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test_cases:seven [2014/12/19 11:10] grenier |
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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) these solutions can be used for benchmarking purposes: "Lack of fidelity to physical processes does not limit ability to serve as benchmark" | ||
- | The paper describes at depth the analytical solutions available, the suggested benchmark cases and SUTRA code runs to compare with these solutions. The recommanded benchmark 2 and 3 are included in the InterFrost project as TH1 cases (differing by flow velocities). The recommanded benchmark 1 (Neuman case) is an option to complement the Lunardini case provided as T1. | + | 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. The recommanded benchmark 2 and 3 are included in the InterFrost project as TH1 cases (differing by flow velocities). The recommanded benchmark 1 (Neuman case) is an option to complement the Lunardini case provided as T1. |
+ | One may refer to " | ||
+ | Another source is the presentation by Barret Kurylyk of these items for the kick off meeting ({{: | ||
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+ | Main points are summed up below. | ||
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+ | Initial and boundary conditions: | ||
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+ | {{ : | ||
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+ | Parameter set: | ||
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+ | Analytical solutions in {{: | ||
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+ | Approach used for SUTRA code: | ||
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+ | {{ : | ||
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- | in 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 |