H2 results from the oxidation of ferrous iron in olivine and pyroxene into ferric iron, and consequently iron oxide (magnetite or hematite forms. However, the mechanisms that control H2 and iron oxide formation are poorly constrained. In this study, we performed serpentinization experiments at 311 °C and 3.0 kbar on olivine (with <5% pyroxene, orthopyroxene, and peridotite. The results show that serpentine and iron oxide formed when olivine and orthopyroxene individually reacted with a saline starting solution. Olivine-derived serpentine had a significantly lower FeO content (6.57 ± 1.30 wt.% than primary olivine (9.86 wt.%, whereas orthopyroxene-derived serpentine had a comparable FeO content (6.26 ± 0.58 wt.% to that of primary orthopyroxene (6.24 wt.%. In experiments on peridotite, olivine was replaced by serpentine and iron oxide. However, pyroxene transformed solely to serpentine. After 20 days, olivine-derived serpentine had a FeO content of 8.18 ± 1.56 wt.%, which was significantly higher than that of serpentine produced in olivine-only experiments. By contrast, serpentine after orthopyroxene had a slightly higher FeO content (6.53 ± 1.01 wt.% than primary orthopyroxene. Clinopyroxene-derived serpentine contained a significantly higher FeO content than its parent mineral. After 120 days, the FeO content of olivine-derived serpentine decreased significantly (5.71 ± 0.35 wt.%, whereas the FeO content of orthopyroxene-derived serpentine increased (6.85 ± 0.63 wt.% over the same period. This suggests that iron oxide preferentially formed after olivine serpentinization. Pyroxene in peridotite gained some Fe from olivine during the serpentinization process, which may have led to a decrease in iron oxide production. The correlation between FeO content and SiO2 or Al2O3 content in olivine- and

  18. Nanoscale variations in 187Os isotopic composition and HSE systematics in a Bultfontein peridotite

    Science.gov (United States)

    Wainwright, A. N.; Luguet, A.; Schreiber, A.; Fonseca, R. O. C.; Nowell, G. M.; Lorand, J.-P.; Wirth, R.; Janney, P. E.

    2016-08-01

    Understanding the mineralogical controls on radiogenic chronometers is a fundamental aspect of all geochronological tools. As with other common dating tools, it has become increasingly clear that the Re-Os system can be impacted by multiple mineral formation events. The accessory and micrometric nature of the Re-Os-bearing minerals has made assessing this influence complex. This is especially evident in cratonic peridotites, where long residence times and multiple metasomatic events have created a complex melting and re-enrichment history. Here we investigate a harzburgitic peridotite from the Bultfontein kimberlite (South Africa) which contains sub-micron Pt-Fe-alloy inclusions within base metal sulphides (BMS). Through the combination of the focused ion beam lift-out technique and low blank mass spectrometry we were able to remove and analyse the Pt-Fe-alloy inclusions for their Re-Os composition and highly siderophile element (HSE) systematics. Six repeats of the whole-rock yield 187Os/188Os compositions of 0.10893-0.10965, which correspond to Re depletion model ages (TRD) of 2.69-2.79 Ga. The Os, Ir and Pt concentrations are slightly variable across the different digestions, whilst Pd and Re remain constant. The resulting HSE pattern is typical of cratonic peridotites displaying depleted Pt and Pd. The Pt-Fe-alloys have PUM-like 187Os/188Os compositions of 0.1294 ± 24 (2-s.d.) and 0.1342 ± 38, and exhibit a saw-tooth HSE pattern with enriched Re and Pt. In contrast, their BMS hosts have unradiogenic 187Os/188Os of 0.1084 ± 6 and 0.1066 ± 3, with TRD ages of 2.86 and 3.09 Ga, similar to the whole-rock systematics. The metasomatic origin of the BMS is supported by (i) the highly depleted nature of the mantle peridotite and (ii) their Ni-rich sulphide assemblage. Occurrence of Pt-Fe-alloys as inclusions within BMS grains demonstrates the genetic link between the BMS and Pt-Fe-alloys and argues for formation during a single but continuous event of silicate melt

  19. Compositional trends among Kaapvaal Craton garnet peridotite xenoliths and their effects on seismic velocity and density

    DEFF Research Database (Denmark)

    Schutt, Derek; Lesher, Charles

    2010-01-01

    We examine the modes and compositions of garnet-bearing peridotite xenoliths from the Kaapvaal Craton to quantify factors governing density and seismic velocity variations within metasomatically altered cratonic mantle. Three distinct compositional trends are resolved by principal component...... analysis. The first reflects differences in residue composition resulting from partial melting. The second is associated with orthopyroxene (opx) enrichment, possibly due to silica addition by subduction zone fluids in the source region of the xenoliths. The third principal component reflects garnet...... and clinopyroxene enrichment possibly as a consequence of melt infiltration. More than half of the mineral mode variance among Kaapvaal Craton xenoliths can be accounted for by opx enrichment. Melt depletion effects can account for as much as 30% of the variance, while less than 20% of the variance is associated...

  20. Lithospheric mantle deformation in the Yerer-Tullu Wellel Volcanotectonic Lineament: A study of peridotite xenoliths

    Science.gov (United States)

    Trestrail, K. R.; Rooney, T. O.

    2014-12-01

    Although a great deal is known about crustal extensional processes in the East African Rift System (EARS), questions remain as to the impact of extension on the continental lithospheric mantle. The northernmost portion of the EARS is the Main Ethiopian Rift (MER), which is divided into three sectors: the Northern, (NMER), Central (CMER), and the Southern Main Ethiopian Rift (SMER). The NMER-CMER transition coincides with the Yerer-Tullu Wellel volcanotectonic lineament (YTVL), and may represent a terrain boundary along which extension was directed during the Cenozoic. Here we present petrographic data from peridotite xenoliths contained within ~6 Ma lavas recovered along the western portion of the YTVL near Nekempte, Ethiopia to examine the characteristics of the lithospheric mantle, and how peridotite has responded to extensional strain. Our preliminary results show that the Nekempte xenoliths are deformed spinel-bearing lherzolites, which previous studies have constrained to the spinel lherzolites field at 1.1 GPa in the lithospheric mantle. Petrographic examination of these xenoliths reveals two generations of crystals. These generations are defined by both size and texture; the first generation (coarse crystals) being up to 4 mm in diameter and the second generation (fine crystals) being less than 1 mm in diameter. The samples contain two generations of olivine (Ol I and Ol II) and orthopyroxene (Opx I and Opx II), one generation of clinopyroxene (Cpx I), spinel (Spl I), amphibole (Amp), and many fluid inclusion trails. We compare these xenoliths to samples from Injibara, Lake Tana Province, approximately 200 km north of Nekempte on the Ethiopian Plateau, a region with less focused extensional strain. Xenoliths from Injibara are also spinel-bearing lherzolites, however they exhibit less strain and metasomatic textures in comparison to xenoliths from along the YTVL. Based on the petrographic and textural analyses performed, we propose that the larger scale

  1. Melt- rock reaction at oceanic peridotite-gabbro transition, through combined EBSD and in-situ mineral geochemistry on the Erro Tobbio peridotitic body (Ligurian ophiolites, Italy).

    Science.gov (United States)

    Basch, Valentin; Rampone, Elisabetta; Ildefonse, Benoit; Godard, Marguerite; Crispini, Laura

    2017-04-01

    Several lines of evidence have stressed that melt-rock reactions acting at the oceanic mantle-crust boundary play an important role in the chemical evolution of MORBs and the formation of the primitive (olivine-rich) lower oceanic crust. To address this issue, we performed detailed structural analyses and in-situ mineral geochemistry on the Erro-Tobbio (ET) ultramafic unit (Ligurian Alps, Italy), where impregnated mantle peridotites are primarily associated to a hectometre-size mafic body composed of troctolite to plagioclase-bearing wehrlite. The troctolitic body exhibits high complexity, with a host troctolite (Troctolite A) crosscut by troctolitic decametre-size pseudo-tabular bodies (Troctolite B). These different generations of troctolites show distinct modal compositions and textures. The host troctolite A displays a dominant millimetre-size corroded granular texture of olivine associated with dunite pods and a layering defined by poikilitic plagioclase enrichment. The contact between the mafic body and the host mantle peridotites is irregular, and defined by troctolite to wehrlite apophyses. The troctolite A shows microstructures and Crystallographic Preferred Orientation (CPO) indicative of a formation after impregnation of a mantle dunite by an olivine-undersaturated melt. This impregnation leads to olivine dissolution, associated with poikilitic plagioclase and clinopyroxene crystallization. This is indicated by a progressive randoming of the Axial-[100] CPO with olivine disaggregation and increasing melt input in the troctolite. The crosscutting troctolite B exhibits significant olivine textural variation, from fine-grained granular to deformed coarse-grained skeletal olivine. Olivine in the troctolite B shows CPO indicative of crystallization after magmatic flow, intrusive into the host troctolite A. Both troctolite types display large major and trace element variations in minerals, e.g. variation of Anorthite content (An = 54-67) in plagioclase at

  2. Poland

    OpenAIRE

    Szlanta, Piotr

    2014-01-01

    Niniejszy materiał jest udostępniony na licencji Creative Commons – Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0 DE. Pełne postanowienia tej licencji są dostępne pod: http://creativecommons.org/licenses/by-nc-nd/3.0/de/legalcode This paper presents the process of building an independent Polish state during the First World War, which, from the Polish perspective, was the most important result of this conflict. The article focuses mainly on the political and military ...

  3. [Malaria in Poland in 2008].

    Science.gov (United States)

    Stepień, Małgorzata

    2010-01-01

    There were 22 malaria cases confirmed according to the European Union cases definition registered in Poland in 2008. All of them were imported, 13 cases (59%) from Africa, 3 from Asia, 5 from Oceania and 1 from South America. Invasion with Plasmodium falciparum was confirmed in 14 cases, P. vivax in 4 cases, mixed invasion in 2 cases and in 2 cases species of Plasmodium was undetermined. There were 13 cases in males and 9 in females. Age at onset ranged from 23 to 58 years and majority of cases were in the age group 25-40. Common reason for travel to endemic countries were tourism (11 cases) and work-related visits (7 cases). Clinical course was severe in 6 cases of P. falciparum malaria and 1 person died because of the disease. Nine cases used chemoprophylaxis during their travel but only one of them appropriately, relevant information was missing in 6 cases.

  4. [Malaria in Poland in 2006].

    Science.gov (United States)

    Rosińska, Magdalena

    2008-01-01

    There were 19 cases of malaria meeting European Union case definition for confirmed case registered in Poland in 2006. All of them were imported, including 1 case of relapse: 17 from Africa, 1 from Asia and 1 from Oceania. Species of Plasmodium was determined for 12 cases (68%): P. falciparum in 12 cases and P. vivax in one. There were 15 cases in males and 4 in females. Age at onset ranged from 17 to 59 years and a considerable number of cases occurred in persons 50 years old or older (5.26%). Common reasons for travel to endemic countries included tourism or family visits (10 cases) and professional or missionary travel (5 cases). Only four cases used chemoprophylaxis and the relevant information was missing in 4 cases. In two cases of malaria caused by Pl. falciparum the clinical course was severe and one of them died.

  5. Uncooled infrared photodetectors in Poland

    Science.gov (United States)

    Piotrowski, J.; Piotrowski, A.

    2006-03-01

    The history and present status of the middle and long wavelength Hg1-xCdxTe infrared detectors in Poland are reviewed. Research and development efforts in Poland were concentrated mostly on uncooled market niche. Technology of the infrared photodetectors has been developed by several research groups. The devices are based on mercury-based variable band gap semiconductor alloys. Modified isothermal vapour phase epitaxy (ISOVPE) has been used for many years for research and commercial fabrication of photoconductive, photoelectromagnetic and other devices. Bulk growth and liquid phase epitaxy was also used. At present, the fabrication of IR devices relies on low temperature epitaxial technique, namely metalorganic vapour phase deposition (MOCVD), frequently in combination with the ISOVPE. Photoconductive and photoelectromagnetic detectors are still in production. The devices are gradually replaced with photovoltaic devices which offer inherent advantages of no electric or magnetic bias, no heat load and no flicker noise. Potentially, the PV devices could offer high performance and very fast response. At present, the uncooled long wavelength devices of conventional design suffer from two issues; namely low quantum efficiency and very low junction resistance. It makes them useless for practical applications. The problems have been solved with advanced 3D band gap engineered architecture, multiple cell heterojunction devices connected in series, monolithic integration of the detectors with microoptics and other improvements. Present fabrication program includes devices which are optimized for operation at any wavelength within a wide spectral range 1-15 μm and 200-300 K temperature range. Special solutions have been applied to improve speed of response. Some devices show picoseconds range response time. The devices have found numerous civilian and military applications.

  6. SW radiative effect of aerosol in GRAPES_GFS

    Science.gov (United States)

    Chen, Qiying

    2017-04-01

    The aerosol particles can scatter and absorb solar radiation, and so change the shortwave radiation absorbed by the atmosphere, reached the surface and that reflected back to outer space at TOA. Since this process doesn't interact with other processes, it is called direct radiation effect. The clear sky downward SW and net SW fluxes at the surface in GRAPES_GFS of China Meteorological Administration are overestimated in Northern multitudes and Tropics. The main source of these errors is the absence of aerosol SW effect in GRAPES_GFS. The climatic aerosol mass concentration data, which include 13 kinds of aerosol and their 14 SW bands optical properties are considered in GRAPES_GFS. The calculated total optical depth, single scatter albedo and asymmetry factor are used as the input to radiation scheme. Compared with the satellite observation from MISER, the calculated total optical depth is in good consistent. The seasonal experiments show that, the summer averaged clear sky radiation fluxes at the surface are improved after including the SW effect of aerosol. The biases in the clear sky downward SW and net SW fluxes at the surface in Northern multitudes and Tropic reduced obviously. Furthermore, the weather forecast experiments also show that the skill scores in Northern hemisphere and East Asia also become better.

  7. SELECTED PROBLEMS OF REVERSE LOGISTICS IN POLAND

    OpenAIRE

    Agata Mesjasz-Lech

    2009-01-01

    This paper presents the essence of reverse logistics and directions of physical and information flows between logistic network partners. It also analyses effects of implementation of the principles of reverse logistics in Poland in the years 2004-2007

  8. Joining NATO: Challenges Ahead for Poland

    National Research Council Canada - National Science Library

    Zakrzewski, Lech

    1999-01-01

    .... Particular research emphasis is placed upon Poland's efforts to redefine and restructure her civil-military relations and the turbulent transfer of control of the Polish military to democratically...

  9. Dr Stanislaw Huskowski, Mayor of Wroclaw, Poland

    CERN Document Server

    Patrice Loïez

    2002-01-01

    Dr Stanislaw Huskowski, Mayor of Wroclaw, Poland visiting the ATLAS magnet assembly hall, building 180 with Mr Carlo Lamprecht, State Councillor, Dr Stanislaw Huskowski and Dr Peter Jenni, ATLAS Spokesperson

  10. Dr Stanislaw Huskowski, Mayor of Wroclaw, Poland

    CERN Multimedia

    Patrice Loïez

    2002-01-01

    Dr Stanislaw Huskowski, Mayor of Wroclaw, Poland visiting the ATLAS magnet assembly hall, building 180. From l to r: Mr Carlo Lamprecht, State Councillor, Dr Stanislaw Huskowski and Dr Peter Jenni, ATLAS Spokesperson

  11. POLAND SYNDROME WITH DEXTROCARDIA: CASE REPORT

    African Journals Online (AJOL)

    2010-11-11

    Nov 11, 2010 ... present the case of Poland syndrome and dextrocardia in a young child and ... are many clinical variations of the syndrome including rib defects, absence of shoulder ... could, for example, explain the chest wall anomalies.

  12. Partial melting and refertilization of mantle peridotites in the Xigaze ophiolite: constraints from whole-rock and mineral geochemistry

    Science.gov (United States)

    Zhang, Chang; Liu, Chuan-Zhou; Wu, Fu-Yuan

    2016-04-01

    Ophiolites along the E-W trending Yarlung-Tsangpo Suture (YTS), which separates the Indian plate from the Eurasian plate, have been regarded as relics of the Neo-Tethyan Ocean. The Xigaze ophiolite in the central YTS has been extensively studied. One of the most intact crust-mantle sequences is preserved in the Luqu (or Beimarang) ophiolite. Mantle peridotites of the Luqu ophiolite are dominated by harzburgites, with 55-65% olivine, 30-40% orthopyroxene, 1-5% clinopyroxene and 1-3% spinel. Minor lherzolites and dunites are also outcropped, and the mode contents of clinopyroxene in lherzolite can be locally up to 10%. This contribution presented whole-rock major element and mineral chemistry including EMPA (Electronic MicroProbe Analysis) and clinopyroxene in situ trace elements. Whole rock Al2O3 (0.23-2.05%) and CaO (0.41-1.7%) contents are very low but show obviously inverse correlation with MgO (39.7-47.0%), indicating that the Luqu peridotites are residues of variable degrees of partial melting. This is supported by the Cr# (=molar Cr/(Cr+Al)) values of spinels which vary from 0.36 to 0.69. Meanwhile, the high Cr# values of spinels and homogenously high Mg# (= molar Mg/(Mg+Fe2+)) values of olivines, clustering at 0.91, indicate high degrees of partial melting. The low REE (rare earth elements) concentrations and chondrite-normalized distribution partterns of clinopyroxenes reflect ultra-depleted natures, with most showing LREE (light REEs) and MREE (medium REEs) depleted patterns and strong fractionations between MREEs and HREE (heavy REEs) ((Sm/Yb)N: 0.021-0.184). Based on the observations and analyses, a model of two-stage melting process was proposed that the primitive mantle underwent 2-8% melting in garnet stability field which was followed by 10-15% melting in spinel stability field. The clinopyroxenes in some peridotites exhibit obvious enrichment of somestrongly incompatible elements (such as sodium and LREE) that reveal later refertilization process for

  13. Convergence on local labour markets in Poland

    OpenAIRE

    Kusideł, Ewa

    2011-01-01

    The purpose of presented study was to verify a hypothesis of convergence on local labor markets in Poland. Convergence phenomenon, understood as economic development levels balancing (falling differentiation) has been known since the mid- 1950s. In Poland the convergence problems have been a specific subject of research since the accession to the European Union and the implementation of cohesion policy whose financing is largely related to co...

  14. Regional Unemployment and Industrial Restructuring in Poland

    OpenAIRE

    Newell, Andrew; Pastore, Francesco

    2000-01-01

    This paper studies regional unemployment inequality in Poland. We find that higher unemployment regions are those experiencing greater change in industrial structure. We also find high unemployment regions are those with higher inflow rates to unemployment rather than longer spells of unemployment. These findings suggest that regional unemployment varies importantly with job destruction in Poland. Econometric analysis of the determinants of employment to unemployment flows reinforces this imp...

  15. Income and its distribution in preindustrial Poland

    OpenAIRE

    Malinowski, Mikołaj; Luiten van Zanden, Jan

    2016-01-01

    This article presents per capita GDP and income distribution estimates for preindustrial Poland. It is based on a social table for the Voivodeship of Cracow in 1578. Our evidence indicates that income in Poland was distributed more equally than in contemporary Holland. However, the extraction rate was much higher than in the North Sea area. Furthermore, income inequality in the countryside of the Voivodeship was higher than inequality in Cracow. This can be explained by the demesne economy ba...

  16. Petrogenesis of fertile mantle peridotites from the Monte del Estado massif (southwest Puerto Rico): a preserved section of Proto-Caribbean oceanic lithospheric mantle?

    Science.gov (United States)

    Marchesi, Claudio; Jolly, Wayne T.; Lewis, John F.; Garrido, Carlos J.; Proenza, Joaquín. A.; Lidiak, Edward G.

    2010-05-01

    The Monte del Estado massif is the largest and northernmost serpentinized peridotite belt in southwest Puerto Rico. It is mainly composed of spinel lherzolite and minor harzburgite with variable clinopyroxene modal abundances. Mineral and whole rock major and trace element compositions of peridotites coincide with those of fertile abyssal peridotites from mid ocean ridges. Peridotites lost 2-14 wt% of relative MgO and variable amounts of CaO by serpentinization and seafloor weathering. HREE contents in whole rock indicate that the Monte del Estado peridotites are residues after low to moderate degrees (2-15%) of fractional partial melting in the spinel stability field. However, very low LREE/HREE and MREE/HREE in clinopyroxene cannot be explained by melting models of a spinel lherzolite source and support that the Monte del Estado peridotites experienced initial low fractional melting degrees (~ 4%) in the garnet stability field. The relative enrichment of LREE in whole rock is not due to secondary processes but probably reflects the capture of percolating melt fractions along grain boundaries or as microinclusions in minerals, or the presence of exotic micro-phases in the mineral assemblage. We propose that the Monte del Estado peridotite belt represents a section of ancient Proto-Caribbean (Atlantic) lithospheric mantle originated by seafloor spreading between North and South America in the Late Jurassic-Early Cretaceous. This portion of oceanic lithospheric mantle was subsequently trapped in the forearc region of the Greater Antilles paleo-island arc generated by the northward subduction of the Caribbean plate beneath the Proto-Caribbean ocean. Finally, the Monte del Estado peridotites belt was emplaced in the Early Cretaceous probably as result of the change in subduction polarity of the Greater Antilles paleo-island arc without having been significantly modified by subduction processes.

  17. Variscan deformation along the Teisseyre-Tornquist Zone in SE Poland: Thick-skinned structural inheritance or thin-skinned thrusting?

    Science.gov (United States)

    Krzywiec, P.; Gągała, Ł.; Mazur, S.; Słonka, Ł.; Kufrasa, M.; Malinowski, M.; Pietsch, K.; Golonka, J.

    2017-10-01

    Recently acquired seismic reflection data provide better insight in the structural style of extensive sedimentary series overlying the SW slope of the East European Craton (EEC) in Poland. The two main seismic datasets - the POLCRUST-01 profile and PolandSPAN survey - yielded contrasting thick - and thin-skinned structural models for the same structural units in SE Poland. We reattempt an interpretation of the POLCRUST-01 profile using techniques of cross-section balancing and restoration aided by 2D forward seismic modelling. An outcome is the thin-skinned structural model is. This solution relies on a continuous top of the EEC crystalline basement well represented in the seismic data as well as on fragmentary, yet conclusive seismic geometries in shallow depth intervals proving the Ediacaran-Palaeozoic series to be thrust and folded. A Variscan (late Carboniferous) compressional regime is consequently invoked to explain thin-skinned structuring of the pre-Permian sedimentary pile and > 20 km of calculated shortening. We demonstrate an ambiguous nature of the top-basement irregularities previously used as indicators of basement-rooted vertical faulting. The tilt and abrupt increase of the top-basement taper under the thin-skinned belt are attributed to pre-Ordovician tectonic processes operating along the SW margin of the EEC. Post-rift subsidence and/or flexural loading giving rise to a broken foreland plate are invoked.

  18. Experimental Studies on Dehydration Embrittlement of Serpentinized Peridotite and Effect of Pressure on Creep of Olivine

    Science.gov (United States)

    Xia, Gang

    The origin of intermediate depth earthquakes has been debated for 90 years yet is still under active discussion. These earthquakes are localized in double seismic zones in descending lithosphere; both zones originate very close to oceanic trenches. A leading proposed initiation mechanism for these earthquakes since 1968 has been dehydration embrittlement of serpentine under stress. Despite the considerable evidence favoring this mechanism, a major argument against it has been that the lower seismic zone initiates at ˜40 km depth almost immediately below trenches and there does not appear to be a vehicle to carry water sufficiently deep to hydrate otherwise dry lithosphere. To directly address this problem, an experimental study has been carried out to investigate the minimum amount of serpentine that is required to trigger the dehydration embrittlement instability in serpentinized peridotite at high pressure (1-3 GPa) and temperature (720-750˚C). The results show that embrittlement occurs during dehydration of antigorite (the phase of serpentine stable at elevated pressure) in a wide range of compositions but both nearly dry peridotite and extensively altered peridotite are ductile. Fresh, unaltered, synthetic harzburgite and harzburgite with 4 vol% distributed antigorite are ductile, as are specimens with greater than 65% antigorite. Only compositions between 8 vol% and 65 vol% antigorite develop the instability. We suggest that very small degrees of serpentinization do not release sufficient H 2O to trigger the instability and that extensive serpentinization avoids the instability because soft, ductile, antigorite becomes the interconnected matrix with olivine and pyroxene existing only as isolated crystals. In that case, dehydration simply facilitates flow. These systematics suggest that small amounts of H2O transported down deep normal (bending) faults at trenches are sufficient to enable the instability in the lower seismic zones, thus providing additional

  19. Mating system parameters in Stylosanthes guianensis (Aubl.) Sw ...

    African Journals Online (AJOL)

    ONOS

    2010-09-06

    Sep 6, 2010 ... Sw. based on RAPD markers. Lucimara ... AFLP, amplified fragment length polymorphism. such as ... guianensis under experimental conditions based on ... Cattle were grown in the field in two randomized block design.

  20. [Tetanus in Poland in 2010].

    Science.gov (United States)

    Zieliński, Andrzej; Rudowska, Jolanta

    2012-01-01

    Epidemiological assessment of the incidence of tetanus in Poland in 2010 was based on the analysis of aggregate data provided by the State Sanitary Inspection and published an annual newsletter: Infectious diseases and intoxications in Poland in 2010, compiled by MP Czarkowski, E Cielebak, B Kondej, E Staszewska, Warsaw in 2011 and based on an annual newsletter: Vaccinations in Poland in 2010, compiled by MP Czarkowski, E Cielebak, B Kondej, E Staszewska, Warsaw 2011. A more accurate characterization of disease was based on the individual reports sent to the Department of Epidemiology, NIPH-NIH. In the last decade the incidence of tetanus has remained below 0.08/100 000 inhabitants. The average annual incidence was lower than in the previous decade, but within the last ten years to the annual variation is difficult to assign a distinct incidence tendency. Rather, they correspond to random fluctuations. In 2010, 16 cases were reported, including which occurred in 2009. All cases was reported as probable--diagnosis based on clinical signs and information about injuries. Overall incidence was 0.042/100 000, which was small and not significanty different from incidence in 2009 (0.05/100 000). All cases in 2010, were over 59 years of age, which is a strong expression of the trend observed for years that the disease is present in older age groups where the level of vaccination against tetanus is particularly low. Among people infected, there were three men and 13 women. Four cases ended with deaths. Three of these were women, among whom mortality was 23.1%, and one death occurred in a man, mortality 33.3%. Three deaths occurred among the 6 cases in people over 79 years of age, mortality 50%. The incubation period of the disease in 3 cases was less than 7 days, in 4 cases 8-14 days, in 4 cases 15-21 days, in 2 cases 22 days and more. Portals of entry of infection in 7 cases accounted for abrasion or laceration, in 6 cases the puncture wound in one it was bitten wound, and

  1. Milestone Report - M31SW030904 - Sigma Team Coordination Meeting

    Energy Technology Data Exchange (ETDEWEB)

    Jubin, Robert Thomas [Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)

    2010-11-24

    This documents the completion of the FCR&D Level 3 milestone for the Off-Gas Sigma Team - ORNL work package (FTOR11SW0309), “Sigma Team Coordination Meeting” (M31SW030904), due 30 November 10. The subject meeting was held at Idaho National Laboratory on October 12 and 13, 2010. The agenda and meeting minutes are attached to this memo.

  2. P Wave and S Wave Acoustic Velocities of Partial Molten Peridotite at Mantle P-T and MHz Frequencies

    Science.gov (United States)

    Weidner, D. J.; Li, L.; Whitaker, M. L.; Triplett, R.

    2016-12-01

    The speed that acoustic waves travel in a partially molten peridotite are crucial parameters to detect not only the presence of melt in the Earth's deep interior, but also understand many issues about the structure and dynamics of the mantle. Technical challenges have hindered such measurements in the laboratory. Here we report the experimental results on the ultrasonic acoustic wave velocities in a partial molten peridotite using multi-anvil high pressure apparatus located at beamline BM6 Advance Photon Source. We use the newly installed ultrasonic equipment using the pulse-echo-overlap method coupled with D-DIA device. X-ray radiography is used to measure sample length at high P-T. The X-ray diffraction spectrum is used to determine the pressure and sample conditions. Precise measurements of P and S wave velocities are obtained at 60 and 35 MHz respectively and are nearly simultaneous. We use a double reflector method to enable measurement of elastic wave velocities of cold-pressed polycrystalline sample which is sintered in situ at high P-T. Experiments were carried out up to 3 GPa and 1500 oC. Our preliminary results indicate that the KLB1 peridotite sample experienced a few percent decrease of both p and s wave velocities as partial melting occurs. The data define a small decrease in the bulk modulus as well as the shear modulus upon melting. This implies that dynamic melting is a significant process at megahertz frequencies.

  3. Hepatitis A in Poland in 2014

    Science.gov (United States)

    Polański, Piotr

    The aim of this article is to assess the epidemiological situation of hepatitis A in Poland in 2014 with the regard to the recent years. The assessment was conducted based on the results of the analysis of data from the bulletins “Infectious diseases and poisonings in Poland in 2014” and “Vaccinations in Poland in 2014”, as well as information from the individual cases questionnaires and reports of epidemiological investigations in outbreaks of hepatitis A, submitted by the sanitary-epidemiological stations to the Department of Epidemiology in NIPH-NIH. In 2014 in Poland there were 76 cases of hepatitis A registered. Incidence per 100 000 inhabitants was 0.20, and in different voivodeships varied from 0.07 (in Dolnosląskie voivodeship) to 0.30 (in Małopolskie voivodeship). The incidence among male and female did not differ (and was 0.20/ 100 000). In 2014 despite the increase in the number of cases (comparing it to the previous year) no significant change in epidemiological situation of hepatitis A was observed. Poland is still regarded as a country of low endemicity of hepatitis A. In routine surveillance system there is no information concerning the professional affiliation of persons being vaccinated, whereas the vaccinations themselves are recommended in the Polish vaccination schedule. Particular attention should be directed towards the vaccinations of persons who take part in berries primal production, product of which Poland is a major exporter of in the EU. In the light of increasing number of international hepatitis A outbreaks (which could be characterized by the prolonged duration, as well as the high possibility of secondary cases appearing- especially in countries of low endemicity) the maintenance of high level routine surveillance in Poland gains importance. The latter could also contribute to the efficiency of epidemiological investigations in multistate outbreaks.

  4. Residential Electricity Consumption in Poland

    Directory of Open Access Journals (Sweden)

    Edyta Ropuszyńska-Surma

    2016-01-01

    Full Text Available Key factors influencing electricity consumption in the residential sector in Poland have been identified. A fixed-effects model was used, which includes time effects, and a set of covariates, based on the model developed by Houthakker et al. This model estimates electricity demand by using lagged values of the dependent variable along with current and lagged values of electricity prices, and other variables that affect electricity demand such as: population, economic growth, income per capita, price of related goods, etc. The model has been identified according to the research results of the authors and those obtained by Bentzen and Engsted. The set of covariates was extended to the lagged electricity price given by a tariff (taken from two years previous to the time of interest and heating degree days index, a very important factor in European Union countries, where the climate is temperate. The authors propose four models of residential electricity demand, for which a confidence interval of 95% has been assumed. Estimation was based on Polish quarterly data for the years 2003-2013. (original abstract

  5. Experimental Investigation and Simplistic Geochemical Modeling of CO2 Mineral Carbonation Using the Mount Tawai Peridotite

    Directory of Open Access Journals (Sweden)

    Omeid Rahmani

    2016-03-01

    Full Text Available In this work, the potential of CO2 mineral carbonation of brucite (Mg(OH2 derived from the Mount Tawai peridotite (forsterite based (Mg2SiO4 to produce thermodynamically stable magnesium carbonate (MgCO3 was evaluated. The effect of three main factors (reaction temperature, particle size, and water vapor were investigated in a sequence of experiments consisting of aqueous acid leaching, evaporation to dryness of the slurry mass, and then gas-solid carbonation under pressurized CO2. The maximum amount of Mg converted to MgCO3 is ~99%, which occurred at temperatures between 150 and 175 °C. It was also found that the reduction of particle size range from >200 to <75 µm enhanced the leaching rate significantly. In addition, the results showed the essential role of water vapor in promoting effective carbonation. By increasing water vapor concentration from 5 to 10 vol %, the mineral carbonation rate increased by 30%. This work has also numerically modeled the process by which CO2 gas may be sequestered, by reaction with forsterite in the presence of moisture. In both experimental analysis and geochemical modeling, the results showed that the reaction is favored and of high yield; going almost to completion (within about one year with the bulk of the carbon partitioning into magnesite and that very little remains in solution.

  6. Slab melting beneath the Cascades Arc driven by dehydration of altered oceanic peridotite

    Science.gov (United States)

    Walowski, Kristina J; Wallace, Paul J.; Hauri, E.H.; Wada, I.; Clynne, Michael A.

    2015-01-01

    Water is returned to Earth’s interior at subduction zones. However, the processes and pathways by which water leaves the subducting plate and causes melting beneath volcanic arcs are complex; the source of the water—subducting sediment, altered oceanic crust, or hydrated mantle in the downgoing plate—is debated; and the role of slab temperature is unclear. Here we analyse the hydrogen-isotope and trace-element signature of melt inclusions in ash samples from the Cascade Arc, where young, hot lithosphere subducts. Comparing these data with published analyses, we find that fluids in the Cascade magmas are sourced from deeper parts of the subducting slab—hydrated mantle peridotite in the slab interior—compared with fluids in magmas from the Marianas Arc, where older, colder lithosphere subducts. We use geodynamic modelling to show that, in the hotter subduction zone, the upper crust of the subducting slab rapidly dehydrates at shallow depths. With continued subduction, fluids released from the deeper plate interior migrate into the dehydrated parts, causing those to melt. These melts in turn migrate into the overlying mantle wedge, where they trigger further melting. Our results provide a physical model to explain melting of the subducted plate and mass transfer from the slab to the mantle beneath arcs where relatively young oceanic lithosphere is subducted.

  7. Chloritoid-bearing assemblages in eclogitised metagabbros of the Lanzo peridotite body (western Italian Alps)

    Science.gov (United States)

    Kienast, J. R.; Pognante, U.

    1988-01-01

    Dykes of metagabbro from the Lanzo peridotite body in the western Italian Alps contain Mg-chloritoidtalc-garnet-Na-pyroxenes ± chlorite or Fe-chloritoid-glaucophane-garnet-Na-pyroxenes eclogitic assemblages of Cretaceous age. In these metagabbros the metamorphic equilibration is incomplete and controlled by local equilibrium conditions; here the chemical gradients, which document the magmatic microstructural domains and the diffusion patterns during metamorphism, survive the eclogitic crystallisation. Concentration of elements like Al, Mg and Fe near the boundaries between the magmatic domains favours the crystallisation, in reaction coronas, of Mg-rich chloritoid in Mg metagabbro and of Fe-rich chloritoid in FeTi metagabbro. Phase compatibilities in the Al 2O 3FeOMgO( ± SiO 2 ± H 2O) system suggest temperatures around 400-500°C at approximate pressures of 15-18 kbar for the eclogitic metamorphism of the Lanzo rocks. In spite of the difficulties and of the inaccuracies of these thermobarometric estimates, the inferred P- T values are in good agreement with determinations involving Na-pyroxenes and garnets.

  8. Experimental determination of CO2 content at graphite saturation along a natural basalt-peridotite melt join: Implications for the fate of carbon in terrestrial magma oceans

    Science.gov (United States)

    Duncan, Megan S.; Dasgupta, Rajdeep; Tsuno, Kyusei

    2017-05-01

    Knowledge of the carbon carrying capacity of peridotite melt at reducing conditions is critical to constrain the mantle budget and planet-scale distribution of carbon set at early stage of differentiation. Yet, neither measurements of CO2 content in reduced peridotite melt nor a reliable model to extrapolate the known solubility of CO2 in basaltic (mafic) melt to solubility in peridotitic (ultramafic) melt exist. There are several reasons for this gap; one reason is due to the unknown relative contributions of individual network modifying cations, such as Ca2+ versus Mg2+, on carbonate dissolution particularly at reducing conditions. Here we conducted high pressure, temperature experiments to estimate the CO2 contents in silicate melts at graphite saturation over a compositional range from natural basalts toward peridotite at a fixed pressure (P) of 1.0 GPa, temperature (T) of 1600 °C, and oxygen fugacity (log ⁡ fO2 ∼ IW + 1.6). We also conducted experiments to determine the relative effects of variable Ca and Mg contents in mafic compositions on the dissolution of carbonate. Carbon in quenched glasses was measured and characterized using Fourier transform infrared spectroscopy (FTIR) and Raman Spectroscopy and was found to be dissolved as carbonate (CO32-). The FTIR spectra showed CO32- doublets that shifted systematically with the MgO and CaO content of silicate melts. Using our data and previous work we constructed a new composition-based model to determine the CO2 content of ultramafic (peridotitic) melt representative of an early Earth, magma ocean composition at graphite saturation. Our data and model suggest that the dissolved CO2 content of reduced, peridotite melt is significantly higher than that of basaltic melt at shallow magma ocean conditions; however, the difference in C content between the basaltic and peridotitic melts may diminish with depth as the more depolymerized peridotite melt is more compressible. Using our model of CO2 content at

  9. Contribution to chorology of Xylobolus frustulatus in Poland

    Directory of Open Access Journals (Sweden)

    Małgorzata Stasińska

    2013-12-01

    Full Text Available Xylobolus frustulatus (Pers.: Fr. Boidin, one of the rare and threatened fungi in Poland, is reported from two new localities in Western Pomerania and Western Carpathians. Updated map of distribution of Xylobolus frustulatus in Poland is provided.

  10. Hypocreopsis lichenoides P. Karst. (Fungi, Ascomycetes, new to Poland

    Directory of Open Access Journals (Sweden)

    Małgorzata Stasińska

    2011-01-01

    Full Text Available Hypocreopsis lichenoides, a fungus found for the first time in Poland, is characterized and illustrated. The paper presents the distribution of the species in Poland and gives its morphological and ecological description.

  11. Practical Development of Modern Mass Media Education in Poland

    Science.gov (United States)

    Fedorov, Alexander

    2012-01-01

    Practical development of modern mass media education in Poland. The paper analyzes the main ways of practical development of modern media education (1992-2012 years) in Poland: basic technologies, main events, etc.

  12. Retail Developments in Poland, Kazakhstan, and Ukraine: A Comparative Analysis

    National Research Council Canada - National Science Library

    Lalita A Manrai; Ajay K Manrai; Dana-Nicoleta Lascu; David Dickerson

    2015-01-01

    ...), and a current CIS country (Kazakhstan). Poland is considered to be the lead country, Ukraine is considered to be the lag country, and Kazakhstan is considered to fall in between Poland and Ukraine in terms of retail developments...

  13. Phlogopite-bearing peridotite from the 25°S oceanic core complex, along the Central Indian Ocean Ridge

    Science.gov (United States)

    Soda, Y.; Igarashi, M.; Ogasawara, Y.; Takagi, H.; Sawaguchi, T.; Neo, N.; Morishita, T.; Nakamura, K.; Kumagai, H.; Yk05-16Leg1 Scientific Party

    2010-12-01

    The 25°S oceanic core complex (OCC) is located nearby the Rodriguez Triple Junction in the Indian Ocean. We performed three dives of manned submersible, SHINKAI 6500, during YK05-16 (Kumagai et al., 2008, Morishita et al., 2009), and corrected samples directly from the surface of the OCC. Deformed rocks described here are peridotite, gabbro, basalt, breccia and their metasomatic products. Peridotite is altered to talc-rich rocks and amphibole schist. Weakly metasomatized part of peridotite consists of olivine, orthopyroxene, phlogopite and Cr-spinel. Olivine and orthopyroxene grains show ductile deformation textures. Phlogopite exists in grain boundaries and fractures of olivine grains. Most of phlogopite grains have undergone chloritization with various degrees. In the phlogopite abounding part, array of them are made up of the foliation. Cr-spinel (altered to ferrite chromite) is surrounded by phlogopite. Serpentine (chrysotile; identified by Laser Raman spectroscopy) occurs only in talc vein walls and solid inclusions (Boschi et al., 2006, Schroeder et al., 2007), the fault rocks from the 25°S OCC show that the strong fluid infiltration and the deformation concentration on metasomatic rocks along the detachment fault surface. However, comparison with occurrences of other OCC regions, it is a difference that absences of serpentinite clasts in the breccia and existences of phlogopite in the peridotite. The deformational and metasomatic properties of the fault rocks from the OCC surface should depend on the depth and timing of fluid circulation in the mantle peridotite. References Boschi, C. et al., 2006, Geochem. Geophys. Geosyst., 7, doi: 10.1029/2005GC001074 Escartin, J. et al., 2003, Geochem. Geophys. Geosyst., 4, doi: 10.1029/2002GC000472 Kumagai, H. et al., 2008, Geofluids, 8, 239-251 Morishita, T. et al., 2009, Jour. Petrol. 50, 1299-1325 Schroeder, T. and John, B.E., 2004, Geochem. Geophys. Geosyst., 5, doi: 10.1029/2004GC000728 Schroeder, T. et al

  14. Russia and Poland: Problems of Inevitable Coexistence

    Directory of Open Access Journals (Sweden)

    Dmitriy V. Ofitserov-Belskiy

    2014-01-01

    Full Text Available Over the last quarter of the century relations between Russia and Poland are balancing between trying to understand the burden of mutual guilt and a desire to construct non-emotional pragmatic relations. Sources of tension vary. In particular, it is the desire of Poland to position itself as a valued player in NATO and the EU and the role distance between the two countries in IR system, which does not allow Russia to maintain an equal political dialogue with Poland. In fact, Poland is not afraid of a direct threat from Russia, but the worst scenario is the one in which Russia without changing the content of its imperial policy can be accepted as a full partner in the international community. The evolution of Russian statehood and national specifics of democracy is largely determined the assessment of the prospects of Russian politics in Poland. The mistake of Polish diplomacy last years was that it took no direct efforts to improve relations with Russia, but only tried to impose the dialogue on Russian authorities. Diplomatic methods were designed to hurt Russian interests and to create a topic for discussion. In response, after 2006 Russia chose the tactic of ignoring Poland. But, ignoring Polish authorities, Russian politicians acted similarly with other political forces. In Poland among influential political forces, there was and there is still no loyalty to Russia. For Russian interests it is no matter who are or will be in power in Poland. However as a rule, it is an important factor that foreign policy decisions are de facto within the competences of the President and the government, as well as experiencing a significant influence of the parliamentary forces. Recent trends show no tangible innovations in bilateral programme. But innovations appear in multilateral and conflict enough issues, such as deployment of US missile defense system in Poland or Polish supervision of "Eastern Partnership" programme. The main problem is low self

  15. IS INLAND SHIPPING NEEDED IN POLAND?

    Directory of Open Access Journals (Sweden)

    Ryszard Rolbiecki

    2014-06-01

    Full Text Available In Poland, inland shipping plays only a mariginal role in transport needs fulfillment. Inland shipping has a share of mere 0,3% in goods transport modal split. The reason for this is poor and variable technical parameters of inland waterways together with adverse legal regulations. Different situation takes place in Western European countries, in which the development of this mode of transport is viewed as a way of road transport develop-ment restraint. In Poland, the need to move some of the volume from road transport to in-land shipping is specifically observed within marine ports surroundings. Because of their complex nature, the investments in inland shipping infrastructure would also be helpful in solving the current problems of water management. Inland waterways in Poland guaran-tee neither an adequate level of flood protection, nor the water needs fulfillment of do-mestic economy. When it comes to water reserves, Poland is one of the most deficient countries in Europe. Thus there is a need to invest in inland waterways in Poland.

  16. Quaternary stratigraphy and palaeogeography of Poland

    Science.gov (United States)

    Marks, Leszek; Dzierżek, Jan; Janiszewski, Robert; Kaczorowski, Jarosław; Lindner, Leszek; Majecka, Aleksandra; Makos, Michał; Szymanek, Marcin; Tołoczko-Pasek, Anna; Woronko, Barbara

    2016-09-01

    Though the stratigraphical and palaeogeographical framework of the Quaternary in Poland is still to be completed, several crucial points have been confirmed recently. The preglacial series, accepted for years as belonging to the Lower Pleistocene, is undoubtedly of Early Pliocene age, with a huge hiatus above almost until the uppermost Lower Pleistocene. The earliest glaciation in Poland (Nidanian) occurred at about 900 ka BP when the ice sheet reached the mid-southern part of the country. The following Podlasian Interglacial embraced the Brunhes/Matuyama boundary in the middle, in a similar fashion to the corresponding Cromerian Complex in Western Europe. The late Early and early Middle Pleistocene interglacials in Poland comprised 2-3 optima each, whereas every one of the younger interglacials was characterised by a single optimum only. The Late Vistulian ice sheet was most extensive in the western part of Poland (Leszno Phase) whereas the younger Poznań Phase was more extensive in the central and eastern part of the country. This was due to the varied distance from the glaciation center in Scandinavia, making the ice sheet margin reach a terminal position in different times. Palaeoclimatological research in the Tatra Mountains has provided new evidence for the atmospheric circulation over Europe. During cold phases of the Pleistocene in Poland a continental climate extended further westwards, quite the opposite that occurring during warmer intervals.

  17. Petrography and mineral chemistry of wehrlites in contact zone of gabbro intrusions and mantle peridotites of the Naein ophiolite

    Directory of Open Access Journals (Sweden)

    Farhad Ghaseminejad

    2014-10-01

    Full Text Available Introduction Geological background Ophiolites have played a major role in our understanding of Earth’s processes ranging from seafloor spreading, melt evolution and magma transport in oceanic spreading centers, and hydrothermal alteration and mineralization of oceanic crust to collision tectonics, mountain building processes, and orogeny. They provide the essential structural, petrological, geochemical, and geochronological evidence to document the evolutionary history of ancient continental margins and ocean basin. Ophiolites include a peridotitic mantle sequence, generally characterized by high-temperature plastic deformation and residual chemistry, and a comagmatic crustal sequence (gabbros, diabase dikes, and submarine basalts, weakly or not deformed. According to this interpretation, ophiolites were allochthonous with respect to their country rocks. They were assembled during a primary accretion stage at an oceanic spreading center, and later tectonically emplaced on a continental margin or island arc (Dilek, 2003. The indigenous dikes of pyroxenites and gabbros that were injected into a melting peridotite, or intrusive dikes of pyroxenite and gabbro that injected when the peridotite was fresh and well below its solidus, are discussed in different ophiolite papers. Pyroxenite formation and contact of gabbro and mantle peridotite are discussed in different articles (Dilek, 2003. When a gabbro intrude a fresh mantle peridotite could not significantly react with it, but if intrusion occurs during the serpentinization, the gabbro will change to rodingite. Geological setting The Naein ophiolitic melanges comprise the following rock units: mantle peridotites (harzburgite, lherzolite, dunite, with associated chromitite, gabbro, pyroxenite, sheeted and swarm dikes, massive basalts, pillow lava, plagiogranite, radiolarian chert, glaubotruncana limestone, rodingite, listvenite, and metamorphic rocks (foliated amphibolitic dike, amphibolite, skarn

  18. Confessional and catechetical nature of religious education in Poland

    Directory of Open Access Journals (Sweden)

    Paweł Mąkosa

    2015-09-01

    Full Text Available This paper aims at bringing to light a presentation of the nature of religious education in Poland. This study will therefore present a brief historical outline of religious upbringing in Poland, its current organisational regulations and the principles of religious education in schools. In our summary, we will present the level of effectiveness of religious education in Poland, and we will also explore the discussion on the reformation of religious education in Poland which is being worked upon.

  19. Wind energy development as a part of Poland's industrial development

    DEFF Research Database (Denmark)

    Stoerring, Dagmara; Hvelplund, Frede Kloster

    2003-01-01

    The paper concludes with recommendations on how to make wind energy development a part of the industrial development in Poland by introducing renewable energy support mechanisms to improve the conditions for companies to develop wind technology in Poland.......The paper concludes with recommendations on how to make wind energy development a part of the industrial development in Poland by introducing renewable energy support mechanisms to improve the conditions for companies to develop wind technology in Poland....

  20. Calcium isotopic fractionation in mantle peridotites by melting and metasomatism and Ca isotope composition of the Bulk Silicate Earth

    Science.gov (United States)

    Kang, Jin-Ting; Ionov, Dmitri A.; Liu, Fang; Zhang, Chen-Lei; Golovin, Alexander V.; Qin, Li-Ping; Zhang, Zhao-Feng; Huang, Fang

    2017-09-01

    To better constrain the Ca isotopic composition of the Bulk Silicate Earth (BSE) and explore the Ca isotope fractionation in the mantle, we determined the Ca isotopic composition of 28 peridotite xenoliths from Mongolia, southern Siberia and the Siberian craton. The samples are divided in three chemical groups: (1) fertile, unmetasomatized lherzolites (3.7-4.7 wt.% Al2O3); (2) moderately melt-depleted peridotites (1.3-3.0 wt.% Al2O3) with no or very limited metasomatism (LREE-depleted cpx); (3) strongly metasomatized peridotites (LREE-enriched cpx and bulk rock) further divided in subgroups 3a (harzburgites, 0.1-1.0% Al2O3) and 3b (fertile lherzolites, 3.9-4.3% Al2O3). In Group 1, δ44/40Ca of fertile spinel and garnet peridotites, which experienced little or no melting and metasomatism, show a limited variation from 0.90 to 0.99‰ (relative to SRM 915a) and an average of 0.94 ± 0.05‰ (2SD, n = 14), which defines the Ca isotopic composition of the BSE. In Group 2, the δ44/40Ca is the highest for three rocks with the lowest Al2O3, i.e. the greatest melt extraction degrees (average 1.06 ± 0.04 ‰, i.e. ∼0.1‰ heavier than the BSE estimate). Simple modeling of modal melting shows that partial melting of the BSE with 103 ln ⁡αperidotite-melt ranging from 0.10 to 0.25 can explain the Group 2 data. By contrast, δ44/40Ca in eight out of nine metasomatized Group 3 peridotites are lower than the BSE estimate. The Group 3a harzburgites show the greatest δ44/40Ca variation range (0.25-0.96‰), with δ44/40Ca positively correlated with CaO and negatively correlated with Ce/Eu. Chemical evidence suggests that the residual, melt-depleted, low-Ca protoliths of the Group 3a harzburgites were metasomatized, likely by carbonate-rich melts/fluids. We argue that such fluids may have low (≤0.25‰) δ44/40Ca either because they contain recycled crustal components or because Ca isotopes, similar to trace elements and their ratios, may be fractionated by kinetic and

  1. Subduction initiation and recycling of Alboran domain derived crustal components prior to the intra-crustal emplacement of mantle peridotites in the Westernmost Mediterranean: isotopic evidence from the Ronda peridotite

    Science.gov (United States)

    Varas-Reus, María Isabel; Garrido, Carlos J.; Bosch, Delphine; Marchesi, Claudio Claudio; Acosta-Vigil, Antonio; Hidas, Károly; Barich, Amel

    2014-05-01

    During Late Oligocene-Early Miocene different domains formed in the region between Iberia and Africa in the westernmost Mediterranean, including thinned continental crust and a Flysch Trough turbiditic deposits likely floored by oceanic crust [1]. At this time, the Ronda peridotite likely constituted the subcontinental lithospheric mantle of the Alboran domain, which mantle lithosphere was undergoing strong thinning and melting [2] [3] coevally with Early Miocene extension in the overlying Alpujárride-Maláguide stacked crust [4, 5]. Intrusive Cr- rich pyroxenites in the Ronda massif records the geochemical processes occurring in the subcontinental mantle of the Alboran domain during the Late Oligocene [6]. Recent isotopic studies of these pyroxenites indicate that their mantle source was contaminated by a subduction component released by detrital crustal sediments [6]. This new data is consistent with a subduction setting for the late evolution of the Alboran lithospheric mantle just prior to its final intracrustal emplacement in the early Miocene Further detailed structural studies of the Ronda plagioclase peridotites-related to the initial stages of ductile emplacement of the peridotite-have led to Hidas et al. [7] to propose a geodynamic model where folding and shearing of an attenuated mantle lithosphere occurred by backarc basin inversion followed by failed subduction initiation that ended into the intracrustal emplacement of peridotite into the Alboran wedge in the earliest Miocene. This hypothesis implies that the crustal component recorded in late, Cr-rich websterite dykes might come from underthrusted crustal rocks from the Flysch and/or Alpujárrides units that might have been involved in the earliest stages of this subduction initiation stage. To investigate the origin of crustal component in the mantle source of this late magmatic event recorded by Cr-pyroxenites, we have carried out a detail Sr-Nd-Pb-Hf isotopic study of a variety of Betic

  2. Sepsis: Medical errors in Poland.

    Science.gov (United States)

    Rorat, Marta; Jurek, Tomasz

    2016-01-01

    Health, safety and medical errors are currently the subject of worldwide discussion. The authors analysed medico-legal opinions trying to determine types of medical errors and their impact on the course of sepsis. The authors carried out a retrospective analysis of 66 medico-legal opinions issued by the Wroclaw Department of Forensic Medicine between 2004 and 2013 (at the request of the prosecutor or court) in cases examined for medical errors. Medical errors were confirmed in 55 of the 66 medico-legal opinions. The age of victims varied from 2 weeks to 68 years; 49 patients died. The analysis revealed medical errors committed by 113 health-care workers: 98 physicians, 8 nurses and 8 emergency medical dispatchers. In 33 cases, an error was made before hospitalisation. Hospital errors occurred in 35 victims. Diagnostic errors were discovered in 50 patients, including 46 cases of sepsis being incorrectly recognised and insufficient diagnoses in 37 cases. Therapeutic errors occurred in 37 victims, organisational errors in 9 and technical errors in 2. In addition to sepsis, 8 patients also had a severe concomitant disease and 8 had a chronic disease. In 45 cases, the authors observed glaring errors, which could incur criminal liability. There is an urgent need to introduce a system for reporting and analysing medical errors in Poland. The development and popularisation of standards for identifying and treating sepsis across basic medical professions is essential to improve patient safety and survival rates. Procedures should be introduced to prevent health-care workers from administering incorrect treatment in cases. © The Author(s) 2015.

  3. Sindrome de Poland: un caso con dextrocardia.

    Directory of Open Access Journals (Sweden)

    Carlos Tori Tori

    1999-04-01

    Full Text Available We report on a case of Poland anomaly (defect of the muscle pectoralis major and symbrachydactyly on the same side with dextrocardia. The absence of the pectoralis major muscle without the limb anomaly can be a variant of the Poland sequence (1.While most of the reported cases of this syndrome is in the right side (2 and without rib defects, in our patient the anomaly was on the left side, accompanied by dextrocardia and with anomalies of the rib cage. ( Rev Med Hered 1999; 10:76-82 .

  4. Distribution of the Common Adder Vipera berus and the Slow Worm Anguis fragils in Silesia, SW Poland

    Directory of Open Access Journals (Sweden)

    Kopij Grzezgorz

    2015-12-01

    Full Text Available During the years 2004-2008 the distribution of the Common Adder and the Slow Worm were studied in Silesia through questionnaire directed to forest inspectorates (n=871; 83.8% of them responded. These data were tested through field work in several randomly selected inspectorates. Both species were found to be widespread in the region, with a few strongholds identified in Sudety Mts. and larger forest complexes. The Common Adder was recorded in 68.5% of forest districts which responded, while the Slow Worm – in 73.6% of those districts. Changes in distribution and population trends could not be derived, since no reliable data were available from previous years.

  5. Raman spectroscopy of organic, solid and fluid inclusions in the Oldest Halite of LGOM area (SW Poland)

    Science.gov (United States)

    Toboła, Tomasz

    2018-01-01

    Raman spectroscopy was applied to determine the degree of recrystallization and the influence of the secondary solution migration on the Oldest Halite (Na1) in Lubin-Głogów Copper District (LGOM). Numerous organic matter (OM) inclusions which generally show weak structural ordering was found in halite crystals. In this context they are similar to solid bitumens or carbonaceous matter of low thermal alteration. The difference in the Raman line-shape of OM indicated various thermal alteration of salt from the Oldest Halite formation due to hot fluid flow. Solutions included in the secondary fluid inclusions often contain dissolved gases such as CH4, N2, H2S. The presence of these gases is connected with migration process from basement to the salt formation. Moissanite in fluid inclusions was accidentally trapped during inclusion formation, i.e. is not a daughter mineral. It was also found in the halite as an individual solid inclusions as well as in the anhydrite concentrations. Raman spectroscopy allowed to determine also such solid inclusions in halite as celestine, magnesite, pyrite, lepidocrocite and goethite as well as hydrocarbons.

  6. Fossil zygospores of Zygnemataceae and other microremains of freshwater algae from two Miocene palaeosinkholes in the Opole region, SW Poland

    Directory of Open Access Journals (Sweden)

    Worobiec Elżbieta

    2014-06-01

    Full Text Available Algal microremains were encountered during palynological investigation of deposits filling two Miocene palaeosinkholes excavated in the Tarnów Opolski and Górażdże quarries. Algal microfossils of 40 species were identified, most of which are frequent non-pollen palynomorphs occurring in Neogene deposits. The microfossils most frequently found in all studied samples belong to the genera Sigmopollis and Botryococcus. Both algal assemblages contain a significant proportion of resting cells (zygospores = hypnozygotes such as Cycloovoidites, Diagonalites, Megatetrapidites, Ovoidites, Stigmozygodites, and Tetrapidites, probably fossil zygospores of members of the Zygnemataceae family (Mougeotia, Spirogyra, Zygnema. Some specimens probably related to desmid zygospores (Closteritetrapidites, Monopunctites, Planctonites, freshwater dinoflagellate cysts, and Prasinophyceae (Leiosphaeridia were found. Most of the identified fossilised remains of algae are often seen in sediments indicating meso- to eutrophic conditions and are characteristic for stagnant or slowly flowing shallow waters. Fossil algae of Pediastrum and Tetraedron genera were recorded in samples from the Górażdże palaeosinkhole, suggesting small differences in the aquatic habitat (e.g. water depth between ponds in the sinkholes. Three new fossil species related to zygospores of the Zygnemataceae are described: Ovoidites vangeelii sp. nov., Tetrapidites grandis sp. nov., and Tetrapidites opolensis sp. nov

  7. The pools of soil organic carbon accumulated in the surface layers of forest soils in the Karkonosze Mountains, SW Poland

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    Szopka Katarzyna

    2016-06-01

    Full Text Available Differentiation of soil organic carbon (SOC concentrations and pools in topsoil horizons of forest soils in the Karkonosze Mountains was examined in relation to environmental and human-induced factors, with special focus on altitudinal gradient, related climatic conditions, and a zonality of vegetation. The samples were collected from the forest litter and soil layers 0–10 cm and 10–20 cm, in 621 plots arranged in a regular network of monitoring established in the Karkonosze National Park. The concentrations of SOC were determined in laboratory and used for calculation of SOC pools. Four elevation zones were distinguished for analysis: 500–750 m, 750–1000 m, 1000–1250 m, and >1250 m. The concentrations of SOC in forest litter (38.3–44.1% showed an insignificant increasing trend with altitude. The concentrations of SOC in the layers 0–10 cm and 10–20 cm, were in a very broad range 0.27–47.6%, thus indicating a high differentiation, and also tended to insignificantly increase along with altitude. The largest share of accumulated SOC pools was proved to be present in the layer 0–10 cm, except for the highest zone >1250 m in which forest litter contains slightly larger amounts of SOC. The pools of SOC accumulated in the 20 cm thick topsoil and forest litter turned out to vary considerably (3.6–58.2 kg·m−2, but the mean values and medians in particular elevation zones fall in a narrow range 10.5–11.9 kg·m−2, close to the values reported from the Alps. The lack of statistical significance of reported tendencies was explained by a monitoring sites-oriented random soil sampling, i.e. in forest stands of various age, species-composition and degradation degree.

  8. Tin and tinned dress accessories from medieval Wroclaw (SW Poland) x-ray fluorescence investigations / Beata Miazga

    Index Scriptorium Estoniae

    Miazga, Beata

    2014-01-01

    Analüüsitakse esemeid, mis on leitud Wrocławi vanalinnas Uue Turu piirkonnas päästekaevamistel 2010-2012. Lisaks hõbedale oli tina ehtematerjalina Euroopas vaesema elanikkonna hulgas laialt levinud. Võib oletada, et Uuel Turul asus tinaesemeid valmistanud käsitöölise töökoda

  9. Post-Variscan thermal history of the Moravo-Silesian lower Carboniferous Culm Basin (NE Czech Republic - SW Poland)

    Science.gov (United States)

    Botor, Dariusz; Dunkl, István; Anczkiewicz, Aneta; Mazur, Stanisław

    2017-08-01

    Apatite fission track analysis (AFT) and zircon (U-Th)/He thermochronology (ZHe) have been carried out for a lower Carboniferous greywacke succession of the Moravo-Silesian Culm Basin in the Nízký Jeseník Mountains. The range of apparent zircon helium ages is 303-233 Ma (late Carboniferous to Early Triassic) in the eastern part of the basin, whilst they are significantly younger in the western part, ranging from 194 to 163 Ma (Early-Middle Jurassic). Apatite fission track central ages range from 152 (Latest Jurassic) to 44 Ma (Eocene), with the majority being grouped between 114 (Aptian) and 57 Ma (Paleocene). All samples experienced substantial post-depositional thermal reset; both the AFT ages and the ZHe are considerably younger than the depositional ages. The mean track length varies in the range between 12.5 and 15.4 μm. The unimodal track length distribution, the relatively short mean track length (in most samples), and their rather low standard deviation values (1.2 to 2.1 μm) indicate that their thermal history was determined by Variscan and post-Variscan heating event(s) followed by a prolonged residence in the apatite partial annealing zone in the Mesozoic and finally by cooling in the Paleogene. Geological evidence combined with thermal modeling based on AFT and ZHe data indicate that the lower Carboniferous strata had already reached maximum palaeotemperatures in the late Carboniferous, however, they were presumably later re-heated during the Permian-Triassic. Post-Variscan extensional tectonics events were responsible for high heat flow that together with Carboniferous burial could account for the reset of both thermochronometers. A major phase of cooling occurred in the Late Cretaceous. Finally, exhumation was probably faster in the Paleogene, causing the present-day exposure of the studied rocks.

  10. The Mirdita Eastern Ophiolite, Albania: petrological evidence for MORB Mantle in the Tropoje peridotite massif?

    Science.gov (United States)

    Ntaflos, Theodoros; Onuzi, Kujtim; Hauzenberger, Christoph; Rice, A. Hugh N.; Proßegger, Peter; Mekshiqi, Nazir; Kaza, Gjon

    2016-04-01

    The Mirdita ophiolites in northern Albania are divided into the Western Mirdita Ophiolite (WMO), with MORB geochemical affinities, and the Eastern Mirdita Ophiolite (EMO), for which suprasubduction geochemical affinities have been reported. Ultramafic massifs in the WMO are often plagioclase bearing lherzolites/harzburgites whereas those in the EMO are strongly depleted spinel harzburgites. The Tropoje ultramafic-mafic complex, which forms the northernmost part of the EMO, consists of spinel harzburgites, wherlites, orthopyroxenites and gabbros. The spinel harzburgites, which experienced variable degrees of serpentinization, are coarse- to medium-grained. One of the most striking features of the Tropoje ultramafic rocks is an outcrop of exceptionally fresh coarse- to medium-grained spinel harzburgites. While occasionally the peridotites exhibit a weak foliation, the prevalent texture is protogranular. Olivine is mainly coarse-grained (up to 6 mm size), typically showing kink-bands that frequently contain submicron-sized spinel exsolution lamellae. Both orthopyroxene and clinopyroxene, with grain size up to 3 mm and 1.5 mm, respectively, carry very thin exsolution lamellae of the other pyroxene. Spinel, up to 1 mm in size, is interstitial between boundaries of the associated silicates. The mineral compositions of the spinel harzburgites indicate that they are strongly depleted in basaltic components. The rock-forming minerals (olivine, orthopyroxene and clinopyroxene) are all highly magnesian and chemically homogenous. The magnesium numbers (Mg#=100xMg/[Mg+Fe]) for olivine and orthopyroxene are fairly homogeneous and vary within the narrow range of 90.9-91.6 and 91.5-91.7, respectively. The clinopyroxene is exceptionally highly magnesian, with Mg# ranging between 93.6 and 95.4. In both orthopyroxene and clinopyroxene, the Al2O3 contents range from 0.95 to 1.75 and from 0.62 to 2.27 wt%, respectively. Spinel shows a considerable variation in Al2O3 and Cr2O3. The

  11. Modern water/rock reactions in Oman hyperalkaline peridotite aquifers and implications for microbial habitability

    Science.gov (United States)

    Miller, Hannah M.; Matter, Jürg M.; Kelemen, Peter; Ellison, Eric T.; Conrad, Mark E.; Fierer, Noah; Ruchala, Tyler; Tominaga, Masako; Templeton, Alexis S.

    2016-04-01

    The Samail ophiolite in Oman is undergoing modern hydration and carbonation of peridotite and may host a deep subsurface biosphere. Previous investigations of hyperalkaline fluids in Oman have focused on fluids released at surface seeps, which quickly lose their reducing character and precipitate carbonates upon contact with the O2/CO2-rich atmosphere. In this work, geochemical analysis of rocks and fluids from the subsurface provides new insights into the operative reactions in serpentinizing aquifers. Serpentinite rock and hyperalkaline fluids (pH > 10), which exhibit millimolar concentrations of Ca2+, H2 and CH4, as well as variable sulfate and nitrate, were accessed from wells situated in mantle peridotite near Ibra and studied to investigate their aqueous geochemistry, gas concentrations, isotopic signatures, mineralogy, Fe speciation and microbial community composition. The bulk mineralogy of drill cuttings is dominated by olivine, pyroxene, brucite, serpentine and magnetite. At depth, Fe-bearing brucite is commonly intermixed with serpentine, whereas near the surface, olivine and brucite are lost and increased magnetite and serpentine is detected. Micro-Raman spectroscopy reveals at least two distinct generations of serpentine present in drill cuttings recovered from several depths from two wells. Fe K-edge X-ray absorption near-edge spectroscopy (XANES) analysis of the lizardite shows a strong tetrahedral Fe coordination, suggesting a mixture of both Fe(II) and Fe(III) in the serpentine. Magnetite veins are also closely associated with this second generation serpentine, and 2-10 μm magnetite grains overprint all minerals in the drill cuttings. Thus we propose that the dissolved H2 that accumulates in the subsurface hyperalkaline fluids was evolved through low temperature oxidation and hydration of relict olivine, as well as destabilization of pre-existing brucite present in the partially serpentinized dunites and harzburgites. In particular, we hypothesize

  12. Serpentinization reactions in peridotite from the Josephine ophiolite: implications for life on Mars

    Science.gov (United States)

    Sonzogni, Y.; Treiman, A. H.

    2012-12-01

    Serpentinization of ocean crustal peridotite, both beneath the seafloor and as ophiolites on land, has been identified as a source of hydrogen that can support microbial activity. The similarity of Mars' crust to terrestrial ocean lithosphere thus suggests that ophiolites may be good analogs to some martian environments where life might have existed and may persist today. However, peridotite-water reactions are poorly understood in detail, and serpentinization is commonly idealized as isovolumetric or isochemical hydration of olivine to form serpentine, brucite, magnetite, and H2 gas. Here, a net-veined serpentinite from the Josephine ophiolite, California, was studied in order to characterize in detail the physical-chemical nature of its serpentinization. The extent of serpentinization in the studied sample is ~60%. Remnants of the original harzburgite include ~30% olivine, ~10% orthopyroxene, and accessory augite and chromite. Two generations of serpentinite veins are present, the distinction between them being in their textures (in SEM imagery); type 1 veins appear striated, while type 2 veins are massive. Both types of veins consist almost entirely of serpentine. Both types contain types of vein was identified as lizardite based on its foliate texture (as shown in SEM images), suggesting that serpentinization occurred at Ttype 1 veins is more magnesian (Mg# 96) than the lizardite in type 2 veins (Mg# 93). Based on the mineral proportions in the serpentinite and original harzburgite and their mineral compositions, this reaction approximates the formation of type 1 serpentine veins: 22.5 Mg1.80Fe0.20SiO4 + 7.5 Mg0.91Fe0.09SiO3 + 31.15 H2O → 15 Mg2.88Fe0.12Si2O5(OH)4 + 1.13 Fe3O4 + 4.13 MgO(aq) + 31.15 H2. This reaction conserves Si and Fe, but is not isovolumetric nor isochemical. Considering that half of the serpentine in our sample is represented by type 1 veins, this reaction results in a 10% volume increase and removal of 10 wt% MgO from the solids by

  13. Evolution of the lithospheric mantle beneath Mt. Baekdu (Changbaishan): Constraints from geochemical and Sr-Nd-Hf isotopic studies on peridotite xenoliths in trachybasalt

    Science.gov (United States)

    Park, Keunsu; Choi, Sung Hi; Cho, Moonsup; Lee, Der-Chuen

    2017-08-01

    Major and trace element compositions of minerals as well as Sr-Nd-Hf isotopic compositions of clinopyroxenes from spinel peridotite xenoliths entrained in Late Cenozoic trachybasalt from Mt. Baekdu (Changbaishan) were used to elucidate lithospheric mantle formation and evolution in the eastern North China Craton (NCC). The analyzed peridotites were mainly spinel lherzolites with rare harzburgites. They consisted of olivine (Fo89.3-91.0), enstatite (Wo1-2En88-90Fs8-11), diopside (Wo45-50En45-51Fs4-6), and spinel (Cr# = 8.8-54.7). The peridotite residues underwent up to 25% partial melting in fertile mid-ocean-ridge basalt (MORB) mantle. Plots of the Cr# in spinel against the Mg# in coexisting olivine or spinel suggested an affinity with abyssal peridotites. Comparisons of Cr# and TiO2 in spinel were also compatible with an abyssal peridotite-like composition; however, harzburgites were slightly enriched in TiO2 because of the reaction with MORB-like melt. Temperatures estimated using two-pyroxene thermometry ranged from 750 to 1010 °C, reflecting their lithospheric mantle origin. The rare earth element (REE) patterns in clinopyroxenes of the peridotites varied from light REE (LREE) depleted to spoon shaped to LREE enriched, reflecting secondary overprinting effects of metasomatic melts or fluids on the residues from primordial melting. The calculated trace element pattern of metasomatic melt equilibrated with clinopyroxene in Mt. Baekdu peridotite showed strong enrichment in large-ion lithophile elements, Th and U together with slight fractionation in heavy REEs (HREEs) and considerable depletion in Nb and Ti. The Sr-Nd-Hf isotopic compositions of clinopyroxenes separated from the peridotites varied from more depleted than present-day MORB to bulk Earth values. However, some clinopyroxene showed a decoupling between Nd and Sr isotopes, deviating from the mantle array with a high 87Sr/86Sr ratio. This sample also showed a significant Nd-Hf isotope decoupling lying

  14. Ultrasonic measurements of the elastic wave velocities of peridotite KLB-1 at mantle P and T

    Science.gov (United States)

    Wang, X.; Liu, W.; Herzberg, C. T.; Li, B.

    2012-12-01

    In situ measurements of sound velocities and densities on individual phases of Earth minerals at high pressure and temperature have provided important data to interpret the seismic structure at depths. When using these data to test compositional models of the mantle (e.g., pyrolite and piclogite), seismic properties of the mineralogical aggregates have to be calculated by using averaging schemes based on the proportion and elasticity of each phase. More importantly, the chemical interactions among various mantle phases are difficult to be accurately included. Since the composition of peridotite KLB-1 closely matches the composition of pyrolite, measurement of it's velocities at relevant mantle conditions will provide the most direct comparison with seismic data. In this study, well-sintered KLB-1 aggregates suitable for ultrasonic measurements were hot-pressed at various P-T conditions up to those of the transition zone. The recovered samples were characterized by X-ray diffraction, optical, and scanning electron microscopy (SEM) and found to be uniform in grain size (around 10 micron), free of macrocracks and to have bulk densities close to theoretical values (small amount of pores/microcracks observable in SEM scale). P and S wave velocities have been accurately measured up to 7 GPa and 800°C using a combined ultrasonic and X-radiation technique with direct measurement of sample length at high P and T. The success of this experiment makes it possible to extend these measurements to the conditions of the transition zone on aggregate samples to directly discriminate the composition of the Earth's mantle.

  15. Meter Scale Heterogeneities in the Oceanic Mantle Revealed in Ophiolites Peridotites

    Science.gov (United States)

    Haller, M. B.; Walker, R. J.; Day, J. M.; O'Driscoll, B.; Daly, J. S.

    2016-12-01

    Mid-ocean ridge basalts and other oceanic mantle-derived rocks do not capture the depleted endmember isotopic compositions present in oceanic peridotites. Ophiolites are especially useful in interrogating this issue as field-based observations can be paired with geochemical investigations over a wide range of geologic time. Grid sampling methods (3m x 3m) at the 497 Ma Leka Ophiolite Complex (LOC), Norway, and the 1.95 Ga Jormua Ophiolite Complex (JOC), Finland, offer an opportunity to study mantle domains at the meter and kilometer scale, and over a one billion year timespan. The lithology of each locality predominately comprises harzburgite, hosting layers and lenses of dunite and pyroxenite. Here, we combine highly siderophile elements (HSE) and Re-Os isotopic analysis of these rocks with major and trace element measurements. Harzburgites at individual LOC grid sites show variations in γOs(497 Ma) (-2.1 to +2.2) at the meter scale. Analyses of adjacent, more radiogenic dunites within the same LOC grid, reveal that dunites may either have similar γOs to their host harzburgite, or different, implying interactions between spatially associated rock types may differ at the meter scale. Averaged γOs values between the mantle sections of two LOC grid sites (+1.3 and -0.4) separated by 5 km indicate km-scale heterogeneity in the convecting upper mantle. Pd/Ir and Ru/Ir ratios are scattered and do not obviously correlate with γOs values. Analyses of pyroxenites within LOC grid sections, thin section observations of relict olivine grains, and whole rock major and trace element data are also examined to shed light on the causes of the isotopic heterogeneities in the LOC. Data from JOC grid sampling will be presented as well.

  16. Gravimetric structure for the abyssal mantle massif of Saint Peter and Saint Paul peridotite ridge, Equatorial Atlantic Ocean, and its relation to active uplift

    Directory of Open Access Journals (Sweden)

    KENJI F. MOTOKI

    2014-06-01

    Full Text Available This paper presents gravimetric and morphologic analyses based on the satellite-derived data set of EGM2008 and TOPEX for the area of the oceanic mantle massif of the Saint Peter and Saint Paul peridotite ridge, Equatorial Atlantic Ocean. The free-air anomaly indicates that the present plate boundary is not situated along the longitudinal graben which cuts peridotite ridge, but about 20 km to the north of it. The high Bouguer anomaly of the peridotite ridge suggests that it is constituted mainly by unserpentinised ultramafic rocks. The absence of isostatic compensation and low-degree serpentinisation of the ultramafic rocks indicate that the peridotite ridge is sustained mainly by active tectonic uplift. The unparallel relation between the transform fault and the relative plate motion generates near north-south compression and the consequent tectonic uplift. In this sense, the peridotite massif is a pressure ridge due to the strike-slip displacement of the Saint Paul Transform Fault.

  17. Multiple metasomatic events recorded in Kilbourne Hole peridotite xenoliths: the relative contribution of host basalt interaction vs. silicate metasomatic glass

    Science.gov (United States)

    Hammond, S. J.; Yoshikawa, M.; Harvey, J.; Burton, K. W.

    2010-12-01

    Stark differences between bulk-rock lithophile trace element budgets and the sum of the contributions from their constituent minerals are common, if not ubiquitous in peridotite xenoliths [1]. In the absence of modal metasomatism this discrepancy is often attributed to the “catch-all”, yet often vague process of cryptic metasomatism. This study presents comprehensive Sr-Nd isotope ratios for variably metasomatized bulk-rock peridotites, host basalts, constituent peridotite mineral phases and interstitial glass from 13 spinel lherzolite and harzburgite xenoliths from the Kilbourne Hole volcanic maar, New Mexico, USA. Similar measurements were also made on hand-picked interstitial glass from one of the most highly metasomatized samples (KH03-16) in an attempt to unravel the effects of multiple metasomatic events. In all Kilbourne Hole peridotites analysed, hand-picked, optically clean clinopyroxenes preserve a more primitive Sr isotope signature than the corresponding bulk-rock; a pattern preserved in all but one sample for Nd isotope measurements. Reaction textures, avoided during hand-picking, around clinopyroxene grains are evident in the most metasomatized samples and accompanied by films of high-SiO2 interstitial glass. The margins of primary minerals appear partially resorbed and trails of glassy melt inclusions similar in appearance to those previously reported from the same locality [2], terminate in these films. Hand-picked glass from KH03-16 reveals the most enriched 87Sr/86Sr of any component recovered from these xenoliths (87Sr/86Sr = 0.708043 ± 0.00009; [Sr] = 81 ppm). Similarly, the 143Nd/144Nd of the glass is amongst the most enriched of the peridotite components (143Nd/144Nd = 0.512893 ± 0.000012; [Nd] = 10 ppm). However, the host basalt (87Sr/86Sr = 0.703953 ± 0.00012; 143Nd/144Nd = 0.512873 ± 0.000013), similar in composition to nearby contemporaneous Potrillo Volcanic Field basalts [3], contains nearly an order of magnitude more Sr and more

  18. Determinants of all cause mortality in Poland.

    Science.gov (United States)

    Genowska, Agnieszka; Jamiołkowski, Jacek; Szpak, Andrzej; Pajak, Andrzej

    2012-01-01

    The study objective was to evaluate quantitatively the relationship between demographic characteristics, socio-economic status and medical care resources with all cause mortality in Poland. Ecological study was performed using data for the population of 66 subregions of Poland, obtained from the Central Statistical Office of Poland. The information on the determinants of health and all cause mortality covered the period from 1st January 2005 to 31st December 2010. Results for the repeated measures were analyzed using Generalized Estimating Equations GEE model. In the model 16 independent variables describing health determinants were used, including 6 demographic variables, 6 socio-economic variables, 4 medical care variables. The dependent variable, was age standardized all cause mortality rate. There was a large variation in all cause mortality, demographic features, socio-economic characteristics, and medical care resources by subregion. All cause mortality showed weak associations with demographic features, among which only the increased divorce rate was associated with higher mortality rate. Increased education level, salaries, gross domestic product (GDP) per capita, local government expenditures per capita and the number of non-governmental organizations per 10 thousand population was associated with decrease in all cause mortality. The increase of unemployment rate was related with a decrease of all cause mortality. Beneficial relationship between employment of medical staff and mortality was observed. Variation in mortality from all causes in Poland was explained partly by variation in socio-economic determinants and health care resources.

  19. Poland's syndrome | Frioui | Pan African Medical Journal

    African Journals Online (AJOL)

    Physical examination showed left anterior chest-wall depression, lateral to the nipple. There were no other anomalies seen on further systemic evaluation. Neurological examination and skeletal survey were normal. Poland's syndrome was diagnosed with absence of left pectoralis major muscle and mammary agenesis.

  20. Species diversity of Trichoderma in Poland

    Science.gov (United States)

    Fifteen species of Trichoderma were identified from among 118 strains originating from different regions and ecological niches in Poland. This low number indicates low species diversity of Trichoderma in this Central European region. Using the ITS1-ITS2 regions, 64 strains were positively identified...

  1. Lyme disease in Poland in 2014

    Science.gov (United States)

    Paradowska-Stankiewicz, Iwona; Chrześcijańska, Irena

    Lyme disease is the most common tick-borne disease, caused by spirochetes of the Borrelia genus transmitted by ticks of the Ixodes genus. Infection caused by Borrelia burgdorferi occur throughout Poland and therefore, according also to ECDC description, the whole country should be considered as an endemic area. The aim of this study was to assess the epidemiological situation of Lyme disease in Poland in 2014 in comparison to the previous years. The descriptive analysis was based on data retrieved from routine mandatory surveillance system and published in the annual bulletin “Infectious diseases and poisonings in Poland in 2014” (MP Czarkowski et al., Warsaw 2015, NIZP-PZH, GIS). The number of cases of Lyme disease in recent years is steadily increasing. In total, 13.870 cases of Lyme disease registered in Poland in 2014, i.e. 8% more cases than in the previous year. The overall incidence in the country was 36.0 per 100,000 population. The highest incidence rate was recorded in Podlaskie voivodeship – 106.8 per 100,000. In 2014, 2.236 people were hospitalized due to Lyme disease. In 2014, the growth rate of incidence decreased significantly. 8% more cases were registered compared with the previous year. There is still a need for bringing awareness of the need for diagnostic laboratory testing according to recommendations.

  2. Rare and new Laboulbeniales from Poland. X

    Directory of Open Access Journals (Sweden)

    Tomasz Majewski

    2014-08-01

    Full Text Available In a consecutive paper in the series concerning Polish Laboulbeniales, several species new for Poland are reported. Similarly as in the earlier papers of this series, all specimens were found by the author (if not otherwise indicated. The specimens are kept in the author's collection at the Mycology Laboratory of the Institute of Botany, Polish Academy of Sciences, Warsaw.

  3. Curricular Models of CLIL Education in Poland

    Science.gov (United States)

    Czura, Anna; Papaja, Katarzyna

    2013-01-01

    Bilingual education in Poland gained in popularity after the political changes in 1989 when Polish society started noticing the importance of foreign language learning. With the emergence of content and language integrated learning (CLIL) in the 1990s, which in the Polish context is still termed as "bilingual education", foreign…

  4. Soil fauna research in Poland: earthworms (Lumbricidae

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    Pączka Grzegorz

    2015-06-01

    Full Text Available Living organisms are the foundation of ecosystem services. Of particular notice is zooedaphone, often underestimated and basically unknown to the general public. The present review summarizes the current state of knowledge related to earthworms occurring in natural and anthropogenically altered habitats in Poland, in the context of the requirement for protection of soil biodiversity.

  5. Control of rabbit myxomatosis in Poland.

    Science.gov (United States)

    Górski, J; Mizak, B; Chrobocińska, M

    1994-09-01

    The authors present an epizootiological analysis of myxomatosis in Poland. The biological, physical and chemical properties of virus strains used for the production and control of 'Myxovac M' vaccine are discussed. The long-term stability, safety and efficacy of the vaccine are demonstrated. Laboratory experiments were confirmed in large-scale field observations.

  6. FASD Prevalence among Schoolchildren in Poland

    Science.gov (United States)

    Okulicz-Kozaryn, Katarzyna; Borkowska, Magdalena; Brzózka, Krzysztof

    2017-01-01

    Background: Prenatal Alcohol Exposure is a major cause of brain damage and developmental delay, known as Fetal Alcohol Spectrum Disorders (FASD) but in Poland is rarely diagnosed and the scale of problem is not known. Methods: An active case ascertainment approach was applied to estimate the prevalence of FASD among 7-9 years olds. Pre-screening…

  7. Parents' Perceptions of Integrated Education in Poland

    Science.gov (United States)

    Bragiel, Józefa

    2016-01-01

    Integrated education in Poland has been implemented since 1993. This alternative form of education very quickly resulted in an increased number of integrated classes in mainstream schools and a decreased percentage of students with disabilities in segregated education. Research indicates that the process of "opening of society to…

  8. Particle Swarm Optimization for HW/SW Partitioning

    OpenAIRE

    Abdelhalim, M. B.; Habib, S. E. &#;D.

    2009-01-01

    In this chapter, the recent introduction of the Particle Swarm Optimization technique to solve the HW/SW partitioning problem is reviewed, along with its “re-exited PSO” modification. The re-exited PSO algorithm is a recently-introduced restarting technique for PSO. The Re-exited PSO proved to be highly effective for solving the HW/SW partitioning problem. Efficient cost function formulation is of a paramount importance for an efficient optimization algorithm. Each component in the design...

  9. Discriminating between pyroxenite and peridotite sources for continental flood basalts (CFB) in southern Africa using olivine chemistry

    Science.gov (United States)

    Howarth, Geoffrey H.; Harris, Chris

    2017-10-01

    Continental Flood Basalts (CFB) result from voluminous outpourings of magma that often precede continental break-up. Notwithstanding the petrogenetic importance of CFBs, the nature of the mantle source for such magmas is contentious, particularly with regard to picrites with Ni-rich olivine phenocrysts. Previous studies have suggested that Ni-rich olivines associated with plume volcanism in regions of thickened (>90 km) lithosphere are related to either source mineralogy differences (peridotite versus pyroxenite) or change in olivine-melt partitioning due to pressure increase. In order to evaluate these two hypotheses, we present trace element data for olivines from the Karoo CFB Tuli and Mwenezi picrites and the Etendeka CFB Horingbaai/LTZ-L type picrites, all of which erupted in regions of thickened (>90 km) lithosphere in southern Africa. Karoo picrite olivines are Ni-rich, Ca- and Mn-poor, and have low (1.4) 100*Mn/Fe, which is more consistent with high temperature melting of a dominantly peridotitic source. We also show that the Karoo and Etendeka olivines are characterized by distinct Mn/Zn ratios of 15, respectively. In addition, bulk rock geochemical data compilations and previously reported olivine δ18O for Karoo and Etendeka CFBs are discussed in order to further constrain source components based on previously described pyroxenite melt geochemical indices such as MgO-CaO systematics, FeO/MnO, Zn/Fe, and FC3MS (FeO/CaO-3*MgO/SiO2). These geochemical indices suggest a pyroxenite-dominated source for Karoo CFBs as well as for Etendeka ferropicrites whereas a peridotite-dominated source is indicated for Etendeka Horingbaai/LTZ-L type picrites analyzed in this study. Based on our data, Ni-enrichment of olivine in plume-related magmas in regions of thickened lithosphere in southern Africa is not ubiquitous. We therefore suggest that mineralogical variation of the source is a more likely major control of olivine chemistry and parent melt variations for Karoo

  10. Assessment of wind energy potential in Poland

    Science.gov (United States)

    Starosta, Katarzyna; Linkowska, Joanna; Mazur, Andrzej

    2014-05-01

    The aim of the presentation is to show the suitability of using numerical model wind speed forecasts for the wind power industry applications in Poland. In accordance with the guidelines of the European Union, the consumption of wind energy in Poland is rapidly increasing. According to the report of Energy Regulatory Office from 30 March 2013, the installed capacity of wind power in Poland was 2807MW from 765 wind power stations. Wind energy is strongly dependent on the meteorological conditions. Based on the climatological wind speed data, potential energy zones within the area of Poland have been developed (H. Lorenc). They are the first criterion for assessing the location of the wind farm. However, for exact monitoring of a given wind farm location the prognostic data from numerical model forecasts are necessary. For the practical interpretation and further post-processing, the verification of the model data is very important. Polish Institute Meteorology and Water Management - National Research Institute (IMWM-NRI) runs an operational model COSMO (Consortium for Small-scale Modelling, version 4.8) using two nested domains at horizontal resolutions of 7 km and 2.8 km. The model produces 36 hour and 78 hour forecasts from 00 UTC, for 2.8 km and 7 km domain resolutions respectively. Numerical forecasts were compared with the observation of 60 SYNOP and 3 TEMP stations in Poland, using VERSUS2 (Unified System Verification Survey 2) and R package. For every zone the set of statistical indices (ME, MAE, RMSE) was calculated. Forecast errors for aerological profiles are shown for Polish TEMP stations at Wrocław, Legionowo and Łeba. The current studies are connected with a topic of the COST ES1002 WIRE-Weather Intelligence for Renewable Energies.

  11. An Experimental Study of the Carbonation of Serpentinite and Partially Serpentinised Peridotites

    Directory of Open Access Journals (Sweden)

    Alicja M. Lacinska

    2017-06-01

    Full Text Available In situ sequestration of CO2 in mantle peridotites has been proposed as a method to alleviate the amount of anthropogenic CO2 in the atmosphere. This study presents the results of 8-month long laboratory fluid-rock experiments on representative mantle rocks from the Oman-United Arab Emirates ophiolite to investigate this process. Small core samples (3 cm long were reacted in wet supercritical CO2 and CO2-saturated brine at 100 bar and 70°C. The extent of carbonate formation, and hence the degree of carbon sequestration, varied greatly depending on rock type, with serpentinite (lizardite-dominated exhibiting the highest capacity, manifested by the precipitation of magnesite MgCO3 and ferroan magnesite (Mg,FeCO3. The carbonate precipitation occurred predominantly on the surface of the core and subordinately within cross-cutting fractures. The extent of the CO2 reactions appeared to be principally controlled by the chemical and mineralogical composition of the rock, as well as the rock texture, with all these factors influencing the extent and rate of mineral dissolution and release of Mg and Fe for subsequent reaction with the CO2. It was calculated that ≈0.7 g of CO2 was captured by reacting ≈23 g of serpentinite, determined by the mass of magnesite formed. This equates to ≈30 kg CO2 per ton of host rock, equivalent to ≈3% carbonation in half a year. However, recycling of carbonate present in veins within the original rock sample could mean that the overall amount is around 2%. The increased reactivity of serpentinite was associated with preferential dissolution of more reactive types of serpentine minerals and brucite that were mainly present in the cross-cutting veins. The bulk of the serpentinite rock was little affected. This study, using relatively short term experiments, suggests that serpentinite might be a good host rock for CO2 sequestration, although long term experiments might prove that dunite and harzburgite could be as

  12. An experimental study of the carbonation of serpentinite and partially serpentinised peridotites

    Science.gov (United States)

    Lacinska, Alicja M.; Styles, Michael T.; Bateman, Keith; Hall, Matthew; Brown, Paul D.

    2017-06-01

    In situ sequestration of CO2 in mantle peridotites has been proposed as a method to alleviate the amount of anthropogenic CO2 in the atmosphere. This study presents the results of eight-month long laboratory fluid-rock experiments on representative mantle rocks from the Oman-United Arab Emirates ophiolite to investigate this process. Small core samples (3 cm long) were reacted in wet supercritical CO2 and CO2-saturated brine at 100 bar and 70°C. The extent of carbonate formation, and hence the degree of carbon sequestration, varied greatly depending on rock type, with serpentinite (lizardite-dominated) exhibiting the highest capacity, manifested by the precipitation of magnesite MgCO3 and ferroan magnesite (Mg,Fe)CO3. The carbonate precipitation occurred predominantly on the surface of the core and subordinately within cross-cutting fractures. The extent of the CO2 reactions appeared to be principally controlled by the chemical and mineralogical composition of the rock, as well as the rock texture, with all these factors influencing the extent and rate of mineral dissolution and release of Mg and Fe for subsequent reaction with the CO2. It was calculated that ≈ 0.7 g of CO2 was captured by reacting ≈ 23 g of serpentinite, determined by the mass of magnesite formed. This equates to ≈ 30 kg CO2 per tonne of host rock, equivalent to ≈ 3% carbonation in half a year. However, recycling of carbonate present in veins within the original rock sample could mean that the overall amount is around 2%. The increased reactivity of serpentinite was associated with preferential dissolution of more reactive types of serpentine minerals and brucite, that were mainly present in the cross-cutting veins. The bulk of the serpentinite rock was little affected. This study, using relatively short term experiments, suggests that serpentinite might be a good host rock for CO2 sequestration, although long term experiments might prove that dunite and harzburgite could be an effective

  13. Carbonation of Peridotite by CO2-rich Fluids: Insights from Listvenites in the Advocate Ophiolite (Newfoundland)

    Science.gov (United States)

    Menzel, Manuel; Garrido, Carlos J.; Marchesi, Claudio; López Sánchez Vizcaíno, Vicente; Hidas, Károly; Escayola, Monica P.; Jamtveit, Bjørn

    2017-04-01

    Listvenites are the result of a sequence of reactions of CO2-rich hydrothermal fluids with serpentinite that forms magnesite-quartz rocks in the last reaction step. Listvenites are natural analogues for carbon sequestration by mineral carbonation, fixing large quantities of carbon in relatively small, confined zones of intense reactive fluid flux within serpentinite. The association of listvenite (magnesite-quartz), soapstone (talc-magnesite) and carbonated serpentinite in the mantle section of the Advocate ophiolite complex in Newfoundland (Canada) is an ideal natural example to study the carbonation of serpentinites because the reaction progress is recorded by the differently carbonated assemblages. The Advocate listvenites crop out in a 20-30 m wide zone that can be followed for about 1 km, surrounded by serpentinite and harzburgite. Quartz and magnesite veins are widespread in the central listvenite domain. This mobilization of silica into a vein network is reflected in a depletion of silica in the most carbonated lithologies, whereas most other major elements remain unchanged over a wide range of CO2-contents. Notably, there is a sharp decrease in bulk rock Fe3+/Fetotal from 0.65 - 0.8 in lizardite-chrysotile serpentinites to 0.1 - 0.3 in talc-magnesite rocks and listvenites. High Cr and Ni contents and preserved red-brown Cr-spinel in the carbonated lithologies demonstrate the mantle peridotites provenance of the listvenites. The presence of thin veins of Cr-mica (fuchsite) suggests that Cr was mobilized to some degree. Fine dispersed magnetite trails in magnesite trace serpentine pseudomorphs after olivine, indicating that no deformation occurred in some domains during the carbonation, while deformation was concentrated in talc-rich lithologies. The rheological contrasts of serpentinites, soapstones and listvenites and, in consequence, the formation of veins in response to shear- or extensional fractures may result in a re-opening of pathways for the influx

  14. Amphibole incongruent melting under Lithospheric Mantle conditions in spinel peridotites from Balaton area, Hungary

    Science.gov (United States)

    Ntaflos, Theodoros; Abart, Rainer; Bizimis, Michel

    2017-04-01

    Pliocene alkali basalts from the western Pannonian Basin carry mantle xenoliths comprising hydrous and anhydrous spinel peridotites. We studied coarse and fine grained fertile to depleted spinel lherzolites, spinel harzubrgites and dunites from Szentbékálla, Balaton, in detail, using XRF, EPMA and LA-ICP-MS and MC-ICP-MS techniques. Pliocene alkali basalts containing mantle xenoliths with three major types of textures are widespread in the studied area: fine-grained primary and secondary equigranular, coarse-grained protogranular and transitional between equigranular and protogranular textures. Melt pockets, are common in the studied xenoliths. The shape of several melt pockets resembles euhedral amphibole. Other samples have thin films of intergranular glass attributed to the host basalt infiltration. Calculations have shown that such xenoliths experienced an up to 2.4% host basalt infiltration. The bulk rock Al2O3 and CaO concentrations vary from 0.75 to 4.1 and from 0.9 to 3.6 wt% respectively, and represent residues after variable degrees of partial melting. Using bulk rock major element abundances, the estimated degree of partial melting ranges from 4 to 20%.. The Primitive Mantle normalized clinopyroxene trace element abundances reveal a complicated evolution of the Lithospheric mantle underneath Balaton, which range from partial melting to modal and cryptic metasomatism. Subduction-related melt/fluids and/or infiltration of percolating undersaturated melts could be account for the metasomatic processes. The radiogenic isotopes of Sr, Nd and Hf in clinopyroxene suggest that this metasomatism was a relatively recent event. Textural evidence suggests that the calcite filling up the vesicles in the melt pockets and in veinlets cross-cutting the constituent minerals is of epigenetic nature and not due to carbonatite metasomatism. Mass balance calculations have shown that the bulk composition of the melt pockets is identical to small amphibole relics found as

  15. The Oceanic Lithosphere as Reactive Filter: Implications for MORB and Abyssal Peridotite Compositions

    Science.gov (United States)

    Luffi, P. I.; Lee, C.; Antoshechkina, P. M.

    2010-12-01

    Melt-rock reaction in the lithosphere is, as suggested by textural observations and compositional data, a ubiquitous phenomenon capable of generating locally diverse peridotite series, such as those observed at oceanic spreading centers and transform faults, and may represent an important mechanism of creating compositional diversity in MORBs [1]. Whereas our understanding of the principles governing reactive melt transport is supported by basic theories and models, studies that attempt to quantify the physical conditions and mechanisms creating heterogeneities in the oceanic lithosphere are still limited in number [e.g. 2]. Using Adiabat_1ph 3.0 [3] in combination with the pMELTS algorithm [4], we have previously shown that reactive percolation of basaltic melts through depleted harzburgites can generate the dunite-(wehrlite)-harzburgite-lherzolite spectrum observed in the abyssal mantle and ophiolites, and that the amplitude of transformations is a function of thermal boundary layer thickness and amount of available melt [5]. To gain further insight into how melt-rock reactions shape the oceanic lithosphere, here we extend our study to show that the major and trace element variability in the oceanic mantle and rising melts are also significantly influenced by the mechanism of melt transport. If associated with cooling, distributed porous melt percolation (simulated by incremental addition of the same amount of melt) more efficiently converts harzburgites into fertile lherzolites and creates more pronounced compositional gradients in the abyssal mantle than imparted during channelized melt influx (simulated as batch addition of large amounts of melt) under otherwise identical circumstances. To remain within the tholeiitic trend observed in MORB, reacted melts must be released before clinopyroxene precipitation peaks. Further reaction with harzburgite causes liquids to evolve toward boninite-like compositions. As reaction progresses with decreasing temperature, the

  16. Kinetics of Peridotite and Pyroxenite-derived Melts Interaction: Implications for the Style and Extent of Melt-rock Reaction in the Mantle

    Science.gov (United States)

    Lo Cascio, M.; Liang, Y.

    2006-12-01

    Distinct geochemical and petrologic features of ocean floor basalts and mantle peridotites suggest that the upper mantle is lithologically heterogeneous, consisting predominantly of peridotite and a small amount of eclogite [1]. An important issue of this marble cake mantle, is the nature of the peridotite and pyroxenite interface during mantle melting. It has been suggested that during mantle melting eclogite and peridotite develop a reactive boundary layer composed of a second generation eclogite and a layer of orthopyroxenite [2]. The existence of such a boundary layer has also been used to explain the observation that oceanic basalts are extracted with only limited interaction with the surrounding peridotite [3]. In spite of recent progresses, the kinetics of peridotite and pyroxenite-derived melts reaction is still not well understood. It is likely that there are two regimes of peridotite-pyroxenite melt interaction: a high T/low P regime where both the peridotite and pyroxenite are partially molten; and a low T/high P regime where only pyroxenite is partially molten. In this study we explored the kinetics of such interactions in both regimes by conducting lherzolite dissolution experiments using a pyroxenite-derived melt at 1300°C and 1-2 GPa. Dissolution couples were formed by juxtaposing pre-synthesized rods of a basaltic andesite (54.6% SiO2, Mg# 0.42), whose composition is similar to pyroxenite derived liquid at 1300°C and 2 GPa [1,4], and a lherzolite (ol+opx+cpx) in a Pt and graphite lined Mo capsule. The lherzolite solidus is below 1300°C at 1 GPa [5], but above 1300°C at 2 GPa. Lherzolite hardly dissolves (~35 μm in 6 hours) into the melt at 2 GPa and a thin opx layer (10.1093/petrology/egg074; [2] Yaxley and Green, 1998, Schweiz. Mineral. Petrogr. Mitt., 78; [3] Hauri and Kurz, 1997, EPSL, 153; [4] Takahashi and Nakajima, 2002, Geoph. Mon. 128; [5] Morgan and Liang, 2005, CMP, 150, doi: 10.1007/s00410-005-0033-8; [6] Petermann and Hirschmann

  17. Verbascum lindae (Scrophulariaceae), a new species from SW Anatolia, Turkey

    DEFF Research Database (Denmark)

    Parolly, Gerald; Tan, Kit

    2007-01-01

    Verbascum lindae, a taxonomically isolated limestone chasmophyte from the vilayet of Isparta in SW Anatolia is described as a species new to science and illustrated. Its affinities with other Anatolian Verbascum species, which have either a chasmophytic habit or at least a woody base, are discussed....

  18. Palaeoenvironmental reconstruction of Hüsamlar coal seam, SW ...

    Indian Academy of Sciences (India)

    The Ören and Yatağan Basins in SW Turkey host several Miocene coal deposits currently under exploitation for power generation. The present study aims to provide insight into the palaeoenvironmental conditions, which controlled the formation of the Hüsamlar coal seam located in Ören Basin. The coal seam displays ...

  19. Heliotropium thermophilum (Boraginaceae), a new taxon from SW Anatolia, Turkey

    DEFF Research Database (Denmark)

    Tan, Kit; Celik, Ali; Gemici, Yusuf

    2008-01-01

    Heliotropium thermophilum Kit Tan, A. Çelik & Y. Gemici (Boraginaceae), is described as a species new to science and illustrated. Its diploid chromosome number of 2n = 16 is a first report. It is restricted to the province of Aydin bordering on Denizli in SW Anatolia and is of interest on account...

  20. Basic Information about How to Use SW-846

    Science.gov (United States)

    This page discusses the Test Methods for Evaluating Solid Waste: Physical/Chemical Methods compendium, or SW-846, which is the EPA’s official collection of methods for use in complying with the Resource Conservation and Recovery Act (RCRA) regulations.

  1. Seaweeds of the Spermonde Archipelago, SW Sulawesi, Indonesia

    NARCIS (Netherlands)

    Verheij, E.; Prud’homme van Reine, W.F.

    1993-01-01

    Seaweeds are important components of tropical reef systems. The present paper deals with the Chlorophyta, Phaeophyta and noncoralline Rhodophyta collected by the first author in the Spermonde Archipelago, SW Sulawesi, Indonesia, during the Buginesia-III project (November 1988-November 1990).

  2. Geochemistry of Archaean supracrustal belts in SW Greenland

    DEFF Research Database (Denmark)

    Szilas, Kristoffer

    This PhD-thesis investigates the geological formation environment of c. 3200-3000 million-year-old volcanic rocks from SW Greenland, using whole-rock geochemical data in combination with U-Pb, Sm-Nd and Lu-Hf isotope data. The following three supracrustal areas were studied: (1) The Tartoq Group ...

  3. Shrub expansion in SW Greenland under modest regional warming

    DEFF Research Database (Denmark)

    Jørgensen, Rasmus Halfdan; Meilby, Henrik; Kollmann, Johannes

    2013-01-01

    Shrub expansion has been observed widely in tundra areas across the Arctic. This phenomenon has been partially attributed to increasing temperatures over the past century. However, relationships among shrub expansion, grazing, and human disturbance have been studied little. SW Greenland is a suba...

  4. Geochemistry of crystalline basement rocks SW Ugep, Nigeria ...

    African Journals Online (AJOL)

    Geochemical data on low-grade metasedimentary phyllites and schists of SW Ugep show that they were derived from predominantly pelitic parent rocks. They form a supracrustal cover on an orthogneiss of granitic composition. The metasediments are enriched in Si02, Al203 and Zr but improverished in Ni. Intrusion of ...

  5. Pharmacognostic Investigation of Leaves of Mitracarpus vilosus (SW)

    African Journals Online (AJOL)

    Pharmacognostic investigation on fresh, powdered and anatomical sections of leaf of Mitracarpus vilosus (S.W) D.C was carried out to determine its macromorphological, micromorphological and chemomicromorphological profiles. Qualitative and quantitative studies indicated presence of amphicribal vascular bundle ...

  6. Textures in spinel peridotite mantle xenoliths using micro-CT scanning: Examples from Canary Islands and France

    Science.gov (United States)

    Bhanot, K. K.; Downes, H.; Petrone, C. M.; Humphreys-Williams, E.

    2017-04-01

    Spinel pyroxene-clusters, which are intergrowths of spinel, orthopyroxene and clinopyroxene in mantle xenoliths, have been investigated through the use of micro-CT (μ-CT) in this study. Samples have been studied from two different tectonic settings: (1) the northern Massif Central, France, an uplifted and rifted plateau on continental lithosphere and (2) Lanzarote in the Canary Islands, an intraplate volcanic island on old oceanic lithosphere. μ-CT analysis of samples from both locations has revealed a range of spinel textures from small < 2 mm microcrystals which can be either spatially concentrated or distributed more evenly throughout the rock with a lineation, to large 4-12 mm individual clusters with ellipsoidal complex vermicular textures in random orientation. Microprobe analyses of pyroxenes inside and outside the clusters show broadly similar compositions. Spinel-pyroxene clusters are the result of a transition of shallow lithospheric mantle from the garnet stability field to the spinel stability field. Both the northern Massif Central and Lanzarote are regions that have experienced significant lithospheric thinning. This process provides a mechanism where the sub-solidus reaction of olivine + garnet = orthopyroxene + clinopyroxene + spinel is satisfied by providing a pathway from garnet peridotite to spinel peridotite. We predict that such textures would only occur in the mantle beneath regions that show evidence of thinning of the lithospheric mantle. Metasomatic reactions are seen around spinel-pyroxene clusters in some Lanzarote xenoliths, so metasomatism post-dated cluster formation.

  7. Mineral chemistry and petrology of mantle peridotites from the Guleman ophiolite (SE Anatolia, Turkey): Evidence of a forearc setting

    Science.gov (United States)

    Rizeli, Mustafa Eren; Beyarslan, Melahat; Wang, Kuo-Lung; Bingöl, A. Feyzi

    2016-11-01

    The mantle section of Guleman ophiolite, southeast (SE) Turkey consists mainly of harzburgites and dunite lenses and large chromitite pods. The average Cr ratio = [100 × Cr/(Cr + Al) atomic ratio] of Cr-spinels in harzburgites and dunites is remarkably high (>63). The forsterite (Fo) content of olivine is between 90.9 and 92.3 in harzburgites and dunites. These features indicate that the harzburgites and dunites resulted from >35% of partial melting of a depleted mantle source. Discriminant geochemical diagrams based on the mineral chemistry of harzburgites indicate a supra-subduction zone (SSZ) origin. Orthopyroxene and clinopyroxene from the Guleman harzburgites have low CaO, Al2O3 and TiO2 contents, resembling those of depleted harzburgites from modern forearcs and contrasting with moderately depleted abyssal peridotites. Consequently, we propose that the Guleman peridotites formed in a forearc setting during the subduction initiation that developed as a result of northward subduction of the southern branch of the Neo-Tethys in response to the convergence between the Arabian and Anatolian plates.

  8. Regolith-geology mapping with support vector machine: A case study over weathered Ni-bearing peridotites, New Caledonia

    Science.gov (United States)

    De Boissieu, Florian; Sevin, Brice; Cudahy, Thomas; Mangeas, Morgan; Chevrel, Stéphane; Ong, Cindy; Rodger, Andrew; Maurizot, Pierre; Laukamp, Carsten; Lau, Ian; Touraivane, Touraivane; Cluzel, Dominique; Despinoy, Marc

    2018-02-01

    Accurate maps of Earth's geology, especially its regolith, are required for managing the sustainable exploration and development of mineral resources. This paper shows how airborne imaging hyperspectral data collected over weathered peridotite rocks in vegetated, mountainous terrane in New Caledonia were processed using a combination of methods to generate a regolith-geology map that could be used for more efficiently targeting Ni exploration. The image processing combined two usual methods, which are spectral feature extraction and support vector machine (SVM). This rationale being the spectral features extraction can rapidly reduce data complexity by both targeting only the diagnostic mineral absorptions and masking those pixels complicated by vegetation, cloud and deep shade. SVM is a supervised classification method able to generate an optimal non-linear classifier with these features that generalises well even with limited training data. Key minerals targeted are serpentine, which is considered as an indicator for hydrolysed peridotitic rock, and iron oxy-hydroxides (hematite and goethite), which are considered as diagnostic of laterite development. The final classified regolith map was assessed against interpreted regolith field sites, which yielded approximately 70% similarity for all unit types, as well as against a regolith-geology map interpreted using traditional datasets (not hyperspectral imagery). Importantly, the hyperspectral derived mineral map provided much greater detail enabling a more precise understanding of the regolith-geological architecture where there are exposed soils and rocks.

  9. Lithosphere destabilization by melt percolation during pre-oceanic rifting: Evidence from Alpine-Apennine ophiolitic peridotites

    Science.gov (United States)

    Piccardo, Giovanni; Ranalli, Giorgio

    2017-04-01

    Orogenic peridotites from Alpine-Apennine ophiolite Massifs (Lanzo, Voltri, External and Internal Ligurides, - NW Italy, and Mt. Maggiore - Corsica) derive from the mantle lithosphere of the Ligurian Tethys. Field/structural and petrologic/geochemical studies provide constraints on the evolution of the lithospheric mantle during pre-oceanic passive rifting of the late Jurassic Ligurian Tethys ocean. Continental rifting by far-field tectonic forces induced extension of the lithosphere by means of km-scale extensional shear zones that developed before infiltration of melts from the asthenosphere (Piccardo and Vissers, 2007). After significant thinning of the lithosphere, the passively upwelling asthenosphere underwent spinel-facies decompression melting along the axial zone of the extensional system. Silica-undersaturated melt fractions percolated through the lithospheric mantle via diffuse/focused porous flow and interacted with the host peridotite through pyroxenes-dissolving/olivine-precipitating melt/rock reactions. Pyroxene dissolution and olivine precipitation modified the composition of the primary silica-undersaturated melts into derivative silica-saturated melts, while the host lithospheric spinel lherzolites were transformed into pyroxene-depleted/olivine-enriched reactive spinel harzburgites and dunites. The derivative liquids interacted through olivine-dissolving/orthopyroxene+plagioclase-crystallizing reactions with the host peridotites that were impregnated and refertilized (Piccardo et al., 2015). The saturated melts stagnated and crystallized in the shallow mantle lithosphere (as testified by diffuse interstitial crystallization of euhedral orthopyroxene and anhedral plagioclase) and locally ponded, forming orthopyroxene-rich/olivine-free gabbro-norite pods (Piccardo and Guarnieri, 2011). Reactive and impregnated peridotites are characterized by high equilibration temperatures (up to 1250 °C) even at low pressure, plagioclase-peridotite facies

  10. Textural evolution of a dunitic matrix during formation of hybrid troctolites: insights from the Monte Maggiore peridotitic body (Corsica, France).

    Science.gov (United States)

    Basch, Valentin; Rampone, Elisabetta; Crispini, Laura; Ildefonse, Benoit; Godard, Marguerite

    2017-04-01

    Many recent studies investigate the formation of hybrid troctolites after melt-rock interactions and impregnation of a dunitic matrix (Drouin et al, 2010; Sanfilippo et al, 2015). They describe the reactive percolation of a melt in a dunite, dissolving olivine and crystallizing interstitial minerals (plagioclase ± clinopyroxene), thus leading to the dismembering of mantle olivines and variations in the olivine crystal number, size and shape (Boudier & Nicolas, 1995). However, despite the number of studies describing a hybrid origin for troctolites, this process is rarely documented in a field-controlled geological setting allowing the observation of a gradient of the amount of melt impregnation in mantle dunites. The Monte Maggiore peridotitic body (Corsica, France) preserves a multi-stage melt-rock reaction decompressional evolution (Rampone et al, 2008), marked by a first episode of olivine-saturated melt percolation at spinel facies, which dissolved mantle pyroxenes and crystallized olivine, thus leading to the formation of replacive dunites. A second diffuse melt impregnation in the spinel peridotites and dunites dissolved olivine and crystallized interstitial plagioclase, orthopyroxene and clinopyroxene at plagioclase-facies conditions. This increasing modal proportion in interstitial phases led to the replacive formation of plagioclase peridotites, plagioclase dunites and hybrid troctolites. This makes the Monte Maggiore peridotites an ideal case study to investigate the formation of hybrid troctolites and the associated textural evolution of the rock-forming minerals by detailed field and microstructural observations. In order to quantify the evolution of the olivine matrix texture (i.e. number of grains, grain size, shape factor, aspect ratio) at thin section scale with ongoing melt impregnation, we used EBSD maps of 12 samples from spinel dunites to plagioclase dunites and troctolites. In these samples, reactive melt percolation and melt entrapment led to

  11. Use of Student Experiments for Teaching Embedded Software Development Including HW/SW Co-Design

    Science.gov (United States)

    Mitsui, H.; Kambe, H.; Koizumi, H.

    2009-01-01

    Embedded systems have been applied widely, not only to consumer products and industrial machines, but also to new applications such as ubiquitous or sensor networking. The increasing role of software (SW) in embedded system development has caused a great demand for embedded SW engineers, and university education for embedded SW engineering has…

  12. File list: Oth.Bon.10.AllAg.IDG-SW3 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available Oth.Bon.10.AllAg.IDG-SW3 mm9 TFs and others Bone IDG-SW3 SRX467367,SRX467366,SRX467...364,SRX467365,SRX467362,SRX467363,SRX467361,SRX467360 http://dbarchive.biosciencedbc.jp/kyushu-u/mm9/assembled/Oth.Bon.10.AllAg.IDG-SW3.bed ...

  13. File list: His.Bon.20.AllAg.IDG-SW3 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available His.Bon.20.AllAg.IDG-SW3 mm9 Histone Bone IDG-SW3 SRX467384,SRX467378,SRX467382,SRX...RX467375,SRX467376,SRX467385,SRX467369 http://dbarchive.biosciencedbc.jp/kyushu-u/mm9/assembled/His.Bon.20.AllAg.IDG-SW3.bed ...

  14. File list: ALL.Bon.20.AllAg.IDG-SW3 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available ALL.Bon.20.AllAg.IDG-SW3 mm9 All antigens Bone IDG-SW3 SRX467384,SRX467378,SRX46738...67376,SRX467385,SRX467387,SRX467369 http://dbarchive.biosciencedbc.jp/kyushu-u/mm9/assembled/ALL.Bon.20.AllAg.IDG-SW3.bed ...

  15. File list: ALL.Bon.05.AllAg.IDG-SW3 [Chip-atlas[Archive

    Lifescience Database Archive (English)

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  1. Poland-Moebius syndrome: a case report.

    Science.gov (United States)

    Kiratli, H; Erdener, U

    2000-01-01

    The primary site of pathology in Moebius syndrome is still unknown, although several studies have variably localized the lesion in the extraocular muscles, cranial nerves, or central nervous system. A 24-year-old man with Poland-Moebius syndrome and acquired progressive bilateral paralytic lower eyelid ectropion is described. In this patient, magnetic resonance imaging studies revealed a barely detectable pontine hypoplasia and normal recti muscles. Nerve conduction studies of the facial nerves showed a severe demyelinating or dysmyelinating type of neuropathy. Bilateral lower eyelid ectropium of the patient was successfully corrected by canthal tightening procedures. Contrary to many reported cases, this patient serves as a rare example of a progressive type of Poland-Moebius syndrome presumably resulting from a combination of a brainstem abnormality and a peripheral neural degenerative process.

  2. Development of laser technology in Poland

    CERN Document Server

    Gajda, J

    2009-01-01

    The paper presents chosen development threads of laser technology and associated branches of optoelectronics in this country. An occasion to summarize the work and show their current status is the 50 th anniversary of construction of the first laser. The first laser in Poland was launched successfully in 1969, almost simultaneously at WAT and PW. Domestic achievements in this area are summarized every three years by Symposium on Laser Technology held traditionally in Swinoujscie. The work carried on in Poland concerns technology of laser materials, construction of new lasers and associated equipment as well as laser applications. Many technical teams participate in laser oriented European structural and framework projects. Ths is an invited paper to present participation of Polish teams in such European projects as EuCARD - European Coordination of Accelerator Research, FLASH - Free ELctron Laser in DESY Hamburg, E-XFEL - European X-Ray FEL, ELI - Extreme Light Infrastructure, and HIPER.

  3. Molecular epidemiology of rabies virus in Poland.

    Science.gov (United States)

    Orłowska, Anna; Żmudziński, Jan Franciszek

    2014-08-01

    The paper describes a phylogenetic study of 58 Polish isolates of rabies virus collected between 1992 and 2010. Sequences of the nucleoprotein (N) and glycoprotein (G) genes approximately 600 bp long were compared with reference sequences (GenBank) of European rabies viruses from neighbouring countries. The study confirmed a very high level of homology (94.4-100 %) of the Polish rabies virus strains irrespective of the date of isolation. Two variants of rabies virus: NEE (Northeastern Europe variant) and CE (Central Europe variant), depending on the geographical place of isolation, were circulating in Poland from 1992 to 2010. The Polish rabies virus isolates showed high similarity to European RABV strains, especially those collected in Ukraine and Romania. They were clearly different from vaccine strains SAD B19 and SAD Bern, which have been used for oral vaccination of foxes against rabies in Poland since 1993.

  4. Health care under transformation in Poland.

    Science.gov (United States)

    Tymowska, K

    2001-05-01

    The general health insurance introduced in Poland in 1999 is essentially a social insurance. In this article, the main features of the present health care system are discussed, i.e. the sources and principles of financing, ownership relations, structures, entitlements to obtain medical services and the rules of access to services. Emphasis has been put on the operations of various entities operating within the health care sector, including opportunistic conduct of the providers of services financed from public sources, cost dumping, establishing provider alliances, methods of cost control, and the fact that some patients leave the publicly financed system. In Poland, a parallel private system has been developing for many years. Systemic transformations have not changed that direction, but increased considerably the significance of household income and education as the factors that differentiate patient in equality. This article is concluded with the note on the opportunities for the development of supplementary private insurance.

  5. Facies studies of bituminous coals in Poland

    Energy Technology Data Exchange (ETDEWEB)

    Nowak, Grzegorz J. [Polish Geological Institute, Lower Silesian Branch, al. Jaworowa 19, 53-122, Wroclaw (Poland)

    2004-04-23

    Polish bituminous coal basins are associated exclusively with Carboniferous deposits, differing in origin and geological structure. This paper presents only short review of papers of Polish authors on coal facies studies of Carboniferous coals occurring in the Lower Silesian Coal Basin (LSCB), Upper Silesian Coal Basin (USCB) and Lublin Coal Basin (LCB) of Poland. Facies investigations of Carboniferous coals of Poland have been in progress over 20 years. The results of these studies have provided new information on such subjects as: (1) recognition of main depositional conditions in paleomires, (2) determine prevailing paleoplant communities, (3) appraisal of peat-forming environment reconstruction-types and characteristics of paleomires. These facies analyses are connected to results of such studies as: pure coal petrology, using maceral and microlithotype composition as parameters of the environment of coal deposition, combined results of petrological, palynological and sedimentological studies.

  6. Poland Syndrome. Case Presentation and Bibliographic Review

    Directory of Open Access Journals (Sweden)

    Lidia Torres Aja

    2016-10-01

    Full Text Available Diverse changes in the morphology and structure of the mammary gland have been described as a result of the variation of the regulatory mechanisms of its development. Amastia is one of the less frequent congenital anomalies of the breast and it consists on the total absence of one or both glands. When it is unilateral it is generally also accompanied by the lack of the major and minor pectoral muscle besides other malformations, constituting what is known as Poland Syndrome. A case of a fifteen year old female patient is presented who shows the congenital absence of the right breast. This is the first case of Poland Syndrome diagnosed in Cienfuegos, this is why the publication of this case is considered of interest for the scientific community.

  7. DEVELOPMENT OF ORGANIC FARMING IN POLAND

    Directory of Open Access Journals (Sweden)

    Zbigniew Gołaś

    2016-12-01

    Full Text Available The main aim of the article is to characterize development of organic farming in Poland in 2004–2014. The research refers to aspects such as the number and structure of organic producers, the structure of ecological land and organization, and the productivity and profi tability of organic farmsin comparison to conventional farms. The research shows that since the accession of Poland into the EU, the domestic organic farming sector has developed dynamically. The number of organic producers increased sevenfold in 2004–2014 and the observed changes were caused by an increase in both the number of ecological farms and organic food processing enterprises. Organic and conventional farms clearly diff er in terms of organization, productivity and profi tability. Conventional farms experienced higher rates of productivity, land profi tability, and work profi tability. Furthermore, the financial situation of organic farms was vastly determined by state subsidies, which constituted almost 80% of income accrued from agricultural production.

  8. Poland, variable geometry and the enlarged European Union.

    OpenAIRE

    Schweiger, Christian

    2014-01-01

    This article examines the role of Poland in the European Union, where the traditional Franco-German leadership axis has been replaced by a new ‘variable geometry’ of leadership constellations across a variety of policy areas. In this setting Poland has the potential to move from maintaining an initially passive role as a policy-taker towards becoming an agenda-setter alongside other larger and more traditionally dominant member states, especially Germany. However, Poland's success in this mat...

  9. A new record of Spergularia marina (Caryophyllaceae from southern Poland

    Directory of Open Access Journals (Sweden)

    Pliszko Artur

    2017-03-01

    Full Text Available Spergularia marina, a rare native halophyte and nationally vulnerable species, is reported from a new locality in southern Poland. It was found on 14 September 2016 in Mogilany, Lesser Poland Voivodeship, growing between paving stones at the Zakopianka road. Map of distribution of S. marina in Poland based on the ATPOL cartogram method is provided, and its possible pathways of introduction are discussed.

  10. New records of Gypsophila perfoliata (Caryophyllaceae in Poland

    Directory of Open Access Journals (Sweden)

    Pliszko Artur

    2016-12-01

    Full Text Available The paper presents two new records of alien Gypsophila perfoliata in Poland. It was found on 16 September 2016 in Bodzanów and Łapczyca, Lesser Poland Voivodeship, southern Poland, growing on roadside slopes and in roadside ditch. The updated map of distribution is presented using the ATPOL cartogram method, and the pathways of introduction and spreading are discussed.

  11. Batrachospermum atrum (Rhodophyta – first record in Poland

    Directory of Open Access Journals (Sweden)

    Kowalski Wojciech A.

    2013-12-01

    Full Text Available The paper gives new data on the occurrence of Batrachospermum atrum (Hudson Harvey, a freshwater Rhodophyta species rare in Poland. It was found growing on stony bottom in a small stream in northwestern Poland; at this site it was associated mainly with Potamogeton nodosus Poir., green algae Cladophora glomerata (L. Kützing and Mougeotia sp. Its occurrence in Poland and some ecological data are discussed, and original photographs of the plant and its habitat are presented.

  12. THE ASSESSMENT AND USE OF INTEGRATED PRODUCT POLICY IN POLAND

    Directory of Open Access Journals (Sweden)

    Anna ANDRYKIEWICZ

    2012-10-01

    Full Text Available The paper presents the implementation of Integrated Product Policy in Poland in the light of the European activities. It analyses the EU laws within this scope. It assesses the progress of LCA implementation, ecolabelling, ecotaxes, EMAS and green public procurement in Poland. It explains the reasons of slow IPP implementation in Polish organisations. It mainly refers to the distribution and promotion of ecolabelling, based on empirical research in Germany and Poland.

  13. Church unions and their consequences in Poland

    Directory of Open Access Journals (Sweden)

    Antoni Mironowicz

    2014-11-01

    Full Text Available Orthodox Christians in Poland have faced numerous attempts to be forced into union with the Roman Catholic Church, ranging from the thirteenth to the twentieth century. The first attempt at a union between the Roman Catholic Church and the Orthodox Church took place as early as the mid-thirteenth century. Another attempt at forcing the Orthodox Church into union with Rome took place during the reign of Ladislaŭ II Yagiello. The problem of church union returned in the reign of Alexander the Yagiellonian. When Ivan III rejected all projects for bringing the Florence such a union into practice, discussion on church union disappeared until the end of the sixteenth century. The mission of the papal legate, Father Antonio Possevino, to Ivan IV, had been intended to draw Moscow into the union, and its failure caused the papacy to concentrate its efforts on the Orthodox Church in Poland. The Ruthenian bishops’ obedience to the Pope was officially announced on the 8 October 1596. The decisions of the Uniate-Catholic synod were met with numerous protests from the Orthodox clergy and nobility. The larger part of the clergy and the faithful, together with bishops remained in the Orthodox camp. Despite the failure of the Brest Synod in fully uniting Orthodox and Roman churches, new union projects concerning the Orthodox Church in Poland continued to arise prior to the end of 18th century. The Vatican’s interest in the Orthodox Church in Central Europe was renewed at the end of the First World War. On April 1st, 1917, the Pope created the Congregation for the Oriental Churches which was responsibile for all issues relating to the activities of all the Eastern denominations. Despite aims at unification, attempts at church union have had a negative influence on the relations between the Roman Catholic and Polish Orthodox Church in contemporary Poland. The result of centuries of attempts at unification under the Pope has been fragmentation and division.

  14. Abortion and women's rights in Poland, 1994.

    Science.gov (United States)

    David, H P; Titkow, A

    1994-01-01

    In 1993, a restrictive abortion law was enacted in Poland. The law allows abortion in public hospitals when 3 physicians certify that the life or health of the woman is at stake, the fetus has a serious and irreversible malformation (supported by prenatal tests in cases of known history of genetic conditions), or a public prosecutor formally proves that a criminal act (i.e., rape or incest) caused the pregnancy. Physicians who perform illegal abortions can be imprisoned up to 2 years and, in cases where the woman dies from complications, up to 10 years. The law calls for the government to offer sex education and to guarantee access to contraceptives nationwide, to which the Catholic Bishops object. Schools have yet to implement sex education. Interviews show that much political and governmental instability exists in Poland. Politicians tend to be passive to prevent political conflict and reduce tensions with the Catholic Church. Women who have enough money and have an unwanted pregnancy can still obtain an abortion within Poland or across the border. Infanticide and infant abandonment are increasing. Illegal adoption is occurring. No one has been arrested for performing clandestine abortions. Young, poor, and rural women are confused and anxious. Many physicians fear referring women for legal abortions. Some hospitals refuse to allow any abortion. Poland is still a patriarchal, conservative country. Most women who use birth control use the rhythm method and withdrawal. Counseling centers are closing. Public educational resources are scarce. Recorded miscarriages have risen from 51,802 in 1992 to 53,027 in 1993. The Ministries of Health and Justice object to the new law. In 1994, the president vetoed a law that would have allowed abortions on social grounds. The birth rate fell from 13.4 to 12.8 births/1000 between 1992 and 1993. The public now ranks the Church behind the military, the police, and the government ombudsman in public trust.

  15. The current state of bioeconomy in Poland.

    Science.gov (United States)

    Woźniak, Ewa; Twardowski, Tomasz

    2016-01-01

    Conversion of scientific achievements to market a product is a key issue and the best description of significance of science for society. In the case of experts in the natural sciences in Poland, we observe a high intellectual potential of researchers and several scientific discoveries. However, Polish inventions are very rarely available on the market and the number of national and international patent applications done by Polish scientists is very limited. For the development of bioeconomy, the progress in biotechnology is critical.

  16. Economic determinants of sport participation in Poland

    OpenAIRE

    Paweł Strawiński

    2010-01-01

    The article presents statistical description of economic factors that determine sport participation in Poland. Utilising data from 2008 Sport Participation Survey the biprobit model that takes into account the dependency between individuals and household attitude to sport participation is estimated. Sport participation is found to slightly decline with age of a person, on the other hand, education is found to be positively related to sport participation. The idiosyncratic factor of sport part...

  17. Interrelations between Consumption and Wealth in Poland

    OpenAIRE

    Magdalena Zachłód-Jelec

    2010-01-01

    This paper studies the long-run relationship between consumption, labour income and asset wealth in Poland. Within cointegrated VAR model dynamic responses of the variables in the system to shocks are studied. In addition, series are decomposed into permanent and transitory components on the basis of the cointegrating relation found in the system. Main conclusion of this paper is that deviations of the three variables from their estimated long-run relationship are better explained with fluctu...

  18. Beyond Viagra: Sex Therapy in Poland

    OpenAIRE

    Kościańska, Agnieszka

    2014-01-01

    In the 1970s and 1980s, Poland, like most other countries in the region, provided not only unlimited access to abortion and contraceptives, but also a liberal sex education. This period moreover constituted a golden age in sexology in the country. Sexual science developed as a holistic discipline, embracing achievements in medicine, psychology, sociology, anthropology, philosophy, history, and religious studies, providing recourses for sex education and therapy. Sexuality was perceived as mul...

  19. Pharmaceutical Distribution Market Channels in Poland

    OpenAIRE

    Agnieszka Woś

    2009-01-01

    Distribution on the pharmaceutical market in Poland is interesting and the most difficult sphere to manage. Numerous varied and specialized companies operating on the market cause that the processes of choosing middlemen in distribution channels are very complex. The hereby article presents the role and location of the companies operating within distribution channels on the pharmaceutical market. It draws attention to the development of non-pharmacy and non-wholesale sales channels.

  20. [Social aspect of clinical research in Poland].

    Science.gov (United States)

    Masełbas, Wojciech; Czarkowski, Marek

    2007-12-01

    Each year more than 400 new clinical studies are registered in Poland. They gather above 50.000 of study participants. Social opinion on clinical trials is an important factor. The paper presents the review of actual opinions on clinical research in Poland. It provides the description of standards of protection of study participants, benefits and risks related to the participation in clinical research and the role of media in creating and influencing of the social perception of clinical trials. Results of conducted questionnaire studies imply that Poles correctly identify and assess the risk of participation in clinical experiments. The primary reason for the participation seams to be the possibility to help other patients, contribution to the progress of science and standards of medical care and potential benefits for other sufferers. The need of testing the safety and efficacy of the new medication in man is generally well recognized. At the same time a substantial part of the society is concerned with the possible corruption of investigators and unethical behaviour of sponsors. The social perception of clinical research in Poland is in majority of analyzed parameters not substantially different from opinions in other member states of EU. However, the medical society should be more active in influencing and changing some negative impressions.

  1. Funding Innovation in Poland through Crowdfunding

    Directory of Open Access Journals (Sweden)

    Katarzyna Kozioł-Nadolna

    2016-01-01

    Full Text Available Funding innovative projects is one of the most serious problems faced by business owners in Poland. Therefore, due to the difficulties of obtaining external sources of financing, crowdfunding may constitute a new source of fundraising for innovative ventures. Therefore, crowdfunding – as a way of raising capital for projects – is the subject of the discussion in this article. The research aim of the article is to identify and evaluate crowdfunding platforms as well as the innovative projects carried out by these platforms in Poland in 2014-2016. The first part characterizes crowdfunding as a source of funding innovation and presents the nature of crowdfunding, its characteristics and models. The empirical part is based on inductive-deductive inference, desk research, i.e. the analysis of crowdfunding market in Poland in two research periods and a case study analysis. The article shows the results of the research on the Polish crowdfunding market in 2014-2016. The author also presents a case study of funding innovation on the Kickstarter.com platform by a Polish company Sher.ly.

  2. CHP plant Legionowo Poland - Final report

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2004-12-01

    In 1997, a new Energy Law was passed in Poland. An important element of the law is that local energy planning is made obligatory. The law describes obligatory tasks and procedures for Polish municipalities related to planning and organisation of the energy sector. With the objective of supporting the Polish municipalities in their obligations according to the energy law of 1997, the project 'Energy Planning in Poland at Municipal Level - Support to Decision Makers' was launched. As part of the project, Municipal Guideline Reports have been elaborated for three model municipalities. These guidelines present the basis for the Energy Supply Plans in these municipalities. For the city of Legionowo, the following was recommended: 1. The planning processes initiated during the project should be continues/followed up, 2. Master Plan for the district heating system should be prepared, 3. The possibilities of establishment of a major natural gas-fired CHP plant of the Combined Cycle type should be investigated. The present report is the final Master Plan based on the following reports: Master Plan for Legionowo - Status Report; Master Plan for Legionowo - Hydraulic Analysis; CHP Plant Legionowo Poland - CHP Feasibility Analysis. The final Master Plan describes the status in the DH Company in Legionowo, possible improvements and an investment plan for the selected scenario. (BA)

  3. The medical physics specialization system in Poland.

    Science.gov (United States)

    Bulski, Wojciech; Kukołowicz, Paweł; Skrzyński, Witold

    2016-07-01

    This paper presents the situation of the profession of medical physicists in Poland. The official recognition of the profession of medical physicist in Polish legislation was in 2002. In recent years, more and more Universities which have Physics Faculties introduce a medical physics specialty. At present, there are about 15 Universities which offer such programmes. These Universities are able to graduate about 150 medical physicists per year. In 2002, the Ministry of Health introduced a programme of postgraduate specialization in medical physics along the same rules employed in the specialization of physicians in various branches of medicine. Five institutions, mostly large oncology centres, were selected as teaching institutions, based on their experience, the quality of the medical physics professionals, staffing levels, equipment availability, lecture halls, etc. The first cycle of the specialization programme started in 2006, and the first candidates completed their training at the end of 2008, and passed their official state exams in May 2009. As of January 2016, there are 196 specialized medical physicists in Poland. Another about 120 medical physicists are undergoing specialization. The system of training of medical physics professionals in Poland is well established. The principles of postgraduate training and specialization are well defined and the curriculum of the training is very demanding. The programme of specialization was revised in 2011 and is in accordance with EC and EFOMP recommendations. Copyright © 2016 Associazione Italiana di Fisica Medica. Published by Elsevier Ltd. All rights reserved.

  4. Additions to the biota of lichenized fungi of Poland

    Directory of Open Access Journals (Sweden)

    Adam Flakus

    2013-12-01

    Full Text Available New records of five lichenized fungi from Poland are provided. Hypotrachyna afrorevoluta, Lecanora quercicola, Rhizocarpon superficiale and Strigula ziziphi are new to Poland. Of these, Strigula ziziphi is reported also as new to Central Europe and Hypotrachyna afrorevoluta as new to the Carpathians. Additionally, Thelenella muscorum var. octospora is recorded from its second locality in Poland as new to the Polish Carpathians. Hypostictic acid chemosyndrome has been noticed for the first time in European (Poland and South American (Bolivia populations of Rhizocarpon superficiale.

  5. Hydrous melts weaken the mantle, crystallization of pargasite and phlogopite does not: Insights from a petrostructural study of the Finero peridotites, southern Alps

    Science.gov (United States)

    Tommasi, Andréa; Langone, Antonio; Padrón-Navarta, José Alberto; Zanetti, Alberto; Vauchez, Alain

    2017-11-01

    This study reports petrostructural observations in the pargasite and phlogopite-bearing Finero peridotite massif (Italian Western Alps), which suggest that the pervasive foliation in this massif was formed by deformation concomitant with percolation of hydrous Si-rich melts: (1) diffuse contacts, but systematic parallelism between the pyroxenitic layers and the foliation of the peridotite (2) strong shape and crystal preferred orientations (SPO and CPO), but subhedral or interstitial shapes and weak intracrystalline deformation of the hydrous phases, (3) CPO, but interstitial shapes of the pyroxenes, (4) very coarse olivine grain sizes, which are correlated to the olivine abundance, and (5) elongated shapes, but weak intracrystalline deformation, and extremely weak and highly variable CPO of olivine. The pervasive deformation of the Finero peridotite occurred therefore under conditions that allowed coexistence of H2O-CO2-bearing melts, pargasite, and spinel, that is, temperatures of 980-1080 °C and pressures dislocation creep to the deformation. The associated increase of the peridotites' strength leads to onset of strain localization. The latter is not correlated to the local abundance in pargasite or phlogopite, implying that crystallization of amphiboles or phlogopite, even at concentrations of 25 vol.%, does not produce rheological weakening in the upper mantle.

  6. Late Palaeozoic to Triassic formations unconformably deposited over the Ronda peridotites (Betic Cordilleras: Evidence for their Variscan time of crustal emplacement

    Directory of Open Access Journals (Sweden)

    Sanz de Galdeano, C.

    2016-06-01

    Full Text Available The age of the emplacement of the Ronda Peridotites has been widely debated during recent decades, and ages ranging from the Palaeozoic to the early Miocene have been proposed, although most of the current interpretations suggest an Oligocene-Miocene age. In this article, we describe two meta-sedimentary formations (the lower one formed by detrital sediments and the upper one by marbles that were unconformably deposited over the Ronda peridotites and now record low-grade metamorphism. The detrital formation contains layers of acidic rocks with an age of 269±9 Ma and the overlying marbles are assumed to be Triassic. The existence of these unconformable formations over the peridotites is crucial for the dating of the exhumation of the latter. The presence of peridotite clasts in the detrital formation indicates that peridotites were exposed during the Permian and other data suggest that peridotites were exhumed during the late Carboniferous. During the Alpine cycle, the peridotites operated as an element situated at the bottom of the tectonically higher Alpujarride/Sebtide unit (the Jubrique unit and forming part of it, then being incorporated to the Alpine thrusts of this unit.La edad del emplazamiento de las peridotitas de Ronda ha sido discutida ampliamente en las últimas décadas, con hipótesis que van desde el Paleozoico al Mioceno inferior, aunque la mayoría de las interpretaciones actuales sugiere una edad oligo-miocena. En este artículo, describimos la existencia de dos formaciones meta-sedimentarias (la inferior formada originalmente por sedimentos detríticos y la superior por carbonatos que se depositaron en discordancia sobre las peridotitas de Ronda y ahora registran un grado bajo de metamorfismo. La formación detrítica contiene capas de rocas ácidas con una edad de 269±9 Ma y los mármoles situados encima se atribuyen al Trías. La existencia de esas dos formaciones es crucial para la datación de la exhumación de las

  7. Significance of the whole rock Re-Os ages in cryptically and modally metasomatised cratonic peridotites: Constraints from HSE-Se-Te systematics

    Science.gov (United States)

    Luguet, Ambre; Behrens, Melanie; Pearson, D. Graham; König, Stephan; Herwartz, Daniel

    2015-09-01

    The Re-Os isotopic system is the geochronometer of choice to constrain the timing of lithospheric mantle root formation and reconstruct the evolution of Earth's dynamics from the "mantle" perspective. In order to constrain the effects of metasomatic processes on the Re-Os isotopic system, eleven peridotites from the Letlhakane kimberlite pipe were investigated for whole rock major and trace elements, highly siderophile elements (HSE), Se, Te and 187Os/188Os signatures. These spinel peridotites (SP), garnet peridotites (GP), garnet-phlogopite peridotites (GPP) and phlogopite peridotites (PP) experienced cryptic metasomatism and the GP-GPP-PP additionally constitute a sequence of increasing modal metasomatism. The cryptically metasomatised SP appear devoid of base metal sulphides (BMS) and show suprachondritic Se/Te ratios (15-40) and extremely Pd- and Pt-depleted HSE patterns. These features are characteristic of high-degree partial melting residues. Their 187Os/188Os signatures are thus considered to be inherited from the partial melting event. This implies a Neoarchean (2.5-2.8 Ga, TRD eruption) stabilisation of the Letlhakane mantle root and supports the Letlhakane mantle root being a westerly extension of the Zimbabwe cratonic root. The modally metasomatised peridotites contain BMS whose abundance significantly increases from the GPP to the GP and PP. The BMS-poor GPP are only slightly richer in Pt and Pd than the BMS-free SP but have similarly high Se/Te ratios. The BMS-rich GP and PP exhibit significant enrichments in Pt, Pd, Se, Te resulting in HSE-Se-Te signatures similar to that of the Primitive Upper Mantle (PUM). Addition of 0.001-0.05 wt.% metasomatic BMS ± PGM (platinum group minerals, i.e., Pt-tellurides) to highly refractory residues, such as the Letlhakane SP, reproduce well the HSE-Se-Te systematics observed in the BMS-poor and BMS-rich modally metasomatised peridotites. In the GPP, the negligible addition of metasomatic BMS ± PGM did not disturb

  8. {Omega}/{Xi} production ratio in S-W

    Energy Technology Data Exchange (ETDEWEB)

    Abatzis, S. [Nuclear Physics Department, Athens University, GR-15771 Athens (Greece); Andrighetto, A.; Antinori, F.; Barnes, R.P.; Bayes, A.C.; Benayoun, M.; Beusch, W.; Carney, J.N.; de la Cruz, B.; Di Bari, D.; Dufey, J.P.; Davies, J.P.; Elia, D.; Evans, D.; Fini, R.; French, B.R.; Ghidini, B.; Helstrup, H.; Holme, A.K.; Jacholkowski, A.; Kahane, J.; Kinson, J.B.; Kirk, A.; Knudson, K.; Lassalle, J.C.; Lenti, V.; Leruste, P.; Manzari, V.; Narjoux, J.L.; Navach, F.; Quercigh, E.; Rossi, L.; Safarik, K.; Sene, M.; Sene, R.; Storas, T.; Vassiliadis, G.; Villalobos Baillie, O.; Volte, A.; Votruba, M.F.; Federico Antinori/CERN & Genova for WA85 Collaboration

    1995-07-20

    We have measured the ({Omega}{sup {minus}}+{bar {Omega}}{sup +})/({Xi}{sup {minus}}+{bar {Xi}}{sup +}) production ratio in central S-W collisions to be 0.8{plus_minus}0.4 at central rapidity and p{sub T}{gt}1.6 GeV/{ital c}. {copyright} 1995 {ital American} {ital Institute} {ital of} {ital Physics}.

  9. Mylonitic deformation in upper mantle peridotites of the North Pyrenean Zone (France): implications for strength and strain localization in the lithosphere

    Science.gov (United States)

    Vissers, R. L. M.; Drury, M. R.; Newman, J.; Fliervoet, T. F.

    1997-09-01

    The Turon de Técouère peridotite in the west of the North Pyrenean Zone contains four types of mylonitic structures: (1) protomylonites, (2) mylonites, (3) platy ultramylonites, each developed in map-scale domains, and (4) cm-scale, vein-like ultramylonites. These mylonites are marked by increasing volume fractions of very fine-grained matrix enclosing mm- to cm-scale porphyroclasts derived from the lherzolite protolith. Progressive mylonitization was associated with the transformation from spinel- to plagioclase-bearing assemblages, which indicates exhumation of the peridotites and suggests that mylonitization was related to lithosphere extension. The mylonites are usually interpreted to have formed during Albian-Aptian rifting. Final emplacement of the peridotites in the upper crust must certainly have occurred in the Cretaceous, but we argue that the mylonitic deformation and initial crustal emplacement could also have taken place during Variscan late-orogenic extension. For lack of a pre-mylonitic protolith, our study of the Turon de Técouère mylonites is supplemented by microstructural data from the Moncaup and Etang de Lhers peridotites. The protomylonites of Turon de Técouère and the selected samples from Moncaup and Etang de Lhers contain microstructures suggesting high-stress dislocation creep and concurrent dynamic recrystallization, but also planar discontinuities with and without extremely fine-grained material suggesting incipient brittle behaviour. Bot ductile and brittle mechanisms may thus have induced strain localization. High flow stress estimates (300-1300 MPa) using piezometry and olivine flow laws indicate that the inferred conditions of incipient mylonitization may indeed have allowed semi-brittle flow. Unlike upper mantle shear zones described from other areas, localization in the North Pyrenean peridotites was independent of the presence of hydrated phases, and we envisage that these shear zones represent a case of effectively dry

  10. Antinociceptive activity of methanolic extract of Acmella uliginosa (Sw.) Cass.

    Science.gov (United States)

    Ong, Hui Ming; Mohamad, Azam Shah; Makhtar, Nor 'Adilah; Khalid, Mohamed Hanief; Khalid, Syamimi; Perimal, Enoch Kumar; Mastuki, Siti Nurulhuda; Zakaria, Zainul Amiruddin; Lajis, Nordin; Israf, Daud Ahmad; Sulaiman, Mohd Roslan

    2011-01-07

    Acmella uliginosa (Sw.) Cass. is a medicinal herbaceous plant that is commonly used by the Malay community in Malaysia to relieve pain often associated with mouth ulcers, toothache, sore throat, and stomach ache. The study was carried out to investigate the antinociceptive effect of the methanolic extract of A. uliginosa (Sw.) Cass. flowers (MEAU) using murine models of chemicals and thermal nociception. Chemicals (acetic acid-induced abdominal constriction and formalin-, capsaicin-, glutamate-induced paw licking test) and thermal models (hot plate test) of nociception in mice were employed to evaluate the MEAU analgesic effect. The extract was given via oral administration at doses of 3, 10, 30 and 100 mg/kg. It was demonstrated that MEAU produced significant antinociceptive response in all the chemical- and thermal-induced nociception models, which indicates the presence of both centrally and peripherally mediated activities. Furthermore, the reversal of antinociception of MEAU by naloxone suggests the involvement of opioid system in its centrally mediated analgesic activity. Moreover, MEAU-treated mice did not show any significant motor performance alterations. No mortality and signs of toxicity were recorded following treatment of the MEAU. The results from the present study appear to support the folkloric belief in the medicinal properties of A. uliginosa (Sw.) Cass. which against pain at both central and peripheral levels, in which the central antinociception is probably due to the participation of the opioid receptors. Copyright © 2010 Elsevier Ireland Ltd. All rights reserved.

  11. Olivine compositions from the Hawaii Scientific Drilling Project, Phase 2: Evidence for a peridotite mantle source region

    Energy Technology Data Exchange (ETDEWEB)

    Putirka, K D; Ryerson, F J

    2008-10-27

    To the extent that mantle plumes reflect whole mantle convection, Hawaii may provide the clearest window into Earth's lower mantle. Samples from the Hawaii Scientific Drilling Project (HSDP) thus provide valuable tests for models of mantle mineralogy and composition. In this vein, it has been argued recently that Hawaiian olivines, especially those from the shield-building phase as sampled by HSDP, are so high in Ni (Sobolev et al., 2005, 2007), and that Hawaiian whole rocks are so low in CaO (Herzberg, 2006) and high in SiO{sub 2} (Hauri, 1996) that a peridotite mantle source cannot generate such compositions. The Hawaiian plume, so the argument goes, is thus supposedly rich in pyroxenite, and possibly olivine-free. However, comparisons of HSDP olivines to lherzolites, and HSDP whole rocks to lherzolites and partial melting experiments belie these premises. Testable predictions of the pyroxenite model also fail. New comparisons instead show that Hawaiian lavas can be produced from a peridotite source. First, it is unclear that the Hawaiian source is enriched in NiO. The NiO contents of olivines hosted by lherzolites (GEOROC) have the same range as olivines from the HSDP; indeed, the maximum NiO for olivines from lherzolites (0.6 wt.%) is as high as that reported for olivines from any oceanic volcano locality. There is a compositional separation between lherzolite- and HSDP-hosted olivines. But HSDP olivines are not NiO enriched so much as lherzolite olivines are higher in Fo at a given NiO. Lower Fo contents at Hawaii (at a given NiO) ensue because olivine compositions there follow a liquid line of descent, where both Ni and Mg decrease with differentiation. In contrast, subsolidus equilibria involving orthopyroxene enforce a higher and less variable Fo content for lherzolite-derived olivines. Moreover, the pyroxenite mantle model predicts that whole rocks with low CaO and high SiO{sub 2} should host olivines with high NiO. But in HSDP samples, neither

  12. Application of Markov Chain Monte Carlo Method to Mantle Melting: An Example from REE Abundances in Abyssal Peridotites

    Science.gov (United States)

    LIU, B.; Liang, Y.

    2015-12-01

    Markov chain Monte Carlo (MCMC) simulation is a powerful statistical method in solving inverse problems that arise from a wide range of applications, such as nuclear physics, computational biology, financial engineering, among others. In Earth sciences applications of MCMC are primarily in the field of geophysics [1]. The purpose of this study is to introduce MCMC to geochemical inverse problems related to trace element fractionation during concurrent melting, melt transport and melt-rock reaction in the mantle. MCMC method has several advantages over linearized least squares methods in inverting trace element patterns in basalts and mantle rocks. First, MCMC can handle equations that have no explicit analytical solutions which are required by linearized least squares methods for gradient calculation. Second, MCMC converges to global minimum while linearized least squares methods may be stuck at a local minimum or converge slowly due to nonlinearity. Furthermore, MCMC can provide insight into uncertainties of model parameters with non-normal trade-off. We use MCMC to invert for extent of melting, amount of trapped melt, and extent of chemical disequilibrium between the melt and residual solid from REE data in abyssal peridotites from Central Indian Ridge and Mid-Atlantic Ridge. In the first step, we conduct forward calculation of REE evolution with melting models in a reasonable model space. We then build up a chain of melting models according to Metropolis-Hastings algorithm to represent the probability of specific model. We show that chemical disequilibrium is likely to play an important role in fractionating LREE in residual peridotites. In the future, MCMC will be applied to more realistic but also more complicated melting models in which partition coefficients, diffusion coefficients, as well as melting and melt suction rates vary as functions of temperature, pressure and mineral compositions. [1]. Sambridge & Mosegarrd [2002] Rev. Geophys.

  13. MOLLUSC SPECIES PROTECTED IN POLAND AND THREATENED IN EUROPE RECORDED IN STEPNICA RIVER (NW POLAND

    Directory of Open Access Journals (Sweden)

    Małgorzata Raczyńska

    2014-10-01

    Full Text Available In the course of the study two bivalve species protected in Poland were found in the river Stepnica: Sphaerium solidum and Sphaerium rivicola. Moreover, the study material collected from the river contained gastropod and bivalve specimens representing the following species from the IUCN Red List of Threatened Species: Theodoxus fluviatilis, Pisidium henslowanum, Pisidium casertanum and Pisidium pseudosphaerium.

  14. Poland 1999 Global Youth Tobacco Survey : Economic Aspects

    OpenAIRE

    Ross, Hana; Przewozniak, Krzysztof

    2004-01-01

    In 1999, Poland was one of the first countries to carry out the Global Youth Tobacco Survey (GYTS), supported by the US Centers for Disease Control and Prevention, and World Health Organization, a standardized school-based survey of teenage smoking behavior, attitudes, and knowledge. This report presents background information on smoking, and tobacco control policies in Poland, and simple ...

  15. Dimensions of health among the elderly in Poland and Croatia

    NARCIS (Netherlands)

    Knurowski, T.; Lazic, D.; van Dijk, J.P.; Geckova, Andrea; Tobiasz-Adamczyk, B.; van den Heuvel, W.J.A.

    2004-01-01

    On the basis of the WHO definition of health, we aimed at exploring the model of health and identifying the most important dimensions of health among the elderly in two Central European countries: Poland and Croatia. Randomly chosen elderly aged 65-85 from Krakow (Poland) and from Zagreb and some

  16. Distribution of some lichenicolous fungi in Poland. II

    Directory of Open Access Journals (Sweden)

    Katarzyna Czyżewska

    2013-12-01

    Full Text Available Twenty six species of lichenicolous fungi, one lichenicolous lichen and one lichenicolous myxomycete are discussed. Vouauxiomyces sp., the anamorph of Abrothallus caerulescens, is reported as new to Poland. Abrothallus microspermus is reported from the Polish lowlands for the first time. Trichonectria hirta and Vouauxiomyces truncatus are reported from Poland for the second time.

  17. Stochastic forecast of the population of Poland, 2005-2050

    NARCIS (Netherlands)

    Matysiak, Anna; Nowok, Beata

    2007-01-01

    Forecasting the population of Poland is very challenging. Firstly, the country has been undergoing rapid demographic changes. In the 1990s, they were influenced by the political, economic, and social consequences of the collapse of the communist regime. Since 2004 they have been shaped by Poland's

  18. Inflation stabilization, fiscal defecits and public debtmanagement in Poland

    NARCIS (Netherlands)

    van Wijnbergen, S.J.G.; Budina, N.

    1999-01-01

    Poland edged towards hyperinflation towards the latter half of 1989,but inflation fell dramatically after drastic reformswere enacted in January of 1990. We analyse the consistency betweenfiscal deficits and inflation targets and assessPoland's domestic and foreign debt management policies and the

  19. Creativity and School Grades: A Case from Poland

    Science.gov (United States)

    Gralewski, Jacek; Karwowski, Maciej

    2012-01-01

    The goal of this study was to describe the relationship between the creative abilities and the school grades of high school students in Poland. Almost six hundred (N = 589) students from 34 high schools from all over Poland participated in the study. Their creative abilities were measured by using the Test of Creative Thinking-Drawing Production…

  20. The development of internet advertisement in Poland throughout recent years

    OpenAIRE

    A. Kisiołek

    2014-01-01

    The article presents basic information regarding online advertisement and its most popular forms in Poland. Some part of the work is devoted to the development of Polish Internet advertisement since 2000, and particularly in 2010-2012. Historical trends in the development of online advertising in Poland are analyzed as well.

  1. Rare combination of dextrocardia with right-sided Poland syndrome.

    Science.gov (United States)

    Lee, Seung Hyun; Kim, Jae Bum; Park, Nam Hee; Keum, Dong Yoon; Kim, Yeo Hyang

    2012-10-01

    The combination of right-sided Poland syndrome and dextrocardia is rare. To our knowledge, reports regarding this subject are lacking in the published literature to date. Previous reports suggested that dextrocardia may be part of the left sided Poland syndrome. We report and discuss this rare combination. Copyright © 2012 The Society of Thoracic Surgeons. Published by Elsevier Inc. All rights reserved.

  2. Leucopaxillus lepistoides, a new steppe fungus in Poland

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    Janusz Łuszczyński

    2013-12-01

    Full Text Available The paper presents information on Leucopaxillus lepistoides (Maire Singer, a new species for Poland. This fungus was found in two localities: the neighbourhood of Busko Zdrój and Chęciny (Little Polish Upland, S-Poland. Both localities were in the xerothermic grasslands belonging to the Cirsio-Brachypodion Order, Festuco-Brometea Class.

  3. Fluoride pollution of atmospheric precipitation and its relationship with air circulation and weather patterns (Wielkopolski National Park, Poland).

    Science.gov (United States)

    Walna, Barbara; Kurzyca, Iwona; Bednorz, Ewa; Kolendowicz, Leszek

    2013-07-01

    A 2-year study (2010-2011) of fluorides in atmospheric precipitation in the open area and in throughfall in Wielkopolski National Park (west-central Poland) showed their high concentrations, reaching a maximum value of 2 mg/l under the tree crowns. These high values indicate substantial deposition of up to 52 mg/m(2)/year. In 2011, over 51% of open area precipitation was characterized by fluoride concentration higher than 0.10 mg/l, and in throughfall such concentrations were found in more than 86% of events. In 2010, a strong connection was evident between fluoride and acid-forming ions, and in 2011, a correlation between phosphate and nitrite ions was seen. Analysis of available data on F(-) concentrations in the air did not show an unequivocal effect on F(-) concentrations in precipitation. To find reasons for and source areas of high fluoride pollution, the cases of extreme fluoride concentration in rainwater were related to atmospheric circulation and weather patterns. Weather conditions on days of extreme pollution were determined by movement of weather fronts over western Poland, or by small cyclonic centers with meteorological fronts. Macroscale air advection over the sampling site originated in the western quadrant (NW, W, and SW), particularly in the middle layers of the troposphere (2,500-5,000 m a.s.l.). Such directions indicate western Poland and Germany as possible sources of the pollution. At the same time in the lower troposphere, air inflow was frequently from the north, showing short distance transport from local emitters, and from the agglomeration of Poznań.

  4. Poland-Moebius syndrome: a case with oral anomalies.

    Science.gov (United States)

    Domingos, A C; Lopes, S L C P; Almeida, S M; Boscolo, F N; Whaites, E J

    2004-11-01

    The combination of Moebius and Poland anomalies is rarely described in the literature. While some authors believe this association is an independent syndrome, others think that Poland, Moebius and Poland-Moebius syndromes are variations of the same condition. We report a case of Poland-Moebius syndrome in a 6-year-old girl who presented with bilateral convergent strabismus, the inability to abduct her eyes beyond the midline and brachydactyly of her right hand. Oral manifestations included incompetent lips and an abnormal tongue. Other facial features included hypoplasia of her mandible and her left ear at a slightly lower level than her right ear. Panoramic and lateral skull radiographs confirmed the absence of certain teeth and the hypoplastic mandible. The diagnosis of Poland-Moebius syndrome was made on the basis of cranial nerve involvement and oro-facial manifestations.

  5. THE E-HEALTH SYSTEMS IN POLAND

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    Zdzisław PÓLKOWSKI

    2013-11-01

    Full Text Available Information Technologies are disruptive technologies that have caused major changes in health system in Poland. Current digital economy is driven by modern information and new IT tools, which offer hospitals, doctors and patient access to any type of information, regardless of its form of existence, storage type or geographical location. These tools encourage the development of new activities, health services. The purpose of this article is to analyze the the current state of development of e-services in Poland in the context of nowadays health system. In the first part of the paper, the authors present various programmes, which enable the access to the medical services and patients’ data online. The next part of the paper is devoted to examining the technical aspects of the said programmes and presenting their advantages as well as the areas which might be improved.The last part of the work will be focused on the websites of the selected health institutions. According to the authors, WWW services provide much information on how the process of computer systems are being implemented, what data the services include and the capacity of the equipment as well as the software, human resources and the knowledge in this sphere. Moreover this section highlights the latest trends in e-health with particular emphasis on aspects such as the use of private and public cloud computer and t heir integration with web sites of health institutions. This study brings its contribution to the understanding of the change of health system in Poland behavior by using a new perspective e-health systems and IT tools above by doctors, officers and patients.

  6. Serbia 1914, Poland 1939… A comparison

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    Šćepanjski Vojćeh S.

    2015-01-01

    Full Text Available The circumstances of implicating Serbia (in 1914 and Poland (in 1939 into world wars by the forces provoking these conflicts, as well as the history of the heroic resistance of both mentioned organisms against the aggressors having numerous advantages, deserve to be constantly reminded as great lessons for the next generations of Europeans. The anniversaries of the break out of both world wars constitute a great opportunity for this type of reminder. In the presented text, compiling the Serbian experiences of the war started in 1914 with the Polish experience of the war which broke out a quarter of century later, the author stresses the follow­ing issues: - the reaction of Serbia/Poland on declaring the wars 1914/1939 (in detail, and also (in general: - the situation of war seclusion of Serbia/Poland in 1914/1939 experienced despite having the allies, - huge discrepancies of the aggressors' and the defenders' forces, as well as the resistance, exceeding the estimated opportunities, of the attacked countries towards the enemies, - the scale of the Serbian martyrdom in the 1st and Polish in the 2nd world wars, - the appearance of the war success, redeemed with extremely great sacrifice, and the presence of the threat for the Serbian/ Polish nation in the order shaped as a result 1st/2nd world war. The fragments of sources quoted in the article as well as the authors' considerations, are exhibited as key terms and simultane­ously as the common features of the Serbs and the Poles, enhanced at the moments of threat for both the nations and their countries: faith (in victory, in the help of Providence, honour, the spirit of fight and being ready for uncompromising resistance to aggressors. These val­ues constitute an essential element of comparison in the search of understanding the Serbian and Polish history and attitudes as well as the choices made by the Serbs and the Poles.

  7. Shrinking Cities in Poland: Demographic Perspective

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    Musiał-Malago Monika

    2017-01-01

    This paper purports to present the issue of “shrinking” cities in Poland. The author has included a general characteristics of the process, considering only the aspect of changes in the population. A typology of population movements was introduced on the basis of a relation between the actual birth rate and the migration balance, whereas the typology was based on Webb’s procedure. The author has also made an attempt to classify the shrinking cities based on the definition adopted by the Shrinking Cities International Research Network (SCIRN. A detailed analysis was conducted on large cities with more than 100 thousand inhabitants and covered the period from 2000 to 2016.

  8. Auriculariopsis albomellea (Agaricales, Schizophyllaceae new for Poland

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    Władysław Wojewoda

    2013-12-01

    Full Text Available The article deals with the taxonomy, ecology, general distribution and threatened status of Auriculariopsis albomellea Bondartsev Kotl. (Basidiomycetes. In Europe it is known only from Czech Republic, France, Sweden and Ukraine, in Africa from Canary Islands, in North America from Canada and United States. In Poland the fungus was found for the first time in NE part of the country, in a pine forest, on dead twigs of Pinus sylvestris. Habitat and distribution of this saprobic fungus in Africa, Europe and North America are described, list of synonyms and important references are cited, Polish name is proposed.

  9. HOME LONG-TERM CARE IN POLAND

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    Ewa Kułagowska

    2011-06-01

    Full Text Available The considerable proportion of the elderly, the chronically ill and the disabled in community is an economic and organizational challenge for the state social policy. It requires a large, steadily increasing financing from the public funds and creating an optional care model to fulfill the needs of citizens and guarantee high quality services. Development of the long-term care is one of the problems to be solved. This paper presents: – a long-term care forms, organization and tasks; – a role of long-term care but particularly home longterm care to protect health in Poland; – problems related with home long-term care functioning.

  10. New constraints on the evolution of the Gibraltar Arc from palaeomagnetic data of the Ceuta and Beni Bousera peridotites (Rif, northern Africa)

    Science.gov (United States)

    Berndt, Thomas; Ruiz-Martínez, Vicente Carlos; Chalouan, Ahmed

    2015-03-01

    The Betic Cordillera and the Moroccan Rif together form one of the smallest and tightest orogenic arcs on Earth and almost completely close the Mediterranean to the west. For the explanation of the geodynamic evolution of the mountain belt, palaeomagnetic data that generally found clockwise block rotations in the Iberian and anticlockwise rotations in the Moroccan part of the mountain belt, have played a key role in recent works. This palaeomagnetic study has found new constraints on the rotations and timing of the peridotitic bodies outcropping in the key position at the westernmost margin of the mountain belt, in Ceuta and Beni Bousera (Rif, northern Africa). Detailed thermal demagnetization of 115 individually oriented samples from 14 sites was combined with rock magnetic and scanning electron microscopic experiments to analyze the magnetic mineralogy responsible for the remanences and the mechanisms and relative times of their acquisition. In Ceuta, up to three magnetic components, and in Beni Bousera, up to two magnetic components have been found, that are all to be interpreted as chemical remanent magnetizations (CRM). The data suggests the following succession of geodynamic events affecting the peridotites until recent times: (1) after their exhumation and subsequent cooling about 20 Ma ago, they recorded a characteristic remanent magnetization of both normal and reversed polarities, carried by (pseudo-)single-domain magnetite grains; (2) after their dismembering, the Ceuta peridotites were tilted southward by 22-34° about a horizontal or tilted axis (up to plunge 50°) with an azimuth of 72-145° and the Beni Bousera peridotites were rotated anticlockwise by 72.3 ± 12.1° about a vertical axis and (3) both recorded another magnetic signal of normal polarity only, carried by multi-domain magnetite grains; and finally (4) the Ceuta peridotites rotated anticlockwise by 19.7 ± 5.9° about a vertical axis. This study provides the first palaeomagnetic data for

  11. Infectious diseases in Poland in 2014

    Science.gov (United States)

    Sadkowska-Todys, Małgorzata; Zieliński, Andrzej; Czarkowski, Mirosław P

    The aim of the study is to assess epidemiological situation of infectious and parasitic diseases in Poland in 2014, and an indication of the potential health risks from communicable diseases occurring in other areas of the globe. This paper is a summary of the analysis and evaluation of the results of epidemiological surveillance of infectious diseases in Poland in 2014, and those elements of European and global epidemiological background, which in this period had an impact on the epidemiological situation in Poland or constituted a threat. The main source of data for this study are statistical reports included in annual bulletins “Infectious diseases and poisoning in Poland in 2014” and “Immunizations in Poland in 2014” (NIPH-PZH, GIS, Warsaw 2015) and the data contained in the articles of „Epidemiological chronicle” presented in the Data on deaths are based on the statement of the Department for Demographic Research and Labour Market CSO presenting numbers of deaths from infectious and parasitic diseases registered in Poland in 2014, and in the previous years. Upper respiratory tract infection classified as “suspected flu and the flu season” in the since many years are the largest position among the diseases subject to disease surveillance. In the last decade, particularly large increase in the incidence of upper respiratory tract infection was reported in the flu season 2013., when the increase in comparison to the median of years 2008-2012 amounted to 189.8%. In 2014. Number of reported cases was 3 137 056 which represented a nonsignificant decrease of 0.8% compared with the previous year. However, compared to the median of the years 2008-2012 it was an increase of 187.4%. Better then based on calendar year is a picture obtained by examining the incidence of seasonal periods in the annual, but counted from 1 September to 31 August of the following year. In such a setup, in the 2012/2013 season were recorded 3 025 258 of cases, and in the season

  12. Development of optical sciences in Poland

    Science.gov (United States)

    Romaniuk, Ryszard S.

    2013-10-01

    Research and technical communities for optics, photonics and optoelectronics is grouped in this country in several organizations and institutions. These are: Photonics Society of Poland (PSP), Polish Committee of Optoelectronics of SEP, Photonics Section of KEiT PAN, Laser Club at WAT, and Optics Section of PTF. Each of these communities keeps slightly different specificity. PSP publishes a quarterly journal Photonics Letters of Poland, stimulates international cooperation, and organizes conferences during Industrial Fairs on Innovativeness. PKOpto SEP organizes didactic diploma competitions in optoelectronics. KEiT PAN takes patronage over national conferences in laser technology, optical fiber technology and communications, and photonics applications. SO-PTF has recently taken a decision to organize a cyclic event "Polish Optical Conference". The third edition of this conference PKO'2013 was held in Sandomierz on 30.06-04.07.2013. The conference scientific and technical topics include: quantum and nonlinear optics, photon physics, optic and technology of lasers and other sources of coherent radiation, optoelectronics, optical integrated circuits, optical fibers, medical optics, instrumental optics, optical spectroscopy, optical metrology, new optical materials, applications of optics, teaching in optics. This paper reviews chosen works presented during the III Polish Optical Conference (PKO'2013), representing the research efforts at different national institutions.

  13. Poland-AOD aerosol research network

    Science.gov (United States)

    Kaminski, Jacek W.; Struzewska, Joanna; Markowicz, Krzysztof

    2017-04-01

    Poland-AOD research network (www.polandaod.pl) was formed in 2011. It is a consortium of Polish institutions that are involved in studies of the atmospheric aerosol impact on the climate system. In 2016 the Poland-AOD network comprised of five stations: Radiative Transfer Laboratory, University of Warsaw (urban station), the research station of the Institute of Oceanology, in Sopot (coastal station), Radiative Transfer Station SolarAOT in Strzyzow (background station in the Carpathian mountains), Meteorology and Climatology Observatory at the Nicolaus Copernicus University in Torun (urban station), and the Research station in Rzecin at Poznan University of Life Sciences (rural station). The primary goal of the network is to carry out measurements of aerosol single scattering properties, radiation budget, simulate radiative transfer and aerosol transport, validate aerosol transport and transformation models such as NAAPS and GEM-AQ, as well as carry out instrument calibration and intercomparison. We will present observations of aerosol properties collected by the network as well as results from the GEM-AQ model simulations for selected episodes of biomass burning and urban aerosol.

  14. The Vistulian aeolian succession in central Poland

    Science.gov (United States)

    Goździk, Jan

    2007-01-01

    Central Poland is situated in the centre of the Late Pleistocene and Holocene "European aeolian sand belt". This area has the highest frequency of round, mat grains of all Europe, due to intense aeolian abrasion. Aeolian processes were very active during several glaciations, but the changes in aeolian activity in the course of an entire glaciation can be studied only for the Vistulian (Weichselian, Wisconsinan). The reason is that a continuous blanket of glacial sediments either covered, or partly eroded older aeolian sediments in central Poland during the Wartanian (Saalian II). Aeolian processes began just after deglaciation and became intense under the periglacial conditions of the Late Wartanian and the whole Vistulian. The evolution of these processes is reconstructed, especially for the interval of the highest and most effective aeolian activity, i.e. the Late Plenivistulian (Oxygen Isotope Stage 2: the coldest stage of the last glaciation). A model of the sequence of periglacial aeolian events during an entire glaciation is presented. This model may be used for the reconstruction of older Pleistocene cycles of high periglacial aeolian activity.

  15. Selected Determinants of Mezzanine Financing in Poland

    Directory of Open Access Journals (Sweden)

    Robert Golej

    2016-01-01

    Full Text Available A very significant form of company activity determining its development and even survival is innovation activity. Raising capital for the implementation of innovation is an important but not the only factor in the introduction of innovation. Characteristics of innovation, and in particular the risk of failure, make for a significant difficulty in obtaining external financing, particularly from third parties, which is an obstacle to their development and implementation. The subject of discussion in the article is the hybrid formula mezzanine type of financing innovative projects implemented both in start-up companies and in already well established companies. The purpose of the article is to discuss the possibilities and to perform an analysis of the practices followed by mezzanine funds in Poland in respect to the innovation activities of Polish companies. Research presented in the article was conducted on the basis of information on investments performed by mezzanine funds in Poland. Of particular importance for the innovativeness of the economy is to have companies from the SME sector, and therefore we also carried out research in this group. Innovations are often initiated in special purpose companies, start-up, etc., that operate in the SME sector. Therefore, the financing of innovation cannot be ignored as a thread of innovation in SMEs. The study involved interviews in several companies in the sector. The study concerned the possibilities of financing innovation involving mezzanine, knowledge of hybrid forms of financing, preparedness for hybrid financing. Studies are not representative, but are rather sounding a view to clarify any further research. Hypothesis: mezzanine financing, utilizing its specific benefits, is increasingly used to finance the gap in the financing of innovation, in particular special purpose companies in the SME sector. So the hypothesis raises two strands of research. The first concerned the financing of innovation

  16. Mesozoic and Cenozoic evolution of the SW Iberian margin

    Science.gov (United States)

    Ramos, Adrià; Fernández, Oscar; Terrinha, Pedro; Muñoz, Josep Anton; Arnaiz, Álvaro

    2016-04-01

    The SW Iberian margin lies at the eastern termination of the Azores-Gibraltar Fracture Zone (AGFZ), the diffuse transform plate boundary between Africa and Iberia (Sartori et al., 1994). It comprises the Gulf of Cadiz and the Algarve Basin, which were developed under two main different regional stages of deformation. During the Mesozoic, the SW Iberian margin evolution since the Late Triassic was dominated by the Pangea break-up and the Central Atlantic opening up to Early Jurssic, followed by the westernmost Tethyan opening up to Mid/Late Jurassic, and the North Atlantic rifting from Late Jurassic to Early Cretaceous (e.g., Schettino and Turco, 2010). This phase of extension led to the formation of E-W to NE-SW trending, basement-involved extensional faults, the triggering of salt tectonics and the uplifting of basement highs (e.g., Guadalquivir Bank). This extensional phase was responsible not only for the sedimentary depocenter distribution, but also for the crustal configuration of this passive margin, extending from continental crust in the proximal part, to oceanic crust in the distal and deepest portion of the margin. Since the Late Cretaceous, the margin was inverted due to the N-S convergence between Africa and Iberia, being still undergoing collision given the dominance of reverse fault earthquake mechanisms (e.g., Zitellini et al., 2009). The shortening in the margin is mainly accommodated by the north-dipping foliation of the basin, expressed by south-directed blind thrusts affecting the present-day bathymetry, re-activating the basement highs and the salt tectonics, and controlling the Cenozoic depocenters. The emplacement of the Betics to the east led to the westward emplacement of the gravitational unit partially overlying the sedimentary basins, corresponding to the Allochthonous Unit of the Gulf of Cadiz (AUGC). Our observations of the margin configuration have been based on the interpretation of 2D and 3D seismic reflection surveys throughout the

  17. Behaviour of fluid mobile elements during subduction and exhumation of abyssal peridotites: Example of serpentinites from Cuba and Dominican Republic

    Science.gov (United States)

    Deschamps, F.; Guillot, S.; Godard, M.; Chauvel, C.; Andreani, M.

    2009-04-01

    Seawater interaction with abyssal peridotites at the sea floor is an important process for chemical exchange between lithosperic mantle and ocean at slow-spreading ridge. Serpentinites from oceanic lithosphere are known to represent an important sink for fluid mobile element, notably boron. In parallel we know extreme enrichment in fluid mobile element (As, Sb, B, U, Li) in high-pressure serpentine minerals (antigorite) coming from part of mantle wedge hydrated by slab's fluids released (Himalaya, Deschamps et al., in prep.). In order to constrain geochemical behaviour of fluid mobile element hosted by serpentine during subduction processes, we examined abyssal serpentinites coming from the accretionary wedge of Greater Carribean (Cuba and Dominican Republic). They represent subducted Atlantic oceanic lithosphere, which have experienced low to high- metamorphism (greenschist to eclogite facies), before being exhumed. These rocks are an opportunity to understand the chemical mobility of fluid mobile element during prograde metamorphism occurring along subduction surface. Here we present bulk-rock and in-situ composition of serpentinites and their primary and alteration-related phase obtained on (LA-)HR-ICP-MS. Except for a few cumulates, serpentinites have depleted compositions in agreement with a refractory mantle, but also strong enrichment in U, Pb, Th, Sr, and other fluid mobile element (e.g., U up to 10xPM) indicating extensive fluid-rock intercation. In-situ composition allows the distinction of two groups of serpentine. Group 1 is characterized by relatively flat and depleted REE patterns (Yb ≈ 0.5xChondrite) reflecting formation after olivine, while group 2 formed after pyroxene is characterized by slightly higher HREE content (Yb ≈ 1xChondrite) but light LREE depleted patterns and displays higher content in Sc, V, Ti and Co. Both groups are strongly enriched in B (up to 120 ppm), and reach values already observed in serpentinites from mantle wedge

  18. Rediscovery of the epiphytic moss Ulota coarctata (Orthotrichaceae in Poland

    Directory of Open Access Journals (Sweden)

    Plášek Vítězslav

    2016-07-01

    Full Text Available Ulota coarctata (P. Beauv. Hammar was recently collected in Poland after more than half a century. This epiphytic moss was found at four localities in the Pojezierze Lubuskie lakeland in the western part of the country. Its diagnostic features are briefly presented, its habitat requirements are considered, the historical and recent findings of the species in Poland are discussed, and its distribution is mapped. It is suggested that the species status should be changed from ‘endangered’ to ‘critically endangered’ on the red list of mosses in Poland.

  19. Microscopic phytopathogenic fungi rare and new for Poland

    Directory of Open Access Journals (Sweden)

    Małgorzata Ruszkiewicz

    2014-08-01

    Full Text Available The paper presents a list of 36 rare species of fungi with remarks about their morphology and distribution in Poland. Three of the species are new for Poland: Romularia asplenii Jaap, R. concomitans Ell. et Holw. and Ascochyta actoeae (Bres. J. J. Davis. Altogether, 13 parasitic species occur on the plans which have not been known as their hosts in Poland, so far, 19 are rare on the listed hosts. The fungi were collected in the area of projected Jurassic National Park, Częstochowa Upland.

  20. Multimodality imaging of Poland syndrome with dextrocardia and limb anomalies.

    Science.gov (United States)

    Iyer, Ramesh S; Parisi, Marguerite T

    2012-08-01

    Poland syndrome is a rare disorder featuring unilateral anterior thoracic and upper extremity anomalies. These include hypoplasia of the pectoralis major costosternal head, absent pectoralis minor, breast hypoplasia, and absent upper rib cartilage. Pulmonary hypoplasia may occur secondarily. The postulated etiology is underdevelopment of the subclavian artery. Less than 50 cases of Poland syndrome with dextrocardia have been reported. Rib anomalies cause rightward cardiac displacement in fetal life. This case of left-sided Poland syndrome in a young girl is unique not only because of dextrocardia, but also because the condition preferentially afflicts the right side and males.

  1. Whole rock and spinel compositions of serpentinized peridotites from the Divriği-Sivas region, eastern Turkey: Implications for their tectonic setting

    Science.gov (United States)

    Ünlü, Taner; Akıska, Sinan; Varol, Ece; Öztürk, Ceyda; Mutlu, Halim

    2017-11-01

    In this study we investigate the spinel and whole rock chemistry of ultramafic rocks in the Divriği-Sivas region hosting one of the largest ophiolite suites in Turkey, which were emplaced following the convergence between the African and Eurasian plates in the Late Cretaceous. The ophiolitic mélange (Güneş Ophiolite) in Divriği is composed of ultramafic rocks, amphibolites, sub-ophiolitic metamorphic rocks and calc-silicates. The ultramafic rock section is made up of serpentinized wehrlites overlain by irregular segregations of pyroxenite levels. Whole rock chemistry of Divriği wehrlites resembles serpentinized peridotites in Himalayas. They have high MgO (average 31.27 wt%) and low Al2O3 (average 0.56 wt%) concentrations and Mg/Si and Al/Si ratios imply that peridotites formed in a supra-subduction zone environment. The U-shaped REE patterns of serpentinized wehrlites are formed by partial melting, coupled with interaction between peridotite and hydrous melts in the mantle wedge. The spinels collected from serpentinized wehrlites show compositions ranging from chromite in the core to ferritchromite and Cr-magnetite at the rims and have high Cr2O3 (46.5-56.2 wt%) and very low TiO2 contents (%35). Parental melt compositions computed (8.69-11.71 wt% for Al2O3 and 0.1 to 0.37 wt% for TiO2) from chromite-melt equilibrium conditions yield a boninitic affinity. Our data suggest that spinels from serpentinized wehrlites in the Divriği area are similar to peridotite xenoliths from the Kamchatka arc and West Bismarck.

  2. Materials to the zygnemaceae of Poland V. Two spirogyra species new for Poland

    Directory of Open Access Journals (Sweden)

    Joanna Z. Kadłubowska

    2014-01-01

    Full Text Available Spirogyra occidentalis (Transeau Czurda 1932 and S. scrobiculata (Stockmayer Czurda 1932, two species new in the Polish flora and S. pseudovarians Czurda 1930, a species only cited in literature, are described in samples collected in central Poland. The diagnosis of S. occidentalis and S. pseudovarians has been supplemented with measuring data of the inflated sterile cells in conjugation filaments. The figures show the hitherto unknown inflated sterile cells.

  3. Melting of metasomatized peridotite at 4-6 GPa and up to 1200 °C: an experimental approach

    Science.gov (United States)

    Kessel, R.; Pettke, T.; Fumagalli, P.

    2015-04-01

    The phase assemblages and compositions in a K-bearing lherzolite + H2O system are determined between 4 and 6 GPa and 850-1200 °C, and the melting reactions occurring at subarc depth in subduction zones are constrained. Experiments were performed on a rocking multi-anvil apparatus. The experiments had around 16 wt% water content, and hydrous melt or aqueous fluid was segregated and trapped in a diamond aggregate layer. The compositions of the aqueous fluid and hydrous melt phases were measured using the cryogenic LA-ICP-MS technique. The residual lherzolite consists of olivine, orthopyroxene, clinopyroxene, and garnet, while diamond (C) is assumed to be inert. Hydrous and alkali-rich minerals were absent from the run products due to preferred dissolution of K2O (and Na2O) to the aqueous fluid/hydrous melt phases. The role of phlogopite in melting relations is, thus, controlled by the water content in the system: at the water content of around 16 wt% used here, phlogopite is unstable and thus does not participate in melting reactions. The water-saturated solidus, i.e., the first appearance of hydrous melt in the K-lherzolite composition, is located between 900 and 1000 °C at 4 GPa and between 1000 and 1100 °C at 5 and 6 GPa. Compositional jumps between hydrous melt and aqueous fluid at the solidus include a significant increase in the total dissolved solids load. All melts/fluids are peralkaline and calcium-rich. The melting reactions at the solidus are peritectic, as olivine, clinopyroxene, garnet, and H2O are consumed to generate hydrous melt plus orthopyroxene. Our fluid/melt compositional data demonstrate that the water-saturated hybrid peridotite solidus lies above 1000 °C at depths greater than 150 km and that the second critical endpoint is not reached at 6 GPa for a K2O-Na2O-CaO-FeO-MgO-Al2O3-SiO2-H2O-Cr2O3(-TiO2) peridotite composition.

  4. CHP plant Legionowo Poland. Description of the electricity market in Poland/CHP-feasibility analysis

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2003-04-01

    In 1997, a new energy law was passed in Poland. An important element of the law is that local energy is made obligatory. The law describes obligatory tasks and procedures for the Polish municipalities related to planning and organisation of the energy sector. With the objective of supporting the Polish municipalities in their obligations according to the energy law, the project 'Energy Planning in Poland at Municipal Level - Support to Decision Makers' was launched. As part of the project, Municipal Guideline Reports have been elaborated for three model municipalities. These guidelines present the basis for energy supply plans in the three municipalities. For the city of Legionowo, the following was recommended: 1. The planning processes initiated during the project should be continued/followed up, 2. Master Plan for the district heating system should be prepared, 3. The possibilities of establishment of a major natural gas-fired CHP plant of the combined cycle type should be investigated. The present report describes the electricity market in Poland, the market in which a CHP plant in Legionowo will have to operate. Furthermore the report presents the results of the feasibility analysis carried out for a new CHP plant in Legionowo. (BA)

  5. Comparing Environmental Impact Assessment (EIA) in Poland and Denmark for Road Construction in Relation to Wildlife and Nature Protection : Report for Poland

    DEFF Research Database (Denmark)

    Sienkiewicz, J.; Adrados, L. C.; Briggs, L

    Project : Fauna Passages under Selected Roads in Poland - Education, Monitoring and Construction - Part A. DANCEE M124/031-0212......Project : Fauna Passages under Selected Roads in Poland - Education, Monitoring and Construction - Part A. DANCEE M124/031-0212...

  6. CERN accelerator school: Introductory course in Poland

    CERN Multimedia

    2006-01-01

    For the first time since the CERN Accelerator School (CAS) was set up, the 'Introduction to Accelerator Physics' course was held in Zakopane, Poland. This course was organised together with the National Atomic Energy Agency, Warsaw, and the AGH University of Science and Technology, Cracow, and was held from 1-13 October 2006 at the foot of the Tatra Mountains. The course was very well attended with 113 participants representing 26 different nationalities. Although most of the participants originated from Europe, some students came from countries as far away as Canada, China, India and North America. The intensive programme comprised 35 lectures, 3 seminars given by local Polish lecturers, 5 tutorials where the students were split into four groups, a poster session where students could present their own work and 7 hours of guided and private study. The participants appreciated these study periods, which encouraged collaboration and knowledge-sharing in solving problems and gave them the opportunity to get t...

  7. INVENTORY IN POLAND - CURRENT SITUATION AND PROSPECTS

    Directory of Open Access Journals (Sweden)

    O. Kemp

    2017-02-01

    Full Text Available Poland poddavalsya inventory changes. His origins are taking beginning in late and early vosemnadtsatoho devyatnadtsatoho century, when Polish state zahvatchyky sozdaly The first kadastrovыe otchetы. Austria, Prussia and Russia sozdalytry kadastrovыe system, three yspolzuyuschye system recovery country yzmerenyya.Vo TIME 1918 - 1939 Manuscript kadastrovыe bыly oriented work on the creation edynoy nalohovoy system for vsey territory of the country. After the war bыly zavershenы work. Modernization of the cadastre prodolzhalas in the direction Increase the accuracy and quality of data. At present Time Inventory Accounting vkljuchaet buildings, premises and plots zemelnыh, as well tesno svjazana with zemelnыm registers / ypotekoy. Information, soderzhaschayasya in Nam, everybody yspolzuetsya participants in the control nedvyzhymostyu (surveyors, otsenschykamy, brokers and upravlyayuschymy nedvyzhymostyu, courts and admynystratyvnыmy authorities zanymayuschyhsya territorial-prostranstvennыm Planning. Polskoy origins cadastral area. The first records of kadastrovыh measurement bыly sdelanы 4.5 million. Years ago. Poland was once zaklyuchalas Business surveyor in oblahorazhyvanyy. At the end trynadtsatoho century bыla Created rank post of High - korolevskyy podkamernыy, tasks kotorogo All selskohozyaystvennыe and lesnыe uhodya bыly ohvachenы oblastyu pochvovedenyya, classification of land osushchestvljaetsja edynoobrazno for vsey country on grounds ofytsyalnoy classes tablytsы land. THIS classification talk at kachestve and soil fertility. Class is determined on a 6-point scale (8 to pahotnыh land. This allows us to Compare Quality of land in any point of the country. By law dolzhna bыt yspolzovana in the Economic Planning and spatial statistics population in sudebnom and administrative razbyratelstve. All ofysы ymeyut access for cadastre data bases online free. Chastnyya Faces and company mogut Require info sobstvennoy REAL

  8. CREDIT ACTIVITIES OF COOPERATIVE BANKS IN POLAND

    Directory of Open Access Journals (Sweden)

    Anna Bieniasz

    2017-03-01

    Full Text Available The aim of the study was to analyze the lending activities of cooperative banks in Poland in the years 2010– 2014, in a size of banks. Elaboration is a review, based on the data of the Polish Financial Supervision Authority. Research indicates that the value of own funds of the cooperative banks was reflected in both the volume of lending, and in the structure of loans. Banks with capital of 5 million euro loans for primarily farmers, individuals, and individual entrepreneurs. In turn, the banks with capital of more than 5 million euro were most involved in the financing of small and medium enterprises and individual farmers. Regardless of the size of banks, the most important in lending loans were investment and operating

  9. FINANCING RENEWABLE ENERGY SOURCES INVESTMENT IN POLAND

    Directory of Open Access Journals (Sweden)

    Jerzy Piotr Gwizdała

    2017-09-01

    Full Text Available In Poland, as in other European Union countries, the project finance structure is used to finance investments in the field of energy. This method investment financing is often used in the world. The upward trend inhibition in recent periods has been due to the global financial crisis and financial instability in the euro zone. On account of the necessity to develop the energy infrastructure associated with renewable sources, the considerable strengthening in the use of project finance techniques can be expected. The particular progression may be observed in the case of public-private partnership (ppp, where public investments are carried out by private companies. Companies, in case of investment realization in the field of ppp, almost always use project finance, because it is a beneficial way to separate the risks associated with an investment from the balance sheet of the compa-ny.

  10. PRISON EDUCATION IN POLAND: SPECIFICS AND CHALLENGES

    Directory of Open Access Journals (Sweden)

    Daria Becker-Pestka

    2017-04-01

    Full Text Available The problems presented in the text refer to the education of convicts in Poland. It has been based on current Polish legal regulations, statistical data and specialist literature. The problems which refer to the education of convicts in Poland are regulated by the Act of 6th June 1997, the Executive Penal Code, the Act on the Education System and executive acts to the above-mentioned regulations. The current situation in the labour market requires people to acquire education and to improve their qualifications. People without education, who are excluded from the access to professional development and in-service training, find themselves in an extremely difficult situation. The lack of qualification and vocational skills usually leads to exclusion from the labour market. People who serve their sentences in prisons find themselves in a particularly difficult situation, because their lack of education may push them back into crime. A very positive tendency that may be observed in Poland is a growing demand for prison education. Convicts may acquire knowledge and raise their qualifications at various levels and in various fields. They may follow the curricula at the level of a primary or secondary school; they may pass their Matura certificate and, after the consent of relevant authorities, they can continue their education at the university level. Convicts may also learn a new profession, change their professional qualifications or acquire new additional skills during specialist courses. The qualifications acquired in this way shall meet current demand in the labour market, and convicts may find employment after they leave prisons. Education allows them to improve their self-esteem and self-reliance, to catch up with any deficiencies and to work on their self-discipline. At the same time, education offers opportunities to expand knowledge, to return to the society and to the labour market. It is important for convicts to obtain opportunities for

  11. Distribution of some lichenicolous fungi in Poland

    Directory of Open Access Journals (Sweden)

    Krystyna Czyżewska

    2014-08-01

    Full Text Available Nineteen species of lichenicolous fungi collected in 129 localities in Poland in the years 1968 and 1970-2003 are reported in the paper. They are as follows: Athelia arachnoidea (Berk. Jülich, Tremella cladoniae Diederich et M.S. Chrst., T. hypogymniae Diederich et M.S. Chris., T. lichecola Diederich, Clypeococcum hypocenomycis D. Hawksw., Polycoccum superficiale D. Hawksw. et Miądlikowska, Nectria lecanodes Ces., Pronectria erythrinella (Nyl. Lowen, Cortocifraga fuckelii (Rehm D. Hawksw. et R. Sant., C. peltigerae (Nyl. D. Hawksw. et R. Sant., Libertiella malmedyensis Speg. et Roum., Lichenoconium erodens M.S. Christ. et D. Hawksw., L. lecanorae (Jaap D. Hawksw., L. pyxidatae (Oudem. Petrak et Sydow, Vouauxiella lichenicola (Lindsay Petrak et Sydow, Bispora christiansenii D. Hawksw., Illosporium carneum Fr., Karsteniomyces peltigerae (P. Karst. D. Hawksw. and Taeniolella beschiana Diederich.

  12. Infectious diseases in Poland in 2011.

    Science.gov (United States)

    Zieliński, Andrzej; Czarkowski, Mirosław P; Sadkowska-Todys, Małgorzata

    2013-01-01

    The aim of the study was assessment of the epidemiological situation of infectious and parasitic diseases in Poland in 2011 MATERIALS AND METHODS: The main source of data to develop the statistical overview was the annual bulletin "Infectious diseases in Poland in 2011," and "Vaccinations in Poland in 2011,"/NIPH-NIH, CSI, 2011 and information contained in the articles of epidemiological journal in which authors depth discussion of the epidemiological situation of 27 diseases or groups of diseases. Data on deaths are based on the statements of the Department of the Central Statistical Office of Demographic Studies. Upper respiratory tract infection classified as "influenza and influenza-like illness" in 2011, were reported in a total number of 1,156,357 cases, which was an 108.0% increase of incidence as compared with 2010. and in relation to the median of the years 2005 - 2009 of 205.9%. In 2011, food infections dominated among the bacterial infections caused by Salmonella, with the continuing decline of incidence and fraction of salmonellosis among other etiologies. Among the diseases that can be prevented by vaccination it was reported 30.7% increase in the incidence of pertussis. In relation to the median of the years 2005-2009 is a decrease of 16.9%. A downward trend in the incidence of mumps was maintained. As compared to 2010, the incidence decreased by 7.0%. When compared to the median of the years 2005 to 2009 the decline was 38.3%. In relation to the median of the years 2005-2009 there have been a decrease of the number of rubella cases by 67.7% and there have been no reported cases of congenital rubella. A further decline in the incidence of invasive disease caused by H. influenzae was observed. The incidence of tuberculosis in 2011 increased as compared to the previous year from 19.7 to 22/100,000 in respect to all forms of tuberculosis, and pulmonary tuberculosis from 18.3 to 20.5/100,000. The number of newly diagnosed HIV-infected persons also

  13. Rheumatology training in Poland vs. United Kingdom.

    Science.gov (United States)

    Lazarewicz, Karina; Chinoy, Hector

    2017-01-01

    When evaluating the quality of Rheumatology specialty training, it can be useful to explore similarities and differences between countries. In this article we compare the training in the UK and Poland. The two training programmes are similar in length and in the competencies that must be achieved, although they do have significant differences in the way the training is structured. The UK-based system is more out-patient based, which can be advantageous, as after completion of training the doctor is more confident in treating common rheumatological problems. On the other hand, having exposure to paediatric rheumatology and orthopaedics like one has in Polish-based training, despite a short placement time, is definitely beneficial for the trainee in gaining all-round knowledge. In conclusion, each system has its merits and can be further enhanced by observing how junior doctors are sub-speciality trained in different countries.

  14. Clean coal-preparation barriers in Poland

    Energy Technology Data Exchange (ETDEWEB)

    Blaschke, W.; Nycz, R. [Polish Academy of Science, Krakow (Poland). Mineral & Energy Economic Research Institution

    2003-04-01

    Poland is the second biggest European producer of hard coal. This raw product is cleaned in 49 preparation plants. Production capacities of the preparation plants depend on the demand for coal. The clean-coal production mostly depends on the quality demands of customers. Polish hard-coal is of good quality. It is enough to remove grains of clean stone to get saleable products of ash content between 8 and 12%. Rarely the ash content is up to 15%. The coal can be cleaned to 4-6% ash content, but there is a very small demand for this type of coal. Gravity separation (via heavy liquids, jigs, cyclones) removes the grains of pure stone. Currently, no preparation of the coal after grinding is conducted.

  15. OZONE CONCENTRATION ATTRIBUTABLE PREMATURE DEATH IN POLAND

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    Krzysztof Skotak

    2010-03-01

    Full Text Available Ozone in the lower part of the atmosphere (troposphere, strong photochemical oxidant, is not directly emitted to the atmosphere but formed through a series of complex reactions. Ozone concentrations depends on ozone precursors air contamination (mainly nitrogen dioxide and non-methane volatile organic compounds and meteorological conditions (temperature and solar radiation. The main sectors emitted ozone precursors are road transport, power and heat generation plants, household (heating, industry, and petrol storage and distribution. Ozone and some of its precursors are also transported long distances in the atmosphere and are therefore considered a transboundary problem. As a result, the ozone concentrations are often low in busy urban areas and higher in suburban and rural areas. Nowadays, instead of particulate matter, ozone is one of the most widespread global air pollution problems. In and around urban areas, relatively large gradients of ozone can be observed. Because of its high reactivity in elevated concentrations ozone causes serious health problems and damage to ecosystems, agricultural crops and materials. Main ill-health endpoints as a results of ozone concentrations can be characterised as an effect of pulmonary and cardiovascular system, time morbidity and mortality series, development of atherosclerosis and asthma and finally reduction in life expectancy. The associations with increased daily mortality due to ozone concentrations are confirmed by many researches and epidemiological studies. Estimation of the level selected ill-health endpoints (mortality in total and due to cardiovascular and respiratory causes as a result of the short-term ozone exposure in Poland was the main aim of the project. Final results have been done based on estimation method elaborated by WHO, ozone measurements from National Air Quality Monitoring System and statistical information such as mortality rate and populations. All analysis have been done in

  16. Infectious diseases in Poland in 2015

    Science.gov (United States)

    Sadkowska-Todys, Małgorzata; Zieliński, Andrzej; Czarkowski, Mirosław P.

    2017-01-01

    This is the next annual analysis of the situation of infectious and parasitic diseases in Poland in 2015 within the framework of the Epidemiological Chronicle of Przegląd Epidemiologiczny - Epidemiological Review. Its purpose is to identify potential threats to the health of populations from infectious diseases occurring in Poland with reference to other parts of the globe. This paper is an introduction to more detailed studies of the epidemiological situation of selected infectious diseases and summarizes the results of the surveillance of infectious diseases in Poland in 2015. References to epidemiological situation in other countries are limited to situations that may affect current or potential occurrence of the disease in Poland. The main source of epidemiological information for this summary is the data from the reports of the State Sanitary Inspection included in the annual bulletins “Infectious Diseases and Poisonings in Poland in 2015” and “Vaccination in Poland in 2015” (1, 2). The epidemiological situation of particular diseases is further elaborated in the Epidemiological Chronicle of the same issue of the Epidemiological Review. Data on deaths are based on the presentation of the Demographic and Labor Market Department of the Central Statistical Office on deaths from infectious and parasitic diseases registered in Poland in 2015 and earlier. For a long time, the most common diseases among epidemiological surveillance it is upper respiratory tract infections classified as “influenza and suspected influenza”. In 2015, the number of cases was 3,843,438 (9 994,7 / 100,000). As to compare with the 2014’s incidence, this was an increase of 22.6%. In 2015, incidence of intestinal infections with etiology of salmonella increased by 2.8% compared to the previous year, but compared to the median of 2009-2013 was 2.5% lower. A serious epidemiological problem is a strong upward trend in nosocomial infections including infections caused by

  17. Treatment of pediatric epilepsy in Poland.

    Science.gov (United States)

    Dunin-Wąsowicz, Dorota; Mazurkiewicz-Bełdzińska, Maria; Steinborn, Barbara; Wheless, James; Jóźwiak, Sergiusz

    2015-05-01

    The many types of childhood epilepsies make the diagnosis and treatment difficult and the outcomes frequently poor. Furthermore, there are few clinical trials in pediatric epilepsy that provide useful results to guide daily practice. Therefore for pediatric neurologists expert opinion may be useful. To provide an overview of current practice in Poland and compare results with European and US clinical guidelines. Polish specialists in pediatric neurology were asked to participate in a survey about pediatric epilepsy. The focus of the questions was on the overall strategy and treatment options for different syndromic diagnoses. The survey was developed and performed according to a previous European survey (Wheless et al., 2007). Fifty-one Polish specialists, working in academic or clinical settings, completed the questionnaire. They limited combination therapy to two or three antiepileptic drugs. Valproate was the treatment of choice for myoclonic, generalized tonic-clonic seizures and Lennox-Gastaut syndrome. For infantile spasms caused by tuberous sclerosis and of symptomatic etiology, vigabatrin was treatment of choice; valproate and ACTH were other first line options. Valproate and ethosuximide were chosen for childhood absence epilepsy and valproate for juvenile absence epilepsy. Carbamazepine was the first-line treatment option for benign partial epilepsy of childhood with centrotemporal spikes and complex partial seizures. In the treatment of juvenile myoclonic epilepsy for males valproate, for females lamotrigine were chosen. Polish pediatric neurologists agreed on the majority of questions. Their views reflect the clinical utility and availability of treatment options in Poland. Results may provide direction for clinicians. Copyright © 2015. Published by Elsevier Ltd.

  18. Marketing Program Standardization: The Experience of TNCs in Poland

    National Research Council Canada - National Science Library

    Sagan, Mariusz

    2016-01-01

    The purpose of this study is to determine the rate of standardization of marketing programs in transnational corporations in the consumer goods market in Poland, which currently is one of the fastest...

  19. Application of activity - based costing in companies in Poland

    National Research Council Canada - National Science Library

    Wnuk-Pel, Tomasz

    2010-01-01

    The purpose of this paper is to explore the application of activity-based costing in companies in Poland, and more specifically, to analyse problems in ABC implementation, the structure of ABC systems...

  20. New localities and new host of Ganoderma pfeifferi in Poland

    Directory of Open Access Journals (Sweden)

    Andrzej Szczepkowski

    2014-08-01

    Full Text Available New lcalities and a new host of Ganoderma pfeifferi Bres. in Pat. in Poland have been presented. Also, fruitbodies and spores, as well as ecology of the species have been described.

  1. The distribution of Nymphaea candida C. Presl (Nymphaeaceae in Poland

    Directory of Open Access Journals (Sweden)

    Maciej Wajda

    2014-01-01

    Full Text Available Nymphaea candida C. Presl is a rare species limited in its distribution to NE Poland. It has often been confused with N. alba L., a much more frequent species. It is probably a threatened species.

  2. Fatal cardiovascular risk in Poland as determined via Internet

    Directory of Open Access Journals (Sweden)

    Bartosz Trzeciak

    2017-05-01

    Automatic monitoring of the incidence of cardiovascular risk factors in Poland provides information for epidemiological studies. The system meets the characteristics of diagnostic programmes that can assist epidemiologic-based and therapeutic decisions.

  3. Civil Military Relations and Defense Reform in Poland

    National Research Council Canada - National Science Library

    Tomaszycki, Marek

    2006-01-01

    .... From the beginning, these changes in the European order included security problems. This paper describes changes in the national security of Poland since 1989 with a focus on the Polish Armed Forces (PAF...

  4. MACROECONOMIC CONDITIONS OF BANKRUPTCY OF ENTERPRISES IN POLAND

    Directory of Open Access Journals (Sweden)

    Anna Bieniasz

    2014-12-01

    Full Text Available The main purpose of this work is to analyse the phenomenon of enterprises’ bankruptcy in Poland in 2004-2013 and attempt to build regression models defining the relationship between the number of bankrupted companies and selected macroeconomic parameters of the national economy. The analysis is based on Coface Poland reports presenting the phenomenon of bankruptcy in Poland of branches, provinces, legal forms of companies and types of bankruptcy proceedings. Studies have shown that the greatest risk of bankruptcy refers to metals production and fabricated metal products enterprises, manufacture of food products and beverages, wholesale trade, construction, micro and small enterprises, enterprises under the age of 10 years and companies from Mazovia region, Silesia and Lower Silesia. The estimated parameters of the regression models showed that the number of bankruptcies in Poland is strongly determined i.a. by the number of registered companies, GDP growth, dynamics of changes in fixed capital formation and changes in foreign exchange rates.

  5. POLAND' SYNDROME: An Incidental findings on routine medical ...

    African Journals Online (AJOL)

    Dr Hamidu

    -Chiesa PL, Repett P, Torre M,. Nobili F, Mazzola C, Martucciello G. Congenital deformities of the chest wall, surgical treatment,. Minerva Pediat. 1997.49: 407. 9. Gatti JE. Poland's deformity reconstruction's with a customized extra soft silicon ...

  6. Dangerous Goods Transport Problems in the European Union and Poland

    Directory of Open Access Journals (Sweden)

    Gabriel Nowacki

    2016-04-01

    Full Text Available The paper refers to threat assessment of dangerous goods (DG in transportation of the European Union and the Republic of Poland. Dangerous goods in the European Union are carried by inland waterways, rail and road. In Poland 87.5% of DG have been carried by road and 12.5% by rail in 2014. DG can cause an accident and lead to fires, explosions and chemical poisoning or burning with considerable harm to people and the environment. There is not monitoring system in Poland to control in real time road transportation of dangerous goods. Proposition of National System of Monitoring Dangerous Goods in Poland was presented. Realization of mentioned kind of system may significantly contribute to improving safety of people and environment.

  7. Timescales between mantle metasomatism and kimberlite ascent indicated by diffusion profiles in garnet crystals from peridotite xenoliths

    Science.gov (United States)

    Jollands, Michael C.; Hanger, Brendan J.; Yaxley, Gregory M.; Hermann, Jörg; Kilburn, Matthew R.

    2018-01-01

    Rare garnet crystals from a peridotite xenolith from the Wesselton kimberlite, South Africa, have distinct zones related to two separate episodes of mantle metasomatism. The garnet cores were firstly depleted through melt extraction, then equilibrated during metasomatism by a potentially diamond-forming carbonate-bearing or proto-kimberlitic fluid at 1100-1300 °C and 4.5-5.5 GPa. The garnet rim chemistry, in contrast, is consistent with later overgrowth in equilibrium with a kimberlite at around 1025 ± 25 °C and 4.2 ± 0.5 GPa. This suggests that the rock was physically moved upwards by up to tens of kilometres between the two metasomatic episodes. Preserved high Ca, Al and Cr contents in orthopyroxenes suggest this uplift was tectonic, rather than magmatic. Diffusion profiles were measured over the transitions between garnet cores and rims using electron microprobe (Mg, Ca, Fe for modelling, plus Cr, Mn, Ti, Na, Al) and nano Secondary Ion Mass Spectrometry (NanoSIMS; 89Y, along with 23Na, Ca, Cr, Fe, Mn and Ti) analyses. The short profile lengths (generally interaction of the mantle xenolith with the host kimberlite magma during a single-stage ascent to the crust (hours to days). The samples offer a rare opportunity to study metasomatic processes associated with failed eruption attempts in the cratonic lithosphere.

  8. 186Os/188Os Isotopic Compositions of Peridotites: Constraints on Melt Depletion and Pt/Os Evolution of the Upper Mantle

    Science.gov (United States)

    Chatterjee, R. N.; Lassiter, J. C.

    2014-12-01

    Global correlations between Al2O3 and Pt/Os in mantle peridotites suggest that Pt behaves incompatibly relative to Os during partial melting [c.f., 1]. Because 190Pt decays to 186Os (t1/2 = 468 Ga), correlations between 186Os/188Os and peridotite fertility can be used to constrain the long-term Pt/Os evolution of the depleted mantle and the initial Pt/Os ratio of the primitive upper mantle (PUM). We examined 186Os/188Os in mantle peridotites from continental (Rio Grande Rift/Colorado Plateau) and oceanic (Lena Trough, Hawaiian Islands) settings that span a wide range in fertility (Al2O3 ~0.67-4.42 %) and 187Os/188Os ratios (0.1138-0.1305). The new data define a narrow range in 186Os/188Os (0.1198338 to 0.1198393, 2 SD~24 ppm), placing constraints on long-term Pt/Os variability in the DMM. 186Os/188Os is broadly correlated with indices of melt depletion including spinel Cr#, clinopyroxene Cr#, and clinopyroxene Yb content, consistent with the inferred relative compatibility of Pt and Os during partial melting. Extrapolation of the alumina-186Os/188Os trend to PUM alumina content (~4.5 wt% Al2O3; [2]) suggests a PUM 186Os/188Os of ~0.1198380±15, similar to the 186Os/188Os of H chondrites (~0.1198398±16; [3]). This 186Os/188Os value is consistent with a PUM Pt/Os of 1.8±0.3, similar to Pt/Os values measured in several classes of chondrites (Carbonaceous ~1.9±0.2, Ordinary ~2.0±0.3 and Enstatite ~1.9±0.2; [3]). Whereas ~84% of peridotites worldwide [excluding low-[Os] samples (age). This suggests that much of the observed Pt/Os variability in mantle peridotites is relatively recent. Close agreement between our inferred Pt/OsPUM with previous estimates inferred from chondrites [3] is consistent with the addition of a chondritic late veneer to explain the HSE abundances in the upper mantle. [1] Becker et al., GCA 2006; [2] McDonough et al., Chem Geo 1995; [3] Brandon et al., GCA 2006

  9. Do Cooperative Banks Really Serve Agricultural Sector in Poland?

    OpenAIRE

    Zawojska, Aldona; Siudek, Tomasz

    2005-01-01

    The aim of the paper is to assess the potential of cooperative banks for serving agricultural sector in Poland and to identify the areas with the most development potential. We discuss the transformation process in the cooperative banking system under market economy, and in particular investigate importance of cooperative banks for farms' financing on the basis of our survey of banks. Moreover, the role of cooperative banks in transmission of Government policy supporting farm sector in Poland...

  10. Soft restructuring process in metallurgical enterprises in Poland

    Directory of Open Access Journals (Sweden)

    B. Gajdzik

    2015-10-01

    Full Text Available This article presents the range and outcomes of soft restructuring in metallurgical enterprises in Poland. The term ‘soft restructuring’ applies to changes in metallurgical enterprises’ employment policy during the period of political transformation in Poland. Steelworks performance under the market economy conditions demanded introducing changes in staff resources. Changes referred both to the staff structure as well as employees’ skills and gradual engaging of the staff in building the steelworks’ competitive advantage.

  11. A new record of Senecio inaequidens (Asteraceae in Poland

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    Pliszko Artur

    2017-11-01

    Full Text Available The paper presents a new Polish record of Senecio inaequidens, a perennial plant native to South Africa. It was found growing on roadside verge in Głogoczów, West-Beskidian Piedmont, southern Poland, on September 22, 2016. A map of distribution of S. inaequidens in Poland is presented using the ATPOL cartogram method and the pattern of its spread along motorways is discussed.

  12. Industrial-Organizational Psychology in Poland: past and current trends

    OpenAIRE

    DRYJANSKA LAURA

    2016-01-01

    The history of Industrial-Organizational (I-O) Psychology in Poland can be divided to three periods: birth and early development, advancements under socialism, and current trends. We may conclude that I-O Psychology in Poland since its birth has had to face numerous diverse challenges over time, related to the geo-political transformations and socio-economic problems. Currently, it is a vibrant field of practice and research, enriched by the unique experiences of many professors who have been...

  13. Puccinia scillae (Uredinales, a new species for Poland

    Directory of Open Access Journals (Sweden)

    Małgorzata Ruszkiewicz-Michalska

    2014-08-01

    Full Text Available The paper presents a rust species new for Poland, that affects the ornamental plant Scilla siberica Haw. The distribution of the fungus and its host plants, both introduced and native in Europe, have been investigated. The data from neighbouring countries indicate that the parasite has been probably overlooked in Poland till now. There is a possibility, however, that the species is currently spreading in central and north-eastern Europe.

  14. 'Other posts in 'other places : Poland through a postcolonial lens?

    OpenAIRE

    Mayblin, Lucy; Piekut, A.; Valentine, G.

    2016-01-01

    Postcolonial theory has tended to focus on those spaces where European colonialism has had a territorial and political history. This is unsurprising, as much of the world is in this sense ?postcolonial?. But not all of it. This article focuses on Poland, often theorised as peripheral to ?old Europe?, and explores the application of postcolonial analyses to this ?other? place. The article draws upon reflections arising from a study of responses to ethnic diversity in Warsaw, Poland. In doing s...

  15. Stochastic forecast of the population of Poland, 2005-2050

    OpenAIRE

    Anna Matysiak; Beata Nowok

    2007-01-01

    Forecasting the population of Poland is very challenging. Firstly, the country has been undergoing rapid demographic changes. In the 1990s, Poland experienced a fundamental shift from a communist regime to a democratic regime and entered the European Union in 2004. The political, economic, and social changes that accompanied the transformation had a profound influence on the demographic patterns in this country. International migration has been one of the first consequences of Poland’s entry ...

  16. Phytopathogenic micromycetes in central Poland. I. Peronosporales and Erysiphales

    OpenAIRE

    Małgorzata Ruszkiewicz-Michalska; Marek Michalski

    2014-01-01

    The present paper begins a new series of studies investigating the occurrence of phytopathogenic micromycetes in Central Poland. Fungi of the orders Peronosporales and Erysiphalas are discussed in part one. Relevant knowledge on the subject is surveyed, and a list of published records (46 taxa) as well as the findings collected by the present authors (99 taxa) is provided. The list comprises 2 species new for biota of Poland - Microsphaera deutziae Bunkina and Microsphaera elevata Burrill, 10...

  17. Poland-Möbius syndrome associated with dextrocardia.

    Science.gov (United States)

    Bosch-Banyeras, J M; Zuasnabar, A; Puig, A; Català, M; Cuatrecasas, J M

    1984-01-01

    A newborn male with Möbius syndrome, Poland anomaly, and dextrocardia is described. This is the second case reported of Poland-Möbius syndrome associated with dextrocardia. The patient presented with strabismus, facial diplegia, difficulty in swallowing, hypoplasia of the left pectoralis major muscle, partial absence of the upper costal cartilages, absence of the left areola, hypoplasia of the left forearm and hand, and dextrocardia without murmurs. Images PMID:6319703

  18. Fethiye-Burdur Fault Zone (SW Turkey): a myth?

    Science.gov (United States)

    Kaymakci, Nuretdin; Langereis, Cornelis; Özkaptan, Murat; Özacar, Arda A.; Gülyüz, Erhan; Uzel, Bora; Sözbilir, Hasan

    2017-04-01

    Fethiye Burdur Fault Zone (FBFZ) is first proposed by Dumont et al. (1979) as a sinistral strike-slip fault zone as the NE continuation of Pliny-Strabo trench in to the Anatolian Block. The fault zone supposed to accommodate at least 100 km sinistral displacement between the Menderes Massif and the Beydaǧları platform during the exhumation of the Menderes Massif, mainly during the late Miocene. Based on GPS velocities Barka and Reilinger (1997) proposed that the fault zone is still active and accommodates sinistral displacement. In order to test the presence and to unravel its kinematics we have conducted a rigorous paleomagnetic study containing more than 3000 paleomagnetic samples collected from 88 locations and 11700 fault slip data collected from 198 locations distributed evenly all over SW Anatolia spanning from Middle Miocene to Late Pliocene. The obtained rotation senses and amounts indicate slight (around 20°) counter-clockwise rotations distributed uniformly almost whole SW Anatolia and there is no change in the rotation senses and amounts on either side of the FBFZ implying no differential rotation within the zone. Additionally, the slickenside pitches and constructed paleostress configurations, along the so called FBFZ and also within the 300 km diameter of the proposed fault zone, indicated that almost all the faults, oriented parallel to subparallel to the zone, are normal in character. The fault slip measurements are also consistent with earthquake focal mechanisms suggesting active extension in the region. We have not encountered any significant strike-slip motion in the region to support presence and transcurrent nature of the FBFZ. On the contrary, the region is dominated by extensional deformation and strike-slip components are observed only on the NW-SE striking faults which are transfer faults that accommodated extension and normal motion. Therefore, we claim that the sinistral Fethiye Burdur Fault (Zone) is a myth and there is no tangible

  19. Van SW-bedrijf naar Centrum voor Werk: interview met Gert Jan Engbers, SOWECO

    NARCIS (Netherlands)

    Cremer, R.

    2008-01-01

    De wet Sociale werkvoorziening wordt uitgevoerd door ongeveer negentig "monopolisten", de huidige SW-bedrijven. Deze krijgen daartoe opdracht van de ongeveer 440 Nederlandse gemeenten, die de uitvoering neerleggen bij één partij: het regionale SW-bedrijf. Dit komt mede omdat de wet de gemeenten tot

  20. The Importance of Interfaces: A HW/SW Codesign Case Study

    DEFF Research Database (Denmark)

    Jensen, Dan C. Raun; Madsen, Jan; Pedersen, Steen

    1997-01-01

    This paper presents a codesign case study in image analysis. The main objective is to stress the importance of handling HW/SW interfaces more precisely at the system level. In the presented case study, there is an intuitive and simple HW/SW interface, which is based upon the functional modules in...

  1. Groundwater vulnerability assessment of the Cork Harbour area, SW Ireland

    Science.gov (United States)

    Allen, A. R.; Milenic, D.

    2007-11-01

    In the Cork Harbour area of SW Ireland, high yield karst and intergranular gravel aquifers are extremely vulnerable to pollution from a variety of sources, mainly due to the limited protection afforded by the thin cover of low permeability glacial and alluvial overburden. The main potential sources of pollution are due to rapid urbanisation of the Cork city area and its attendant infrastructure, and increased industrialisation in the area, with numerous new industries, particularly pharmaceutical and chemical industries, located around Cork Harbour. Other potential sources of pollution are a number of landfills in the area and an oil refinery near the mouth of Cork Harbour. Traditional agricultural sources of pollution also exist, due to increased use of chemical fertilisers. Finally, the susceptibility to saline intrusion of the karst and gravel aquifers around Cork Harbour is high due to the long coastline of the harbour and the low-lying nature of the karst synclines with their superimposed buried valleys.

  2. Nuclear medicine training and practice in Poland

    Energy Technology Data Exchange (ETDEWEB)

    Teresinska, Anna [Institute of Cardiology, Department of Nuclear Medicine, Warsaw (Poland); Birkenfeld, Bozena [Pomeranian Medical University, Department of Nuclear Medicine, Szczecin (Poland); Krolicki, Leszek [Warsaw Medical University, Department of Nuclear Medicine, Warsaw (Poland); Dziuk, Miroslaw [Military Institute of Medicine, Department of Nuclear Medicine, Warsaw (Poland)

    2014-10-15

    In Poland, nuclear medicine (NM) has been an independent specialty since 1988. At the end of 2013, the syllabus for postgraduate specialization in NM has been modified to be in close accordance with the syllabus approved by the European Union of Medical Specialists and is expected to be enforced before the end of 2014. The National Consultant in Nuclear Medicine is responsible for the specialization program in NM. The Medical Center of Postgraduate Training is the administrative body which accepts the specialization programs, supervises the training, organizes the examinations, and awards the specialist title. Specialization in NM for physicians lasts for five years. It consists of 36 months of training in a native nuclear medicine department, 12 months of internship in radiology, 3 months in cardiology, 3 months in endocrinology, 3 months in oncology, and 3 months in two other departments of NM. If a NM trainee is a specialist of a clinical discipline and/or is after a long residency in NM departments, the specialization in NM can be shortened to three years. During the training, there are obligatory courses to be attended which include the elements of anatomy imaging in USG, CT, and MR. Currently, there are about 170 active NM specialists working for 38.5 million inhabitants in Poland. For other professionals working in NM departments, it is possible to get the title of a medical physics specialist after completing 3.5 years of training (for those with a master's in physics, technical physics or biomedical engineering) or the title of a radiopharmacy specialist after completing 3 years of training (for those with a master's in chemistry or biology). At present, the specialization program in NM for nurses is being developed by the Medical Centre of Postgraduate Education. Continuing education and professional development are obligatory for all physicians and governed by the Polish Medical Chamber. The Polish Society of Nuclear Medicine (PTMN) organizes

  3. The Impact of Trust on Entrepreneurship in Poland

    Directory of Open Access Journals (Sweden)

    Marta Młokosiewicz

    2017-01-01

    Full Text Available In the global rankings of generalized trust, Poland occupies a lowly positon. Only 1/3 of Poles have a strong trust in strangers and roughly the same number believe that trust in business generally pays of. At the same tme, only half of them believe that a market economy based on private enterprise is the best economic system for the country. According to the literature review a major factor in the development of entrepreneurship is trust in other economic actors. The aim of the artcle is to present the relaton between trust and entrepreneurial actvites in Poland. In this paper the hypothesis was adopted that the level of trust in the public sphere, especially in business relatons in Poland, had an impact on the intensity of entrepreneurial actvites. The analysed period comprises the years from 2002 to 2016. The artcle presents changes in the potental for social trust, including trust in business. Indicators of confdence include the percentage of people that have trust in diferent actors in Poland. A further part of the paper is devoted to the phenomenon of entrepreneurship in Poland. Among the indicators of entrepreneurship are the number of newly registered and deregistered enttes, and enttes that are new or deregistered from the REGON register per 10 thousand of populaton. Moreover, the innovaton actvity of enterprises in Poland has been described. At the end, relatons between trust and entrepreneurial actvites in Poland were examined. The data was analysed statstcally with Pearson’s correlaton coefcients. The analysis of confdence and entrepreneurship is based mainly on the data published by the Polish Central Statstcal Ofce and Public Opinion Research Centre.

  4. Chinese Tourists in Cracow, Poland: Their Profile, Expectations, and Perceptions

    Directory of Open Access Journals (Sweden)

    Guszkiewicz Paulina

    2017-03-01

    Full Text Available Introduction. In 2012, China became the largest spender in international tourism, benefiting many destinations worldwide. Even if for Poland it is not an important source market yet, the Polish authorities have undertaken some marketing activities in China. The main aim of the paper is to explore the profile, motivations, and perceptions of the Chinese tourists visiting Cracow. The secondary aim is to check the effectiveness of the marketing efforts dedicated to the Chinese market undertaken by Poland since 2010. Material and methods. Data for the study (n = 100 were collected using a paper survey in English carried out among mainland Chinese tourists in Cracow in 2015. Results. The Chinese usually visit Poland for the first time, often in transit. They are prompted by the information found online and by word of mouth. Their main reasons to come are tradition, culture, historical sites, landscapes, and low costs. These expectations are well fulfilled, and the tourists′ overall satisfaction is very high. The Chinese find Poland to be different from other Western European countries. For them, Poland is a remarkable, traditional, safe, and developing country. Yet, their knowledge about the destination is limited. The main problem encountered is the language barrier, both online and once on site. The marketing efforts undertaken by Poland in the Chinese market have had weak and ambivalent effects. Conclusions. In order to attract Chinese tourists, there is a need to intensify expenditure not only on promotion (mainly online but also on the removal of language-based communication problems. There is also scope for expanding the tourist offer dedicated to Chinese tourists - both in Poland and in cooperation with other Central European countries.

  5. Genesis and tectonic setting of peridotitic spinels from the Divriǧi-Sivas region, eastern Turkey

    Science.gov (United States)

    Kırat, Ece; Ünlü, Taner; Akıska, Sinan; Kızılkanat, Ceyda; Mutlu, Halim

    2017-04-01

    The majority of the metallic ore deposits in Turkey, which hosts a series of complex tectono-magmatic process including subduction, collision, rifting and magmatism, are formed along the suture zones and associated with ophiolite complexes. The Divriǧi area is one of such unique districts in Anatolia. In this study, we examine whole rock and spinel chemistry of ultramafic rocks in the Divriǧi-Sivas region. Most of studied samples consist of wherlites and are represented by compositions varying from chromite at the core to ferritchromite and Cr-magnetite at the rims. Spinel samples have rather high Cr2O3 (46.50-56.24 wt. %) and very low TiO2 contents (chromites in Turkey, Divriǧi spinels are found to have slightly lower Fe2O3 and Al2O3 contents and Fe+2/Fe+3 ratios. Like spinels in some other ophiolite complexes in Turkey, compositions of all spinel samples are within the range of supra-subduction zone peridotites which display high degree partial melting (>35 %). Experimentally determined parental melt compositions of Divriǧi spinels (0.32-1.89 wt. % for FeO/MgO), (8.69-11.71 wt % for Al2O3) and (0.1-0.37 wt. % for TiO2) point out an arc setting with boninite composition. Prism diagrams constructed for the measured spinel compositions reveal that chromite is the most abundant phase comprising 50 % of the core. In consequence of alteration, mineral composition at the rims is varied and chromite content is lowered to nearly 20% and magnetite becomes the main phase with an abundance of about 90%. Keywords: Divriǧi-Sivas region, chromite, spinel, microprobe, geochemistry

  6. Vertical changes of the Co and Mn speciation along a lateritic regolith developed on peridotites (New Caledonia)

    Science.gov (United States)

    Dublet, Gabrielle; Juillot, Farid; Brest, Jessica; Noël, Vincent; Fritsch, Emmanuel; Proux, Olivier; Olivi, Luca; Ploquin, Florian; Morin, Guillaume

    2017-11-01

    Because they can host significant amounts of Co, the Mn-oxides are commonly considered as the major Co-bearing mineral species in lateritic environments. However, little is known about the process leading to the formation and/or the weathering of these Co-rich Mn-oxides. This lack of knowledge is mainly due to the fact that Co concentrations are too low in primary silicates for classical speciation analysis. In this study, we investigated both Co and Mn speciation in a 64 m thick lateritic regolith developed upon peridotites in New Caledonia, by combining High Energy Resolution Fluorescence Detection X-ray absorption Near Edge Structure (HERFD-XANES) spectroscopy at the Co K-edge with classical XANES spectroscopy at the Mn K-edge, bulk chemistry (ICP) and mineralogy (XRD). The results obtained provide new insights into the evolution of Co and Mn speciation as a function of the weathering stages. Co and Mn primarily occur as Co(II) and Mn(II,III) in olivine and serpentine in the bedrock. During the first weathering stage, these forms of Co and Mn are progressively oxidized toward Co(III) and Mn(III,IV), which occur mainly as Co(III)-bearing Mn(III/IV)-oxides in the transition between the saprolite and the laterite. In the uppermost lateritic horizons, long-time weathering resulted in a strong leaching of Co and Mn, and the remaining of these elements occurs as Co(II) and Mn(III) substituting for Fe(III) in goethite. This latter scavenging process emphasizes the importance of Fe-oxides for the long-term stabilization of Co and Mn in such deeply weathered laterites.

  7. Paired stable isotopes (O, C) and clumped isotope thermometry of magnesite and silica veins in the New Caledonia Peridotite Nappe

    Science.gov (United States)

    Quesnel, Benoît; Boulvais, Philippe; Gautier, Pierre; Cathelineau, Michel; John, Cédric M.; Dierick, Malorie; Agrinier, Pierre; Drouillet, Maxime

    2016-06-01

    The stable isotope compositions of veins provide information on the conditions of fluid-rock interaction and on the origin of fluids and temperatures. In New Caledonia, magnesite and silica veins occur throughout the Peridotite Nappe. In this work, we present stable isotope and clumped isotope data in order to constrain the conditions of fluid circulation and the relationship between fluid circulation and nickel ore-forming laterization focusing on the Koniambo Massif. For magnesite veins occurring at the base of the nappe, the high δ18O values between 27.8‰ and 29.5‰ attest to a low temperature formation. Clumped isotope analyses on magnesite give temperatures between 26 °C and 42 °C that are consistent with amorphous silica-magnesite oxygen isotope equilibrium. The meteoric origin of the fluid is indicated by calculated δ18Owater values between -3.4‰ to +1.5‰. Amorphous silica associated with magnesite or occurring in the coarse saprolite level displays a narrow range of δ18O values between 29.7‰ and 35.3‰. For quartz veins occurring at the top of the bedrock and at the saprolite level, commonly in association with Ni-talc-like minerals, the δ18O values are lower, between 21.8‰ and 29.0‰ and suggest low-temperature hydrothermal conditions (∼40-95 °C). Thermal equilibration of the fluid along the geothermic gradient before upward flow through the nappe and/or influence of exothermic reactions of serpentinization could be the source(s) of heat needed to form quartz veins under such conditions.

  8. New calibration of Ji - Di clinopyroxene barometer for Eclogites, pyroxenites and peridotites and eclogite - pyroxenite mantle geotherms.

    Science.gov (United States)

    Ashchepkov, Igor; Vishnyakova, Elena

    2010-05-01

    Checking the universe clinopyroxene JD-Di barometer on the experimental system showed that it better to use the separate schemes for the eclogite and peridotite systems. The clinopyroxene barometer based on the internal exchange of Jd-Di components for the Al. It allow using the temperature calculated with the (Krogh, 1988) method for the The barometer was calibrated on the 200 experimental runs for the eclogitic system (Yaxley,Brey,2004; Spandler ea, 2008; Konzett ea, 2008; Hanrahan ea, 2009 and references there in). It reproduces the pressure range to 120 kbar with the r= 0.91 (S=8) for 180 experimental runs. P(Ash2010 Ecl)=0.32 (1-0.215*Na/Al+0.012*Fe/Na)*Kd^3/4*ToK/(1+Fe)*(1+5*Fe)- 35*ln(1273/ToK)*(Al+Ti+2.5Na+1.5Fe3+)+(0.9-xx(2,8))*10+xx(2,9)/xx(2,3)* ToK /200-1.5 P1=(0.00004*P^3-0.0091*P^2+1.3936*P)*1.05 Where KD = Na*Mg/xAlCr*/Ca; XAlCr= Al+Cr+4*Ti-K-(Fe-0.21)*0.75 The tests on the natural associations form the eclogitic xenoliths with and without the diamonds and omphacite diamond inclusions (Taylor ea, 2006; Shatsky ea, 2008; Jacob ea, 2009) have shown very good agreement with the position of the Graphite -Diamond (Kennedy, Kennedy, 1977) boundary and to the conductive geotherms which are close to 34-36mvm-2 geotherms while for the South Africa they are more close to 40mvm-2 geotherms. For the zonal omphacites it produces the range of the nearly equal pressures or more rarely advective paths. The levels of the maximum enrichments in eclogites which are close to 50-60 kabr beneath 360ma Siberian kimberlites coincides with the levels of heating according to the monomineral and polymineral thermobarometry. South Africa eclogite geotherms often split into 2-3 branches: subductional (35) conductive (40) for Paleozoic-Mesozoic mantle lithosphere and the hottest advective close o 45 mv/m-2. For the pyroxenite compositions the barometer was rearranged to by the adding the temperature influence on Al , Ta, Fe exactly in KD as following: P(Ash2010 Per-Pxt)=0

  9. The Development of Explosive Metalworking in Poland

    Directory of Open Access Journals (Sweden)

    Babul W.

    2014-10-01

    Full Text Available The author coordinated the research in Poland by the collaboration with civil and military scientific and research centres. In result they elaborated detonation process of spraying coats designed and constructed stands equipped with detonative devices, they also elaborated the techniques of basic coating parameter measurement and built devices for commercial and scientific services. In the research the author's achievements within the range of explosive welding have been used. The experience of the scientific teams was very effective. It was observed that many phenomena that take place in the processes of detonative layer coating and explosive welding are the same. In order to obtain a required connection the plastic strain of the connected material surfaces has to be achieved and cumulative flows have to be formed. There are a similar range of the connecting process conditions and the mechanisms of plastic strain. The highest connection strength is obtained when an intermediate zone is formed. The zone has to be composed of the two connected materials. The intermediate layer is formed as a result of mechanical alloying of the materials due to large plastic strain. The plastic strain leads to forming meta-stable phases that have properties of pseudo solid solution, chemical compounds, intermetallic phases and fragmentation corresponding to nanomaterials and amorphous states.

  10. Science popularization and European citizenship in Poland

    Directory of Open Access Journals (Sweden)

    Jacek Piotr Szubiakowski

    2007-09-01

    Full Text Available The idea to link European citizenship and science education is surely new and uncommon in Poland, but we think, as SEDEC project, that can enrich both the panorama of science popularization outside and inside school system. I checked carefully curricula for every stage of school education looking for the topics concerning the developing of the European citizenship. I found that they are usually connected to the history, geography and some activities developing of the knowledge about generally defined citizenship. The spare topics connected directly to the science are present especially in grammar school curriculum. They may be divided into three groups: exploiting the common heritage, common object of interest and scientific community respectively. In that paper I would like to show how the activities in each of the group may influence the EU citizenship developing process. I am going to emphasize the good choice of science as a context or a medium for EU citizenship education. It may be an important point especially in Central Europe. Additionally I would like to present some auxiliary events that are enable through the external educational resources such as museum and planetarium.

  11. [Infectious diseases in Poland in 2000].

    Science.gov (United States)

    Mazurek, Jacek; Czarkowski, Mirosław P

    2002-01-01

    The decreasing tendency in incidence of infectious diseases observed in Poland in previous years as compared with 2000 has weakened or stopped. Increase in the incidence of selected infectious diseases can be linked with the improvement of surveillance resulting from the better diagnostics and greater attention paid to these diseases (including borreliosis, salmonella, and Haemophilus influenzae meningitis). Between 1999 and 2000, the most intense decrease in the number of mumps, measles, and scarlet fever cases as an effect of the end of epidemics was observed. At the same time increase in the number of pertussis, rubella, chickenpox, and meningitis cases was noticed. In 2000, the first case of human rabies since 1986 has been reported. In 2000, compared with 1999, among all notified deaths percentage of deaths attributed to infectious diseases (0.83%) and infectious diseases death rate (0.79 per 10,000) were slightly higher and were the highest in the last decade. As in 1999 the observed increase was effect of the influenza deaths increase (358 deaths, mortality 0.022%). The main disease causing the largest number of deaths, as in previous years, was tuberculosis (36.5% of total infectious diseases deaths).

  12. Radioactive Contamination of Agricultural Products in Poland

    Energy Technology Data Exchange (ETDEWEB)

    Muszynski, W.; Grabowski, D.; Rubel, B.; Kurowski, W.; Swietochowska, J.; Smagala, G. [Central Laboratory for Radiological Protection, Radioactive Contamination Department, Warsaw (Poland)

    2003-06-01

    Radiological contamination of the environment is caused by nuclear activities on the globe: nuclear weapon tests and the Chernobyl accident. The transfer of radionuclides to the organism via ingestion is one of the sources of doses obtained by people. To assess the doses received by humans the intake of isotopes with daily diet was defined. The concentration of radionuclides in foodstuffs was determined. The network of Service for Measurement of Radioactive Contamination systematically controls all kinds of important agricultural products such as milk, meat, vegetables, fruit, cereals and forest products: mushrooms, blueberries etc. Measurement stations involved in food monitoring act within Sanitary-Epidemiological Stations, Veterinary Hygiene Units and Chemical-Agricultural Stations. All activities are co-ordinated by the Central Laboratory for Radiological Protection. The level of activity of caesium isotopes has regularly been monitored in collected samples originating from different administrative districts of Poland. Since 1994 the {sup 134}Cs concentration has been below the detection limit. The activity of {sup 137}Cs has been measured to determine long-term effect of the accident on the contamination of milk, meat and other foodstuffs. (orig.)

  13. Thallium in mineral resources extracted in Poland

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    Bojakowska I.

    2013-04-01

    Full Text Available Thallium concentrations in primary mineral commodities extracted in Poland and processed in high temperatures were determined by ICP-MS method. Samples of hard and brown coal, copper-silver and zinclead ores, argillaceous and calcareous rocks of different genesis and age were analyzed. The highest thallium concentrations occur in the zinc-lead ores, the average content being of 52.1 mg/kg. The copper ores contain in average 1.4 mg/kg of thallium. Hard coals from the Upper Silesian Coal Basin display higher thallium content than those exploited in the Lublin Coal Basin. Brown coals from Turow deposit distinguish by much higher values, 0.7 mg/kg Tl, than those from huge Bełchatów and smaller Konin-Turek region deposits. Average thallium concentrations in clays used for ceramic materials are lower than 1 mg/kg, except of Mio-Pliocene Slowiany deposit. The average content of thallium in the studied limestone and dolomite raw materials for cement, lime, and metallurgical flux, and refractories is very low in comparison to the average amounts in the world carbonate rocks.

  14. Development of laser technology in Poland: 2016

    Science.gov (United States)

    Jankiewicz, Zdzisław; Jabczyński, Jan K.; Romaniuk, Ryszard S.

    2016-12-01

    The paper is an introduction to the volume of proceedings and a concise digest of works presented during the XIth National Symposium on Laser Technology (SLT2016) [1]. The Symposium is organized since 1984 every three years [2-8]. SLT2016 was organized by the Institute of Optoelectronics, Military University of Technology (IO, WAT) [9], Warsaw, with cooperation of Warsaw University of Technology (WUT) [10], in Jastarnia on 27-30 September 2016. Symposium Proceedings are traditionally published by SPIE [11-19]. The meeting has gathered around 150 participants who presented around 120 research and technical papers. The Symposium, organized every 3 years is a good portrait of laser technology and laser applications development in Poland at university laboratories, governmental institutes, company R&D laboratories, etc. The SLT also presents the current technical projects under realization by the national research, development and industrial teams. Topical tracks of the Symposium, traditionally divided to two large areas - sources and applications, were: laser sources in near and medium infrared, picosecond and femtosecond lasers, optical fiber lasers and amplifiers, semiconductor lasers, high power and high energy lasers and their applications, new materials and components for laser technology, applications of laser technology in measurements, metrology and science, military applications of laser technology, laser applications in environment protection and remote detection of trace substances, laser applications in medicine and biomedical engineering, laser applications in industry, technologies and material engineering.

  15. Medieval Multilingualism in Poland: Creating a Corpus of Greater Poland Court Oaths (Rotha

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    Kopaczyk Joanna

    2016-12-01

    Full Text Available In this paper we introduce the research plan for the preparation of a searchable electronic repository of the earliest extant legal oaths from medieval Poland drawing on the expertise in historical corpus-building developed for the history of English. The oaths survive in the overwhelmingly Latin land books from the period between 1386 and 1446 for six localities Greater Poland, in which the land courts operated: Poznań, Kościan, Pyzdry, Gniezno, Konin and Kalisz. A diplomatic edition of the oaths was published in five volumes by Polish historical linguists (Kowalewicz & Kuraszkiewicz 1959–1966. The edition is the only comprehensive resource of considerable scope (over 6300 oaths from the years 1386–1446 for the study of the earliest attestations of the Polish language beyond glosses. Recognising some limitations, but most of all its unparalleled coverage of the coexistence of Latin and the vernacular, the ROThA project embarks on transforming the edition into an open up-to-date digital resource. We thus aim to facilitate research into the history of Polish and Latin as well as of the legal system and the related social and linguistic issues of the period.

  16. Poland: A Dark Side of Church Cultural Policy

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    Szocik Konrad

    2015-12-01

    Full Text Available The cultural policy of the Roman Catholic Church in Poland is incorporated into state-run cultural policies. The organs of public authority enforce the objectives of Church regardless of Church’s actual ability to influence the society. It should be pointed out that the secularization of religion in Poland is frequently misinterpreted and usually equated with its deprivatization. It is worth mentioning that Catholicism is the dominant religion of the country and the Roman Catholic Church has hold a special position in Poland and play a major role in the country’s social and political life. In practice, however, Polish society appears to be religiously indifferent. This paper proves that the official, state-run cultural policy in Poland is based on favoritism of the Roman Catholic Church, regardless of Church’s actual ability to wield influence on society. Thus, there is a variety of implicit and explicit cultural policies implemented by the authorities to support Church. This work also aims at addressing the question of social attitudes to women, especially the one concerning the UN and EU law embracing women’s rights, until recently still not implemented in Poland. This paper further explores some peculiarities of this topic as an example of a specific outcome of Church cultural policy and its impact on both the past and present-day society.

  17. Bioethical committees and data protection issues in Poland

    Science.gov (United States)

    Ligocka, Danuta

    2008-01-01

    In Poland there are only Regional Bioethical Committees. Unlike most EU countries Poland has no coordinating centre on bioethics for human research. However, the Ministry of Health and Welfare has established a Bioethics Appeals Committee. The functioning of the Bioethical Committees in Poland is regulated in detail by the Regulation of the Ministry of Health and Welfare of 1999. All regulations comply with important guidelines such as: the Helsinki Declaration, The Rules of Good Clinical Practice, EU Directives and legal regulations binding in Poland, mainly the Act of the Medical Doctor Profession and the Dentist Profession, as well as the Act of Pharmaceutical Law. In the framework of the Human Biomonitoring Programme, the application for bioethical evaluation will be submitted to the Bioethical Committee at the Nofer Institute of Occupational Medicine in Lodz. The data protection legislation in Poland according to the Act of the Protection of Personal Data of 29th of August 1997 with latest amendments fulfils EU regulations. The Act also contains detailed provisions regarding the duties of the Inspector General for Data Protection. The paper presents data on the activities of the Bureau of the Inspector General for Personal Data Protection in 2005, 2006 and 2007. PMID:18541070

  18. Modification of an ancient subcontinental lithospheric mantle by continental subduction: Insight from the Maowu garnet peridotites in the Dabie UHP belt, eastern China

    Science.gov (United States)

    Chen, Yi; Su, Bin; Chu, Zhuyin

    2017-05-01

    Orogenic mantle-derived peridotites commonly originate from the subcontinental lithospheric mantle (SCLM) and thus provide a key target to investigate the modification of the SCLM by a subducting slab. The Maowu ultramafic rocks from the Dabie ultrahigh-pressure (UHP) metamorphic belt have formerly been debated as representing cumulates or mantle-derived peridotites. Detailed petrological and geochemical data presented in this study provide new constraints on the origin and formation of the peridotites involving melt depletion in the ancient SCLM and deep crustal metasomatism. The Maowu garnet dunites have refractory bulk compositions characterized by high Mg# (91.9-92.0) and Ni (2537-2892 ppm) values and low Al2O3 (0.26-0.76 wt.%), CaO (0.05-0.32 wt.%), TiO2 (enrichment in incompatible elements. Mineral and whole-rock chemistry indicate that these veins represent metasomatic products between the wall dunites and silica-rich hydrous melts under UHP conditions. The veins show large variations in platinum-group element (PGE) signatures and Re-Os isotopes. The garnet-poor orthopyroxenite veins are characterized by low Al2O3 ( 6 wt.%) and S (99-306 ppm) contents and show melt-like PGE patterns and high 187Os/188Os ratios (up to 0.36910). These features, combined with the occurrence of interstitial sulfides in the garnet-rich orthopyroxenite veins, suggest that crust-derived sulfur-saturated silicate melts may have significantly modified the PGE signature and destroyed the Re-Os systematics of the SCLM. However, when the crust-derived silicate melts became sulfur-depleted, such melts would not significantly modify the PGE patterns, radiogenic Os-isotope compositions or the Re-depletion model ages of the SCLM. Consequently, deep crust-mantle interactions in continental subduction zones could induce high degrees of Os isotopic heterogeneity in the SCLM wedge.

  19. PGE and Re-Os Isotope Behaviour in a Subduction-Modified Mantle Wedge: A Fresh Look into the Peridotites from the Ulten Zone, Eastern Alps

    Science.gov (United States)

    Aulbach, S.; Braga, R.; Gudelius, D.; Prelevic, D.; Meisel, T. C.

    2015-12-01

    Peridotites in the upper Austroalpine Ulten zone (Eastern Italy) sample the subduction-modified Variscan mantle wedge. Metasomatism of peridotites during four stages of mantle wedge evolution includes: (1) Intrusion of alkaline melts from an inner, subduction-modified wedge and cryptic enrichment of spinel lherzolites (SL); (2) Reaction with siliceous crustal melts after pressure increase, generating coarse-grained garnet amphibole peridotites (GAP); (3) Crystallisation of abundant amphibole (± apatite and dolomite) from residual hydrous fluids during and/or after peak metamorphism recorded by fine-grained GAP; [4] Subsequent influx of crustal fluids, causing retrograde formation of spinel chlorite amphibole peridotites (SAP) [1-5]. SL and coarse GAP are apparently more fertile, whereas fine GAP and SAP retain the most depleted major-element characteristics. Overall, samples fall on partial melting trends consistent with extraction of low degrees of melt (F≤0.15) at 2-1 GPa. SL and coarse GAP have ±flat PGE patterns normalised to Primitive Upper Mantle (PUM), or show small decreases or increases from compatible to incompatible PGE. This suggests retention of primary sulphide liquid at low degrees of melting, during which PGE concentrations are little fractionated [6]. Indeed, broad positive correlations between the PGE suggest a common host, likely sulphide, observed in the samples as assemblages of pn ± po and cpy. Most fine-GAP share these patterns, indicating robustness against massive hydrous fluid influx, while Os/Ir > PUM argue against strong Os scavenging by highly oxidising hydrous fluids. Nevertheless, elevated Ru/IrPUM in a subgroup of samples may indicate a role for spinel addition under oxidising conditions. Most samples have 187Os/188Os >PUM, despite sub-PUM Re/Os, which requires addition of, or isotopic equilibration with, 187Os-rich crustal components, most likely via the precipitation of metasomatic sulphide. [1] Nimis and Morten (2000) J

  20. Subduction of shallowly formed arc cumulates: Evidence from clinopyroxene compositions of garnet peridotites in the Rio San Juan Complex, northern Dominican Republic

    Science.gov (United States)

    Hattori, K.; Tubrett, M.; Saumur, B.-M.; Guillot, S.

    2009-04-01

    Garnet peridotites are very rare in oceanic subduction complexes, with only two reported occurrences. One is in the Sambagawa metamorphic belt in Shikoku, Japan, and the other example is in the southern part of the Rio Juan Complex, northern Dominican Republic. In both locations, garnet peridotite occurs in close association with eclogites in high metamorphic grade of the terranes. The Rio Juan Complex represents rocks formed during the southwestern subduction of the Proto-Caribbean oceanic plate below the Carribean Plate during late Cretaceous to early Eocene. Garnet peridotites (clinopyroxene[Cpx]-bearing dunite, wehrlite, olivine clinopyroxenite) occur as large (The rocks are all low in Ir-group PGE (Ir, Ru, Os), indicating that they are cumulates of a melt, since these remain in the residue during partial melting. A cumulate origin of the ultramafic rocks is consistent with relatively low Mg contents of olivine (Fo 74-83) compared to olivine in mantle peridotites. Extended trace element plots of the bulk rocks show a so-called "arc geochemical signature" with high fluid-mobile element concentrations, such as Sr, U, and Pb, and low HFSE, such as Nb and Zr, indicating that formation of the parental magmas were related to subduction. Two representative garnet-bearing samples (wehrlite and clinopyroxenite) were selected for trace element analysis of Cpx grains using a LA HR ICP-MS. The data show a negatively sloped normalized pattern of REE; low contents of light REE (0.1-0.3 of the primitive mantle values) and similar concentrations of middle to heavy REE (1-2 of the primitive mantle values). Extended trace element patterns of Cpx are similar between two samples and also to that of the bulk rocks, with low Nb and Zr and high fluid-mobile elements. The Y and heavy REE patterns of Cpx do not show anomalies between the samples. As these elements would be preferentially incorporated into garnet, the lack of anomalies indicates early crystallization of Cpx and later

  1. Palaeoenvironmental reconstruction of Hüsamlar coal seam, SW Turkey

    Science.gov (United States)

    Büçkün, Zeynep; İnaner, Hülya; Oskay, Riza Görkem; Christanis, Kimon

    2015-06-01

    The Ören and Yatağan Basins in SW Turkey host several Miocene coal deposits currently under exploitation for power generation. The present study aims to provide insight into the palaeoenvironmental conditions, which controlled the formation of the Hüsamlar coal seam located in Ören Basin. The coal seam displays many sharp alternations of matrix lignite beds and inorganic, lacustrine sediment layers. The coal is a medium-to-high ash lignite (10.47-31.16 wt%, on dry basis) with high total sulphur content (up to 10 wt%, on dry, ash-free basis), which makes it prone to self-combustion. The maceral composition indicates that the peat-forming vegetation consisted of both arboreal and herbaceous plants, with the latter being predominant in the upper part of the seam. Mica and feldspars contribute to the low part of the seam; carbonates are dominant in the upper part, whereas quartz and pyrite are present along the entire coal profile. The sudden transitions of the telmatic to the lacustrine regime and reverse is attributed to tectonic movements that controlled water table levels in the palaeomire, which affected surface runoff and hence, clastic deposition.

  2. Melitofilia em Canavalia rosea (Sw. DC. (Leguminosae-Papilionoideae

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    Fábio Verçoza

    2010-11-01

    Abstract. This work aimed to study the floral biology and the pollination’s ecology of Canavalia rosea (Sw. DC. (Leguminosae-Papilionoideae by bees in the sandbank vegetation of the Grumari Environmental Protection Area (EPA , located in the western zone of Rio de Janeiro’s city. The study was developed between the months of June of 2008 to June of 2009. Sampling on morphology, color and odor of the flowers of the species were made. The number of open flowers per day in each individual was recorded, as well as the opening steps, determining the period of anthesis. The occurrence of floral visitors was recorded through the observation of the visit’s time, of the adaptability for pollination, of the ease of access to the reward and of the intra-floral behavior played. C. rosea occurs in psamophily communities and in post-beach sandbank of Grumari’s EPA. It presents typical characteristics of mellitophily (pollination by bees and the flowers are pollinated by Xylocopa frontalis Oliver. It also receives visits from Tetragonisca angustula Latreille, Trigona spinipes Fabricius and Apis mellifera Linnaeus, which collects pollen without pollinating the flowers. X. frontalis proved to be the only effective pollinator of C. rosea in the Grumari sandbank, making the plant directly dependent on this species for fruit and seed’s production in this location.

  3. On Economics in Poland in 1949-1989: Introduction

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    Czarny Bogusław

    2014-10-01

    Full Text Available This article is a concise introduction into the history of economics in totalitarian Poland in 1949-1989. In it, I attempt to show the degradation of economics in Poland in this period. The main theses of the article are three. First, academic economics and the institutions necessary for the normal functioning of science were destroyed in Poland at the turn of the 1940s and 1950s. Pseudo science was substituted for the science of economics. Second, these events had a damaging impact on the quality of research in the years that followed. In my opinion, the alleged achievements of Polish economists, e.g., Oskar Lange's monograph Ekonomia polityczna, as well as the works of Włodzimierz Brus and members of the so-called “Wakar School,” were of only “outside” importance. Third, after 1949, the teaching of economics degenerated as well.

  4. Ecology and taxonomy ofFusarium species in Poland.

    Science.gov (United States)

    Kwaśna, H; Chełkowski, J

    1991-03-01

    The paper presents 21Fusarium species occurring in Poland on the field crops /mostly on cereals, maize, potato and Papilionaceae plants/, woody plants, grasses, vegetables and ornamentals as well as on kernels or seeds of these hosts and soils. Additionally the commonly observed symptoms on above-mentioned plants and the informations about regions of the highest disease occurrence are added.However the paper results mainly from authors' investigation on theFusarium species occurrence in Poland, it encloses also the available, post-war literature data on the fusariosis in Poland in the past.Majority ofFusarium species cited had been identified according to Nelson et al, taxonomic system. Comparative listing of the monographs / 1,11, 21/ is presented.

  5. Driver fatigue and road safety on Poland's national roads.

    Science.gov (United States)

    Jamroz, Kazimierz; Smolarek, Leszek

    2013-01-01

    This paper presents an overview of factors causing driver fatigue as described in the literature. Next, a traffic crash database for 2003-2007 is used to identify the causes, circumstances and consequences of accidents caused by driver fatigue on Poland's national roads. The results of the study were used to build a model showing the relationship between the concentration of road accidents and casualties, and the time of day. Finally, the level of relative accident risk at night-time versus daytime is defined. A map shows the risk of death and severe injury on the network of Poland's national roads. The paper suggests to road authorities steps to reduce fatigue-related road accidents in Poland.

  6. Water Quality and Management Changes Over the History of Poland.

    Science.gov (United States)

    Szalinska, Ewa

    2018-01-01

    Poland is one of the countries distinguished by a long and colorful past. Undergoing numerous turbulent socio-economic changes forced by the course of history, Poland is now one of the member states of the European Union. Experiencing low water quantity and high contamination levels in surface waters, Poland is following other EU countries in the effort to reach a "good" water status. Herein are presented impacts of changes in Polish history on water legislation, management, and research, as well as explanations for the perceptible split between engineering and scientific approaches to the aquatic issues. Drawbacks caused by unsatisfactory state research funding for the sciences and division of the water related contemporary scientific interests are also discussed.

  7. Geographical distribution of {sup 90}Sr contamination in Poland

    Energy Technology Data Exchange (ETDEWEB)

    Gaca, P.; Mietelski, J.W. [The Henryk Niewodniczanski Inst. of Nuclear Physics (IFJ PAN), Krakow (Poland); Skwarzec, B. [Univ. of Gdansk, Dept. of Chemistry, Gdansk (Poland)

    2006-07-01

    The paper presents results on determination of {sup 90}Sr in bilberry and cowberry leaves (Vaccinium myrtillus and Vaccinium vitis-idaea) and the use of these plants as bio-monitors of radiostrontium contamination in Poland. Radiostrontium was determined by mean of liquid scintillation spectrometry preceded by radiochemical separation using Sr-resin and {sup 85}Sr tracer. The approximate map of {sup 90}Sr contamination of Poland is presented. The activity ratio between {sup 90}Sr and obtained earlier data for {sup 137}Cs in the same samples is discussed. The enhancement of radiostrontium content observed in northeastern Poland seems to be the trace of hot-particles fallout from initial Chernobyl cloud, which passed over Polish territory toward Scandinavia. (orig.)

  8. An annotated checklist of the Aphids (Hemiptera: Aphidomorpha of Poland

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    Wojciechowski Wacław

    2015-12-01

    Full Text Available The paper presents a comprehensive compilation of 764 taxa (species and subspecies, distributed over 167 genera, belonging to 17 subfamilies, three families and three superfamilies of Aphidomorpha recorded to date from Poland. The systematic positions of 19 taxa have been revised in accordance with recent changes in nomenclature. The presence in the Polish aphidofauna of Drepanosiphum oregonensis and Coloradoa huculaki, previously included without any distribution data in checklists of Polish aphids, has been confirmed. One species Sitobion (Sitobion alopecuri is recognized as being new to Poland. At least 44 species (6% of local fauna of Aphidomorpha are alien to Poland; among them 11 species collected from plants imported or cultivated in indoor conditions are listed.

  9. Phytopathogenic micromycetes in central Poland. I. Peronosporales and Erysiphales

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    Małgorzata Ruszkiewicz-Michalska

    2014-08-01

    Full Text Available The present paper begins a new series of studies investigating the occurrence of phytopathogenic micromycetes in Central Poland. Fungi of the orders Peronosporales and Erysiphalas are discussed in part one. Relevant knowledge on the subject is surveyed, and a list of published records (46 taxa as well as the findings collected by the present authors (99 taxa is provided. The list comprises 2 species new for biota of Poland - Microsphaera deutziae Bunkina and Microsphaera elevata Burrill, 10 rare and many common fungal species that had not been previously re00rded in this area as well as 21 plant taxa, mostly species of deliberate or accidental anthropogenic origin, that are new hosts of the parasites formerly listed in Poland.

  10. THE TRADE POSITION OF POLAND IN THE ICT SERVICES SECTOR

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    Sylwia Talar

    2016-09-01

    Full Text Available The paper includes analysis and assessment of trade in the ICT services performance of Poland. This study is looked at the trade position, essentially on the basis of the share in the world ICT services exports, revealed comparative advantage (RCA, and trade coverage ratio. It also identifies trends of the world trade in the ICT services. The statistics are derived from the basis of UNCTAD and Eurostat. International trade in the ICT ser-vices sector has specific characteristics and the interpretation of results of this trade is to take account of the particular nature of the ICT services. Poland is currently not revealed comparative advantage in the ICT services exports, but has had positive balance. Practically all trade indicators for Poland show very strong growth, which indicate a significant improvement in its ICT services trade position.

  11. A case of Poland Syndrome associated with dextroposition

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    Guerrini Pietro

    2010-02-01

    Full Text Available Abstract Classical Poland Syndrome (PS is characterized by unilateral, partial or complete absence of the sternocostal head of the major pectoral muscle and brachysyndactyly of fingers on the same side. We report the case of a newborn infant with dextrocardia and PS located on the left side. This association is very rare: to date only 19 cases have been described in scientific literature. In all reported cases, as in the present, the Poland defect involved the left side and was associated to rib defects, whereas most cases of PS are on the right side and few have rib defects. This case supports the view that dextrocardia follows the loss of volume of the left hemithorax caused by Poland sequence and that the combination of PS and dextrocardia is not coincidental.

  12. A case of Poland Syndrome associated with dextroposition

    Science.gov (United States)

    2010-01-01

    Classical Poland Syndrome (PS) is characterized by unilateral, partial or complete absence of the sternocostal head of the major pectoral muscle and brachysyndactyly of fingers on the same side. We report the case of a newborn infant with dextrocardia and PS located on the left side. This association is very rare: to date only 19 cases have been described in scientific literature. In all reported cases, as in the present, the Poland defect involved the left side and was associated to rib defects, whereas most cases of PS are on the right side and few have rib defects. This case supports the view that dextrocardia follows the loss of volume of the left hemithorax caused by Poland sequence and that the combination of PS and dextrocardia is not coincidental. PMID:20170539

  13. Abortion, church and politics in Poland.

    Science.gov (United States)

    Jankowska, H

    1992-01-01

    In early 1991 the abortion debate in Poland entered its new stage. The prolife and prochoice options had already clashed in the early 1930s over a new penal code and backstreet abortions. According to the code of 1932, induced abortion was allowed in cases of rape, incest, or for medical indications. Abortion was legalized in 1956, but subsequently it came under attack from Catholic circles, and by 1989 the Unborn Child Protection Bill was drafted which criminalized abortion. Only 11% of Polish women use modern contraceptives. The less efficient methods are the most prevalent: the natural method (Ogino-Knaus calendar), 35% of couples; coitus interruptus, 34%; condoms, 15%; oral contraceptives 7%; chemical spermicides, 2.5%; and the IUD 2%. According to size of Catholic Church estimate there are 600,000 abortions yearly. In contrast, official statistics indicate that the number of abortions is decreasing: 137,950 in 1980; 105,300 in 1988; 80,100 in 1989; 59,400 in 1990. In January 1991 the Constitutional Tribunal dismissed the motion of the Polish Feminist Association against the restrictive regulations of the Ministry of Health concerning abortion. After a parliamentary stalemate on the Unborn Child Protection Bill a commission consisting of 46 persona (1.2 of them women, 20 persons from the prochoice and 24 from the prolife lobby) continued the debate on the bill. Public opinion polls conducted by independent groups in November 1990 showed that about 60% of citizens were against the Senate's draft. Since then interest in the abortion issue has dwindled, and only 200 women and men took part in a prochoice demonstration in front of the parliament on January 25, 1991. In the spring of 1989 and in September 1990 thousands had participated in similar demonstrations. The prevailing attitude is that if the antiabortion bill is passed nothing can be done.

  14. Expert views from Poland and Estonia

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    Kaja Põlluste

    2016-12-01

    Full Text Available Background . Home care (HC is placed between the health and social welfare systems, and the clients of HC mostly need health services. Along with other providers, family doctors (FDs are usually involved in the provision of care. Objectives. This paper aims to describe and compare the involvement of HC providers to elderly and disabled persons in Poland and Estonia. Material and methods . This study is part of the international project EURHOMA P (Mapping Professional Home Care in Europe. Data was collected in 2008–2010. Experts from different areas of health and social care were queried by using a questionnaire containing structured case narratives, which were hypothetical descriptions of the situations of elderly or disabled persons living at home and in need of care. Results. There are a number of HC services, e.g. nursing, medical and social, available in both countries. The application for HC is mostly made by the patient or a close family member; the point of entry to HC can differ and depends on the client’s primary problem. FDs, together with social workers, play an important role in the provision of HC services in both countries. However, due to a shortage of round-the-clock professional services at a client’s home, families are also expected to play a large role in providing HC . Conclusions . Health care professionals, mainly those working in primary health care, play a remarkable role in access to and provision of HC services. Nevertheless, responsibility for 24-hour care lies, to a large extent, with the client’s immediate family. This situation seems to be typical in Eastern European countries.

  15. Internal migration and urban change in Poland.

    Science.gov (United States)

    Kupiszewski, M; Durham, H; Rees, P

    1998-09-01

    This study examined population change and internal migration among communes and municipalities in Poland during 1984-94. Data were obtained from the National Population Censuses of 1978 and 1988 and from records for 3030 communes and municipality units. During 1980-90, the number of units losing population declined considerably from 1281 to 1061 during 1980-90 and 1990-94. The slowing of migration is attributed to economic difficulties in the 1990s and a reduced labor market. Large cities gained population in the 1980s and then lost it in the 1990s. 33% of communes each suffered migration losses below and above 5/1000 population. 33% gained migrant population. Large and medium-size towns were gainers, with three exceptions. Medium-size towns that were new regional capitals, monofunctional industrial towns linked with development of socialist investments, and towns linked with mining and heavy industry were the losers. The pace of growth in large cities was the slowest. Wroclaw was the only large city that was growing in the 1990s. Towns of 10,000-100,000 grew in the 1980s and halved their growth in the 1990s. Towns of 5000-25,000 were the fastest growing in the 1990s. Most of the growth during 1984-94 occurred in towns of 10,000-100,000. Rural areas all lost population to urban areas, especially among female inhabitants. Warsaw lost population, but suburban areas gained population. Distances to cities with basic amenities are analyzed. Population density was weakly associated with growth. Growth was concentrated in high-density bands. Population change was positive in all bands except for two with the lowest population density.

  16. Pedestrian Safety in Road Traffic in Poland

    Science.gov (United States)

    Budzynski, Marcin; Jamroz, Kazimierz; Mackun, Tomasz

    2017-10-01

    Every third road accident in Poland involves a pedestrian as a participant or, most of the time, a casualty. Pedestrian accidents are usually the result of complex situations and the outcome of a number of factors related to driver and pedestrian behaviour and road infrastructure. Safety depends largely on how well the traffic condition is perceived and on visibility in traffic. The paper presents the results of analyses of methodologies for systematic studies of pedestrian behaviour and pedestrian-driver relations. The effects of the location of the site, type of cross-section and other selected parameters on pedestrian and driver behaviour are demonstrated. The analyses showed that pedestrians are most often put at risk by too long pedestrian crossings, vehicles going too fast around pedestrian crossings, lack of proper sight distance and poorly lit or unlit pedestrian crossings. The reason for such defective infrastructure is that planners, designers, contractors and maintenance services are not receiving any support from design, marking and maintenance regulations for pedestrian traffic. In addition, the Road Traffic Law is not restrictive enough when it comes to drivers’ obligations towards pedestrian safety. Polish design regulations allow long pedestrian crossings up to four lanes in one direction or three lanes in two directions irrespective of traffic control and speed limits. Pedestrian crossings should be kept at a maximum of three lanes. There is nothing in the design regulations about the required driver-pedestrian sight distance. Neither does the Road Traffic Law help engineers with that. It is legal to park vehicles within 10 m of a pedestrian crossing which does not guarantee the necessary sight distance. Drivers must be able to see a pedestrian waiting or stepping onto the crossing from a distance that will help them come to a stop safely. It is safer to follow the principle of providing adequate pedestrian sight distance. Recommendations for

  17. Extreme Precipitation in Poland in the Years 1951-2010

    Science.gov (United States)

    Malinowska, Miroslawa

    2017-12-01

    The characteristics of extreme precipitation, including the dominant trends, were analysed for eight stations located in different parts of Poland for the period 1951-2010. Five indices enabling the assessment of the intensity and frequency of both extremely dry and wet conditions were applied. The indices included the number of days with precipitation ≥10mm·d-1 (R10), maximum number of consecutive dry days (CDD), maximum 5-day precipitation total (R5d), simple daily intensity index (SDII), and the fraction of annual total precipitation due to events exceeding the 95th percentile calculated for the period 1961-1990. Annual trends were calculated using standard linear regression method, while the fit of the model was assessed with the F-test at the 95% confidence level. The analysed changes in extreme precipitation showed mixed patterns. A significant positive trend in the number of days with precipitation ≥10mm·d-1 (R10) was observed in central Poland, while a significant negative one, in south-eastern Poland. Based on the analysis of maximum 5-day precipitation totals (R5d), statistically significant positive trends in north-western, western and eastern parts of the country were detected, while the negative trends were found in the central and northeastern parts. Daily precipitation, expressed as single daily intensity index (SDII), increased over time in northern and central Poland. In southern Poland, the variation of SDII index showed non-significant negative tendencies. Finally, the fraction of annual total precipitation due to the events exceeding the 1961-1990 95th percentile increased at one station only, namely, in Warsaw. The indicator which refers to dry conditions, i.e. maximum number of consecutive dry days (CDD) displayed negative trends throughout the surveyed area, with the exception of Szczecin that is a representative of north-western Poland.

  18. Plagioclase-wehrlites and peridotites on the East Pacific Rise (Hess Deep) and the Mid-Atlantic Ridge (DSDP Site 334): evidence for magma percolation in the oceanic upper mantle

    Science.gov (United States)

    Girardeau, Jacques; Francheteau, Jean

    1993-03-01

    Textural and petrological data are presented that record the formation of plagioclase-bearing wehrlites and peridotites at slow-spreading and fast-spreading ridges that are comparable to the wehrlites and peridotites formed in ophiolitic complexes. Evidence is provided for locally pervasive magma percolation in the oceanic residual upper mantle. The samples studied come from the East Pacific Rise (EPR) (Hess Deep) and the Mid-Atlantic Ridge (MAR) (DSDP Site 334). At both sites, parts of the peridotites display poikilitic textures with oikocrysts of clinopyroxene and interstitial plagioclase that include xenocrysts of strained and partly annealed olivine and subidiomorphic spinel crystals. Petrofabric data for olivine suggest a magmatic origin for the Hess Deep wehrlite. Its phase chemistry is comparable to intrusive plagioclase-wehrlites and lherzolite from ophiolites that are thought to have crystallized from a crystal mush. It differs drastically from the associated Hess Deep diopside-bearing harzburgites and dunites, which are quite similar to oceanic and ophiolitic residual peridotites. The EPR wehrlite is therefore considered as an intrusive rock. The Leg 37 plagioclase-peridotites display a weak lattice fabric of olivive which may have resulted from high-temperature plastic flow; these rocks have a phase chemistry that is typical of ophiolitic and oceanic residual rocks. These rocks are hence interpreted as residual dunite or harzburgite which has been pervasively impregnated by a melt from which the clinopyroxene and plagioclase crystallized. These peridotites could have an intrusive origin or may have formed in situ at the crust-mantle transition in association with intrusions of large gabbro bodies.

  19. Amphibians and agrochemicals: Dermal contact and pesticide uptake from irrigated croplands in SW Georgia

    Science.gov (United States)

    Background/Question/Methods Although isolated wetlands comprise a significant portion of amphibian breeding habitats throughout the United States, they are not protected under the Clean Water Act. In SW Georgia where agriculture is dominant within the landscape, many isolated ...

  20. Study on Invasion of Artesunate on Inhibiting Human Colon Cancer Cell SW620

    Directory of Open Access Journals (Sweden)

    Yu Fan

    2013-09-01

    Full Text Available Objective: To observe the invasive effect of Chinese extraction artesunate on human colon cancer cell SW620 and explore its possible mechanisms. Methods: Colon cancer cell SW620 was managed by different concentrations of artesunate, and soft agar colony-cultivating trial was applied to detect anchorage independent proliferation of cancer cells, Boyden chamber model method to detect the invasive capability of cancer cells and Western blot method to detect the change of intercellular adhesion molecule-1 (ICAM-1 proteins. Results: Artesunate can effectively inhibit malignant proliferation and invasive capability of colon cancer cell SW620, and was dose-dependent (P < 0.01. Artesunate can effectively inhibit the expression of cancer cell ICAM-1 gene proteins, and was time- and concentration-dependant (P <0.01. Conclusion: Artesunate can significantly inhibit the invasion of colon cancer cell SW620, which can be related to down-regulation of ICAM-1 protein level.

  1. Participative environmental management and social capital in Poland

    DEFF Research Database (Denmark)

    Hunka, Agnieszka; De Groot, Wouter T

    2011-01-01

    with a ubiquitous top-down approach taken by institutional decision-makers. The paper addresses this problem from the perspective of social capital theory. A study of administrative culture and decision-making processes shows the way decisions are currently made. We also propose a way to achieve more participative......Eastern European countries, such as Poland, are often used as exemplary in social capital studies. Upon entering the European Union, the low social capital level in Poland posed problems with implementing new regulations, particularly in the environmental policy field. Environmental issues often...... environmental management....

  2. An overview of occupational voice disorders in Poland

    Directory of Open Access Journals (Sweden)

    Ewa Niebudek-Bogusz

    2013-10-01

    Full Text Available Occupational voice disorders make the most frequently certified category of occupational diseases in Poland, making up approximately 20% of all cases. This study presents the current knowledge of the etiopathogenesis of occupational voice disorders. It stresses the importance of the evaluation of vocal loading by means of objective measurements. Furthermore, this study discusses the medico-legal aspects of the procedure of certifying occupational voice disorders in Poland. The paper also describes the preventive programs addressed particularly to teachers, including multidisciplinary and holistic management of occupational dysphonia. Their role in the improvement of occupational safety and health (OSH arrangement for vocally demanding professions is emphasized.

  3. [Dietary intake of dieldrin and aldrin in Poland].

    Science.gov (United States)

    Falandysz, J

    1999-01-01

    Dieldrin and aldrin exposure from a particular food items in Poland in 1970-1996 was calculated by multiplying its annualized mean consumption rates by residue concentration in the food. Estimated daily dietary intakes of dieldrin and aldrin were from 1.0 do 1.3 micrograms per person in 1970-1985 and from 0.50 do 0.58 microgram per person in 1990-1996, on the average. Fish and dairy products are a main source of dieldrin in a total diet in Poland.

  4. Reliability of Power Units in Poland and the World

    Directory of Open Access Journals (Sweden)

    Józef Paska

    2015-09-01

    Full Text Available One of a power system’s subsystems is the generation subsystem consisting of power units, the reliability of which to a large extent determines the reliability of the power system and electricity supply to consumers. This paper presents definitions of the basic indices of power unit reliability used in Poland and in the world. They are compared and analysed on the basis of data published by the Energy Market Agency (Poland, NERC (North American Electric Reliability Corporation – USA, and WEC (World Energy Council. Deficiencies and the lack of a unified national system for collecting and processing electric power equipment unavailability data are also indicated.

  5. Technical and Economic Aspects of Low Emission Reduction in Poland

    Science.gov (United States)

    Dzikuć, M.; Łasiński, K.

    2017-12-01

    The paper presents the problem of excessive air pollution in Poland caused mainly by low emission. The emission arises in result of heating flats by means of old and energetically inefficient heating installations. In Poland and Bulgaria the inhaled air is of the worst quality out of all EU countries. The paper presents economic and technical problems related to low emission occurring during the combustion of solid fuels in local boiler houses. Furthermore, the most significant economic issues, connected with the reduction of low emission are discussed, as well as technological possibilities of efficient reduction of the amount of pollution in the atmosphere. Conclusions are presented at the end of the article.

  6. First detection of bluetongue virus serotype 14 in Poland.

    Science.gov (United States)

    Orłowska, Anna; Trębas, Paweł; Smreczak, Marcin; Marzec, Anna; Żmudziński, Jan F

    2016-07-01

    Here, we present the first detected cases of bluetongue virus (BTV) in native cattle from Poland. The virus was found in animals located near the Polish-Belarusian and Polish-Lithuanian borders. The positive animals were detected through an official epidemiological surveillance program. A combination of type-specific real-time RT-PCR and phylogenetic tests revealed the presence of BTV serotype 14 (BTV-14). This serotype is highly homologous to the vaccine strain and BTV-14 present in Russia, Lithuania, and Spain (from an animal imported from Lithuania). The most probable route of virus introduction to Poland was transmission through midges. All of the cases were subclinical.

  7. Challenges of coal conversion for decarbonized energy in Poland

    Energy Technology Data Exchange (ETDEWEB)

    Sciazko, Marek; Jalosinski, Krzysztof; Majchrzak, Henryk; Michalski, Mieczyslaw; Tymowski, Henryk; Witos, Tadeusz; Wroblewska, Elzbieta

    2010-09-15

    Carbon dioxide is considered to be the main challenge for the coal-based power generation as well as for any other industrial application of coal. Poland's energy sector is primarily based on coal combustion that covers almost 90% of demand. Future development of that sector depends on the restriction on value of carbon dioxide emission or trading allowances. There are two main technological approaches to development of new coal based generation capacity, namely: gasification and pre-combustion capture; supercritical combustion and post-combustion capture. The current situation in development of three this type projects in Poland is presented.

  8. Dosimetric properties of a Solid Water High Equivalency (SW557) phantom for megavoltage photon beams.

    Science.gov (United States)

    Araki, Fujio

    2017-07-01

    The dosimetric properties of the recently developed SW557 phantom have been investigated by comparison with those of the existing SW457 phantom in megavoltage photon beams. The electron fluence ratio φplw, and chamber ionization ratio kpl, of water to SW457 and water to SW557 for 4-15MV photons were calculated as a function of depth using Monte Carlo simulations, and compared with measured values. Values of φplw for SW457 were in the range of 1.004-1.014 for 4MV, and 1.014-1.018 for 15MV photons. The φplw for SW557 ranged from 1.005 to 1.008 for 4MV and from 1.010 to 1.015 for 15MV photons and the variation of φplw with depth for each beam energy was within ±0.5%. Values of kpl were obtained with a PTW 30013 Farmer-type ionization chamber. The kpl for SW457 ranged from 0.997 to 1.011 for 4-15MV photons. Values of kpl for SW557 were almost unity for 4 and 6MV photons, while in the case of 10 and 15MV photons they were less than 1.006, excepting the build-up region. The measured and calculated kpl values of water to SW557 were in the range of 0.997-1.002 and 1.000-1.006, respectively, for 4-15MV photons, at a depth of 10cm with a source-to-axis distance of 100cm. The measured and calculated kpl values were in agreement within their uncertainty ranges. As a water-equivalent phantom, SW557 can be used with a dosimetric difference within±0.6%, for 4-15MV photons, and is more water-equivalent than SW457 in megavoltage photon beams. Copyright © 2017 Associazione Italiana di Fisica Medica. Published by Elsevier Ltd. All rights reserved.

  9. Sea urchins, their predators and prey in SW Portugal

    Directory of Open Access Journals (Sweden)

    Nuno Mamede

    2014-06-01

    Full Text Available Sea urchins play a key role structuring benthic communities of rocky shores through an intense herbivory. The most abundant sea urchin species on shallow rocky subtidal habitats of the SW coast of Portugal is Paracentrotus lividus (Echinodermata: Echinoidea. It is considered a key species in various locations throughout its geographical distribution by affecting the structure of macroalgae communities and may cause the abrupt transformation of habitats dominated by foliose algae to habitats dominated by encrusting algae - the urchin barrens. The removal of P. lividus predators by recreational and commercial fishing is considered a major cause of this phenomenon by affecting the trophic relationships between predators, sea urchins and algae communities. Marine protected areas (MPAs usually lead to the recovery of important predator species that control sea urchin populations and restore habitats dominated by foliose macroalgae. Therefore, MPAs provide a good opportunity to test cascading effects and indirect impacts of fishing at the ecosystem level. The ecological role of P. lividus was studied on rocky subtidal habitats of the SW coast of Portugal (Alentejo considering three trophic levels: population of P. lividus, their predators (fish and shellfish and their prey (macroalgae communities. Several studies were conducted: (1 a non-destructive observational study on the abundance and distribution patterns of P. lividus, their predators and preys, comparing areas with different protection; (2 a manipulative in situ study with cages to assess the role of P. lividus as an herbivore and the influence of predation; (3 a descriptive study of P. lividus predators based on underwater filming; (4 and a study of human perception on these trophic relationships and other issues on sea urchin ecology and fishery, based on surveys made to fishermen and divers. Subtidal studies were performed with SCUBA diving at 3-12 m deep. Results indicate that in the

  10. Tamarugite from Diana Cave (SW Romania) -first true karst occurrence

    Science.gov (United States)

    Pušcaš, C. M.; Onac, B. P.; Effenberger, H. S.; Povarǎ, I.

    2012-04-01

    Diana Cave is located within the town limits of Baile Herculane (SW Romania) and develops as a 14 m long, westward oriented, unique passage guided by the Diana fault [1]. At the far end of the cave, the thermo-mineral Diana Spring wells forth. In the early 1970s a mine gallery that intersected the cave was created to drain the water into a pumping station and the original cave passage was somewhat altered and reinforced with concrete. Today the concrete and the silty limestone cave walls are heavily corroded by H2SO4 outgassing from the hot water (ca. 50°C) and display abundant gypsum crusts, soggy aggregates of native S, and a variety of more exotic sulfates. Among them, a mineral that has been previously identified in caves only in connection to volcanic activity, either as thermal springs or fumaroles [2]: tamarugite [NaAl(SO4)26H2O]. It was [3] that first mentioned the occurrence of this Na and Al sulfate in Diana Cave, our research aiming to give a detailed description of this mineral, its paragenesis, and mechanisms of precipitation. Recently, tamarugite has also been identified in a sulfuric acid cave from Greece [4]. Along with powder X-ray diffractions coupled with Rietveld refinement, scanning electron microscope, and electron probe micro-analysis, δ18O and δ34S compositions of the sulfate mineral as well as precipitates from the water were analyzed to identify and better constrain the genesis of this rare sulfate. Regrettably, the crystal size of our specimens is inappropriate for identification by means of single crystal X-ray diffraction. Physical and chemical parameters of Diana Spring were as well measured on several occasions. Geochemical analysis suggests that the minute, white tamarugite flakes precipitated in Diana Cave as a result of the interactions between the thermo-mineral water or water vapor and the original limestone bedrock and concrete that blankets the mine gallery. [1] Povara, I., Diaconu, G., Goran, C. (1972). Observations pr

  11. Microseismicity and active deformation of Messinia, SW Greece

    Science.gov (United States)

    Papoulia, J.; Makris, J.

    By deploying a 30 3-component digital seismic array in the Messiniakos gulf and the surrounding region, we recorded for a period of 45 days the microseismic activity. With a minimum of six records per event, we located 1121 earthquakes corresponding to an average of 20 events per day. For the hypocenter location we used a local velocity model adopted to two controlled source seismic experiments. Within the array, traveltime residuals were within ± 0.2 s and the epicentral accuracy in the order of ± 2 km, while the hypocentral one is twice this value. Correlation of the seismicity with the tectonic elements indicated that most of the NW-SE oriented faults are active with strike-slip movement along this orientation and extension perpendicular to it. The neogene basins of Messini, Meligalas and Megalopolis are seismically very active and their eastern flanks are delineated by higher seismic activity than their western ones. This indicates that the basins are asymmetric with master faults defining their eastern-northeastern flanks. This hypothesis is supported by the asymmetric structure mapped at the offshore Messiniakos basin as densely spaced high resolution reflection seismic profiles have revealed. The western margins of the basins are less deformed and the seismic activity is dispersed over several minor NW-SE faults. Since the NW-SE striking faults onshore are truncated by major NE-SW oriented ones, their overall length is shortened, reducing their seismic potential and capacity to store large stresses that could produce events above Ms6.1. Offshore western Messinia, in the Ionian Sea, the size and activity of the faults is significantly larger and prone to develop events of larger magnitudes. Subcrustal seismicity indicates a deepening of the foci to the east-northeast.

  12. Preliminary Results of EEWS Parameters for SW Iberia

    Science.gov (United States)

    Carranza, Marta; Buforn, Elisa; Pro, Carmen; Zollo, Aldo; Pazos, Antonio; Lozano, Lucia; Carrilho, Fernando

    2013-04-01

    SW Iberia is an area where potential large and damaging earthquakes may occur such as the 1755 (Lisbon Imax=X), 1969 (S. Vicente Cape Ms=8,1) or 1964 (Gulf of Cádiz Ms=6.5) shocks. We have estimated the peak displacement (Pd) and mean period (τc) for a rapid estimation of the potential damage for earthquakes occurring in this region (ALERT-ES project), from the first seconds of the beginning of P-waves. This estimation is carried out by the correlation of these parameters with the magnitude and the peak ground velocity (PGV) of recorded shocks. The database is formed by earthquakes with epicentres at S. Vicente Cape and Gulf of Cadiz regions, occurred on the period 2006-2011 with magnitude larger than 3.8 and recorded at regional distances (less than 500 km) at real time broad-band seismic stations. We have studied different lengths of time-windows (2 to 20s) and applied different filters. Due to the off-shore foci occurrence and the bad azimuthal coverage, we have corrected the Pd parameter by the radiation pattern obtained from focal mechanisms of the largest earthquakes of this region. We have normalized the Pd value to a reference distance (200 km) and after that we have obtained empirical correlation laws for Pd and τc versus magnitude. We have also obtained an empirical correlation between Pd parameter and the PGV estimated over the total seismogram. The PGV could be correlated to the earthquakes damages through the Modified Mercalli Intensity (IMM). Applying the scaling laws obtained (Pd and PGV), we have estimated the theoretical intensity maps for the 2007 and 2009 earthquakes occurred in this area.

  13. Enrichment ratios of elements in selected plant species from black coal mine dumps in Lower Silesia (Poland)

    Energy Technology Data Exchange (ETDEWEB)

    Samecka-Cymerman, A.; Kempers, A.J. [University of Wroclaw, Wroclaw (Poland)

    2003-07-01

    Concentration of the metals Al, Ba, Cd, Co, Cr, Cu, Mn, Ni, Pb, Sr, Zn and V as well as N, P, K, Ca, Mg, Fe and S were measured in soils and in two tree species (leaves of Betula pendula and Salix caprea) and two herbs (whole above-ground parts of Solidago canadensis and Tanacetum vulgare) sampled from dumps in the Walbrzych coal mine area (Lower Silesia, SW Poland). These plants, as used to evaluate the distribution of elements in the examined dumps, contained elevated levels of Cd, Co, Cu, Mn, Ni, Pb and Zn. Especially the highest levels of Mn in Betula pendula seriously exceed background values. Betula pendula characterized also the highest enrichment ratio for Mn, Salix caprea for Ni and Sr and Tanacetum vulgare for Cu. Test-t indicated that from both herbs Tanace-tum vulgare accumulated much more K, N, S and Zn than Solidago canadensis and of both trees Salix caprea accumulated significantly more Cd, Cu, K and Ca than Betula pendula, while this last species accumulated significantly more Fe and Mn than Salix caprea. A post hoc LSD test indicated that all examined plants had similar enrichment ratios for Al, Pb and V.

  14. Road Infrastructure Safety Management in Poland

    Science.gov (United States)

    Budzynski, Marcin; Jamroz, Kazimierz; Kustra, Wojciech; Michalski, Lech; Gaca, Stanislaw

    2017-10-01

    The objective of road safety infrastructure management is to ensure that when roads are planned, designed, built and used road risks can be identified, assessed and mitigated. Road transport safety is significantly less developed than that of rail, water and air transport. The average individual risk of being a fatality in relation to the distance covered is thirty times higher in road transport that in the other modes. This is mainly because the different modes have a different approach to safety management and to the use of risk management methods and tools. In recent years Poland has had one of the European Union’s highest road death numbers. In 2016 there were 3026 fatalities on Polish roads with 40,766 injuries. Protecting road users from the risk of injury and death should be given top priority. While Poland’s national and regional road safety programmes address this problem and are instrumental in systematically reducing the number of casualties, the effects are far from the expectations. Modern approaches to safety focus on three integrated elements: infrastructure measures, safety management and safety culture. Due to its complexity, the process of road safety management requires modern tools to help with identifying road user risks, assess and evaluate the safety of road infrastructure and select effective measures to improve road safety. One possible tool for tackling this problem is the risk-based method for road infrastructure safety management. European Union Directive 2008/96/EC regulates and proposes a list of tools for managing road infrastructure safety. Road safety tools look at two criteria: the life cycle of a road structure and the process of risk management. Risk can be minimized through the application of the proposed interventions during design process as reasonable. The proposed methods of risk management bring together two stages: risk assessment and risk response occurring within the analyzed road structure (road network, road

  15. First patient with hereditary spastic paraplegia type 8 in Poland.

    Science.gov (United States)

    Bogucki, Piotr; Sobczyńska-Tomaszewska, Agnieszka

    2017-09-01

    SPG 8 is an autosomal dominant HSP, which phenotype results from KIAA0196 gene mutations. There have been twelve types of KIAA0196 mutations described in HGMD, which are located in conservative region of gene encoding strumpellin. We describe first patient in Poland, simultaneously second in the world with KIAA0196 mutation - p.V620A.

  16. First patient with hereditary spastic paraplegia type 8 in Poland

    OpenAIRE

    Bogucki, Piotr; Sobczy?ska?Tomaszewska, Agnieszka

    2017-01-01

    Key Clinical Message SPG 8 is an autosomal dominant HSP, which phenotype results from KIAA0196 gene mutations. There have been twelve types of KIAA0196 mutations described in HGMD, which are located in conservative region of gene encoding strumpellin. We describe first patient in Poland, simultaneously second in the world with KIAA0196 mutation ? p.V620A.

  17. Facilities of Early Rehabilitation after Stroke in Poland 2010

    Science.gov (United States)

    Opara, Jozef A.; Langhorne, Peter; Larsen, Torben; Mehlich, Krzysztof; Szczygiel, Jaroslaw

    2012-01-01

    The aim of this work was to survey the contemporary facilities for early post-stroke rehabilitation in Poland. The main research questions were as follows: what is the availability of inpatient rehabilitation for post-stroke patients in neurological departments and in rehabilitation departments? The growing costs of healthcare are encouraging…

  18. Was Mendelian genetics taught during the Lysenkoist period in Poland?

    OpenAIRE

    Köhler, Piotr

    2014-01-01

    The content of Polish textbooks of botany, zoology and rudiments of evolutionism of Lysenkoist times was analysed, along with a methodological manual for biology and a set of guidelines. On this basis, and taking into account the memories of eyewitnesses, it can be stated that Mendelian genetics was not taught in schools in Poland during the Lysenkoist period.

  19. The environmental energy sector programme. Poland: Appendices to feasibility study

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1998-07-01

    The appendices contain Energy Law, Act of 10 April 1997 and also more specific details from the feasibility study for the procurement of a financial solution to the modernisation of the combined heat and power plant in the city of Zielona Gora, Poland. (EHS)

  20. Educational Challenges to Poland at the Time of Transition.

    Science.gov (United States)

    Adamski, Wladyslaw

    1994-01-01

    Describes the educational challenges facing Poland as it makes the transition from state socialism to a free market economy. Reviews probable changes to the country's agricultural workers, working class, intelligentsia, and the newly self-employed. Discusses the decline of the value of education beginning in the 1980s and the implications for…

  1. POLAND' SYNDROME: An Incidental findings on routine medical ...

    African Journals Online (AJOL)

    Dr Hamidu

    muscular anomalies of the ipsilateral chest wall. Recognised complications ... and no family history of congenital anomalies. Physical examination ... Table 1. Summary of frequency and types of abnormalities on record in 55 cases of Poland's syndrome. J.W. Mace. Abnormalities. Incidence. Incidence( %). Absent Pectoralis ...

  2. Equity Block Transfers in Transition Economies : Evidence from Poland

    NARCIS (Netherlands)

    Trojanowski, G.

    2002-01-01

    This Paper investigates valuation effects of share block transfers and employs agency theory to explain the determinants of block premia. A sample of transactions from Poland is used to measure benefits and costs of ownership concentration. Block premia are found to be substantially lower than in

  3. Experiences of cancer patients in Poland throughout diagnosis and treatment.

    Science.gov (United States)

    Godlewski, D; Adamczak, M; Wojtyś, P

    2017-03-01

    Previous studies have failed to explain why the mortality rate of cancer patients is higher in Poland than other countries in the European Union. We aimed to evaluate the health care system in Poland during the diagnosis and treatment of cancer. In this multicentre study, 125 cancer patients treated at 15 centres across Poland participated in focus group interviews in 2014. We identified and assessed crucial elements that affect a patients' experience from the early onset of symptoms, through to diagnosis and treatment. We found that the majority of patients were dissatisfied with the length of time taken to diagnose cancer. Throughout diagnosis, treatment and follow-up, patients reported a lack of communication from health care professionals. While dealings with oncologists and medical staff were viewed favourably, patients felt the cancer centres were not well organised. Patients recommended that having one doctor in charge of an individual's treatment and follow-up would improve patient care and well-being. A late cancer diagnosis may be contributing to the high mortality rate observed in Poland. In the future, new policies should be developed to reduce the time to cancer diagnosis, increase communication with health care professionals and improve the organisation of cancer care for patients. © 2016 John Wiley & Sons Ltd.

  4. Epichloë clarkii - a new graminicolous species for Poland

    Directory of Open Access Journals (Sweden)

    Andrzej Chlebicki

    2014-08-01

    Full Text Available Epichloë clarkii White, described in 1993 from England has been noted from Wielkopolski National Park in Poland. The eggs and feed marks of hyperparasitic fly, Botanophila sp. have been found on teleomorph stromata of E. clarkii.

  5. The Reform of the Inservice Teacher Education System in Poland.

    Science.gov (United States)

    Zawadoska, Janina

    1995-01-01

    Poland is in the midst of sweeping educational reform, including reform of inservice teacher education. The system is abandoning totalitarianism for democracy. Most Polish teachers are specialized in only one subject, and there are surpluses of teachers in some subjects, so inservice education is focusing on helping teachers change specialties.…

  6. A new record of Linaria genistifolia (Plantaginaceae in Poland

    Directory of Open Access Journals (Sweden)

    Pliszko Artur

    2017-11-01

    Full Text Available In this paper, a new Polish record of Linaria genistifolia is presented. It was found on 27 August 2017 in Zabrze, Silesia Province, growing at the foot of the reclaimed slag heap. The updated map of its distribution in Poland is provided using the ATPOL cartogram method.

  7. Organic food consumption in Poland: Motives and barriers.

    Science.gov (United States)

    Bryła, Paweł

    2016-10-01

    This paper aims to investigate selected aspects of organic food consumption in Poland. We conducted a survey in a representative sample of 1000 consumers. Polish consumers are convinced that organic food is more expensive, healthier, more environmentally friendly, more tasty and more authentic than conventional food. They believe its arouses more trust, has a better quality, is subject to more strict controls, and is produced in a more traditional way. According to Polish consumers, the most important characteristics of organic food are healthiness and high quality. The perceived authenticity of organic food depends on its natural taste, product quality, labelling, in particular having a European quality sign, as well as the retailer type and a separate exposition place in the points of purchase (merchandising). The critical barrier to the development of the organic food market in Poland is the high price, followed by an insufficient consumer awareness, low availability of organic products, short expiry dates and low visibility in the shop. The principal motives of organic food selection in Poland include: healthiness, ecological character of the product, food safety considerations, superior taste, and quality assurance. We identified the motives for and barriers to organic food consumption in Poland. Copyright © 2016 Elsevier Ltd. All rights reserved.

  8. The first locality of Chalciporus rubinus (Boletales, Basidiomycota in Poland

    Directory of Open Access Journals (Sweden)

    Marek Halma

    2013-12-01

    Full Text Available Chalciporus rubinus (W.G. Sm. Singer, described in 1868 from England, was found in a city park in Wrocław. This is the first record of the species from Poland. Macro- and micromorphological characters of the Polish specimens are described and illustrated. The delimitation of Ch. rubinus, the knowledge of its distribution, ecology and conservation status is summarised.

  9. Mniaecia jungermanniae and Puttea margaritella (lichenized Ascomycota found in Poland

    Directory of Open Access Journals (Sweden)

    Paweł Czarnota

    2013-06-01

    Full Text Available Two hepaticolous fungi, Mniaecia jungermanniae and Puttea margaritella rarely recorded in Europe have recently been found in Polish Western Carpathians. Both species are also reported here for the first time from Poland. Notes on their taxonomy, ecology and distribution are provided.

  10. Absconditella fossarum and A. sphagnorum (Lichenes, Stictidaceae in NW Poland

    Directory of Open Access Journals (Sweden)

    Mirosława Ceynowa-Giełdon

    2014-08-01

    Full Text Available The paper presents Absconditella fossarum, a species new to Poland, found on sands in the Noteć river valley and A. sphagnorum from the new stands found on peated shore of pure, forest lakes in the Tuchola Forest (Bory Tucholskie region.

  11. Gender Relations, Education and Social Change in Poland.

    Science.gov (United States)

    Watson, Peggy

    1992-01-01

    Discusses the following issues in Poland: formal gender equality during state Socialism; public provision of child care; the domestic division of labor; women's educational careers; women's labor market position; gender inequalities in social consciousness; separation between public and private domains; and transition from a society to civil…

  12. Reactive Energy Billing in Operator Tariffs in Poland

    OpenAIRE

    Paweł Bućko; Artur Wilczyński

    2015-01-01

    The paper describes the current method of reactive energy billing in the tariffs of distribution grid operators in Poland. The current solutions are subject to critical assessment. Issues related to the motivation effect of the current solutions on consumers are analysed. Problems that occur in relation with connecting distributed generators to the distribution grid and challenges related to prosumer billing are indicated.

  13. Educational Struggles and Citizenship Education. The Case of Poland

    Science.gov (United States)

    Popow, Monika; Sáez-Rosenkranz, Isidora

    2016-01-01

    The aim of the paper is to analyse the relation between educational struggles and citizenship education in contemporary Poland. It adopts the critical pedagogy perspective and broadly defines the concept of educational struggle as struggling over the content of education, as social tensions in the field of education, as well as the students' and…

  14. Stochastic forecast of the population of Poland, 2000-2050

    NARCIS (Netherlands)

    Matysiak, A.; Nowok, B.

    2007-01-01

    Forecasting the population of Poland is very challenging. Firstly, the country has been undergoing rapid demographic changes. In the 1990s, they were influenced by the political, economic, and social consequences of the collapse of the communist regime. Since 2004 they have been shaped by Poland’s

  15. Stochastic forecast of the population of Poland, 2005-2050

    Directory of Open Access Journals (Sweden)

    Beata Nowok

    2007-11-01

    Full Text Available Forecasting the population of Poland is very challenging. Firstly, the country has been undergoing rapid demographic changes. In the 1990s, they were influenced by the political, economic, and social consequences of the collapse of the communist regime. Since 2004 they have been shaped by Poland's entry into the European Union. Secondly, the availability of statistics for Poland on past trends is strongly limited. The resulting high uncertainty of future trends should be dealt with systematically, which is an essential part of the stochastic forecast presented in this paper. The forecast results show that the Polish population will constantly decline during the next decades and Poland will face significant ageing as indicated by a rising old-age dependency-ratio. There is a probability of 50 % that in 2050 the population will number between 27 and 35 millions compared to 38.2 in 2004 and that there will be at least 63 persons aged 65+ per 100 persons aged 19-64.

  16. Professional Training of Specialists in International Marketing in Poland

    Science.gov (United States)

    Zukowski, Wojciech

    2015-01-01

    Polish experience in training specialists in international marketing in the context of globalization and integration processes has been studied. A range of theoretical resources, namely Market Entry Strategy for Poland; the articles dedicated to international marketing and economy development (W. Grzegorczyk, M. Viachevskyi, M. Urbanetst); program…

  17. Entoloma albotomentosum (Agaricales, Basidiomycota, a species new to Poland

    Directory of Open Access Journals (Sweden)

    Marek Halama

    2013-12-01

    Full Text Available The first record of Entoloma albotomentosum Noordel. & Hauskn., a member of the subgenus Claudopus and section Claudopus, is reported from Poland. A full description and illustration of the species based on Polish specimens are given and its taxonomy, ecology, and general distribution are also provided.

  18. Armillaria ectypa, a rare fungus of mire in Poland

    Directory of Open Access Journals (Sweden)

    Małgorzata Stasińska

    2015-08-01

    Full Text Available Armillaria ectypa is a saprotroph that occurs on active raised bogs and alkaline fens, as well as Aapa mires and transitional bogs. It is a very rare and threatened Eurasian species and one of the 33 fungal species proposed for inclusion into the Bern Convention. Its distribution in Poland, ecological notes and morphology of basidiocarp based on Polish specimens are presented.

  19. Becoming a Mother in Hungary and Poland during State Socialism

    Directory of Open Access Journals (Sweden)

    2004-04-01

    Full Text Available In this paper, we study the transition to motherhood in the first co-residential union in the dual-earner context of state socialism, namely in Hungary and Poland between the late 1960s and the end of the 1980s. Our analyses are based on data extracted from the Polish and the Hungarian Fertility and Family Surveys of the early 1990s. We use the hazard regression method as our analytical tool. Our results for Hungary indicate that women's employment does not necessarily reduce the propensity to become a mother if the combination of labor-force participation and family life has been facilitated by policy measures. In Poland however, this was more difficult, and state support was somewhat less generous, thus part-time workers and housewives had substantially higher first-birth intensity than full-time employed women. Even so, we find indication for Poland, that as policy measures increasingly improved the conditions to combine employment and family responsibilities, the propensity to have the first child increased. The timing of first birth varied greatly across educational levels. Highly educated women were more likely to postpone the transition to motherhood, which in turn resulted in their overall lower propensity to have the first child in both countries, but less so in Hungary than in Poland.

  20. Overt and covert narcissism in Poland and the Netherlands

    NARCIS (Netherlands)

    Zondag, H.J.; Halen, C.P.M. van; Wojtkowiak, J.

    2009-01-01

    This article reports a study of the relation between narcissism as a personality characteristic and the cultural dimension of individualism/collectivism. Participants from a more collectivistic society (Poland; n = 167) were compared with participants from a more individualistic society (The

  1. The State of Development of Digital Libraries in Poland

    Science.gov (United States)

    Gorny, Miroslaw; Catlow, John; Lewandowski, Rafal

    2010-01-01

    Purpose: The purpose of this paper is to describe the state of development of Polish digital libraries. Design/methodology/approach: The paper describes the establishment of the first digital library in Poland, the creation of the Wielkopolska Digital Library and other regional digital libraries. The organisational and technological solutions used…

  2. NATO Enlargement: Strategic Impact on Poland’s Security

    Science.gov (United States)

    2004-01-01

    Byelorussia, another Soviet successor, were less than encouraging. The leaders of Byelorussia’s independence movement viewed Poland with suspicion as a...Rukh” independence movement , fearing that, even if at present claims were no more than a minor annoyance, they might become a source of constant

  3. Adult Education in Poland before and after "Solidarity."

    Science.gov (United States)

    Bron-Wojciechowska, Agnieszka

    1982-01-01

    The author provides a historical approach to understanding the political, economic, and cultural motives that shaped adult education's philosophy in Poland. Analysis of the pre and post "Solidarity" movement is provided to demonstrate the role of adult education in an ongoing process of learning democratic principles. (SSH)

  4. Poland's Syndrome: A case report | Gashegu | East and Central ...

    African Journals Online (AJOL)

    Poland's Syndrome is a rare congenital condition. It is classically characterized by absence of unilateral chest wall muscles and sometimes ipsilateral symbrachydactyly (abnormally short and webbed fingers). The condition typically presents with unilateral absence of the sternal or breastbone portion of the pectoralis major ...

  5. The distribution of Montia fontana L. (Portulacaceae in Poland

    Directory of Open Access Journals (Sweden)

    Zofia Sotek

    2011-01-01

    Full Text Available The distribution of Montia fontana L. in Poland is described, based on accessible data. Maps showing the distribution of M. fontana agg., subsp. amporitana, subsp. chondrosperma are presented, as well as lists of localities with brief descriptions of taxonomic characteristics of the subspecies and their habitats.

  6. INVASIVE ALIEN PLANTS ON DECAYING WOOD AND ON TREE-FALL DISTURBANCES IN FORESTS IN THE KARKONOSZE MTS (SUDETEN, SW POLAND

    Directory of Open Access Journals (Sweden)

    Monika Staniaszek-Kik

    2014-10-01

    Full Text Available Three invasive anthropophytes, i.e. two vascular plants Digitalis purpurea L. and Impatiens parviflora DC. as well as one moss Orthodontium lineare Schwägr, were recorded on decaying wood and tree-fall disturbances (pit-mound-root plate complex. It contributes only 1.9% to the flora of analyzed habitats (1.1% of moss flora, 2.9% of vascular plant flora and 3.5% of neophytes known in Sudeten Mts. They grew, sporadically and with a low frequency, on 3.5% of studied objects (on 3.1% of decaying logs and stumps and 5.6% of tree-fall disturbances in all types of forest communities in the area of Karkonosze National Park and in the vicinity. Nowadays, invasive neophytes do not pose a threat to diversity of endangered epixylic flora. Described habitats seem to be resistant to penetration by anthropophytes.

  7. First radon measurements and occupational exposure assessments in underground geodynamic laboratory the Polish Academy of Sciences Space Research Centre in Książ Castle (SW Poland).

    Science.gov (United States)

    Fijałkowska-Lichwa, Lidia; Przylibski, Tadeusz A

    2016-12-01

    The article presents the results of the first radon activity concentration measurements conducted continuously between 17th May 2014 and 16th May 2015 in the underground geodynamic laboratory of the Polish Academy of Sciences Space Research Centre in Książ. The data were registered with the use of three Polish semiconductor SRDN-3 detectors located the closest (SRDN-3 No. 6) to and the furthest (SRDN-3 No. 3) from the facility entrance, and in the fault zone (SRDN-3 No. 4). The study was conducted to characterize the radon behaviour and check it possibility to use with reference to long- and short-term variations of radon activity concentration observed in sedimentary rocks strongly fractured and intersected by systems of multiple faults, for integrated comparative assessments of changes in local orogen kinetics. The values of radon activity concentration in the underground geodynamic laboratory of the Polish Academy of Sciences (PAN) Space Research Centre in Książ undergo changes of a distinctly seasonal character. The highest values of radon activity concentration are recorded from late spring (May/June) to early autumn (October), and the lowest - from November to April. Radon activity concentrations varied depending on the location of measurement points. Between late spring and autumn they ranged from 800 Bq·m-3 to 1200 Bq·m-3, and even 3200 Bq·m-3 in the fault zone. Between November and April, values of radon activity concentration are lower, ranging from 500 Bq·m-3 to 1000 Bq·m-3 and 2700 Bq·m-3 in the fault zone. The values of radon activity concentration recorded in the studied facility did not undergo short-term changes in either the whole annual measuring cycle or any of its months. Effective doses received by people staying in the underground laboratory range from 0.001 mSv/h to 0.012 mSv/h. The mean annual effective dose, depending on the measurement site, equals 1 or is slightly higher than 10 mSv/year, while the maximum dose exceeds 20 mSv/year. The estimated annual effective doses are comparable to the standard value of 20 mSv/year defined by Polish law for people employed in the conditions of radiation exposure. They are also in the range of annual effective dose value (8 mSv/year) recommended in workplaces by International Commission on Radiation Protection. Copyright © 2016 Elsevier Ltd. All rights reserved.

  8. Plants' healthiness assessment as part of the environmental monitoring of protected mountainous area in the example of Karkonosze (Giant) Mts. (SW Poland).

    Science.gov (United States)

    Pusz, Wojciech

    2015-10-01

    The aim of phytopathological monitoring is to check the healthiness of plants and observe the changes that occur in their populations. In the vast majority, these types of observations are conducted in agriculture and forestry. An interesting aspect of phytopathological monitoring is the assessment of the origin of the plant species. The research of fungal communities (including pathogens) in plants may, for example, indicate the relic nature of the plant species. Reduction of the occurrence or disappearance of fungi species associated with its host plant can evidence slow decline of their habitats. This applies mainly to arctic-alpine fungal species. On the other hand, for some plant hosts, colonization of their organs by polyphagous fungi is being recorded. One such example is the downy willow, on which six species of fungi were found in the Karkonosze Mts. In 2014, there were no fungi found on this plant. However, comparing the species composition of fungi associated with downy willow given by Schroeter (1908) to the contemporary one and to the study results of other researchers, a decrease in the number of fungi species is clearly visible. This may be related to the environmental pollution, which took place in the Sudetes in the second half of the twentieth century. For instance, the species of the genus Rhytisma colonize the leaves of trees and shrubs and are particularly sensitive to the concentration of SO2 in the air, but nobody has looked for this fungus on this host in the past. Yet, presently, we were able to find Rhytisma fungus in Karkonosze Mts. Phytopathological monitoring was conducted in the years of 2014-2015 in the sub-alpine zone of the Karkonosze (Giant) Mts. It has been shown that, compared to similar studies conducted in the 1990s of the twentieth century, the species composition of fungi infesting Rubus chamaemorus and Betula carpactica has changed. Is this the beginning of changes that will occur in populations of plants?

  9. Local energy policies in Poland and the Czech Republic

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    2001-07-01

    Both the Czech Republic and Poland as former Communist countries, are transforming their economies from central planning to a free market. This applies equally to energy planning and because they are starting from the same point, they have come up with very comparable solutions despite strong cultural differences, so that the parallels are striking. This study analyzes the energy management in local authorities in Poland and the Czech Republic with the objective of better: identifying the current situation, identifying the opportunities for action both now and in an extended European Union, identifying the constraints that may hinder full integration of East European municipalities in European Union programmes, improve the integration of municipalities in the countries concerned in pan-European networks of municipalities interested in energy issues. The study reviews the powers and responsibilities of local authorities in the energy field and the institutional framework within which local authorities work. There are now 16 directly elected regional authorities in Poland and the local authorities have been restructured into two levels, the Powiad and the Gmina. Similarly, in the Czech Republic 14 elected regional authorities have been established. This document brings together 2 reports: the final report and the study report about the energy policies in Poland and in the Czech republic: structure of local government, general and institutional aspects, national political organisation, national administrative organisation, municipal role in production and distribution, regulation and planning, energy issues, energy management policies, specific aspects at local level etc... The conclusions from two review seminars (Jablonec nad Nison (Czech republic), 25-26 January 2001, and Bielsko Biala (Poland), 22-23 February 2001) and some fact files on 4 large Czech towns and 4 large Polish towns complete the study. (J.S.)

  10. Genesis of Ultra-High Pressure Garnet Pyroxenite in Orogenic Peridotites and its bearing on the Isotopic Chemical Heterogeneity in the Mantle Source of Oceanic Basalts

    Science.gov (United States)

    Varas Reus, María Isabel; Garrido, Carlos J.; Marchesi, Claudio; Bosch, Delphine; Hidas, Károly

    2017-04-01

    The genesis of ultra-high pressure (UHP) garnet pyroxenites in orogenic peridotite massifs and its implications on the formation of chemical heterogeneities in the mantle and on basalt petrogenesis are still not fully understood. Some UHP (diamond-bearing) garnet pyroxenites have isotopic, and major and trace element compositions similar to the recycled oceanic crustal component observed in oceanic basalts [1-6]. These pyroxenites hence provide an exceptional opportunity to investigate in situ the nature and scale of the Earth's mantle chemical heterogeneities. Here, we present an integrated geochemical study of UHP garnet pyroxenites from the Ronda (Betic Belt, S. Spain) and Beni Bousera (Rif Belt, N. Morocco) peridotite massifs. This investigation encompasses, in the same sample, bulk rock major and trace elements, as well as Sr-Nd-Pb-Hf isotopic analyses. According to their Al2O3 content, we classify UHP garnet pyroxenites into three groups that have distinct trace elements and Sr-Nd-Pb-Hf isotopic signatures. Group A pyroxenites (Al2O3: 15 - 17.5 wt. %) are characterized by low initial 87Sr/86Sr, relatively high 143Nd/144Nd, 206Pb/204Pb and 176Hf/177Hf ratios, and highly variable 207Pb/204Pb and 208Pb/204Pb ratios. Group B pyroxenites (Al2O3 element, and isotopic compositions of the studied Ronda and Beni Bousera UHP garnet pyroxenites lend support to the "Marble Cake Mantle" model [7] for the genesis of these pyroxenites. This model envisions the mantle source of oceanic basalts as a mélange of subducted, ancient oceanic crust —-represented by garnet pyroxenites in orogenic peridotites—- intimately mixed with peridotites by mantle convection. The present study reveals, however, that besides this exotic component of ancient recycled oceanic crust, the genesis of these pyroxenites requires a previously unnoticed component of recycled lower continental crust akin to the lower crustal section of the lithosphere where these UHP garnet pyroxenites now reside in

  11. Late Permian basalts in the Yanghe area, eastern Sichuan Province, SW China: Implications for the geodynamics of the Emeishan flood basalt province and Permian global mass extinction

    Science.gov (United States)

    Li, Hongbo; Zhang, Zhaochong; Santosh, M.; Lü, Linsu; Han, Liu; Liu, Wei

    2017-02-01

    We report the finding of a ∼20 m thick sequence of massive pyroxene-plagioclase-phyric basalt lava flows in the Yanghe area of the northeastern Sichuan Basin, within the Yangtze craton of SW China, which were previously considered to be located outside the Emeishan flood basalt province. This basaltic sequence above the middle Permian Maokou Formation (Fm.) is overlain by the late Permian Longtan Fm. Thus, the Yanghe basalts should be stratigraphically correlated with the Emeishan flood basalts. The Yanghe basalts show typical oceanic island basalt (OIB) affinity, and geochemically resemble Emeishan basalts, especially in the case of high-Ti (HT) basalts from the eastern domain of the Emeishan flood basalt province. The rocks have low age-corrected (87Sr/86Sr)t (t = 260 Ma) ratios (0.704158-0.704929) and Pb isotopic ratios [206Pb/204Pb(t) (18.264-18.524), 207Pb/204Pb(t) (15.543-15.58), and 208Pb/204Pb(t) (38.147-38.519)], and positive εNd(t) values (+3.15 to +3.61), suggesting that the lavas have not undergone any significant crustal contamination. The crystallization temperature of clinopyroxene is estimated to be 1368-1420 °C, suggesting anomalously thermal inputs from a mantle source and a possible plume-head origin. The fractionation of middle rare earth elements (MREE) to heavy REE (HREE) suggests that these rocks were produced by small degrees of partial melting of mantle peridotite within the garnet-spinel transition region. The stratigraphic relationships and similar geochemical signatures with the Emeishan flood basalts suggest that the Yanghe basalts are part of the Emeishan flood basalt province and can be considered as the northeastern limit of the Emeishan flood basalt province. Our finding extends the diameter of the Emeishan flood basalt province to ∼1200-1400 km, covering an area of up to ∼7 × 105 km2, two times more than previously estimated. The larger areal extent and giant eruption volume, incorporating the Sichuan Basin, lend support

  12. Depletion, cryptic metasomatism, and modal metasomatism of central European lithospheric mantle: evidence from elemental and Li isotope compositions of spinel peridotite xenoliths, Kozákov volcano, Czech Republic

    Czech Academy of Sciences Publication Activity Database

    Medaris Jr., L. G.; Ackerman, Lukáš; Jelínek, E.; Magna, T.

    2015-01-01

    Roč. 104, č. 8 (2015), s. 1925-1956 ISSN 1437-3254 Institutional support: RVO:67985831 Keywords : Central European lithospheric mantle * geochemistry * geothermometry * Li isotopes * spinel peridotite xenoliths Subject RIV: DD - Geochemistry Impact factor: 2.133, year: 2015

  13. Metasomatism along fluid pathways in the ultra-high pressure Svartberget garnet-peridotite (Western Gneiss Region, Norway): Implications for the transport of slab-derived fluids within the mantle wedge

    NARCIS (Netherlands)

    Vrijmoed, J.C.; Austrheim, H.; John, T.; Hin, R.C.; Corfu, F.; Davies, G.R.

    2013-01-01

    Garnet-peridotites often contain veins or layers of pyroxenite and eclogite of uncertain origin. We investigate the Svartberget garnetperidotite from the northernmost ultrahigh-pressure domain in the Western Gneiss Region (WGR) in Norway and show that the observed layering represents a sequence of

  14. Study of morphological and mechanical features of multinuclear and mononuclear SW480 cells by atomic force microscopy.

    Science.gov (United States)

    Liu, Jinyun; Qu, Yingmin; Wang, Guoliang; Wang, Xinyue; Zhang, Wenxiao; Li, Jingmei; Wang, Zuobin; Li, Dayou; Jiang, Jinlan

    2017-10-09

    This article studies the morphological and mechanical features of multinuclear and mononuclear SW480 colon cancer cells by atomic force microscopy to understand their drug-resistance. The SW480 cells were incubated with the fullerenol concentrations of 1 mg/ml and 2 mg/ml. Morphological and mechanical features including the height, length, width, roughness, adhesion force and Young's modulus of three multinuclear cell groups and three mononuclear cell groups were imaged and analyzed. It was observed that the features of multinuclear cancer cells and mononuclear cancer cells were significantly different after the treatment with fullerenol. The experiment results indicated that the mononuclear SW480 cells were more sensitive to fullerenol than the multinuclear SW480 cells, and the multinuclear SW480 cells exhibited a stronger drug-resistance than the mononuclear SW480 cells. This work provides a guideline for the treatments of multinuclear and mononuclear cancer cells with drugs. © 2017 Wiley Periodicals, Inc.

  15. Using nanogranite and glassy inclusions to unravel anatexis in the crustal footwall of the Ronda peridotites (Betic Cordillera, S Spain)

    Science.gov (United States)

    Bartoli, Omar; Acosta-Vigil, Antonio; Cesare, Bernardo; Remusat, Laurent; Tajčmanová, Lucie; Wälle, Markus; Heinrich, Christoph; Poli, Stefano; Bodnar, Robert J.

    2015-04-01

    The application of melt inclusion (MI) studies to migmatites and granulites is a recent, small-scale approach to a better understanding of melting in the continental crust [1]. Being trapped by growing peritectic phases at suprasolidus conditions, these MI represent a window into the pre-peak anatectic history of partially melted terranes, and may provide a wealth of microstructural and compositional information on crustal anatexis [2, 3, 4]. The crustal footwall of the Ronda peridotites consists of an inverted metamorphic sequence with migmatites and mylonites at the top. Mylonites represent strongly deformed former diatexites. To shed light on the nature and mechanisms of melting in the migmatites of the Ojén traverse, a detailed microstructural and geochemical study has been conducted on primary 2-10 µm MI hosted in peritectic garnet of i) metatexites at the bottom of the migmatitic sequence and ii) mylonitic former diatexites close to the contact with the mantle rocks. Both metatexites and mylonites have compositions corresponding to peraluminous greywackes. Phase equilibria modeling shows P-T conditions of equilibration of 4.5-5 kbar and 660-700 °C, and of 820-830 °C and 5.5-6.0 kbar for metatexites and mylonites, respectively. Clusters of MI in the metatexites are rounded and preferentially located at the core of small garnet crystals, whereas these clusters may have a sigmoidal to spiral-like shape in garnets of mylonites. MI show a variable degree of crystallization ranging from totally glassy to fully crystallized (i.e., nanogranites), consisting of Qtz+Pl+Kfs+Bt+Ms aggregates (often modal Kfs > Pl in mylonites). Piston cylinder remelting experiments led to the complete rehomogenization of nanogranites in metatexites at the conditions inferred for anatexis: 700 °C and 5 kbar. Rehomogenized nanogranites in metatexites and glassy MI in mylonites are all leucogranitic, although generally plot away from minimum melt compositions. Systematic compositional

  16. Tuberculosis in homeless persons in Poland.

    Science.gov (United States)

    Korzeniewska-Koseła, Maria; Kuś, Jan; Lewandowska, Katarzyna; Siemion-Szcześniak, Izabela

    2015-01-01

    The fall in rates of tuberculosis (TB) in many countries has been accompanied by the concentration of cases in the social risk groups including homeless persons. Comparison of TB features in homeless persons and in non-homeless patients. TB cases reported to National TB Register in Poland in whom information about the social status was available (the data about the social status were collected obligatorily in the years 2004-2013 only) were analysed. The results of DSTs were obtained from laboratory records and were available for the cases reported since 2010. Treatment outcome after 12 months was analysed for the cases registered between 2004-2012. The significance (Si) of the differences in proportions was assessed with chi-square test. Phomeless persons (HP) and 72,989 other patients (OP) with TB were included. In the group of HP, there was a greater proportion of males in comparison with OP (90.5% vs. 66.3%) (Si). The mean age of HP was 49.8 years (SD±10.9); of OP-52.9 years (SD±17.5) (Si). 16.6% of HP and 10.4% of OP were previously treated for TB (Si). The previous treatment was adequate in 62.2% of HP and in 85.8% of OP (Si). Pulmonary TB was in 98.0%, extrapulmonary TB in 2.0% of HP and, respectively, in 92.5% and 7.5% of OP (Si). Pulmonary TB was confirmed by culture in 76.3% of HP and in 64.5% of OP (Si). Sputum smears were positive in 70.7% of HP and in 62.5% of OP (Si). Caseous pneumonia occurred in 2.7% of homeless subjects and in 1.1% of OP (Si); infiltrative TB in 95.5% of HP and in 97.5% of OP (Si). Resistance to isoniazid was observed in 2.9% of HP and in 3.1% of OP; to rifampicin in 0.0% of HP and in 0.2% of OP; to isoniazid and rifampicin in 0.4% of HP and in 0.8% of OP. These differences were not Si. Treatment success rate among HP was 44.1%; default rate 24.8%; 4.0% of HP died from tuberculosis; 3.2% died from other causes; 5.2% were transferred and their outcomes were unknown; 0.4% were still on treatment; 0.4% had treatment failure; in 17

  17. Carbon isotope fractionation during diamond growth in depleted peridotite: Counterintuitive insights from modelling water-maximum CHO fluids as multi-component systems

    Science.gov (United States)

    Stachel, T.; Chacko, T.; Luth, R. W.

    2017-09-01

    Because of the inability of depleted cratonic peridotites to effectively buffer oxygen fugacities when infiltrated by CHO or carbonatitic fluids, it has been proposed recently (Luth and Stachel, 2014) that diamond formation in peridotites typically does not occur by rock-buffered redox reactions as previously thought but by an oxygen-conserving reaction in which minor coexisting CH4 and CO2 components in a water-rich fluid react to form diamond (CO2 + CH4 = 2C + 2H2O). In such fluid-buffered systems, carbon isotope fractionation during diamond precipitation occurs in the presence of two dominant fluid carbon species. Carbon isotope modelling of diamond precipitation from mixed CH4- and CO2-bearing fluids reveals unexpected fundamental differences relative to diamond crystallization from a single carbon fluid species: (1) irrespective of which carbon fluid species (CH4 or CO2) is dominant in the initial fluid, diamond formation is invariably associated with progressive minor (responsible for diamond formation. Specifically, precipitation of diamonds with δ13C values in the range -4 to -6‰ from mantle-derived fluids with an average δ13C value of -5‰ (derived from evidence not related to diamonds) requires that diamond-forming fluids were relatively reduced and had methane as the dominant carbon species (XCO2 = 0.1-0.5). Application of our model to a recently published set of in-situ carbon isotope analyses for peridotitic diamonds from Marange, Zimbabwe (Smit et al., 2016), which contain CH4 fluid inclusions, allows us to perfectly match the observed co-variations in δ13 C, δ15 N and N content and at the same time explain the previously counter-intuitive observation of progressive 13C enrichment in diamonds that appear to have grown from a fluid with methane as the dominant carbon species. Similarly, the almost complete absence in the published record of progressive 13C depletion trends within diamonds likely reflects ubiquitous precipitation from CH4- and CO

  18. Constraining late stage melt-peridotite interaction in the lithospheric mantle of southern Ethiopia: evidence from lithium elemental and isotopic compositions

    Science.gov (United States)

    Alemayehu, Melesse; Zhang, Hong-Fu; Seitz, Hans-Michael

    2017-10-01

    Lithium (Li) elemental and isotopic compositions for mineral separates of coexisting olivine, orthopyroxene and clinopyroxene of mantle xenoliths from the Quaternary volcanic rocks of southern Ethiopian rift (Dillo and Megado) reveal the influence of late stage melt-peridotite interaction on the early depleted and variably metasomatized lithospheric mantle. Two types of lherzolites are reported (LREE-depleted La/Sm(N) = 0.11-0.37 × Cl and LREE-enriched, La/Sm(N) = 1.88-15.72 × Cl). The depleted lherzolites have variable range in Li concentration (olivine: 2.1-5.4 ppm; opx: 1.1-2.3 ppm; cpx: 1.0-1.8 ppm) and in Li isotopic composition (δ7Li in olivine: -9.4 to 1.5‰; in opx: -4.5 to 3.6‰; in cpx: -17.0 to 4.8‰), indicating strong disequilibrium in Li partitioning and Li isotope fractionation between samples. The enriched lherzolites have limited range in both Li abundances (olivine: 2.7-3.0 ppm; opx: 1.1-3.1 ppm; cpx: 1.1-2.3 ppm) and Li isotopic compositions (δ7Li in olivine: -1.3 to +1.3‰; in opx: -2.0 to +5.0‰; in cpx: -7.5 to +4.8‰), suggest that the earlier metasomatic event which lead to LREE enrichment could also homogenize the Li contents and its isotopes. The enriched harzburgite and clinopyroxenite minerals show limited variation in Li abundances and variable Li isotopic compositions. The Li enrichments of olivine and clinopyroxene correlate neither with the incompatible trace element enrichment nor with the Sr-Nd isotopic compositions of clinopyroxene. These observations indicate that the metasomatic events which are responsible for the LREE enrichment and for the Li addition are distinct, whereby the LREE-enrichment pre-dates the influx of Li. The presence of large Li isotopic disequilibria within and between minerals of depleted and enriched peridotites suggest that the lithospheric mantle beneath the southern Ethiopian rift has experienced recent melt-peridotite interaction. Thus, the Li data set reported in this study offer new

  19. The geological record of base metal sulfides in the cratonic mantle: A microscale 187Os/188Os study of peridotite xenoliths from Somerset Island, Rae Craton (Canada)

    Science.gov (United States)

    Bragagni, A.; Luguet, A.; Fonseca, R. O. C.; Pearson, D. G.; Lorand, J.-P.; Nowell, G. M.; Kjarsgaard, B. A.

    2017-11-01

    We report detailed petrographic investigations along with 187Os/188Os data in Base Metal Sulfide (BMS) on four cratonic mantle xenoliths from Somerset Island (Rae Craton, Canada). The results shed light on the processes affecting the Re-Os systematics and provide time constraints on the formation and evolution of the cratonic lithospheric mantle beneath the Rae craton. When devoid of alteration, BMS grains mainly consist of pentlandite + pyrrhotite ± chalcopyrite. The relatively high BMS modal abundance of the four investigated xenoliths cannot be reconciled with the residual nature of these peridotites, but requires addition of metasomatic BMS. This is especially evident in the two peridotites with the highest bulk Pd/Ir and Pd/Pt. Metasomatic BMS likely formed during melt/fluid percolation in the Sub Continental Lithospheric Mantle (SCLM) as well as during infiltration of the host kimberlite magma, when djerfisherite crystallized around older Fe-Ni-sulfides. On the whole-rock scale, kimberlite metasomatism is visible in a subset of bulk xenoliths, which defines a Re-Os errorchron that dates the host magma emplacement. The 187Os/188Os measured in the twenty analysed BMS grains vary from 0.1084 to >0.17 and it shows no systematic variation depending on the sulfide mineralogical assemblage. The largest range in 187Os/188Os is observed in BMS grains from the two xenoliths with the highest Pd/Ir, Pd/Pt, and sulfide modal abundance. The whole-rock TRD ages of these two samples underestimate the melting age obtained from BMS, demonstrating that bulk Re-Os model ages from peridotites with clear evidence of metasomatism should be treated with caution. The TRD ages determined in BMS grains are clustered around 2.8-2.7, ∼2.2 and ∼1.9 Ga. The 2.8-2.7 Ga TRD ages document the main SCLM building event in the Rae craton, which is likely related to the formation of the local greenstone belts in a continental rift setting. The Paleoproterozoic TRD ages can be explained by

  20. Hungary and Poland: The Transformation from a Command to a Market Economy, 1989-1998. Fulbright-Hays Summer Seminars Abroad Program, 1998 (Hungary/Poland).

    Science.gov (United States)

    Levine, Michael

    This paper examines the economic changes that have taken place in recent years in two central European countries, Hungary and Poland. Findings in the paper are based on materials gathered during the summer of 1998 on a Fulbright-Hays seminar visit to Hungary and Poland and from talks with officials and professors in those countries. Observations…

  1. Evidence for an intra-oceanic affinity of the serpentinized peridotites from the Mt. Pollino ophiolites (Southern Ligurian Tethys): Insights into the peculiar tectonic evolution of the Southern Apennines

    Science.gov (United States)

    Mazzeo, F. C.; Zanetti, A.; Aulinas, M.; Petrosino, P.; Arienzo, I.; D'Antonio, M.

    2017-07-01

    A detailed petrochemical investigation of the peridotites from the Mt. Pollino area (Basilicata, Southern Italy) allowed to provide the first comprehensive reconstruction of the evolution and geodynamic setting of ophiolitic mantle from the Southern Apennines. These mantle peridotites firstly acquired strongly-refractory modal and chemical compositions consistent with large degrees of partial melting (≥ 23%). This process was presumably assisted by concomitant injection of melt increments rising from deeper levels of the mantle column, as suggested by relatively large Al and Fe contents of Ol, Opx and Sp. The porous flow ascent of melt increments produced by deeper near-fractional melting continued after the end of the partial melting, as recorded by precipitation of disseminated clinopyroxene out of thermal and chemical equilibrium with the other rock-forming minerals. The Pollino mantle sequence locally experienced reheating associated to a new episode of porous flow migration of melts with REE composition approaching that of N-MORB. The petrological evolution recorded by the peridotites of Mt. Pollino, their high equilibrium T (up to 1100 °C) and the absence of pyroxenites show remarkable analogies with modern abyssal peridotites, pointing to an intra-oceanic setting of the Jurassic Ligurian Tethys for this mantle sequence. According to the present knowledge about the Southern Apennines, the abyssal-like peridotites with the associated terrigenous sediments and continental crustal rocks were incorporated in the Ligurian Accretionary Complex and reached HP/LT conditions during a subduction event starting in Upper Oligocene, to be later exhumed in the Tortonian. The results of this study strongly support the existence of significant differences in terms of geodynamic evolution between Southern and Northern Apennines.

  2. The distribution of H2O between silicate melt and nominally anhydrous peridotite and the onset of hydrous melting in the deep upper mantle

    Science.gov (United States)

    Novella, Davide; Frost, Daniel J.; Hauri, Erik H.; Bureau, Helene; Raepsaet, Caroline; Roberge, Mathilde

    2014-08-01

    The partitioning of H2O between a mantle peridotite assemblage and low degree hydrous melt has been investigated at 6 GPa (corresponding to ∼180 km depth) at a temperature of 1400 °C. Peridotite mineral phases were analysed from 6 melting experiments performed in a natural chemical system. The experiments contained ∼80 wt% of a low degree hydrous melt that was obtained through a series of experiments where the melt composition was iteratively adjusted until saturation with the appropriate peridotite assemblage was achieved. The melt is fluid-undersaturated at the conditions of the experiment. Ion microprobe measurements of the mineral phases indicate olivine H2O concentrations of 434±61 ppm wt and average clinopyroxene (cpx) concentrations of 1268±173 ppm wt H2O. Orthopyroxene (opx) and garnet contain 700±46 ppm wt and 347±83 ppm wt H2O, respectively. The H2O content of the hydrous melts was determined by mass balance to be 11±0.5 wt% H2O. H2O partition coefficients between minerals and melt (DH2Omin/melt=XH2Omin/XH2Omelt) are 0.0040±0.0006 for olivine, 0.0064±0.0004 for opx, 0.0115±0.0016 for cpx and 0.0032±0.0008 for garnet. Using the determined H2O partition coefficients the onset and extent of melting at conditions equivalent to 180 km below mid-ocean ridges was determined as a function of mantle H2O content. Current estimates for the H2O content of the depleted mantle (50-200 ppm wt H2O) are insufficient to induce mantle melting at this depth, which requires ∼700 ppm wt H2O to produce 0.1% melting and 1600 ppm wt H2O for 1% melting, along an adiabat with a potential temperature of 1327 °C. Melting can occur at these conditions within the mantle source of ocean island basalts, which are estimated to contain up to 900 ppm wt H2O. If adiabatic temperatures are 200 °C higher within such plume related sources, then melt fractions of over 1% can be reached at 180 km depth. In addition, a model for the distribution of H2O between peridotite mineral

  3. District Energy Corporation SW 40th Street Thermal Energy Plant

    Energy Technology Data Exchange (ETDEWEB)

    Davlin, Thomas [District Energy Corporation, Lincoln, NE (United States)

    2014-06-06

    The overall deliverable from the project is the design, construction and commissioning of a detention facility heating and cooling system that minimizes ownership costs and maximizes efficiency (and therefore minimizes environmental impact). The primary deliverables were the proof of concept for the application of geothermal systems for an institutional facility and the ongoing, quarterly system operating data downloads to the Department of Energy . The primary advantage of geothermal based heat pump systems is the higher efficiency of the system compared to a conventional chiller, boiler, cooling tower based system. The higher efficiency results in a smaller environmental foot print and lower energy costs for the detention facility owner, Lancaster County. The higher efficiency for building cooling is primarily due to a more constant compressor condensing temperature with the geothermal well field acting as a thermal “sink” (in place of the conventional system’s cooling tower). In the heating mode, Ground Couple Heat Pump (GCHP) systems benefits from the advantage of a heat pump Coefficient of Performance (COP) of approximately 3.6, significantly better than a conventional gas boiler. The geothermal well field acting as a thermal “source” allows the heat pumps to operate efficiently in the heating mode regardless of ambient temperatures. The well field is partially located in a wetland with a high water table so, over time, the project will be able to identify the thermal loading characteristics of a well field located in a high water table location. The project demonstrated how a large geothermal well field can be installed in a wetland area in an economical and environmentally sound manner. Finally, the SW 40th Street Thermal Energy Plant project demonstrates the benefits of providing domestic hot water energy, as well as space heating, to help balance well filed thermal loading in a cooling dominated application. During the period of August 2012 thru

  4. An introduction of Markov chain Monte Carlo method to geochemical inverse problems: Reading melting parameters from REE abundances in abyssal peridotites

    Science.gov (United States)

    Liu, Boda; Liang, Yan

    2017-04-01

    Markov chain Monte Carlo (MCMC) simulation is a powerful statistical method in solving inverse problems that arise from a wide range of applications. In Earth sciences applications of MCMC simulations are primarily in the field of geophysics. The purpose of this study is to introduce MCMC methods to geochemical inverse problems related to trace element fractionation during mantle melting. MCMC methods have several advantages over least squares methods in deciphering melting processes from trace element abundances in basalts and mantle rocks. Here we use an MCMC method to invert for extent of melting, fraction of melt present during melting, and extent of chemical disequilibrium between the melt and residual solid from REE abundances in clinopyroxene in abyssal peridotites from Mid-Atlantic Ridge, Central Indian Ridge, Southwest Indian Ridge, Lena Trough, and American-Antarctic Ridge. We consider two melting models: one with exact analytical solution and the other without. We solve the latter numerically in a chain of melting models according to the Metropolis-Hastings algorithm. The probability distribution of inverted melting parameters depends on assumptions of the physical model, knowledge of mantle source composition, and constraints from the REE data. Results from MCMC inversion are consistent with and provide more reliable uncertainty estimates than results based on nonlinear least squares inversion. We show that chemical disequilibrium is likely to play an important role in fractionating LREE in residual peridotites during partial melting beneath mid-ocean ridge spreading centers. MCMC simulation is well suited for more complicated but physically more realistic melting problems that do not have analytical solutions.

  5. The Mantle Wedge of the Mariana Subduction Factory: Investigation on Peridotite Clasts Cored at South Chamorro Seamount, Site 1200, ODP Leg 195

    Science.gov (United States)

    D'Antonio, M.; Spadea, P.; Savov, I.

    2002-12-01

    The South Chamorro Seamount is a serpentine mud volcano located in the Mariana forearc region. It has been cored during Ocean Drilling Program Leg 195 (March-May 2001; Site 1200). It is made up of serpentine mud coming from the downgoing Pacific plate, which is about 30 km deep beneath the seamount. The mud encloses clasts of ultramafic rocks from the overriding plate. The clasts are mostly harzburgite, with minor dunite and lherzolite, strongly serpentinized and tectonized. The primary mineralogy includes olivine, orthopyroxene, clinopyroxene and chromium-spinel. The samples show typical mesh and hourglass serpentine textures, and contain veins of serpentine, brucite and chlorite. Whole-rock chemistry shows Mg# = 91-93, and high Ni and Cr contents. Low CaO and Al2O3 contents, and very low REE contents with U-shaped, strongly LREE-enriched and HREE-depleted, patterns confirm that most of the analyzed samples are highly residual peridotites which suffered extensive partial melting (20-25%), and contain an enriched component. The only lherzolite sample shows a significantly lower degree of depletion, slightly higher than 15%. In the analyzed sample set, olivine has Fo = 91.5-92.5, with Ni content in the 2200-4200 ppm range, enstatite has Al2O3 = 0.8-2.6 wt.% and CaO = 0.2-2.1 wt.%. Also diopside is chemically variable, with Mg# = 93-99, and low to very low Cr, Na and Al contents. Diopside from the lherzolite sample has higher Al and significantly lower Na than in most harzburgites. Chemical variations and textural differences of pyroxenes suggest that the peridotites underwent recrystallization and metasomatism after melt extraction.

  6. NEW DATA ON MIDDLE DEVONIAN CONODONTS FROM SW-SARDINIA:THE SU NUARGI II SECTION REVISITED

    Directory of Open Access Journals (Sweden)

    SOFIE GOUWY

    2013-11-01

    Full Text Available The conodont collection from the nodular limestone beds of the Su Nuargi II outcrop near Domusnovas in SW-Sardinia (Italy is restudied for the purpose of reassessing the outcrop and updating the conodont collection to the most recent taxonomy. Su Nuargi II is the most important outcrop in the SW of the island exposing Middle Devonian rocks. Forty-five conodont taxa have been identified in the collection, positioning the outcrop within the interval covering the timorensis to latifossatus zones (Lower to Middle Givetian slightly widening the interpretation of Olivieri (1985. A new morphotype of Polygnathus linguiformis linguiformis is described. The genera Tortodus and Schmidtognathus are identified for the first time in the Middle Devonian of Sardinia. Additionally, a second Middle Devonian outcrop is discovered in the SW of the Island. 

  7. Big Words, Little Results: the Chinese Investments in Poland from the Political Perspective

    Directory of Open Access Journals (Sweden)

    Michał Lubina

    2017-12-01

    Full Text Available In 2017 statistics showed that Chinese Foreign Direct Investments (FDI in Poland for 2016 amounted to a more than half of all Chinese FDI in Poland for the 2000–2016. Yet the overall amount of Chinese FDI remains modest in comparison with Western Europe or even with Hungary. Despite much proclaimed Sino-Polish rapprochement in 2015–2016 and high hopes for OBOR/BRI initiative in Poland, cooperation with China has not been a breakthrough for Poland in terms of economic results. There have not been ground-breaking Sino-Polish projects and Polish government’s desire to strengthen ties with China loosened in late 2016/early 2017 (though it may revive now.There are several reasons for that, from the perception of Poland as non-attractive for majority Chinese investments, via lack of overall Polish strategy of attracting these investors to discrepancies of economic interests between Poland and China.

  8. Identification and Characterization of Bacillus cereus SW7-1 in Bombyx mori (Lepidoptera: Bombycidae).

    Science.gov (United States)

    Li, Guan-Nan; Xia, Xue-Juan; Zhao, Huan-Huan; Sendegeya, Parfait; Zhu, Yong

    2015-01-01

    The bacterial diseases of silkworms cause significant reductions in sericulture and result in huge economic loss. This study aimed to identify and characterize a pathogen from diseased silkworm. SW7-1, a pathogenic bacterial strain, was isolated from the diseased silkworm. The strain was identified on the basis of its bacteriological properties and 16S rRNA gene sequence. The colony was round, slightly convex, opaque, dry, and milky on a nutrient agar medium, the colony also exhibited jagged edges. SW7-1 was Gram-positive, without parasporal crystal, and 0.8-1.2 by 2.6-3.4 µm in length, resembling long rods with rounded ends. The strain was positive to most of the physiological biochemical tests used in this study. The strain could utilize glucose, sucrose, and maltose. The results of its 16S rRNA gene sequence analysis revealed that SW7-1 shared the highest sequence identity (>99%) with Bacillus cereus strain 14. The bacterial strain was highly susceptible to gentamycin, streptomycin, erythromycin, norfloxacin, and ofloxacin and moderately susceptible to tetracycline and rifampicin. It exhibited resistance to other antibiotics. SW7-1 had hemolytic activity and could produce extracellular casease, lipase, and amylase. SW7-1 could reproduce septicemia-like symptoms with high mortality rate when re-fed to healthy silkworm. .The median lethal concentration (LC50) was 5.45 × 10(4) cfu/ml. Thus, SW7-1 was identified as B. cereus, which is a pathogen for silkworm and human infections are possible. © The Author 2015. Published by Oxford University Press on behalf of the Entomological Society of America.

  9. Targeted pancreatic cancer therapy with the small molecule drug conjugate SW IV-134.

    Science.gov (United States)

    Hashim, Yassar M; Spitzer, Dirk; Vangveravong, Suwanna; Hornick, Mary C; Garg, Gunjal; Hornick, John R; Goedegebuure, Peter; Mach, Robert H; Hawkins, William G

    2014-07-01

    Pancreatic adenocarcinoma is highly resistant to conventional therapeutics and has been shown to evade apoptosis by deregulation of the X-linked and cellular inhibitors of apoptosis proteins (XIAP and cIAP). Second mitochondria-derived activator of caspases (Smac) induces and amplifies cell death by reversing the anti-apoptotic activity of IAPs. Thus, Smac-derived peptide analogues (peptidomimetics) have been developed and shown to represent promising cancer therapeutics. Sigma-2 receptors are overexpressed in many proliferating tumor cells including pancreatic cancer. Selected ligands to this receptor are rapidly internalized by cancer cells. These characteristics have made the sigma-2 receptor an attractive target for drug delivery because selective delivery to cancer cells has the potential to increase therapeutic efficacy while minimizing toxicity to normal tissues. Here, we describe the initial characterization of SW IV-134, a chemically linked drug conjugate between the sigma-2 ligand SW43 and the Smac mimetic SW IV-52 as a novel treatment option for pancreatic adenocarcinoma. The tumor killing characteristics of our dual-domain therapeutic SW IV-134 was far greater than either component in isolation or in an equimolar mix and suggests enhanced cellular delivery when chemically linked to the sigma-2 ligand. One of the key findings was that SW IV-134 retained target selectivity of the Smac cargo with the involvement of the NF-κB/TNFα signaling pathway. Importantly, SW IV-134 slowed tumor growth and improved survival in murine models of pancreatic cancer. Our data support further study of this novel therapeutic and this drug delivery strategy because it may eventually benefit patients with pancreatic cancer. Copyright © 2014 Federation of European Biochemical Societies. Published by Elsevier B.V. All rights reserved.

  10. Distribution of Azolla filiculoides Lam. (Azollaceae in Poland

    Directory of Open Access Journals (Sweden)

    Ewa Szczęśniak

    2011-01-01

    Full Text Available Azolla filiculoides has been an ephemeral plant in Poland since the end of the 20th century. In the last 15 years this species appeared in 5 locations in south-west Poland. Habitat and plants of two populations became destroyed, three other still exist. A. filiculoides occurs in eutrophic or even polluted water where it forms dense mats, up to 10 cm thick. It stays sterile and propagates only in a vegetative manner. Frost resistance of Lower Silesia populations is higher than reported so far; fern may winter and rebuild the population after frost reaching 22oC. Size of the populations is changeable during the vegetation season. A. filiculoides occurs in water habitats and plant communities in which it substitutes Lemna minor.

  11. Education for Sustainability in Poland – A Narrative Literature Review

    Directory of Open Access Journals (Sweden)

    Magda Scrobota

    2014-12-01

    Full Text Available As a member state of the European Union, Poland is committed to sustainability by endorsing the principles of sustainable development in its Constitution and adopting European standards. However, to overcome the societal, environmental and economic demands, a society needs to integrate sustainability concepts into daily practices, education playing a crucial role in achieving this objective. This paper aims to provide an overview of the education for sustainability in Poland and its impact on Polish society. Designed as a narrative literature review, the paper reports on how education for sustainability was carried out between 1994 and 2013, building a detailed picture of the educational programs and actions conducted in business and non –profit organizations. Additionally it is revealed that although challenging, creating community-based learning can increase people’s awareness and potential to contribute to a sustainable future by reducing the de-coupling effect between organizational actual practices and declarations.

  12. DIFFERENTIATION OF WELFARE OF RURAL HOUSEHOLDS IN POLAND IN 2012

    Directory of Open Access Journals (Sweden)

    Krystyna Hanusik

    2014-03-01

    Full Text Available The subject of the research in focus was the material welfare of households. In particular, there were analysed the level and differentiation of the welfare of rural households in 2012, after more than twenty years of developing of market economy in Poland. In addition, there was examined the relationship between income, consumer spending and household equipment and the level and differentiation of measures of the welfare distinguished by the criterion of the main sources of income of households groups. In the study both econometrical and statistical analysis was used. The study was based on primarily source of information coming from the panel study of household budgets conducted by the Central Statistical Office, as well as the data contained in the statistical yearbooks of the Republic of Poland.

  13. Continuous model of the regional velocity field for Poland

    Science.gov (United States)

    Bogusz, J.; Figurski, M.; Kontny, B.; Grzempowski, P.; Klos, A.

    2012-04-01

    The poster presents modern determinations of the regional velocity field for Poland. The research is based on the ASG-EUPOS, Polish multifunctional GNNS network and performed within the developmental project of the Polish Ministry of Science and Higher Education. The network of the satellite-based sites consisted of above 130 Polish sites together with the selected number of European sites operating within EPN (EUREF Permanent Network). Data came from three-year period, which is the minimum number for the horizontal velocity determinations. The velocities were calculated within the discrete network related to the GNSS sites' distribution and then interpolated to the regular grid. The discussion on the interpolation methods is also included. To the interpolation of the velocity field kriging, spline and other functions were used. Assessment of the accuracy of the velocity on the interpolated points and tests of significance were also described. Developed models of the velocities field could indicate geodynamical activity on the area of Poland.

  14. The national alpha-1 antitrypsin deficiency registry in Poland.

    Science.gov (United States)

    Chorostowska-Wynimko, Joanna; Struniawski, Radoslaw; Sliwinski, Paweł; Wajda, Beata; Czajkowska-Malinowska, Małgorzata

    2015-05-01

    The alpha-1 antitrypsin deficiency (AATD) targeted screening program, together with the National Registry, were established in Poland in 2010 soon after the AATD diagnostics became available. Between 2010 and 2014 a total of 2525 samples were collected from respiratory patients countrywide; 55 patients with severe AAT deficiency or rare mutations were identified and registered, including 36 PiZZ subjects (65%). The majority of AATD patients were diagnosed with COPD (40%) or emphysema (7%), but also with bronchial asthma (16%) and bronchiectasis (13%). Therefore, the registry has proved instrumental in setting-up the AATD-dedicated network of respiratory medical centres in Poland. Since augmentation therapy is not reimbursed in our country, the smoking cessation guidance, optimal pharmacotherapy of respiratory symptoms as well the early detection, and effective treatment of exacerbations is absolutely essential.

  15. Poland syndrome (anomaly with congenital hemangioma: A new association

    Directory of Open Access Journals (Sweden)

    Riyaz Najeeba

    2006-01-01

    Full Text Available Unilateral defect of pectoral muscle and ipsilateral syndactyly constitute Poland syndrome. Absence or hypoplasia of the breast and nipple, axillary hair loss and dermatoglyphic abnormalities have also been reported in this syndrome. The primary defect could be in the development of the proximal subclavian artery with early deficit of blood flow to the distal limb and the pectoral region, resulting in partial loss of tissue in those regions. However, the association of congenital hemangioma with Poland sequence has not been observed so far. Such an association is being reported here in a 1-year-old infant, second-born of nonconsanguineous parents, who also had polydactyly instead of the documented syndactyly.

  16. Masculist Groups in Poland: Aids of Mainstream Antifeminism

    Directory of Open Access Journals (Sweden)

    Katarzyna Wojnicka

    2016-06-01

    Full Text Available This paper addresses the role masculist groups currently play in fostering resistance to feminist-influenced efforts to advance the autonomy and equality of women in Poland, where the strong influence of the Polish Catholic Church continues to shape attitudes and actions in professional, governmental and civil society spheres. The paper argues that Polish public discourse since 1989 has been strongly dominated by antifeminist rhetoric advanced by masculist groups. This rhetoric is not only used in the media and in political discourse; it also influences legislation and thus hinders efforts to secure a satisfactory level of equality for women, evidenced in struggles over abortion reform, the Convention on Preventing and Combating Violence Against Women, and the trivialisation of rape. The findings of the paper are based on qualitative social research on men’s social movements in Poland between 2009 and 2012 and on qualitative media discourse analysis of articles published between 2009 and 2014.

  17. DERECHO - CHARACTERISTICS OF THE PHENOMENON, THE DANGER ZONE IN POLAND

    Directory of Open Access Journals (Sweden)

    CELIŃSKI-MYSŁAW D.

    2015-03-01

    Full Text Available The aim of the paper is to characterize the occurrence of derecho phenomenon in Poland between 2007 and 2014 and to describe threats that this phenomenon causes. The number of derecho cases in Central Europe in that period was determined on the basis of the identification criteria proposed by R. Johns and W. Hirt. Also, conditions for the occurrence of derecho were characterized and destruction that it caused was described. Additionally, the ranges of the individual derecho cases enabled the determination of the most vulnerable areas of Poland to the occurrence of this phenomenon. Reports on dangerous meteorological phenomena, SYNOP and METAR reports, MSL pressure maps, upper air maps at 500 hPa and 850 hPa, upper air sounding plots, radar depictions and satellite images were used in this paper.

  18. Facilities of Early Rehabilitation post Stroke in Poland 2010

    DEFF Research Database (Denmark)

    Opara, Jozef; Langhorne, Peter; Larsen, Torben

    2012-01-01

    Rationale -The aim of this work was to survey the contemporary facilities for early poststroke rehabilitation in Poland. The main research questions were: what is the availability of inpatient rehabilitation for post-stroke patients in neurological departments and in rehabilitation departments......? Aims - Growing costs of health care are encouraging healthcare planners to look for new organizational solutions of services which could enable rehabilitation as early as possible after disease onset. Early post-stroke rehabilitation consists of many elements that provide for early onset rehabilitation...... and its continuation after discharge from stroke unit. Participants - Two questionnaires evaluating neurorehabilitation of people who underwent stroke was designed and distributed: first to 221 neurological wards and second to 154 rehabilitation departments in Poland. Design - We asked about delay before...

  19. Problem of rubella in Poland after compensatory outbreak in 2013

    Science.gov (United States)

    Abramczuk, Edyta; Częścik, Agnieszka; Pancer, Katarzyna; Gut, Włodzimierz

    The attempt to estimate the real number of rubella cases in the years 2015-2016 in Poland was presented in this paper. The relations between number of reported cases of measles in 2006-2015y., the number of laboratory-confirmed cases of rubella among cases suspected of measles and the proportion of rubella among patients suspected of measles in the last 10 years as well as the results of serological examination in samples from 74 patients suspected of rubella collected in the first half of 2016 year were analysed. The sera from patients suspected of rubella were collected in cooperation with the State Sanitary Inspection. The analysis of data collected during the study-cases of suspected measles (2006-2016) and rubella infections (in 2016y.) indicated high over-registration of rubella in recent years in Poland, which is associated with a very low rate of laboratory confirmed cases.

  20. Occupational exposure to medical X rays in Poland

    Energy Technology Data Exchange (ETDEWEB)

    Jankowski, J.; Nowak, B.; Liniecki, J. (Inst. of Occupational Medicine, Lodz (Poland))

    1991-01-01

    Personal dosimetry in Poland indicates that exposure to X rays of workers engaged in surgical radiology is higher than that among other radiologists and auxiliary personnel, 0.9 as against 0.4 mSv per annum. This information, however, does not provide detailed insight into the exposures. To study this problem, the exposure of personnel employed in operating theatres and utilising fluoroscopy was investigated. With TL dosemeters, the distribution of doses to the body was measured on the surface of protective aprons and on the forehead, the wrist and the shoulder. The study embraced 20 centres in Poland engaged in cardiac pacemaker insertion, haemodynamic examinations of the heart, transcutaneous removal of kidney stones, radiological control of biliary routes and orthopaedic surgery. The results enable one to assess the average annual effective dose equivalent H{sub E} for workers and the corresponding dose equivalents H to the lens of the eye and the hands. (author).

  1. Beyond convergence: Poland and Turkey en route to high income

    Directory of Open Access Journals (Sweden)

    Martin Raiser

    2016-03-01

    Full Text Available This paper compares and contrasts the policy reform experiences of Poland and Turkey en route to high income. For both countries, globalization has presented unprecedented opportunities to catch up, unleased by integration into European and global markets and the establishment of macroeconomic discipline. These opportunities were reinforced by the creation of economic institutions to strengthen competition and support private entrepreneurship, catalyzed by the convergence process with the European Union. Both Poland and Turkey have shown resilience following the 2008 global crisis, but continued success will require renewed structural reform measures. Dealing with the challenging of aging while at the same time finding a way to sustain productivity growth through greater domestic innovation is shaping Poland’s policy agenda. Turkey's structural and demographic potential as well as its strategic location between the markets of Europe and Asia offers attractive value proposition to investors, which could be further enhanced with improvements in business regulations and economic governance.

  2. THE SOCIAL AND ECONOMIC EVOLUTION OF POLAND AND ROMANIA FOR THE LAST 100 YEARS

    OpenAIRE

    IVANOV LAURENTIU

    2016-01-01

    In terms of size of territory and population, Poland and Romania are the largest former socialist countries, now, members of the European Union. In the last 25 years of transition to a market economy, Poland has excellent managed its natural potential and is, now, an economic model for other former socialist countries, including Romania. Poland has not experienced economic recession; its positive economic evolution was completely different from the evolution of the largest Europea...

  3. DIRECT PAYMENTS AND THEIR IMPACT ON THE LAND MARKET IN POLAND

    OpenAIRE

    Dziemianowicz, Ryta Iwona; Przygodzka, Renata; Sadowski, Adam

    2008-01-01

    The article makes an attempt to answer the question: how direct payments affected the land market in Poland? The first part of the article explains the theoretical aspects of direct payments as an instrument of agricultural policy and their prospective effectiveness. Also the special character of the solutions adopted by Poland in relation with the use of this instrument was shown. The second part presents the main problems of the land market in Poland, taking into account both the supply and...

  4. Financial support of the European Union in the process of modernization of agriculture in Poland

    OpenAIRE

    DARIUSZ KUSZ

    2014-01-01

    The integration of Poland and the European Union has substantially changed the conditions for the functioning of Polish agriculture, among others, financing for development and modernization. The aim of the study is to present and assess the level of financial support of the European Union in the process of modernization of farms in Poland. It points out the significant role of public support under the EU funds in the modernization of agriculture in Poland.

  5. Materials for the flora of myxomycetes of central Poland

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    Ewa Kalinowska-Kucharska

    2014-11-01

    Full Text Available The author investigated the Myxomycetes flora in the environment of Łódź. A collection made between 1967-1972 contains 58 species an 3 varieties. Among Myxomycetes found in this territory are species rare in Poland: Badhamia affinis Rost, Comatrichia pulchella (Bab. Rost., Clastoderma debaryanum Blytt., Lycogala conicum Pers., Lycogala exiguum Morgan, Trichia incospicua Rost. and Trichia olivacea (Maylan Krzem.

  6. Social and economic determinants of higher education choices in Poland

    OpenAIRE

    Tomasz Gajderowicz; Gabriela Grotkowska; Jerzy Mycielski; Leszek Wincenciak

    2014-01-01

    The aim of this paper is to find determinants of the choice of the field of study made by individuals undertaking higher education in Poland. One the most striking elements of the Polish transition process is a fundamental change of the conditions of the tertiary education market. With growing popularity of higher studies, choices related to this aspect of educational paths of young people gain more and more importance. In this empirical study we apply conditional multinomial logit model in o...

  7. Assessment of cyanobacteria impact on bathing water quality in Poland

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    Krzysztof Skotak

    2012-12-01

    Full Text Available Introduction: Quality of bathing water is of key importance for bathers’ health, mainly due to the fact, that each year millions of people use bathing sites as places for recreation and sport activities. Most of the bathing sites are of adequate quality of water, but still there are cases of health risk because bathing water is polluted. One of the main health risk factor in bathing water are cyanobacteria and their blooms. Cyanobacteria are microorganisms of morphological features of bacteria and algae. They live in colonies, which in large quantities show up as streaks, dense foam on the water surface. The aim of this paper was to assess the impact of cyanobacteria blooms on health regarding bathing water quality in Poland. Materials and methods: Assessment covered all bathing sites in Poland supervised by Polish National Sanitary Inspection (PIS in the period from 2007 to 2009. The base was data collected during bathing water monitoring conducted by PIS and their formal decisions of bathing bans introduced in response to revealed bathing water pollution. Results and discussion: The results of assessment indicate, that about one-fourth of all bathing bans in Poland was due to cyanobacteria blooms. Conclusions: Every fifth bathing sites located on artificial lake or water reservoir and every tenth on the sea bathing sites were polluted. Average period of bathing ban due to cyanobacteria blooms in Poland varies. Relatively the shortest bathing bans were observed on the sea bathing sites (no longer than one week on average. Much longer were bathing bans on lakes and artificial lakes (one month on average.

  8. Blind Politics of Ambition: Shale Gas in Poland

    OpenAIRE

    Niemuth, Stephanie; Westphal, Sophie

    2014-01-01

    Ever since the impacts of the shale gas revolution in the US have unfolded their measurable effects – as significantly declining natural gas prices – impressive euphoria among those states which are identified to bear high potentials of unconventional gas is widely spread. As for Poland, essentially linked to the hope of profitably producing shale gas is the political will to strive for independence from Russian energy supply and thus, enhance energy supply security. Hence, liberalizing its g...

  9. Syndrome de Poland | Jellouli | Pan African Medical Journal

    African Journals Online (AJOL)

    La fonction rénale était normale, la numération de la formule sanguine était normale de même que le bilan d'hémostase. ... d'un syndrome de Poland avec hypoplasie du grand pectoral et une brachymésophalangie gauche sans malformations associées en particulier pas d'atteinte cardiaque ou d'anomalie génito-urinaire.

  10. Chinese Tourists in Cracow, Poland: Their Profile, Expectations, and Perceptions

    OpenAIRE

    Guszkiewicz Paulina; Nessel Karolina

    2017-01-01

    Introduction. In 2012, China became the largest spender in international tourism, benefiting many destinations worldwide. Even if for Poland it is not an important source market yet, the Polish authorities have undertaken some marketing activities in China. The main aim of the paper is to explore the profile, motivations, and perceptions of the Chinese tourists visiting Cracow. The secondary aim is to check the effectiveness of the marketing efforts dedicated to the Chinese market undertaken ...

  11. Chinese tourists in Cracow, Poland : their profile, expectations, and perceptions

    OpenAIRE

    Guszkiewicz, Paulina; Nessel, Karolina

    2017-01-01

    Introduction. In 2012, China became the largest spender in international tourism, benefiting many destinations worldwide. Even if for Poland it is not an important source market yet, the Polish authorities have undertaken some marketing activities in China. The main aim of the paper is to explore the profile, motivations, and perceptions of the Chinese tourists visiting Cracow. The secondary aim is to check the effectiveness of the marketing efforts dedicated to the Chinese market undertaken ...

  12. Transformation on steel products distribution in Poland and Slovakia

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    R. Stefko

    2012-01-01

    Full Text Available Steel industry is one of the most globalized branch, globalization has had the influence on iron ore supply, steel production and distribution as well. In last years, steel products distribution process has changed significantly, because of rising competitiveness due to common world market influence and main global players actions. The paper presents changes in steel products distribution in Poland and Slovakia focusing on main steel producers activity in distribution as well as distributors response on new market situation.

  13. Anticipated Impacts of GMO Introduction on Production Pattern In Poland

    OpenAIRE

    Maciejczak, Mariusz; Was, Adam

    2008-01-01

    The paper takes one significant element of the agriculture production – use of genetically modified organisms (GMO) – and considers it in relation to the production pattern in Polish farms. It asks if under the ceteris paribus conditions the use of GMO plants in Polish farms will have influence on the cropping structure. To answer this question only a scientific and theoretical assumption has been applied that GMO cultivation is permitted without restrictions in Poland. The approach combines ...

  14. The vegetation of kettle-holes in central Poland

    OpenAIRE

    Kaźmierczak, Ewa

    1997-01-01

    The study aimed at an investigation of the vegetation of kettle-holes in the agricultural landscape of the Ziemia Chelminska region in northern central Poland. Most of these kettle-holes have been influenced strongly by human activities. 120 community types were described with regard to their species composition, structure, differentiation, synanthropization, ecological conditions and dynamics, as well as their affinities to similar plant communities from other regions in Europe. The signific...

  15. Music in Nazi-Occupied Poland between 1939 and 1945

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    Naliwajek-Mazurek Katarzyna

    2016-12-01

    Full Text Available The paper is a survey of research on music in territories of occupied Poland conducted by the author in recent years, as well as a review of selected existing literature on this topic. A case study illustrates a principal thesis of this essay according to which music was used by the German Nazis in the General Government as a key elements of propaganda and in appropriation of conquered territories as both physical and symbolic spaces.

  16. Innovation in the tourism sector in greater Poland

    OpenAIRE

    Przybylska, Anna

    2014-01-01

    Innovation in the tourism sector is increasingly becoming a source of competitive advantage. The factors which have most influenced this process include: advances in technology, increasingly demanding consumers, the limited life-span of a tourism product and growing competition. The paper presents the results of research into innovative solutions applied by tourism enterprises based in the Greater Poland market, taking into account above all the nature of the service industry. The ...

  17. Tyhula subvariabilis new species in the mycoflora of Poland

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    Maria Dynowska

    2014-08-01

    Full Text Available Typhula subvariabilis Berthier is a new species in the mycoflora of Poland. U has been discovered on the leaves of Corylus avellana L. at Wójtowo near Olsztyn. Considering the morphology and anatomy of the fruit bodies the presented species resemble those of T. variabilis Riess (B e r t h i e r, 1976. The most significant differences between the two species concern the structure of the sclerotia (Dynowska, 1986.

  18. SMALL HYDRO PLANTS IN LAND USE SYSTEM PLANNING IN POLAND

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    Anita Bernatek

    2014-10-01

    Full Text Available Small hydropower plants are present in the land use system planning in Poland. At the national level the important role of spatial planning in the development of renewable energy was highlighted, included small hydroplants. However, it seems that at the regional level this demand has not been realized. The necessity of developing small hydroplants as a renewable energy was highlighted, but negative environmental impact was not indicated. At local level legal instrument of small hydropower plants is specified.

  19. The politics of toleration: Dissenters in Poland (1587-1648)

    OpenAIRE

    Wilson, Katherine Alina

    2005-01-01

    This thesis shows how religion and politics interacted inextricably in early modern society, by a study of the szlachta (nobility) in Great Poland under the first Waza kings, Zygmunt III (1587-1632) and Wladyslaw IV (1632-48). Both affirmed the 1573 Warsaw Confederation, ensuring all Christians freedom of confession as equal dissidentes de religione. In a Europe where wars were fought over religion, Polish toleration was exceptional, with implications for understanding the early modem church ...

  20. Does it pay to study abroad? Evidence from Poland

    OpenAIRE

    Liwiński, Jacek

    2017-01-01

    Purpose: This paper tries to identify the impact of international student mobility on the first wages of tertiary education graduates in Poland. Design/methodology/approach: The author uses data from the nationwide tracer survey of Polish graduates (Graduate Tracer Study 2007) and regresses the hourly net wage rate in the first job after graduating from a higher education institution (HEI) on a rich set of individuals' characteristics. In order to reduce the bias due to selection to internati...