Rainfall-induced landslide is one of the most destructive natural disasters that can jeopardize public safety and lead to costly repair works. This natural disaster occurs frequently in residual soil slopes in many tropical areas. Infiltrating water from rainfall events enter the slope, resulting in a decrease of matric suction due to an increase in pore-water pressure in the slope, which in turns reduce the shear strength of the soil. Capillary Barrier, a fine-grained soil layer (overlying layer) placed over a coarse-grained layer (underlying layer), appears to have high potential to be used in slope to prevent or minimize rainwater infiltration. The difference in particle or pore sizes between the fine-grained layer and the...
Residual soil slope failure due to rainfall infiltration is one of geotechnical hazards receiving mu...
Rainfall induced slope failure is prevalent in tropical countries for instance, Singapore where lan...
Rainfall-induced slope failures commonly occur in residual soil slopes. Slope failures are triggered...
A capillary barrier as a cover system is a two‐layer system of distinct hydraulic properties to prev...
A capillary barrier is a two-layer cover system having distinct hydraulic properties to minimize wat...
A capillary barrier is a two-layer cover system having distinct hydraulic properties to minimize wat...
Slope instability due to rainfall infiltration constitutes major natural disasters in many tropical ...
Slope instability due to rainfall infiltration constitutes major natural disasters in many tropical ...
Capillary barrier system (CBS) is a soil cover system which consists of two layers of soil with dist...
Rainfall-induced slope failures frequently occur in residual soil slopes in tropical regions. Previo...
Rainfall-induced slope failures frequently occur in residual soil slopes in tropical regions. Previo...
Rainfall-induced slope failures commonly occur in residual soil slopes. Slope failures are triggered...
Slope instability is often caused by decreases in suction due to heavy and prolonged rainfall. In th...
The most common cause of slope instability is intense or sustained rainfall, which may induce reduct...
Rainfall induced slope failure is prevalent in tropical countries for instance, Singapore where lan...
Residual soil slope failure due to rainfall infiltration is one of geotechnical hazards receiving mu...
Rainfall induced slope failure is prevalent in tropical countries for instance, Singapore where lan...
Rainfall-induced slope failures commonly occur in residual soil slopes. Slope failures are triggered...
A capillary barrier as a cover system is a two‐layer system of distinct hydraulic properties to prev...
A capillary barrier is a two-layer cover system having distinct hydraulic properties to minimize wat...
A capillary barrier is a two-layer cover system having distinct hydraulic properties to minimize wat...
Slope instability due to rainfall infiltration constitutes major natural disasters in many tropical ...
Slope instability due to rainfall infiltration constitutes major natural disasters in many tropical ...
Capillary barrier system (CBS) is a soil cover system which consists of two layers of soil with dist...
Rainfall-induced slope failures frequently occur in residual soil slopes in tropical regions. Previo...
Rainfall-induced slope failures frequently occur in residual soil slopes in tropical regions. Previo...
Rainfall-induced slope failures commonly occur in residual soil slopes. Slope failures are triggered...
Slope instability is often caused by decreases in suction due to heavy and prolonged rainfall. In th...
The most common cause of slope instability is intense or sustained rainfall, which may induce reduct...
Rainfall induced slope failure is prevalent in tropical countries for instance, Singapore where lan...
Residual soil slope failure due to rainfall infiltration is one of geotechnical hazards receiving mu...
Rainfall induced slope failure is prevalent in tropical countries for instance, Singapore where lan...
Rainfall-induced slope failures commonly occur in residual soil slopes. Slope failures are triggered...