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Untersuchungen über Zusammensetzung und Transport von Schwebstoffen in einigen Schweizer Flüssen

Bibliographic Data

ID18999994
AuthorsB E Peters-Kümmerly (corresponding author)
Year1973
Volume28
Issue3
Pages137-151
Publication date1973-09-30
Open AccessYes
TypeARTICLE
VenueGeographica Helvetica (JOURNAL)
Journal identifiersISSN: 0016-7312 • E-ISSN: 2194-8798
PublisherCopernicus Publications (PUBLISHER • DE)
DOI10.5194/gh-28-137-1973
OpenAlexW2318805771
LanguageDE
Citations received2

The amount and composition of suspended load from 19 stations in Swiss rivers werestudied. Generally, the correlation between the amount of suspended load and of water discharge is good, although measurements over short periods of time show large fluctuations. The denudation rate was calculated from the suspended load discharge, the amount of elements in Solution, and the water discharge. Values of about 0.05 mm/yr were obtained for drainage areas consisting mainly of crystalline rocks and about 0.25 mm/yr for drainage areas dominated by sedimentary rocks. The mineralogical composition of the suspended load determined by X-ray diffraction can be correlated with the rock types in the drainage areas. Composition changes resulting from transportation were not observed. The clay fraction is mainly composed of illite and chlorite which was, for the most part, formed during mechanical weathering in the Alps

Chlorite · Clay minerals · Denudation · Drainage · Geochemistry · Geomorphology · Geotechnical engineering · Hydrology (agriculture) · Illite · Kaolinite · Mineralogy · Quartz · Sedimentary rock · Tectonics · Weathering · Geology · Hydrology and Watershed Management Studies · Integrated Water Resources Management · Karst Systems and Hydrogeology

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Citations per year0.13
Citation span2011 - 2012 (2)
Highly citedNo

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