Abstract
The filtration model of the hydrate-equilibrium zone (HEZ) in the mixture of liquid-ice solutions and gas with possible solid-phase salt sedimentary inclusions in a porous medium is studied. Various types of saturating the liquid-ice mixture with gas and salt, as well as salt sediment in HEZ in the absence of a liquid phase are considered. Based on the Gibbs phase rule, various types of dissociative bonds between thermodynamic variables in the problems under consideration are determined for systems with one thermodynamic degree of freedom.
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