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Summary Permeabilities of Paleozoic and Mesozoic rocks in the western mountain areas of Germany have been tested and observed on a large scale basis for applied engineering purposes during the last 10 years. Data of fracture-measurements, water pressure tests, pumping tests, dye tests, run-off measurements (springs, rivers, tunnels) and seepage losses of dams have been evaluated and compiled in a synoptic nomogram, classified in decimal steps of permeability-coefficients and attributed to the differnt rock types.
Summary Permeabilities of Paleozoic and Mesozoic rocks in the western mountain areas of Germany have been tested and observed on a large scale basis for applied engineering purposes during the last 10 years. Data of fracture-measurements, water pressure tests, pumping tests, dye tests, run-off measurements (springs, rivers, tunnels) and seepage losses of dams have been evaluated and compiled in a synoptic nomogram, classified in decimal steps of permeability-coefficients and attributed to the differnt rock types.
Determination of regional rock-mass permeabilities
Krapp, L. (Autor:in)
1982
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
BKL:
56.00$jBauwesen: Allgemeines
/
38.58
Geomechanik
/
38.58$jGeomechanik
/
56.20
Ingenieurgeologie, Bodenmechanik
/
56.00
Bauwesen: Allgemeines
/
56.20$jIngenieurgeologie$jBodenmechanik
RVK:
ELIB18
Determination of regional rock-mass permeabilities
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