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The seismic displacement of a block sliding on an inclined plane with resistance varying with the distance moved

机译:块在倾斜平面上滑动的地震位移,其阻力随移动距离而变化

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The paper considers a rigid block on an inclined plane. First, the typical response measured along slip surfaces of sands and clays under both drained and undrained conditions is identified. Then, for any expression simulating this change in shear stress with displacement along the boundary between the block and the plane, the paper derives an equation which predicts the equivalent friction angle which, when applied, computes the same seismic displacement of the block. The paper also proposes, validates and calibrates a simple constitutive equation which simulates the typical shear stress-displacement response measured in ring shear tests for both sands and clays sheared under both drained and undrained conditions. Next, the paper for the constitutive law above simulating the change in shear stress with displacement along the slip surface, derives equations which predict the equivalent friction angle which, when applied, computes the same seismic displacement of the block. Finally, based on these equations, the paper proposes an easy-to-apply methodology predicting the seismic displacement of slopes along slip surfaces with strain softening with the aid of the seismic displacement predicted by the conventional sliding-block model and applies this methodology in order (a) to validate it against results of elaborate numerical analyses and (b) to modify the Ambraseys-Menu expressions predicting the seismic displacement of the conventional sliding-block model for soils exhibiting strain softening.
机译:本文考虑了在倾斜平面上的刚性块。首先,确定了在排水和不排水条件下沿着沙子和粘土的滑动面测量的典型响应。然后,对于模拟剪切应力随沿砌块与平面之间的边界位移而变化的任何表达式,本文得出了一个方程,该方程可预测等效摩擦角,应用该公式可计算出砌块的相同地震位移。本文还提出,验证和校准了一个简单的本构方程,该方程可模拟在排水和不排水条件下剪切的砂土和粘土在环剪试验中测得的典型剪切应力-位移响应。接下来,针对上述本构定律的论文模拟了剪切应力随沿滑移面位移的变化,得出了可预测等效摩擦角的方程,当应用该方程时,可计算出块体的相同地震位移。最后,基于这些方程,本文提出了一种易于应用的方法,借助传统滑动块模型所预测的地震位移,通过应变软化来预测滑坡沿坡面的地震位移,并按顺序应用该方法。 (a)根据详尽的数值分析结果对其进行验证,以及(b)修改Ambraseys-Menu表达式,以预测传统滑动块模型对表现出应变软化作用的土壤的地震位移。

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