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test_cases:seven [2014/07/29 18:00] grenier |
test_cases:seven [2014/12/19 14:28] grenier |
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- | Advection with constant velocity is added to conduction and phase change. Analytical solution from Kuryly | + | Advection with constant velocity is here added to conduction and phase change. Analytical solution |
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+ | 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 " | ||
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+ | A presentation of the TH1 Case by Barret Kurylyk was made during the kick off meeting ({{: | ||
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+ | The recommanded benchmark Kurylyk et al 2014 Cases 2 and 3 are included in the InterFrost project as two TH1 cases differing by the flow velocity considered: Velocities of 10 and 100 m/yr should be considered. | ||
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+ | Benchmark 1 (Neuman case) recommanded by Kurylyk et al 2014 is an option to complement the Lunardini case provided in the InterFrost project as T1. | ||
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+ | **TH1 Test Case** | ||
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+ | Initial and boundary conditions: | ||
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+ | Parameter set: | ||
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+ | The analytical solutions of Kurylyk et al 2014 are accessible here as as xls {{: | ||
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+ | The approach used for SUTRA code is summed up in two figures from Kurylyk et al 2014 as a source of inspiration. They provide the simulated domain and the approach for the freezing curve function in order to approximate the step function with a linear curve: | ||
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- | Paper 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 |