In addition to landslides of different types and extent, the clayey slope of the Orvieto hill is affected by extremely slow movements at relatively high depths (up to 33 m) and by very slow movements at shallower depths (up to 10 m). These movements are strictly re-lated to rainfall regimes and to the consequent pore pressure distribution inside the hill. The influence of rainfall regimes on the hy-draulic conditions and movement rates was reconstructed by means of piezometric and inclinometric measurements performed overthe last twenty years.
Twenty-year monitoring of the Orvieto overconsolidated clayey slope (Italy) / TOMMASI, P.; BOLDINI, D.; RIBACCHI, Renato. - 3:(2005), pp. 2595-2598. (Intervento presentato al convegno 16th International Conference on Soil Mechanics and Geotechnical Engineering tenutosi a Osaka; Japan).
Twenty-year monitoring of the Orvieto overconsolidated clayey slope (Italy)
BOLDINI D.;RIBACCHI, Renato
2005
Abstract
In addition to landslides of different types and extent, the clayey slope of the Orvieto hill is affected by extremely slow movements at relatively high depths (up to 33 m) and by very slow movements at shallower depths (up to 10 m). These movements are strictly re-lated to rainfall regimes and to the consequent pore pressure distribution inside the hill. The influence of rainfall regimes on the hy-draulic conditions and movement rates was reconstructed by means of piezometric and inclinometric measurements performed overthe last twenty years.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
