A THERMODYNAMICALLY CONSISTENT MODEL OF A SOLVENT SUBSTANCE TRANSPORT IN A POROELASTIC CLAY SHALE
B. ImomnazarovNovosibirsk National Research State UniversityПетр В. КоробовFederal State Budgetary Institution Arctic and Antarctic Research (AARI)Ilkhom KhaydarovNational University of Uzbekistan named after Mirzo Ulugbek (NUUz)
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Аннотация
In this paper, we discuss a chemically inert elastically deformable rock with allowance for only changes in the stress and the pore pressure: the chemistry of a porous fluid does not directly affect deformation [1]. In such a situation, chemical effects affect a change in the pore pressure and in the rock deformation. This theory has been applied for mathematical modeling of the solvent and solute transport through a semi-permeable shale.
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