摘要
为了研究冻土在π平面上的强度特征,利用冻土空心圆柱仪对冻结黏土开展了-6.0℃条件下4个平均主应力p(1.0,3.0,4.5和10.0MPa)和5个应力Lode角θσ(-30.0°,-16.1°,0°,16.1°和30.0°)的定向剪切试验.结果表明:定向剪切路径下冻结黏土的应力-应变曲线均呈现应变硬化特征;随着中主应力系数b值的增加,轴向强度逐渐降低;随着平均主应力p值的增大,中主应力系数b值对广义剪应力-剪应变曲线的影响逐渐减弱;在平均主应力p值较小时,中主应力系数b值的变化对破坏应力比的影响较大,而在平均主应力p值较大时,这一影响则较小;在相同中主应力系数b值下,破坏应力比随着平均主应力的增大而减小.随着平均主应力的增加,π平面上冻结黏土的破坏曲线形状从光滑外凸三角形渐变为圆形,非线性广义强度理论能较好描述这种演化规律.
To study the strength properties of frozen soil in theπ-plane,a series of directional shear tests were carried out on frozen clay under five stress Lode angles(θσ=-30.0°,-16.1°,0°,16.1°,and 30.0°)and four mean principal stresses(p=1.0,3.0,4.5,and 10.0MPa)at-6.0℃.The results show that the stress-strain behavior of frozen clay performs as strain hardening under directional shearing.With the coefficients of intermediate principal stress(b-value)increases,the axial strength decreases gradually.With the increase of the mean principal stress(p-value),the influence of the b-value on the curve of generalized shear stress-strain weakens.The influence of the b-value on the ratio of failure stress is greater when p-value is small and vice versa.The ratio of failure stress decreases with the p-value increase under the same b-value.In theπ-plane,the failure curve of frozen clay changes from a curve-sided triangle to a circle.Simulation of the test results in this study shows that the generalizednonlinear strength theory(GNST)can describe this evaluation rule better than others.
引文
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