Influence of compressibility of “water-retaining” rocks on the filtration process in aquifers
Abstract
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.
Область исследования:
(Archived) Without section
Funding:
None
References
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