常规三轴压缩条件下岩石本构模型OA
Conventional Three-Axis Compression Rock Constitutive Model
基于对岩石材料内部结构特征的分析,岩石材料抵抗外界应力的机制可分为两个部分,即弹性应力和摩擦应力.剪应力是剪应变的四次多项式函数.当不考虑材料弹性的非线性和摩擦应力时,该模型可退化为胡克定律.岩石初始压密效应存在临界值.当围压超过临界值时,岩石初始压密效应消失,据此提出了临界状态方程.体积应变可分解为由剪应力单独引起的体积应变项与平均体积应力单独引起的体积应变项之和.采用公开发表的文献中6 组不同来源岩石的常规三轴压缩试验数据对该模型进行验证.结果表明,该模型能够较好地描述岩石在不同应力条件下的力学行为,证明了该模型的合理性与适用性.
Based on the analysis of the internal structural characteristics of rock materials,the mechanism by which rock materials resist external stress can be divided into two parts:elastic stress and frictional stress.The shear stress has a quartic function relationship with shear strain.When neglecting the nonlinearity of material elasticity and fric-tional stress,this model can be simplified as Hooke's law.There is a critical value for the initial compression effect of rocks,and when the confining pressure exceeds the critical value,the initial compaction effect of the rock disap-pears.Based on this,a critical state equation is proposed.Volume strain can be decomposed into the sum of the vol-ume strain term caused solely by shear stress and the volume strain term caused solely by average volume stress.The model is validated using conventional triaxial compression test data for six different types of rocks from published lit-erature.The results show that the model can effectively describe the mechanical behavior of rocks under different stress conditions,demonstrating its rationality and applicability.
黄家军;刘发明
宿州学院资源与土木工程学院,安徽 宿州,234000||宿州市埇桥区科学技术局,安徽 宿州,234000宿州学院资源与土木工程学院,安徽 宿州,234000
矿业与冶金
本构方程胡克定律弹性应力摩擦应力压密效应临界状态方程
constitutive equationHooke's lawelastic stressfrictional stresscompaction effectcritical state equa-tion
《宿州学院学报》 2026 (3)
37-45,9
非财政资金横向项目(2023xhx320)宿州学院重点建设课程项目(szxy2018zdkc24)安徽省质量工程项目大学生创客试验室(2016ckjh200).
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