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Liquefaction and deformation of silty and fine-grained soils

机译:粉质和细粒土的液化和变形

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The evaluation of hazards associated with liquefaction of silty and other fine-grained soils is an important consideration for many engineering projects. Over the past few years important progress has been made on this issue. The objective of this paper is to review and evaluate standard practice and recent developments relative to liquefaction resistance and ground deformation potential for silty and fine-grained soils. Findings from the study are as follows: (1) The SPT and CPT criteria presented in this report predict the occurrence and nonoccurrence of liquefaction with h igh reliability. (2) The Chinese criteria as listed in Table 1 are reliable for predicting liquefaction of fine grained sediments and are generally conservative. (3) Sensitive soils subject to loss of strength during seismic shaking typically have clay contents and liquid limits that exceed the Chinese criteria as listed in Table 1. The criteria in Table 3 may be used as screens for sensitive soils. (4) The post-liquefaction or residual strength of loose silty sediments is commonly less than that of sands. Moderately dense silts at shallow depths are generally dilative, making them generally more resistant to ground deformation than cleaner sands.
机译:与粉质粉土和其他细粒土壤液化有关的危害评估是许多工程项目的重要考虑因素。在过去的几年中,在这个问题上已经取得了重要的进展。本文的目的是回顾和评估粉质和细粒土的抗液化性和地面变形潜力的标准实践和最新进展。研究结果如下:(1)本报告中提出的SPT和CPT标准可以高度可靠地预测液化的发生和不发生。 (2)表1中列出的中国标准对于预测细颗粒沉积物的液化是可靠的,并且通常是保守的。 (3)在地震震动过程中易受强度损失的敏感土壤,其粘土含量和液体含量通常超过表1所列的中国标准。表3中的标准可用作敏感土壤的筛网。 (4)疏松粉质沉积物的后液化或残余强度通常小于砂土。浅深度的中等致密粉尘通常较易扩张,因此与清洁砂相比,它们通常更耐地面变形。

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