The paper discusses first the effect of rainfall on the stability of slopes and it focusses on the role of permeability. Existing or induced discontinuities are shown to have a remarkable effect on the slope safety. Also, the relevance of changes in hydraulic properties in weathered profiles is discussed through a real case. The performance of modern “Lagrangian particle” methods and their capabilities to deal with large displacements is presented. The cases solved refer to brittle materials, a common situation in overconsolidated high plasticity clays.Peer ReviewedPostprint (published version
Rainfall is one of the most common triggering factors of landslides. Due to the usual large extensio...
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...
AbstractThe paper discusses first the effect of rainfall on the stability of slopes and it focusses ...
The paper discusses first the effect of rainfall on the stability of slopes and it focusses on the r...
AbstractThe paper discusses first the effect of rainfall on the stability of slopes and it focusses ...
The need to predict the conseq uences of atmospheric conditions on the stability of slopes is widely...
During intense and persistent rainfall events, shallow landslides are frequently triggered in mounta...
The topic of this thesis is the quantification of the influence of preferential flow on landslide-tr...
The topic of this thesis is the quantification of the influence of preferential flow on landslide-tr...
Atmospheric phenomena such as rainfall and evapotranspiration contribute to slope movements in unsat...
The behaviour of natural and artificial slopes is controlled by their thermo-hydro-mechanical condit...
The behaviour of natural and artificial slopes is controlled by their thermo-hydro-mechanical condit...
Seepage and slope stability issues concerning infiltration in unsaturated slopes are investigated an...
Rainfall is recognized as a major precursor of many types of slope movements. The technical literatu...
Rainfall is one of the most common triggering factors of landslides. Due to the usual large extensio...
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...
AbstractThe paper discusses first the effect of rainfall on the stability of slopes and it focusses ...
The paper discusses first the effect of rainfall on the stability of slopes and it focusses on the r...
AbstractThe paper discusses first the effect of rainfall on the stability of slopes and it focusses ...
The need to predict the conseq uences of atmospheric conditions on the stability of slopes is widely...
During intense and persistent rainfall events, shallow landslides are frequently triggered in mounta...
The topic of this thesis is the quantification of the influence of preferential flow on landslide-tr...
The topic of this thesis is the quantification of the influence of preferential flow on landslide-tr...
Atmospheric phenomena such as rainfall and evapotranspiration contribute to slope movements in unsat...
The behaviour of natural and artificial slopes is controlled by their thermo-hydro-mechanical condit...
The behaviour of natural and artificial slopes is controlled by their thermo-hydro-mechanical condit...
Seepage and slope stability issues concerning infiltration in unsaturated slopes are investigated an...
Rainfall is recognized as a major precursor of many types of slope movements. The technical literatu...
Rainfall is one of the most common triggering factors of landslides. Due to the usual large extensio...
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...