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 / F. Ronchetti; L. Borgatti; F. Cervi; A. Corsini. - In: BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT. - ISSN 1435-9529. - STAMPA. - 69:(2010), pp. 267-274. [10.1007/s10064-009-0249-3]
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.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
