In the northern Apennines, four representative large and deep seated landslides affecting weak rock masses have been studied before, during and after reactivation events. Semi-continuous and continuous monitoring in the 2004–2006 period included the dormancy, reactivation and suspension phases, allowing some comments to be put forward as regards the hydro-mechanical conditions that drive the reactivations. The data have highlighted the interactions between groundwater and displacement rates in different sections of the slope.

Hydro-mechanical features of landslide reactivation in weak clayey rock masses

BORGATTI, LISA;CERVI, FEDERICO;
2010

Abstract

In the northern Apennines, four representative large and deep seated landslides affecting weak rock masses have been studied before, during and after reactivation events. Semi-continuous and continuous monitoring in the 2004–2006 period included the dormancy, reactivation and suspension phases, allowing some comments to be put forward as regards the hydro-mechanical conditions that drive the reactivations. The data have highlighted the interactions between groundwater and displacement rates in different sections of the slope.
2010
F. Ronchetti; L. Borgatti; F. Cervi; A. Corsini
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11585/78618
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