When groundwater head decreases by the value S, effective stresses in rocks increase by the value γ0S(γ0 - volumetric weight of water), as a result of which rocks undergo additional compression, which is accompanied by outflow of part of pore water.
How to cite:
Mironenko V.A., Serdyukov L.I., Kotov I.G. Influence of compressibility of “water-retaining” rocks on the filtration process in aquifers // Journal of Mining Institute. 1971. Vol. 62. Iss. 2. p. 39-46.
