...
首页> 外文期刊>International journal of geomechanics >Impact of Static Preshearing on Undrained Anisotropy and Shear Characteristics of Sand
【24h】

Impact of Static Preshearing on Undrained Anisotropy and Shear Characteristics of Sand

机译:静态预剪对砂土不排水各向异性和剪切特性的影响

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

The preshearing history of soil is a prominent factor governing its mechanical behavior at various loading conditions. An experimental program was developed to study the effects of preshearing at drained compression and extension conditions on the undrained behavior of saturated sand. Triaxial compression and extension tests on both loose and medium-dense sand showed distinctly different behaviors: the response in compression was dominated by stable and dilative behavior, whereas instability occurred in extension with strain softening. The initial inclination of the effective stress path varying with the preloading history is related to the fabric anisotropy of the soils, characterized by their stiffness values at very small strains, whereas at intermediate to large strains, the undrained stiffness tends to decrease in triaxial compression but grows in triaxial extension with the preshearing stress ratio. Moreover, the instability behavior of sand characterized by the reduction of shear strength is governed by the magnitude and direction of the preshearing stress. The stress ratio at which the instability occurs is not unique and can be correlated with the proposed state index accounting for the combined influences of the preshearing stress and relative density of the sand. In contrast, a unique phase-transformation line exists that is independent of the preshearing stress conditions. This is probably due to the gradual diminishing of the stress-induced anisotropy that is created by the static preshearing during the subsequent undrained loading. (C) 2018 American Society of Civil Engineers.
机译:土壤的预剪历史是决定其在各种载荷条件下的力学行为的重要因素。开发了一个实验程序来研究在排水压缩和伸展条件下的预剪力对饱和砂土的不排水行为的影响。在松散和中等密度的砂土上进行的三轴压缩和拉伸试验显示出截然不同的行为:压缩响应主要由稳定和扩张行为决定,而在拉伸过程中随着应变软化而发生不稳定性。有效应力路径的初始倾角随预加载历史的变化而变化,与土壤的织物各向异性有关,其特征是在很小的应变下其刚度值,而在中等到较大的应变下,三轴压缩时不排水的刚度趋于降低,但随着预剪应力比而在三轴延伸方向上增长。此外,以抗剪强度降低为特征的砂土失稳行为受预剪应力的大小和方向控制。发生不稳定性的应力比不是唯一的,并且可以与提出的状态指数相关,该系数考虑了预剪应力和砂的相对密度的综合影响。相反,存在一条独特的相变线,该线与预剪切应力条件无关。这可能是由于应力诱发的各向异性逐渐减小的缘故,该各向异性是在随后的不排水荷载期间由静态预剪力产生的。 (C)2018美国土木工程师学会。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号