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Forecasting the reworking of karstic shores of reser voirs composed of sulfate rocks
Conclusions 1. The development of sulfate karstic shores on reservoirs differs fundamentally from the development of shores composed of sand-gravel rocks. 2. Reworking of karstic shores occurs mainly due to solution of rock. Since they consist of 85–95% CaSO4. 2H2O, no abrasion shoal is formed near the shores. Clay particles in suspension are carried away into the reservoir. 3. The unique character of shore destruction and the absence of inshore shoals (benches) cause the unabating rate of the process. 4. The linear relation between the volume of caved and dissolved rocks and time permits predicting destruction of a previously unobserved section of the shore, which is especially important for occassional geological engineering investigations on the shores of reservoirs.
Forecasting the reworking of karstic shores of reser voirs composed of sulfate rocks
Conclusions 1. The development of sulfate karstic shores on reservoirs differs fundamentally from the development of shores composed of sand-gravel rocks. 2. Reworking of karstic shores occurs mainly due to solution of rock. Since they consist of 85–95% CaSO4. 2H2O, no abrasion shoal is formed near the shores. Clay particles in suspension are carried away into the reservoir. 3. The unique character of shore destruction and the absence of inshore shoals (benches) cause the unabating rate of the process. 4. The linear relation between the volume of caved and dissolved rocks and time permits predicting destruction of a previously unobserved section of the shore, which is especially important for occassional geological engineering investigations on the shores of reservoirs.
Forecasting the reworking of karstic shores of reser voirs composed of sulfate rocks
Pecherkin, I. A. (Autor:in)
Hydrotechnical Construction ; 2 ; 1060-1063
01.12.1968
4 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
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