Three-dimensional benchmark for variable-density flow and transport simulation: matching semi-analytic stability modes for steady unstable convection in an inclined porous box

被引:0
|
作者
Voss, Clifford I. [1 ]
Simmons, Craig T. [2 ]
Robinson, Neville I. [2 ]
机构
[1] US Geol Survey, Reston, VA 20192 USA
[2] Flinders Univ S Australia, Adelaide, SA 5001, Australia
关键词
Analytical solutions; Groundwater density/viscosity; Numerical modeling; Benchmark; Variable-density groundwater; EVAPORATING SALT LAKE; NUMERICAL-SIMULATION; GROUNDWATER-FLOW;
D O I
10.1007/s10040-009-0556-6
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This benchmark for three-dimensional (3D) numerical simulators of variable-density groundwater flow and solute or energy transport consists of matching simulation results with the semi-analytical solution for the transition from one steady-state convective mode to another in a porous box. Previous experimental and analytical studies of natural convective flow in an inclined porous layer have shown that there are a variety of convective modes possible depending on system parameters, geometry and inclination. In particular, there is a well-defined transition from the helicoidal mode consisting of downslope longitudinal rolls superimposed upon an upslope unicellular roll to a mode consisting of purely an upslope unicellular roll. Three-dimensional benchmarks for variable-density simulators are currently (2009) lacking and comparison of simulation results with this transition locus provides an unambiguous means to test the ability of such simulators to represent steady-state unstable 3D variable-density physics.
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页码:5 / 23
页数:19
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