Abstract
On the basis of the test definitions of specific isothermal mass capacity coefficient and analysis of mass transfer it was shown that moisture transfer in rock mass can be evaluated by the potential, offered by Tsimermanis L. B.
This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.
Copyright (c) 2021 O. Lanchava, Sh. Oniani
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