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Constitutive model equation for various types of rock specimen subjected to uniaxial compression loading

机译:单轴压缩载荷各种岩石标本的本构模型方程

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Right from the outset of the experimental determination of rock stress-strain response, researchers are performing uniaxial and tri-axial compression testing on the cylindrical specimens. In the last two-three decades' researchers have made an attempt to develop constitutive model considering anisotropy, rheological behavior and flaws in rock. In this project, static uniaxial compression tests are performed on cylindrical specimens of Kota sandstone, dolomitic limestone and three weathering classes of Delhi quartzite. Stress-strain curves have been plotted and a general constitutive model equation is derived for all the rock specimens. By observing stress-strain plot of different rock specimen, a parabolic relation between stress and strain is proposed containing two parameters m and n. The fitted results by these models for all types of rock are compared with the experimental data and with the Hooke's law. It is concluded that the amended damage constitutive model can describe the stress-strain behavior of rock quite accurately.
机译:从实验确定岩石应力 - 应变反应的实验结果开始,研究人员在圆柱形样品上进行单轴和三轴压缩测试。在过去的两十年的研究人员中,试图制定考虑各向异性,流变行为和岩石中的缺陷的本构模型。在该项目中,静态的单轴压缩测试是在甲砂砂岩,白云岩石灰石和三种风化德里石英岩等风化等级的圆柱形标本上进行的。已经绘制了应力 - 应变曲线,并且为所有岩石标本导出了一般的本构体模型方程。通过观察不同岩石标本的应力 - 应变图,提出了含有两个参数M和N的应力和菌株之间的抛物线关系。将所有类型的岩石的这些模型的拟合结果与实验数据和胡克定律进行了比较。结论是,修正的损伤本构模型可以非常准确地描述岩石的应力 - 应变行为。

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