It is well known that many landslides, which occur every year in the world, are triggered by rainfall. The mechanics of slope movements due to pore pressure changes are not completely understood, however, and thus are the focus of this paper. Both the case of first-time slides and that of landslide reactivation are examined. It is shown that simple models can reproduce the processes of slope failure and may help in predicting slope behaviour
Rainfall is inevitably one of the main factors that trigger landslides. However, not much study has ...
Drains are widely used in civil engineering as control works against slope instability in saturated ...
The hydrologic behavior of shallow weathered soils commonly involved in slope failure is discussed. ...
It is well known that many landslides, which occur every year in the world, are triggered by rainfal...
It is well known that a large part of the landslides which every year occur in the world are trigge...
Landslides triggered by hydraulic perturbations are initiated by a decrease in the effective stress,...
Failures occurring along natural slopes often involve the shallow weathered horizon of soil and are ...
Field observations and theoretical analysis have been used in the literature to assess slope instabi...
Slow-moving landslides show complex mechanical and fluid interactions. They show among others non li...
Field observations and theoretical analysis have been used in the literature to assess slope instabi...
Hydrological processes, such as slope saturation by water, are a primary cause of landslides. This e...
Active slow-moving landslides in clayey soils exhibit continuous movements generally controlled, bot...
In slope stability research a ground water level increase is often the critical factor for failure....
Knowledge of the groundwater regime, which is generally necessary in studying the stability of slope...
Rainfall is inevitably one of the main factors that trigger landslides. However, not much study has ...
Drains are widely used in civil engineering as control works against slope instability in saturated ...
The hydrologic behavior of shallow weathered soils commonly involved in slope failure is discussed. ...
It is well known that many landslides, which occur every year in the world, are triggered by rainfal...
It is well known that a large part of the landslides which every year occur in the world are trigge...
Landslides triggered by hydraulic perturbations are initiated by a decrease in the effective stress,...
Failures occurring along natural slopes often involve the shallow weathered horizon of soil and are ...
Field observations and theoretical analysis have been used in the literature to assess slope instabi...
Slow-moving landslides show complex mechanical and fluid interactions. They show among others non li...
Field observations and theoretical analysis have been used in the literature to assess slope instabi...
Hydrological processes, such as slope saturation by water, are a primary cause of landslides. This e...
Active slow-moving landslides in clayey soils exhibit continuous movements generally controlled, bot...
In slope stability research a ground water level increase is often the critical factor for failure....
Knowledge of the groundwater regime, which is generally necessary in studying the stability of slope...
Rainfall is inevitably one of the main factors that trigger landslides. However, not much study has ...
Drains are widely used in civil engineering as control works against slope instability in saturated ...
The hydrologic behavior of shallow weathered soils commonly involved in slope failure is discussed. ...