Liu Xiangjun, Zhuang Dalin, Xiong Jian, Zhou Yishan, Liu Junjie, Deng Chong, Liang Lixi, Ding Yi, Jian Xuemei
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引用次数: 0
Abstract
To obtain the influence of anisotropy and energy evolution characteristics on wellbore stability, the acoustic and mechanical anisotropy characteristics of shales are studied through various experiments, including scanning electron microscopy, ultrasonic pulse transmission, and uniaxial compression experiments, with the Longmaxi Formation shale in the southern area of the Sichuan Basin as the research object. The energy evolution characteristics of the Longmaxi Formation shale under different bedding angles are analyzed. The influence of anisotropy on the wellbore stability of shale formation is discussed on this basis. The results show that the acoustic and mechanical parameters, failure mode, and energy evolution characteristics of shale have significant anisotropy. Furthermore, the P-wave and S-wave time differences decrease with an increase in bedding angle. The compressive strength and Poisson’s ratio decrease first and then increase with an increase in bedding angle. Meanwhile, the elastic modulus gradually increases with an increase in bedding angle. Rock samples with different bedding angles show diverse failure modes in mechanical tests, including splitting, shear, and shear-splitting failure. The total energy and elastic energy decrease first and then increase with an increase in bedding angle. Finally, the formation anisotropy affects the wellbore stability: the higher the formation anisotropy, the more vulnerable is the wellbore to instability.
为了获得各向异性和能量演化特征对井筒稳定性的影响,以四川盆地南部地区龙马溪地层页岩为研究对象,通过扫描电镜、超声脉冲透射、单轴压缩实验等多种实验,研究了页岩的声学和力学各向异性特征。分析了龙马溪地层页岩在不同层理角度下的能量演化特征。在此基础上讨论了各向异性对页岩地层井筒稳定性的影响。结果表明,页岩的声学和力学参数、破坏模式和能量演化特征具有明显的各向异性。此外,P 波和 S 波的时差随着垫层角的增大而减小。抗压强度和泊松比随着铺层角度的增大先减小后增大。同时,弹性模量也随着包埋角的增大而逐渐增大。不同埋入角的岩石样本在力学测试中表现出不同的破坏模式,包括劈裂破坏、剪切破坏和剪切-劈裂破坏。总能量和弹性能量先减小后增大,随着层理角度的增大而增大。最后,地层各向异性会影响井筒稳定性:地层各向异性越大,井筒越容易失稳。
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.