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Estimation of undrained shear strength for saturated clay using shear wave velocity

机译:剪切波速度估计饱和粘土的不驱动剪切强度

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摘要

Undrained shear strength is a fundamental parameter for estimating the stability of soft soils. This study explores the relationship between undrained shear strength, void ratio, and shear wave velocity for saturated and normally consolidated clay specimens. The undrained shear strength void ratio-shear wave velocity relationship was correlated to empirically determined parameters of selected marine clay specimens. To verify the proposed relationship between undrained shear strength and shear wave velocity, in situ flat dilatometer tests were used for determining the undrained shear strength, and downhole tests were used to assess the shear wave velocity on a natural soil deposit at various depths. The undrained shear strength estimated from the in situ shear wave velocities was compared to the undrained shear strength obtained in the field. The results show that the inferred undrained shear strength yield similar values and follow the same trends as the in situ undrained shear strength data. This method using shear wave velocity can help to nondestructively estimate the undrained shear strength of soft soils in the field and be used in both on-shore and off-shore geotechnical engineering projects.
机译:不介绍的剪切强度是估算软土的稳定性的基本参数。该研究探讨了饱和且通常综合粘土标本的不介的剪切强度,空隙率和剪切波速度之间的关系。不介绍的剪切强度空隙率 - 剪切波速度关系与所选海洋粘土标本的凭经质确定的参数相关。为了验证不介绍的剪切强度和剪切波速度之间的建议关系,原位平坦的膨胀计试验用于确定未润湿的剪切强度,并且使用井下试验来评估各种深度的天然土壤沉积物上的剪切波速度。将由原位剪切波速度估计的不介质的剪切强度与在该领域中获得的未润湿的剪切强度进行比较。结果表明,推断不介绍的剪切强度产生类似的值,并遵循与原位不介绍的剪切强度数据相同的趋势。这种使用剪切波速度的方法可以有助于非破坏性地估计该领域的软土的未染色剪切强度,并用于岸上和离岸岩土工程工程。

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