Viscous response in shear of clayey geomaterial
Translational slides in clays are often characterized by long-lasting intermittent movements associated with the fluctuations of pore-water pressures. These are in turn associated with either the rise or fall of the groundwater table for the case where the failure surface develops in the saturated z...
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University of Strathclyde
2016
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.698545 |