Rainfall-induced slope failures commonly occur in the unsaturated zone above groundwater table in many steep residual soil slopes. Dynamic variations in groundwater table and flux boundary conditions across ground surface result in changes in pore-water pressure in the unsaturated zone. During a prolonged dry period, excessive evaporation and evapo-transpiration on the ground surface causes soil desiccation and tension cracks to develop on the slope surface, increasing permeability of soils near the ground surface. In addition, the groundwater table can go down to deeper depths during the dry period. As a result, pore-water pressures in the unsaturated zone will become more negative, contributing to the shear strength of soil. During a rain...
The combined effect of soil moisture in unsaturated soil layers and pore-water pressure in saturated...
In the past 30 years, research on rainfall-induced landslides has grown remarkably. The contribution...
The combined effect of soil moisture in unsaturated soil layers and pore-water pressure in saturated...
Rainfall-induced slope failures commonly occur in the unsaturated zone above groundwater table in ma...
Excessive rainfalls due to climatic changes can trigger an increase in rainfall-induced slope failur...
Excessive rainfalls due to climatic changes can trigger an increase in rainfall-induced slope failur...
Slope instability in unsaturated residual soils and loose fills has attracted increasing attention i...
Rainfall is identified as the factor for triggering slope failure and inducing leachate from a landf...
Rainfall is identified as the factor for triggering slope failure and inducing leachate from a landf...
Steep residual soil slopes are generally characterized by a deep ground water table and a significan...
Steep residual soil slopes are generally characterized by a deep ground water table and a significan...
Rainfall is the most important cause of slope failure. The variation in stress state of soils due to...
The combined effect of soil moisture in unsaturated soil layers and pore-water pressure in saturated...
The understanding of unsaturated soil mechanics principles is of interest to a wide spectrum of geot...
This paper presents results of saturated and unsaturated stability analysis of typical residual slop...
The combined effect of soil moisture in unsaturated soil layers and pore-water pressure in saturated...
In the past 30 years, research on rainfall-induced landslides has grown remarkably. The contribution...
The combined effect of soil moisture in unsaturated soil layers and pore-water pressure in saturated...
Rainfall-induced slope failures commonly occur in the unsaturated zone above groundwater table in ma...
Excessive rainfalls due to climatic changes can trigger an increase in rainfall-induced slope failur...
Excessive rainfalls due to climatic changes can trigger an increase in rainfall-induced slope failur...
Slope instability in unsaturated residual soils and loose fills has attracted increasing attention i...
Rainfall is identified as the factor for triggering slope failure and inducing leachate from a landf...
Rainfall is identified as the factor for triggering slope failure and inducing leachate from a landf...
Steep residual soil slopes are generally characterized by a deep ground water table and a significan...
Steep residual soil slopes are generally characterized by a deep ground water table and a significan...
Rainfall is the most important cause of slope failure. The variation in stress state of soils due to...
The combined effect of soil moisture in unsaturated soil layers and pore-water pressure in saturated...
The understanding of unsaturated soil mechanics principles is of interest to a wide spectrum of geot...
This paper presents results of saturated and unsaturated stability analysis of typical residual slop...
The combined effect of soil moisture in unsaturated soil layers and pore-water pressure in saturated...
In the past 30 years, research on rainfall-induced landslides has grown remarkably. The contribution...
The combined effect of soil moisture in unsaturated soil layers and pore-water pressure in saturated...