The paper presents novel results from the advanced numerical modelling of the effect of cycling pore water pressures on landslide processes. It combines the sta-bility analysis of a prototype natural slope through a hydro-mechanical non-linear fi-nite element approach with the calibration of a kinematic hardening model against rep-resentative laboratory data, to draw conclusions of significance to both researchers and designers. The analyses have been carried out for two permanent hydraulic steady-state conditions representing the average pore water pressure regime at the end of the winter and summer season, thus replicating in a simplified way the seasonal fluctua-tions of the piezometric levels resulting from transient seepage processes generated by the slope-atmosphere interaction. The work shows the ability of the constitutive law, seldom used in these kind of analyses, to predict a progressive accumulation of plastic deformations during the cyclic fluctuation of pore water pressures associated to cli-mate. More importantly, the output of the advanced modelling are useful to support the phenomenological interpretation of the landslide processes associated to natural haz-ards and to provide guidance for the sustainable management of marginally stable slopes affected by a constant evolution of permanent displacements.
Analysis of the effects of seasonal pore pressure variations on the slope stability through advanced numerical modelling
Falcone G;
2019
Abstract
The paper presents novel results from the advanced numerical modelling of the effect of cycling pore water pressures on landslide processes. It combines the sta-bility analysis of a prototype natural slope through a hydro-mechanical non-linear fi-nite element approach with the calibration of a kinematic hardening model against rep-resentative laboratory data, to draw conclusions of significance to both researchers and designers. The analyses have been carried out for two permanent hydraulic steady-state conditions representing the average pore water pressure regime at the end of the winter and summer season, thus replicating in a simplified way the seasonal fluctua-tions of the piezometric levels resulting from transient seepage processes generated by the slope-atmosphere interaction. The work shows the ability of the constitutive law, seldom used in these kind of analyses, to predict a progressive accumulation of plastic deformations during the cyclic fluctuation of pore water pressures associated to cli-mate. More importantly, the output of the advanced modelling are useful to support the phenomenological interpretation of the landslide processes associated to natural haz-ards and to provide guidance for the sustainable management of marginally stable slopes affected by a constant evolution of permanent displacements.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.