The application of a finite volume multigrid method to three-dimensional flow problems in a highly viscous fluid with a variable viscosity

被引:60
作者
Trompert, RA
Hansen, U
机构
[1] Institute of Earth Sciences, 3508 TA, Utrecht
关键词
earth's mantle; mantle convection; infinite Prandtl number; numerical simulation; finite volume discretization; multigrid methods;
D O I
10.1080/03091929608208968
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
In this paper we discuss the application of a finite-volume multigrid method to solve three-dimensional thermally driven convection in a highly viscous, incompressible fluid with a variable viscosity. The conservation laws are solved in the primitive variable formulation. A second-order control volume method is used as discretization. Two schemes are used for time stepping, a second-order implicit-explicit scheme based on the Crank-Nicolson and Adams-Bashforth method, and a fully-implicit theta-method. The implicit system of nonlinear equations are solved using multigrid iteration with the SIMPLER method as smoother. In this paper, we describe the implemented multigrid method and investigate its efficiency and the robustness for different viscosity contrasts. fs. Convergence tests showed that with a small modification of the SIMPLER method, the multigrid method exhibits a satisfactory convergence rate even for viscosity contrasts up to 10(9). Three cases of time-dependent thermally driven convection with viscosity contrasts up to 10(5) are considered and discussed and the multigrid method has demonstrated its robustness also for these cases. Further, we have also compared the computational efficiency of the two time stepping methods. It appeared that the fully-implicit scheme is a little more efficient than the implicit-explicit scheme for a constant viscosity and it was considerably more efficient for a viscosity contrast of 10(3).
引用
收藏
页码:261 / 291
页数:31
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