Abstract
The effect of the boundary condition imposed on the underlying surface on the propagation of lava flows is studied in the case in which the non-Newtonian properties of the medium should be taken into account. The problem of lava spreading over a plane horizontal plane is solved. The no-slip condition on the underlying surface is replaced by the partial slip condition. The lava is modeled as a power-law fluid. The flow is assumed to be axisymmetric. In the thin layer approximation the problem reduces to the solution of one nonlinear partial differential second-order equation with an additional integral condition. In the case of the power-law time dependence of the lava flow rate a self-similar solution is obtained; however, it exists only under some constraints on the problem parameters. The non-self-similar solution is considered numerically. It is shown that the lava propagation velocity can be considerably higher, when the slip is taken into account.
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