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test_cases:seven [2014/12/19 14:26]
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test_cases:seven [2014/12/19 14:27]
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-Advection with constant velocity is here added to conduction and phase change. Analytical solution are proposed from Kurylyk et al. 2014 paper based on a reassessment of solutions by Lunardini. Although not physically realistic (constant velocity) these solutions can be used for benchmarking purposes: "Lack of fidelity to physical processes does not limit ability to serve as benchmark"+Advection with constant velocity is here added to conduction and phase change. Analytical solution are proposed from Kurylyk et al. 2014 paper based on a reassessment of solutions by Lunardini. Although not physically realistic (constant velocity independant of temperature) these solutions can be used for benchmarking purposes: "Lack of fidelity to physical processes does not limit ability to serve as benchmark"
  
 The paper Kurylyk et al. 2014 describes at depth the analytical solutions available, the suggested benchmark cases and SUTRA code runs to compare with these solutions. One may refer to "Analytical solutions for benchmarking cold regions subsurface water flow and energy transport models: One-dimensional soil thaw with conduction and advection" by B. Kurylyk, J. McKenzie, K. MacQuarrie, C. Voss in Advances in Water Resources 70 (2014) 172–184 The paper Kurylyk et al. 2014 describes at depth the analytical solutions available, the suggested benchmark cases and SUTRA code runs to compare with these solutions. One may refer to "Analytical solutions for benchmarking cold regions subsurface water flow and energy transport models: One-dimensional soil thaw with conduction and advection" by B. Kurylyk, J. McKenzie, K. MacQuarrie, C. Voss in Advances in Water Resources 70 (2014) 172–184