Abstract
Variations in the hydraulic and mechanical behaviour of soils caused by rainfall infiltration are major causes of slope failure. In previous studies, hydraulic hysteresis was commonly ignored to simplify seepage analysis, but this can cause an inaccurate representation of the hydromechanical behaviour of soils and the stability of the associated slopes. In the present study, the effects of hysteretic soil water characteristic curves (SWCC) on the hydromechanical behaviour and slope stability associated with rainfall were assessed, and the results were compared with those obtained using the non-hysteretic SWCC. Hysteresis associated with the capillary and air entrapment effects was considered, and these were incorporated into the analysis of the hydromechanical framework. The hydraulic response and slope stability were analyzed using numerical modelling. Effects of the hydraulic hysteresis on the hydromechanical behaviour within the slope under transient rainfall conditions were then explored. The infiltration fluxes linked to the non-hysteresis and hysteresis conditions differ, impacting the water flow regime and slope stability. Hysteresis involving higher air entrapment shortens the failure time compared to the non-hysteresis condition. The present study demonstrates that hydraulic hysteresis involving air entrapment is important for an adequate assessment of the hydromechanical response of silty soil and the stability of the associated slope.
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Ya-Sin Yang: Conceptualization, data analysis, simulation, and interpretation, mythology, writing-original draft, visualization; Hsin-Fu Yeh: Supervision, conceptualization, writing-reviewing and editing.
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Yang, YS., Yeh, HF. Effects of hysteretic soil water characteristic curves on the hydromechanical behaviour. J Earth Syst Sci 132, 136 (2023). https://doi.org/10.1007/s12040-023-02146-6
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DOI: https://doi.org/10.1007/s12040-023-02146-6