Landslides in partially saturated pyroclastic slopes are strongly linked to rainwater infiltration, which is the main factor responsible for pore pressure and shear strength variations in shallow subsoil. Monitoring of the groundwater regime allows the most critical period for slope stability to be identified and the rela-tionship between critical pore pressure and rainfall to be explored. This paper de-scribes the monitoring of an unsaturated pyroclastic slope instrumented at Monteforte Irpino in southern Italy (Pirone et al., 2010), where suction and volu-metric water content measured at different depths were collected from 2006 to 2011. Using this database, typical aspects of the groundwater regime are de-scribed. The maximum water conte...
We monitored positive pore water pressure in a clay slope in the Apennines to investigate how rainfa...
In Orvieto (central Italy), overconsolidated clay slopes are affected by intermittent slow movements...
Hydrological monitoring of slope susceptible to shallow landslides allows for identifying the trigge...
Landslides in partially saturated pyroclastic slopes are strongly linked to rainwater infiltration, ...
Slope failures in partially saturated pyroclastic slopes are often induced by rainwater infiltration...
Slope failures in partially saturated pyroclastic slopes are often induced by rainwater infiltration...
In the last 15 years, a series of catastrophic flowslides involving pyroclastic unsaturated soils ha...
In Campania (Italy) there have been rapid landslides in recent decades caused by heavy rainfall on u...
Flowslides in granular soils pose a major threat to life and the environment. Their initiation in un...
Rainwater infiltration is the major cause of failure in unsaturated slopes. Analyses carried out to ...
Slopes covered with unsaturated shallow pyroclastic deposits, lying upon fractured limestone bedrock...
We monitored positive pore water pressure in a clay slope in the Apennines to investigate how rainfa...
In Orvieto (central Italy), overconsolidated clay slopes are affected by intermittent slow movements...
Hydrological monitoring of slope susceptible to shallow landslides allows for identifying the trigge...
Landslides in partially saturated pyroclastic slopes are strongly linked to rainwater infiltration, ...
Slope failures in partially saturated pyroclastic slopes are often induced by rainwater infiltration...
Slope failures in partially saturated pyroclastic slopes are often induced by rainwater infiltration...
In the last 15 years, a series of catastrophic flowslides involving pyroclastic unsaturated soils ha...
In Campania (Italy) there have been rapid landslides in recent decades caused by heavy rainfall on u...
Flowslides in granular soils pose a major threat to life and the environment. Their initiation in un...
Rainwater infiltration is the major cause of failure in unsaturated slopes. Analyses carried out to ...
Slopes covered with unsaturated shallow pyroclastic deposits, lying upon fractured limestone bedrock...
We monitored positive pore water pressure in a clay slope in the Apennines to investigate how rainfa...
In Orvieto (central Italy), overconsolidated clay slopes are affected by intermittent slow movements...
Hydrological monitoring of slope susceptible to shallow landslides allows for identifying the trigge...