Abstract
The application of a hydrodynamic model of the two-velocity media flow of to non-stationary problems of the heterophase flows motion in channels is considered. Various flow regimes of such media are studied for given penetration rates for initially inhomogeneous flow at various values of channel inclination.
The presented mathematical model can be used for describing various types of geological fluid, fluid-magmatic, hydrothermal systems, as well as for describing convective heat and mass transfer in ore-magmatic systems.
Keywords
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