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Tematem pracy jest ocena struktury ekologicznej wybranych gmin wiejskich Kotliny Sandomierskiej w celu określenia roli parków wiejskich w krajobrazie rolniczym. Badania przeprowadzono w obrębie dziewięciu gmin wiejskich, zlokalizowanych wzdłuż Wisły. Badania terenowe obejmują rozpoznanie typów ekosystemów według ich stopnia naturalności, a także określenie struktury pokrycia w badanych gminach. Do opracowania wyników badań wykorzystano program CORINE Land Cover 2006 (CLC), a także badania terenowe. W strukturze ekologicznej gmin dominują ciągi ekologiczne II i III rzędu. Korytarze ekologiczne mają charakter dolinny i leśny.
Life form spectrum is an informative parameter in a comparative analysis of ecological structure of Collembola communities, and a valuable indicator of conditions of soil environment. This suggests a search of adequate methods of its determination. In the present study, two methods of evaluation of life form spectra in springtail communities are compared. A usual approach is a determination of the species composition and abundance, with a subsequent formal distribution of the species present among the life form categories of a chosen system, e.g. among epedaphic, hemiedaphic and euedaphic life forms considered as dwellers of litter surface and upper horizon, of litter depth and topsoil, and of soil horizon, respectively (Hopkin 1997). By this method (A) all the specimens of a given species are attributed to the same life form. However, species populations contain juveniles with smaller body size, thinner cuticle and weaker pigmentation, which tend to be more sensitive to environmental constraints and to dwell deeper in soil than adults. Therefore the attribution of juveniles and adults of a given species to the same life form may not be accurate. Another approach is a direct attribution of a life form category to each collembolan individual during the determination process, according to the visual assessment of its morphological characters (body size and development of pigmentation, number and pigmentation of ommatidia). In that case representatives of a given species might be attributed to more than one life form category, e.g. adults to epedaphic whereas juveniles to hemiedaphic life form, or to hemi- and euedaphic life form, respectively (method B). To compare both methods, mass collembolan material of a microcosm experiment carried out in a beech-oak forest at Mikolajki Research Station (NE Poland) and aimed at investigation of mesofauna/ earthworm interactions, was used. The comparison showed a statistically significant bias between the spectra of Collembola life forms estimated by methods A and B: the latter spectrum was shifted to the favour of euedaphic forms. The range of the bias was larger in soil than in litter horizon. Method B is suggested to be closer to a real life form distribution in a collembolan community and may be used for corrections of the data obtained by the traditional taxonomic method A.
The main disturbancies in hydrological and chemical features of the Upper Vistula River were discussed as well as geological structure and soils of its drainage basin. Examined section of the river is 337 km long. Catchment area of 28 000 km² inhabited by 50 to 800 residents km⁻². Three main problems concerning the river were considered: salinity, pollution and water management. Between 89 and 95 km the river obtaines salty water from coal mines and down the 95 km of the river - huge load of pollution by the Przemsza River. The inflow supplying 91% of Vistulian flow at this point. This unusual proportion is caused by far transfer of drinking water from submontainous part of the Vistula or its tributaries. Polluted water comes back to the river by Przemsza River. Vistula had here too much of suspension, phosphorus, nitrite and ammonia, and sometimes zinc. Water quality between 90 and 170 km was useless for cyprinid fishes according to EC directive. Vistula River and its affluents flow through holocenic river terraces - covered with alluvial and fluvioglacial deposits. In the region of Cracow there are small areas of upper Jurassic origin (marls and lime) and from the Cretaceous period. Holocenic terrace of the river is covered by alluvial soils. On the left bank, between the Przemsza and Nida rivers, there are large areas of loesses. Investigations were carried out in the period between 3rd March 1997 and March 4th 1998. Also the present state of investigations of the Vistula River is discussed. In 1997 in the period from 7th to 15th of July extreme and disastrous flood in the Vistula occurred. Flows, which usually in Cracow (on 165 km) provide 50 to 100 m³ s⁻¹, grew up to 1430 m³ s⁻¹ and during the culmination of wave up to 2400 m³ s⁻¹.
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