A meso‐damage‐based constitutive model for yellow sandstone under dry–wet cycles

Zhe Qin, Runchang Zhang, Weizheng Mao, Jihuan Han, Zhiwen Li, Sunhao Zhang
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引用次数: 1

Abstract

The mechanical properties of rocks weaken under dry–wet cycles. This weakening may significantly modify the safety reserve of underground caverns or reservoir bank slopes. However, meso‐damage has not been carefully studied based on micromechanical observations and analyses. Therefore, in this study, meso‐damage of a yellow sandstone is investigated and a meso‐damage‐based constitutive model for dry–wet cycles is proposed. First, computed tomography scanning and uniaxial compression tests were conducted on yellow sandstones under different dry–wet cycles. Second, the evolution of rock mesostructures and the damage mechanism subjected to dry–wet cycles were simulated using the discrete element method with Particle Flow Code in 2 Dimensions (PFC2D) software. Third, a constitutive model was proposed based on the meso‐statistical theory and damage mechanics. Finally, this constitutive model was verified with the experimental results to check its prediction capability. It is found that the radius and number of pore throats in the sandstone increase gradually with the number of dry–wet cycles, and the pore structure connectivity is also improved. The contact force of sandstone interparticle cementation decreases approximately linearly and the continuity of the particle contact network is continuously broken. The meso‐deformation and strength parameters show similar declining patterns to the modulus of elasticity and peak strength of the rock sample, respectively. This meso‐damage‐based constitutive model can describe well the rock deformation in the initial pressure density stage and the damage stage under the coupling effect of dry–wet cycles and loads.
干湿循环条件下基于中观损伤的黄砂岩构成模型
岩石的机械特性在干湿循环下会减弱。这种削弱可能会极大地改变地下溶洞或水库岸坡的安全储备。然而,基于微观力学观察和分析的中观破坏尚未得到仔细研究。因此,本研究对黄砂岩的中观损伤进行了研究,并提出了基于中观损伤的干湿循环构成模型。首先,对不同干湿循环条件下的黄砂岩进行了计算机断层扫描和单轴压缩试验。其次,利用离散元方法和二维粒子流代码(PFC2D)软件模拟了干湿循环条件下岩石介观结构的演变和损伤机制。第三,在介观统计理论和损伤力学的基础上提出了一个构成模型。最后,用实验结果验证了这一构成模型,以检验其预测能力。研究发现,随着干湿循环次数的增加,砂岩中孔隙节理的半径和数量逐渐增加,孔隙结构的连通性也得到改善。砂岩颗粒间胶结接触力近似线性下降,颗粒接触网络的连续性不断被打破。中观变形和强度参数分别与岩样的弹性模量和峰值强度呈现类似的下降模式。在干湿循环和荷载的耦合作用下,这种基于中观破坏的构造模型能够很好地描述岩石在初始压力密度阶段和破坏阶段的变形。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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