Evolution of anisotropy with saturation and its implications for the elastoplastic responses of clay rocks
Evolution of anisotropy with saturation and its implications for the elastoplastic responses of clay rocks
复制标题
各向异性随饱和度的演化及其对粘土岩弹塑性响应的影响
DOI:
10.1002/nag.3289
复制
发表时间:
2021-11
影响因子:
4
通讯作者:
S. C. Ip;R. Borja
中科院分区:
文献类型:
--
作者:
S. C. Ip;R. Borja
Many clay rocks have distinct bedding planes. Experimental studies have shown that their mechanical properties evolve with the degree of saturation (DOS), often with higher stiffness and strength after drying. For transversely isotropic rocks, the effects of saturation can differ between the bed‐normal (BN) and bed‐parallel (BP) directions, which gives rise to saturation‐dependent stiffness and strength anisotropy. Accurate prediction of the mechanical behavior of clay rocks under partially saturated conditions requires numerical models that can capture the evolving elastic and plastic anisotropy with DOS. In this study, we present an anisotropy framework for coupled solid deformation‐fluid flow in unsaturated elastoplastic media. We incorporate saturation‐dependent strength anisotropy into an anisotropic modified Cam‐Clay (MCC) model and consider the evolving anisotropy in both the elastic and plastic responses. The model was calibrated using experimental data from triaxial tests to demonstrate its capability in capturing strength anisotropy at various levels of saturation. Through numerical simulations, we demonstrate the role of evolving stiffness and strength anisotropy in the mechanical behavior of clay rocks. Plane strain simulations of triaxial compression tests were also conducted to demonstrate the impacts of material anisotropy and DOS on the mechanical and fluid flow responses.