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A simple approach for evaluating slope movements induced by groundwater variations

机译:一种简单的方法,用于评估地下水变化引起的斜率运动

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Landslides reactivated by groundwater variations are usually characterized by low displacement rate with deformations essentially concentrated within a narrow shear zone above which the unstable soil mass moves like a rigid body. A simplified method was recently proposed by Conte and Troncone [1] for a preliminary evaluation of the mobility of these landslides. In the present study, this method is extended by incorporating a calibration procedure for a direct evaluation of some parameters which are difficult to obtain experimentally. Some case studies are analysed to validate the present approach.
机译:通过地下水变化重新激活的山体滑坡通常具有低位移率,变形基本上集中在一个窄的剪切区内,不稳定的土壤质量像刚体一样移动。 最近通过CONTE和Troncone [1]提出了一种简化的方法,以初步评估这些山垫片的流动性。 在本研究中,通过结合校准程序来延长该方法,用于直接评估一些难以通过实验获得的参数。 分析了一些案例研究以验证目前的方法。

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