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Vol 34 Iss. 2
Pages:
80-93
Download volume:
RUS
Article

Tentative determination of water permeability coefficient of fractured rocks by washing fluid absorption

Authors:
E. E. Kerkis
Date submitted:
1957-08-12
Date accepted:
1957-10-11
Date published:
1958-09-27

Abstract

Absorption of washing fluid is a clear sign of water permeability of rocks passed by boreholes. It is especially important to take into account the absorption of flushing fluid by fractured and karsted rocks, where the absorption of even clay solutions is often significant and can be used for preliminary judgment of the water permeability of these rocks (before the production of experimental hydrogeological work).

Область исследования:
(Archived) Without section
Funding:

None

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References

  1. Pavlovsky N.N. Hydraulic Reference Book. ONTI, 1937. (in Russian)
  2. Shchelkachev V.N. and Lapuk B.B. Underground Hydraulics. Gostoptekhizdat, 1949. (in Russian)
  3. Shchelkachev V.N. Elastic mode of formation water-supply systems. Gostoptekhizdat, 1948 (in Russian)
  4. Shishchenko R.I. Hydraulics of Clay Solutions. Aznefteizdat, 1951. (in Russian)
  5. Shishchenko R.I. and Baklanov B.D. . Azerbaydzhanskoe neftyanoe khozyaystvo, 1932, No. 7. (in Russian)
  6. Kerkis E.E. To the question of groundwater movement in fractured rocks, Zapiski Gornogo Instituta, 1948, vol. XXII. (in Russian)
  7. Kerkis E.E. Determination of the radius of influence in the calculation of water inflows. Uglegrotekhizdat, 1955. (in Russian)

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