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Ecological conflicts in Poland 总被引：1，自引：0，他引：1
Transformation of the political system, observed in Poland for 10 years in connection with economic restructuring and basic
socio-economic reforms to harmonise with European Union structures, is also evident in terms of environmental management.
Pollution has been reduced in many ways but the rise in living standards, linked with the rapid growth of cars and other forms
of consumption, has had a negative effect and environmental conditions have deteriorated in the central areas of large cities.
The growth of waste water and refuse is a considerable problem. More areas are now officially protected and the three levels
of local government established at the beginning of January 1999 (voivodeship, district and community) all have certain defined
environmental protection responsibilities which are cumulatively greater than before. Meanwhile there is a greater awareness
in society of environmental issues, although it does not yet lead to a high level of participation in protection work. However,
there are strongly-expressed opinions on the ecological acceptability of certain economic developments and conflicts are frequently
arising within communities and local governments and also between investors on the one side and ecological organisations and
environmental protection institutions on the other. Most controversial are new roads, power stations (like the Zarnowiec nuclear
project) and reservoirs like the one on the Dunajec river at Czorsztyn. Local communities frequently resist plans for waste
dumps, incinerating plants and other developments which are seen as injurious to health or the quality of life. The planned
reprivatisation of the state-owned forests is also criticised by foresters and ecological movements. Conflicts are likely
to grow as economic development accelerates but better information and greater public understanding of the need for sustainability
should make for consensus.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
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We discuss Arp's hypothesis that the HII regions are more numerous and more conspicuous on the side of a galaxy facing its companion. Arp's hypothesis seems not to be true if we add to Hodge's sets of galaxies only the most probably tidally-interacting cases. 相似文献
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Krzysztof Pleskot Rik Tjallingii Mirosław Makohonienko Norbert Nowaczyk Witold Szczuciński 《Journal of Paleolimnology》2018,59(4):443-459
Western Poland is located in the central European climatic transition zone, which separates the mild and humid Atlantic climate of Western Europe and the East European continental climate. This region is sensitive to lateral shifts of the European climate zones and is particularly suitable for reconstructing Holocene climate variability. This paper presents detailed analyses of the sedimentary record from Lake Strzeszyńskie since the Late Pleistocene. These include smear-slide and thin-section observations, X-ray fluorescence core scanning, magnetic susceptibility measurements, pollen analyses, and radiocarbon dating. The sediment record reveals three distinct sedimentary units consisting of: (1) an alternation of sand layers and laminated silt and clay deposits accumulated prior to 14,600 cal yr BP; (2) faintly laminated calcareous sediments intercalated with organic matter-rich layers deposited between 14,600 and 10,200 cal yr BP; and (3) massive calcareous mud deposited after 10,200 cal yr BP. The Holocene period is marked by nine phases of organic-rich sedimentation and enhanced Fe deposition, which occurred at ca. 10.1, 9.3, 6.4–6.1, 5.5–5.1, 4.7–4.5, 2.7–2.4, 1.3–1.2, 0.8–0.6, 0.4–0.2 kyr cal BP. These phases are associated with high lake levels and correspond with wet periods recognized in several other records from Poland and central Europe. These phases partly coincide with North Atlantic cold periods, which may suggest that high lake levels are triggered by an ocean-continent linking mechanism. 相似文献
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Mirosław Jastrzębski 《International Journal of Earth Sciences》2009,98(8):1901-1923
Structural, petrological and geochronological data from marbles and mica schists combined with those from highly disputable
gneisses and eclogites of the Orlica-Śnieżnik Dome (OSD), gave new insights into Variscan evolution of eastern borderland
of the West Sudetes. It is shown that the Variscan tectonometamorphic evolution of the OSD began with E–W oriented subhorizontal
shortening (D1 stage) related to the collision of the West Sudetes terranes and the Brunovistulian terrane. The shortening
led to generally upright folding, which resulted in formation of the steep N–S trending metamorphic planar fabric S1, thickening
of the lithosphere and burial of the Stronie Formation under greenschist facies conditions. As a consequence of subsequent,
near-coaxial gravity-controlled vertical shortening (D2), the S1 foliation was deformed in tight recumbent folds F2. The flattening
strain was associated with the progression to amphibolite-facies conditions (from ca. 510 upto ca. 620°C) and uplift from
depths corresponding to 9–10 kbar to depths corresponding to 7–8 kbar. On microscale, the flattening strain is documented
by rotation of the mineral fabric overgrown by syn-D2 prograde garnet porphyroblasts. The Sm–Nd Grt–WR isochron age, correlated with the D2 event yields 346.5 ± 4.4 Ma. Further
deformation and progressive metamorphism led to development of the subhorizontally disposed S2 axial plane schistosity, which
terminated at the metamorphic temperature peak. During retrogression but still under ductile conditions of deformation, the
S2 planes were reactivated during successive top-to-the-N shear movement of the OSD (D3 stage). Due to the mutual interaction
of the OSD with the adjacent terranes the shear deformations were localized within marginal parts of these units. Finally,
as a result of the NE–SW and the NW–SE oriented shortenings (D4 stage and D5 stage, respectively), both the structural surfaces
and metamorphic isograds were regionally folded with W(NW)-ward plunges. A synthesis of new and existing data shows an overall
similarity in sequence of Variscan deformations (D1–D2–D3) in the West Sudetes borderland to that observed in the eastern
flank of the Moldanubian domain. 相似文献
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Environmental and land use factors affecting phosphate hysteresis patterns of stream water during flood events (Carpathian Foothills,Poland) 总被引：1，自引：0，他引：1
Flood events play a substantial role in the circulation of catchment phosphate (PO43?). The purpose of the research was to analyze the factors determining PO43? hysteresis patterns (direction and width) during four types of floods: short and long rainfall floods and snowmelt floods on frozen and thawed soil. The research took place in small catchments (forested, agricultural, mixed‐use) in the Carpathian Foothills in Poland. Anticlockwise hysteresis was identified in the forested catchment during short and long rainfall floods. Under the same conditions, the clockwise direction was observed in the agricultural catchment. In the mixed‐use catchment, the direction of PO43? hysteresis loops was various, driven by the share of water flowing from each part of the catchment. For snowmelt floods, the PO43? hysteresis pattern was similar in all the streams studied (usually clockwise). The direction of PO43? hysteresis loops depends on water circulation patterns, which are determined by the different influx times of particular runoff components. The stream recharge mechanism during a flood event is affected both by the factor initiating the event (precipitation, snowmelt) as well as by land use in the given catchment. Hysteresis loop width was determined by the pool of PO43? in a given catchment during the time period immediately preceding a flood event as well as by the quantity of PO43? flushed out of the soil. The greater a catchment's pool of PO43? and the greater its ability to flush PO43? out of the soil and into surface flow, the wider the hysteresis loops. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献
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Joanna Mirosław-Grabowska Monika Niska Elwira Sienkiewicz 《Journal of Paleolimnology》2009,42(4):467-481
We present isotope, cladoceran and diatom results from investigations of Eemian sediments of the palaeolake at Ruszkówek,
central Poland. Our analyses of the 15-m-thick sediments indicate that sandy silts occur on the bottom, followed by calcareous
gyttja, interbedded with lake marl. The upper part of the sequence contains peat and peaty sands. Values of δ18O change from −9.4‰ to −3.3‰ and δ13C values oscillate between −3.2‰ and +7.0‰. Nine isotope zones (Is) were defined and characterized using stable isotope analysis
of carbonates. Fifteen species of subfossil Cladocera were found and six faunal zones were distinguished (Cladocera zones).
One hundred and twenty-three diatom taxa, representing 31 genera were identified, enabling us to discern six Diatom Assemblage
Zones. The isotope, cladoceran, and diatom data correlate well with pollen data that define seven phases of evolution of the
palaeolake at Ruszkówek. The palaeolake began during the final phase of the Wartanian (Late Saalian Glaciation). During the
early Eemian, the palaeolake reached its maximum depth. During the Early Vistulian glaciation, the palaeolake declined. Changes
in the cladoceran and diatom communities indicate initial oligotrophic conditions in the lake, then an increase to mesotrophy,
and finally eutrophic conditions. 相似文献
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Constraining the time span between the Early Holocene Hässeldalen and Askja‐S Tephras through varve counting in the Lake Czechowskie sediment record,Poland 
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