1973
DOI: 10.1007/bf02377193
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Engineering-geologic justification of the planning of antiseepage measures

Abstract: The impervious curtains, screens, and upstream aprons of most of the existing dams were designed and constructed by taking into account, to a greater or lesser extent, the engineering-geologic and hydrogeologic conditious which characterized the seepage through the rock in contact with the structure. However, in most cases, the evaluation of these conditions was mainly of a qualitative nature. The writer does not know of any dams for which the parameters of the impervious elements, and primarily of the impervi… Show more

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Cited by 1 publication
(3 citation statements)
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“…An analysis of more than 500 experimental pourings and injections of water into boreholes at the Nurek hydro development site, whose foundation is composed of intercalating strata of sandstones and siltstones, and the Toktogul hydro development, where crystalline limestones are widespread, showed [2] that the magnitude of specific water absorption, calculated on the basis of discharge during the first 30 min of injection, is quite close to the results obtained upon stabilization of the discharge with an incremental duration of 3 h-The coefficient of correlation of the indicated quantities varies from 0.8 to 0.9, increasing for larger values of water absorption. Lykoshin [1] and L. P. Konyarova [3] arrived at the same conclusions. A.…”
supporting
confidence: 54%
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“…An analysis of more than 500 experimental pourings and injections of water into boreholes at the Nurek hydro development site, whose foundation is composed of intercalating strata of sandstones and siltstones, and the Toktogul hydro development, where crystalline limestones are widespread, showed [2] that the magnitude of specific water absorption, calculated on the basis of discharge during the first 30 min of injection, is quite close to the results obtained upon stabilization of the discharge with an incremental duration of 3 h-The coefficient of correlation of the indicated quantities varies from 0.8 to 0.9, increasing for larger values of water absorption. Lykoshin [1] and L. P. Konyarova [3] arrived at the same conclusions. A.…”
supporting
confidence: 54%
“…* Continuation of the discussion of A. G. Lykoshin's article [1]; see also the article of E. E. dallas and the editor's comment, Gidrotekhnicheskoe Stroitel 'stvo, No. 4, 38-42 (1974).…”
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confidence: 99%
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