吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (5): 1544-1550.doi: 10.13278/j.cnki.jjuese.20200289
张琦1, 杨忠年1, 时伟1, 凌贤长1,2, 涂志斌1
Zhang Qi1, Yang Zhongnian1, Shi Wei1, Ling Xianzhang1,2, Tu Zhibin1
摘要: 为探究冻融循环条件下初始含水率对膨胀土偏应力-应变关系和剪切特性的影响,本文对不同初始含水率的非饱和膨胀土进行了不固结不排水三轴剪切试验。结果表明:1)非饱和膨胀土的偏应力-应变曲线的形式随含水率增大由应变软化逐渐转变为应变硬化,偏应力峰值随含水率增大而降低;2)非饱和膨胀土的抗剪强度随初始含水率的增加呈线性下降趋势;3)非饱和膨胀土在第1次冻融循环后偏应力及抗剪强度大幅度下降,在3~7次冻融循环后达到稳定。初始含水率是影响非饱和膨胀土力学性质的主要原因。
中图分类号:
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