Abstract
The problem of convection in a thin porous elliptic ring located in an impermeable rock mass is considered. The geothermal gradient is assumed to deviate by a certain angle α from the vertical axis of the ellipse. An analytic solution of the problem is obtained in the hydraulic approximation. The stability of the solutions obtained is investigated for a circular ring. The profile of the thermal anomaly in the outer mass due to convection in the contour is given.
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