Experimental Study on Permeability and Deformation Characteristics of Bedding Shale under Triaxial Shear-Seepage Coupling

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geofluids Pub Date : 2023-07-19 DOI:10.1155/2023/6314590
Zhinan Lin, Shihong Feng, Jia-quan Wang, Qiang Zhang, Haifeng Long, Guangming Chen
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Abstract

The bedding structure of shale is generated during the deposition and formation, which results in shales with prominent anisotropic characteristics. It depends on stability, control of oil and gas storage, and deep exploitation. In addition, the mechanical and permeability parts of bedding shale are very complex when it is under deep underground space with coupled high stress and high seepage. In this study, the black bedding shale was used as the research object, and a series of triaxial shear-seepage coupling tests were carried out. Firstly, the triaxial shear stress-shear strain curves and permeability-shear stress curves of different bedding shales under other triaxial shear-seepage coupling conditions were obtained. Secondly, the failure characteristics and shear deformation characteristics of shale under the shear-seepage coupling effect were explored. The shear stress threshold and permeability evolution law at each stage of shear failure were discussed. Thirdly, the shear strength, failure mode, and mechanism parameters of the black bedding shale under different normal stress and seepage pressure were studied. Fourthly, the linear M-C criterion, Ramamurthy criterion, and Hoek-Brown criterion characterize the variation of damage strength of shale with bedding orientation under triaxial shear-seepage coupling. Those results provide an experimental basis for exploring the anisotropic mechanical characteristics and failure mechanism of bedding shale under shear-seepage coupling.
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三轴剪切-渗流耦合作用下顺层页岩渗透率及变形特性试验研究
页岩的层理结构是在沉积和形成过程中形成的,具有明显的各向异性特征。这取决于稳定、对石油和天然气储存的控制以及深度开采。此外,当层理页岩处于深部高应力高渗流耦合作用下时,其力学和渗透性部分非常复杂。本研究以黑色层理页岩为研究对象,进行了一系列三轴剪切-渗流耦合试验。首先,得到了不同层理页岩在其他三轴剪切-渗流耦合条件下的三轴剪应力-剪切应变曲线和渗透率-剪应力曲线。其次,探讨了剪切-渗流耦合作用下页岩的破坏特征和剪切变形特征。讨论了剪切破坏各阶段的剪应力阈值和渗透率演化规律。再次,研究了不同正应力和渗流压力下黑色层理页岩的抗剪强度、破坏模式及机理参数。第四,采用线性M-C准则、Ramamurthy准则和Hoek-Brown准则表征了三轴剪切-渗流耦合作用下页岩损伤强度随层理方向的变化规律。研究结果为探讨剪切-渗流耦合作用下层理页岩各向异性力学特性及破坏机制提供了实验依据。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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