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1)  initial shearing stress
初始剪切应力
2)  initial shear stress
初始剪应力
1.
Effect of initial shear stress on static and dynamic behavior of soft clay under cyclic loading
初始剪应力对饱和软粘土静、动力学性能影响——试验研究
2.
Undrained triaxial compressive tests are carried out on Hangzhou saturated soft clay to investigate the coupling effects of initial shear stress and loading rate on the monotonic characteristics of soft clay.
重点分析加荷速率与初始剪应力的耦合作用对杭州软黏土静力特性的影响。
3.
The stress-strain curves is approximately symmetrical around origin when there is no initial shear stress.
当土样不存在初始剪应力时,随着循环次数的增加,土样的应力-应变关系曲线近似原点对称,但随着初始剪应力的增大,应力-应变关系曲线逐渐表现为一系列平行曲线,峰值孔压与循环孔压幅值均逐渐减少;同时,轴应变的发展加快,但循环应变幅值逐渐减小。
3)  initial shear
初始剪切
4)  initial stress
初始应力
1.
Three-dimensional finite element analysis of initial stress around screw implant;
螺旋形种植体骨界面初始应力的三维有限元分析
2.
Bounding surface equation of initial stress anisotropy;
初始应力各向异性的边界面方程
3.
Regression analysis and 3 D fitting of initial stress;
初始应力的回归与三维拟合
5)  original shear modulus
初始剪切模量
1.
Relationship between original shear modulus and void ratio or standary penetration test blow count;
土的初始剪切模量与孔隙比及标准贯入值相关关系
2.
The power function relationship of original shear modulus versus embedded depth to account,time scaling factor of input earthquake wave on shaking board were determined by similar resonant frequency,and acceleration amplitude factor of input wave was obtained by strength parameters(cohesion c and internal friction angle φ) of soils.
基于Mohr-Cou lomb破坏准则和双曲线动本构模型恢复力骨干曲线,提出在保持归一化的剪应变比一致条件下,兼顾振动性态和破坏相似的振动台模型实验相似律:由土体初始剪切模量随埋深的幂函数变化规律,按振动性态相似原则确定台面输入地震波波形的时间压缩比,再以岩土材料的强度参数(c,φ值)按破坏相似原则确定台面输入波形的幅值比,得到各主要物理量的相似律。
6)  initial shearing stiffness
初始剪切刚度
1.
The testing result shows that the conditions(dry or saturated) have more significant effect on the shear strength than soil type or base,and the conditions(dry or saturated) and base are significant factors of initial shearing stiffness.
试验研究表明:砂的干湿状态对抗剪强度(竖直附加力的峰值)影响最大;砂的干湿状态,基底对初始剪切刚度的影响均较显著。
补充资料:剪切应力
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性质: 平行与试样原始工作面的作用力与其工作面截面积之比。对熔体或液体的流动而言,是指流层在截面上相互滑动或沿流道壁滑移(呈层流状)时,在流体内部所产生的层间应力。

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