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)
ABI
Abstract
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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