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Estimation of minimum undrained shear strength for flow liquefaction using the CPT

机译:使用CPT估算液化的最小不排水剪切强度

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Sensitive clays, metastable silts and very loose sands can strain soften following earthquake loading resulting in possible instability. This instability is often referred to as flow liquefaction. The minimum undrained shear strength is an important parameter in a stability analysis for soils than can strain soften during undrained shear. However, the estimation of this minimum undrained shear strength is often difficult, especially for sandy soils. Research has shown that the undrained shear strength of soils is usually a function of direction of loading, with compression loading often stronger than simple shear and triaxial extension. For many conditions in practice simple shear often represents the average direction of loading. A method is proposed to estimate the minimum undrained shear strength of soils in simple shear using the CPT.
机译:敏感的粘土,亚稳的淤泥和非常疏松的沙子会在地震荷载作用下应变软化,从而导致不稳定。这种不稳定性通常称为流动液化。最小不排水抗剪强度是土壤稳定性分析中的重要参数,这比不排水剪切时的应变软化更为重要。但是,通常很难估算出最小的不排水剪切强度,特别是对于沙质土壤。研究表明,土壤不排水的剪切强度通常是荷载方向的函数,压缩荷载通常比简单的剪切和三轴延伸要强。实际上,在许多情况下,简单的剪切通常代表平均载荷方向。提出了一种使用CPT估算简单剪切作用下土壤最小不排水剪切强度的方法。

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