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- W2023275028 abstract "Tests in three different areas of the Austrian Alps showed that in mountainous areas, soil samples taken at the break of slope are an alternative sampling medium to stream sediments for regional geochemical exploration even if taken at the unusually low density of 1 sample/km2. B-horizon soil samples from the nearest break of slope were collected in conjunction with stream sediment orientation studies. The minus 0.2 mm fraction of all samples was routinely analyzed for the total contents of 36 elements. The results for the indicator elements in the three test areas (Area 1: Cu; Area 2: Ag, As, Cu, Pb, Sb, Sn, Zn; Area 3: As, Cu) showed that break-of-slope soil samples more clearly indicate known mineralization than drainage geochemistry. In the soils, almost all elements showed a higher natural variability of the data with considerably higher metal contents. In mountaineous regions, each soil sample will have a clearly defined area of influence. The break of slope represents a site where clastically and hydromorphically dispersed elements are concentrated. It is concluded that soil samples can be used for regional exploration using low sampling densities in mountaineous areas. At the same time they will provide valuable information for other fields of science (e.g. agriculture, forestry, environmental sciences) and are thus superior to stream sediments." @default.
- W2023275028 created "2016-06-24" @default.
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- W2023275028 date "1988-12-01" @default.
- W2023275028 modified "2023-10-16" @default.
- W2023275028 title "Comparison of stream sediment and soil sampling for regional exploration in the eastern Alps, Austria" @default.
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- W2023275028 doi "https://doi.org/10.1016/0375-6742(88)90038-6" @default.
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