Constitutive modeling of a laumontite-rich tight rock and the application to poromechanical analysis of deeply drilled wells

Sina Heidari , Biao Li , Antoine B. Jacquey , Bin Xu
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引用次数: 2

Abstract

Geological formations containing laumontite-rich rock are usually treated as problematic for geo-energy production projects because the presence of laumontite mineral can promote complex mechanical behaviors. Previous laboratory results indicate that rock formations with a higher laumontite content display severe stress sensitivity in poromechanical responses. With an increase in confining pressure, there is a transition from dilation to compression regime and the resulting localization styles range from shear dilation to compaction bands. In this study, we conduct finite element modeling of constitutive behaviors of rocks retrieved from the tight glutenite reservoir formation using a thermodynamic-consistent plasticity model. The shear dilation to compaction transition is well characterized. Poromechanical analysis is also conducted to analyze the plastic zone development around a borehole drilled in an over pressured reservoir. The simulated stress-paths of key points around the borehole are used to demonstrate the plastic strain development processes. The impact of in-situ stress on the wellbore stability is highlighted, and a comparison with the results from using the traditional plastic constitutive model is conducted.

富laumonite致密岩本构建模及在深井孔隙力学分析中的应用
含有富含laumontite岩石的地质构造通常被视为地质能源生产项目的问题,因为laumontite矿物的存在会促进复杂的力学行为。先前的实验室结果表明,laumontite含量较高的岩层在孔隙力学响应中表现出严重的应力敏感性。随着围压的增加,出现了从膨胀到压缩的转变,由此产生的局部化样式从剪切膨胀到压实带。在本研究中,我们使用热力学一致塑性模型对从致密砂砾岩储层中提取的岩石的本构行为进行了有限元建模。剪切膨胀-压实转变具有良好的特征。还进行了孔隙力学分析,以分析超压储层中钻孔周围的塑性区发育。利用钻孔周围关键点的模拟应力路径来演示塑性应变的发展过程。强调了地应力对井筒稳定性的影响,并与传统塑性本构模型的结果进行了比较。
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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