非饱和压实土的屈服特性

V. Sivakumar, I. G. Doran
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引用次数: 10

摘要

非饱和土的弹塑性本构模型假定在p:s应力平面上存在荷载-坍塌屈服轨迹(LC)和吸力-增加屈服轨迹(SI)。近年来,LC产量轨迹的特征已经得到了相当好的确立,但与SI产量轨迹相比,存在更大程度的不确定性。在本文所报道的工作中,在改进的三轴仪中对非饱和压实高岭土样品进行了许多p:s平面上的应力路径试验。对压实到相同初始条件的样品进行了两系列测试,以确保测试前土壤结构均匀。系列1中测试的样品经过三个阶段:在恒定平均净应力下润湿、在恒定平均纯应力下干燥以及各向同性压缩和润湿的组合。在各向同性压缩之前,将系列2中测试的样品取至预先选择的吸力值。从这些试验中获得的数据表明,非饱和压实土壤可能存在单一屈服轨迹。数据还表明,最初由压实过程施加的屈服轨迹的位置将受到后续润湿过程的影响。版权所有©2000 John Wiley&;有限公司。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Yielding characteristics of unsaturated compacted soils

The elasto-plastic constitutive model for unsaturated soils postulates the existence of a loading collapse yield locus (LC) and a suction increase yield locus (SI) in the p:s stress plane. The characteristics of the LC yield locus have been reasonably well established in recent years but there is a much greater degree of uncertainty in relation to the SI yield locus. In the work reported in this paper a number of stress path tests in the p:s plane were conducted on samples of unsaturated compacted kaolin in a modified triaxial apparatus. Two series of tests were conducted on samples compacted to an identical initial condition so as to ensure a uniform soil structure prior to testing. Samples tested in Series 1 were taken through three stages: wetting at constant mean net stress, drying at constant mean net stress and a combination of isotropic compression and wetting. Samples tested in Series 2 were taken to pre-selected values of suction prior to isotropic compression. Data obtained from these tests indicate a possible form of single yield locus for unsaturated compacted soil. The data also indicate that the position of the yield locus, initially imposed by the compaction process will be influenced by the subsequent wetting process. Copyright © 2000 John Wiley & Sons, Ltd.

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