Research Article

A Coupled Thermo-Hydromechanical Model of Soil Slope in Seasonally Frozen Regions under Freeze-Thaw Action

Figure 9

Distribution of the slope moisture isoline at different times. (a) t = 193 d, T = 23.00°C; (b) t = 290 d, T = 0.18°C; (c) t = 375 d, T = −18.30°C; (d) t = 430 d, T = −9.76°C; (e) t = 459 d, T = −0.27°C; (f) t = 480 d, T = 7.14°C.
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