吸水后层状页岩和垫层页岩的地质力学性质:中国鄂尔多斯盆地长7页岩案例研究

IF 7 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL
Pengfei Zhao , Xiangyu Fan , Xingzhi Wang , Xiang Wang , Xin Zhou , Qiangui Zhang , Yufei Chen
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引用次数: 0

摘要

我国大陆页岩地层中蕴藏着丰富的油气资源,这些地层往往含有砂质层、凝灰岩质层和碳酸盐岩质层,与基底面平行,地质力学性质复杂。在钻井过程中,页岩内部力学薄弱的表层结构和钻井液的水化作用容易造成井筒失稳,降低钻井的安全性和效益。为探讨层状页岩和层状页岩吸水后的地质力学性质,对鄂尔多斯盆地长 7 层状页岩和层状页岩进行了一系列试验。结果表明,层状页岩和垫层页岩的抗压强度和弹性模量随着(垫层/层状页岩与应力方向的夹角)的不断增大呈先减小后开始减小的趋势,层状页岩的各向异性较强,抗压强度和弹性模量较低。层状页岩和垫层页岩的含水量会随着浸泡时间的增加而增加,从而导致抗压强度降低。与垫层页岩相比,层状页岩达到水饱和的速度更快,含水量更高。根据页岩水化前后的宏观和微观图像,可以得出结论:层状页岩与页岩基质之间的界面容易形成天然微裂隙,天然微裂隙边缘的脆性矿物容易脱落,从而增加了水化面积,加剧了水化过程。根据现场数据,与层状页岩层相比,层状页岩层的孔径伸长比更大,更容易坍塌。本研究揭示了层状页岩在各向异性和水化作用双重影响下的地质力学特性,为此类地层的钻井设计提供了支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geomechanical properties of laminated shale and bedding shale after water absorption: A case study of the Chang 7 shale in Ordos basin, China

There are abundant oil and gas resources in China's continental shale formations, and these formations often contain sandy lamina, tuffaceous lamina and carbonate lamina parallel to the bedding planes, resulting in complex geomechanical properties. During the drilling process, the mechanical weak surface structure inside the shale and the hydration effect of drilling fluid may easily cause wellbore instability, which reduces the safety and benefit of drilling. To explore the geomechanical properties of laminated shale and bedding shale after water absorption, a series of tests were conducted on the Chang 7 laminated shale and bedding shale in the Ordos Basin. The result indicates that the compressive strength and elastic modulus of laminated shale and bedding shale show a trend of decreasing first and then starting to drop as β (the angle between bedding/lamina and the direction of stress) keeps increasing, and laminated shale has stronger anisotropy, lower compressive strength and elastic modulus. The moisture content of laminated shale and bedding shale increases as the soaking time increases, which leads to a decrease in the compressive strength. Compared to bedding shale, laminated shale reaches water saturation faster and has a higher moisture content. Based on the macroscopic and microscopic images before and after shale hydration, it can be concluded that natural microfractures are easily formed at the interface between the lamina and shale matrix, and brittle minerals at the edges of natural microfractures are prone to detachment, thereby increase the hydration area and intensify the hydration process. Compared to bedding shale formations, laminated shale formations have a higher hole-size elongation ratio and are more prone to collapse according to on-site data. This study reveals the geomechanical properties of laminated shale under the dual influence of anisotropy and hydration, provides support for drilling design in such formations.

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来源期刊
CiteScore
14.00
自引率
5.60%
发文量
196
审稿时长
18 weeks
期刊介绍: The International Journal of Rock Mechanics and Mining Sciences focuses on original research, new developments, site measurements, and case studies within the fields of rock mechanics and rock engineering. Serving as an international platform, it showcases high-quality papers addressing rock mechanics and the application of its principles and techniques in mining and civil engineering projects situated on or within rock masses. These projects encompass a wide range, including slopes, open-pit mines, quarries, shafts, tunnels, caverns, underground mines, metro systems, dams, hydro-electric stations, geothermal energy, petroleum engineering, and radioactive waste disposal. The journal welcomes submissions on various topics, with particular interest in theoretical advancements, analytical and numerical methods, rock testing, site investigation, and case studies.
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