Investigating the effect of Antecedent Rainfall on Pore-Water Pressure Distribution Characteristics in Residual Soil Slopes under Tropical Rainfall

The main characteristics of fluctuations in pore-water pressure distribution are connected with unsaturated soil slope instability. Flux boundary conditions at the soil–atmosphere interface have a direct impact on them (rainfall infiltration, evaporation, and evapo-transpiration). Two slopes at the Universiti Teknologi

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