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Rossella Bovolenta, Alessandro Iacopino, Roberto Passalacqua and Bianca Federici
Monitoring changes in soil saturation is important for slope stability analyses. Soil moisture capacitive sensors have recently been developed; their response time is extremely fast, they require little maintenance, and they are relatively inexpensive. T...
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Thilanki Dahigamuwa, Manjriker Gunaratne and Mingyang Li
The infiltration of rainwater into soil slopes leads to an increase of porewater pressure and destruction of matric suction, which causes a reduction in soil shear strength and slope instability. Hence, surface moisture and infiltration properties must b...
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Raül Oorthuis, Marcel Hürlimann, Alessandro Fraccica, Antonio Lloret, José Moya, Càrol Puig-Polo and Jean Vaunat
Slope mass-wasting like shallow slides are mostly triggered by climate effects, such as rainfall, and soil?vegetation?atmosphere (SVA) interactions play a key role. SVA interactions are studied by a full-scale embankment with different orientations (Nort...
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Marisol Lara,Sergio A. Sepúlveda,Constanza Celis,Sofía Rebolledo,Pablo Ceballos
Pág. 433 - 442
The urban expansion of Santiago city includes areas with geomorphological and geological conditions with potential to be affected by landslide processes. This work presents compiled landslide susceptibility maps for the Andean foothills of Santiago city,...
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Oreste Terranova, Stefano Luigi Gariano, Pasquale Iaquinta, Valeria Lupiano, Valeria Rago and Giulio Iovine
GASAKe is an empirical-hydrological model aimed at forecasting the time of occurrence of landslides. Activations can be predicted of either single landslides or sets of slope movements of the same type in a homogeneous environment. The model requires a r...
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J. Michael Johnson and Hugo A. Loáiciga
Shallow translational slides are common in slopes during heavy rainfall. The classic model for the occurrence of translational slides in long slopes assumes rising saturation above a slip surface that reduces the frictional strength by decreasing the eff...
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