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- W2186440496 abstract "The studies were carried out within a catena of loess soils of the West Roztocze region. These are typical grey-brown podzolic soils (Haplic Luvisols) in various stages of erosion and deluvial soil (Eutric Fluvisol). Research shows the great variation in the morphology and the physical-chemical properties of the soils. Differences observed included the content of humus, range of soil reaction, depth of decalcification, hydrolytic acidity, and the content of exchangeable cations. The reasons for such a differentiation lie in various forms of economic human influence on the surface formations of the lithosphere, including the soil cover, occurring both now and in the past. The soils derived from loess formations, and due to their specific character on the one hand show properties favourable to plant cultivation, and on the other a significant susceptibility to degradation, caused mainly by erosion processes. These have formed, and still do, an agreeable research field for many soil-scientists (2,4-8,10,12,14-17,19). The definition of loess as a rock formation, as well as the genesis, stratigraphy, and classification of loess soils formed the subjects of research for many geographers. Detailed research on the loess soils in the Lublin Upland region and partly in the West-Volhynia region, and especially the research carried out in the catena structures, showed that there is not always a clear relation between the morphology and properties of the investigated soils and the contemporary relief (5,7). Therefore, the main aim of this paper was to investigate and present the described relations for the example of the selected loess soil catena in the West Roztocze" @default.
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- W2186440496 date "2006-01-01" @default.
- W2186440496 modified "2023-10-18" @default.
- W2186440496 title "CHANGES IN THE PROPERTIES OF THE ERODED LOESS SOILS CULTIVATED SINCE THE 18th CENTURY" @default.
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