The effect of bedrock originated groundwater on the triggering mechanism of different landslides in Switzerland
Cornelia Broennimann, Laurent Tacher, Michel Jaboyedoff, Denis Jongmans, Sarah M. Springman, Amin Askarinejad
Abstract
Cornelia Broennimann, Laurent Tacher, Michel Jaboyedoff, Denis Jongmans, Sarah M. Springman, Amin Askarinejad
Abstract
It is well known that the most important triggering mechanism for rapid landslides is the infiltration of precipitation water at the surface of slopes which decreases the soils shear strength. However, the present study put focus on the exfiltration of groundwater from the substratum and its effect on the triggering of overlying landslides. Which is the origin of this groundwater? Which role does the hydrogeology play on the triggering mechanism of landslides? Is the bedrock locally feeding (springs) or draining (fractures) the overlying soil material in slopes?
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It is well known that the most important triggering mechanism for rapid landslides is the infiltration of precipitation water at the surface of slopes which decreases the soils shear strength. However, the present study put focus on the exfiltration of groundwater from the substratum and its effect on the triggering of overlying landslides. Which is the origin of this groundwater? Which role does the hydrogeology play on the triggering mechanism of landslides? Is the bedrock locally feeding (springs) or draining (fractures) the overlying soil material in slopes?
Key concepts: Landslide, Bedrock, Geology, Groundwater, Landslide mitigation, Hydrogeology, Infiltration (HVAC), Geomorphology