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.
2019
Istituto di Geologia Ambientale e Geoingegneria - IGAG
slope-atmosphere interaction
pore pressure cycles
stability analysis
FEM
advanced constitutive modelling
File in questo prodotto:
Non ci sono file associati a questo prodotto.

I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/360074
Citazioni
  • ???jsp.display-item.citation.pmc??? ND
  • Scopus ND
  • ???jsp.display-item.citation.isi??? ND
social impact