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A Constitutive Model for Shear Behavior of Rock Joints Based on Three-Dimensional Quantification of Joint Roughness

机译:基于节理粗糙度三维量化的节理本构模型

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摘要

A new constitutive model to describe the shear behavior of rock joints under constant normal stiffness (CNS) and constant normal load (CNL) conditions is proposed. The model was developed using an empirical approach based on the results of a total of 362 direct shear tests on tensile fractured rock joints and replicas of tensile joints and on a new quantitative roughness parameter. This parameter, the active roughness coefficient C_r, is derived from the features of the effective roughness mobilized at the contact areas during shearing. The model involves a shear strength criterion and the relations between stresses and displacements in the normal and shear directions, where the effects of the boundary conditions and joint properties are considered by the shape indices C_d and C_f. The model can be used to predict the shear behavior under CNS as well as CNL conditions. The shear behavior obtained from the experimental results is generally in good agreement with that estimated by the proposed model, and the effects of joint roughness, initial normal stress, and normal stiffness are reasonably reflected in the model.
机译:提出了一种新的本构模型,描述岩石节理在恒定法向刚度(CNS)和恒定法向载荷(CNL)条件下的剪切行为。该模型是使用经验方法开发的,该模型基于总共362次对拉伸断裂的岩石节理和拉伸节理的副本进行直接剪切测试的结果以及新的定量粗糙度参数。主动粗糙度系数C_r是从剪切过程中在接触区域处移动的有效粗糙度的特征得出的。该模型涉及抗剪强度准则以及法向和剪切方向上的应力与位移之间的关系,其中边界条件和接头特性的影响由形状指标C_d和C_f考虑。该模型可用于预测CNS以及CNL条件下的剪切行为。从实验结果获得的剪切行为通常与所提出的模型估算的剪切行为良好吻合,并且在模型中合理地反映了接头粗糙度,初始正应力和法向刚度的影响。

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