HIGHLIGHTS
SUMMARY
In the process of rainwater infiltration into the slope, the water content and weight of the soil mass increase, generating the seepage force and pore water pressure in the slope (Huang et_al 2022). Due to the vast uncertainty of natural slope materials, accurately quantifying the impact of rainfall on slope failures remains a major challenge, physical model test is still one of the most effective methods to study landslides. Chinkulkijniwat et_al established the relationship between the critical hydrological state, rainfall intensity, and soil properties according to the model test, analyzed the slope stability under . . .
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