基于计算流体力学的寒区土壤水热耦合模型研究
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Simulating thermo-hydrologic processes in cold region soil system: a computational fluid dynamics study
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图7. 冰包裹体融化算例在不同时刻的液态水饱和度演变 |
Fig.7. Melting of ice inclusion case: evolution of liquid water saturation at t=7 200 s (a), t=21 600 s (b), t=43 200 s (c), and t=64 800 s (d) |
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