Delaware盆地泥盆系和志留系CO2储层地质力学研究及井筒稳定性分析

S. Nguyen, T. Nguyen, H. Yoo, G. El-kaseeh
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摘要

该项目的目标是为二氧化碳(CO2)在碳酸盐地层中的潜在地质封存建立一个一维力学地球模型。该研究对分析深注井可能出现的井筒失稳问题具有重要意义。此外,所建立的模型基本上可以用于评估盖层的长期CO2储存完整性,并提供断层滑动潜力的初步分析评估。本文描述了为实现三个最终目标而广泛构建地质力学模型的过程。各种岩石物理解释、剪切波速模型和Mogi-Coulomb失效准则的初步建立,为特拉华盆地(二叠纪盆地的一个子盆地)的超压坡道提供了一个安全的钻井泥浆比重窗口。利用岩石特性和强度的可靠输出,随后通过计算脆性指数和拉伸破坏临界压力来确定顶部密封质量。最后,综合孔隙压力、剪切应力、摩擦角和地应力,预测深层含水层碳酸盐岩断层滑动初步分析的最大可持续注入压力。根据孔隙压力和裂缝梯度预测,确定了Wolfcamp页岩和Barnett页岩两个不同的超压区存在井筒不稳定。这些压力坡具有较低的抗压强度,导致崩溃压力超过孔隙压力,成为钻井泥浆重量的下限。井眼稳定性模拟还显示,Woodford页岩盖层脆性指数低,破裂压力阈值高。这意味着盖层可能更能抵抗裂缝的生长和破坏,表明在注入储层上方存在有效的顶部密封。同时,当临界注入流体压力接近解析计算的预测阈值时,可以有针对性地进行密切观察,以评估泥盆系和志留系地层的断层滑动潜力。这项研究的结果将有助于进一步了解钻井实践和二氧化碳封存下的井眼稳定性。适当的应用可以优化套管和钻井泥浆比重设计,同时还可以调整注入流体压力。此外,估计的岩石性质、地层压力和主应力将是建立特定注入年份后气体羽流分布的流体动力学模拟的重要因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geomechanical Study and Wellbore Stability Analysis for Potential CO2 Storage into Devonian and Silurian Formations of Delaware Basin
The objective of this project is to construct a 1D mechanical earth model for the prospective geological sequestration of carbon dioxide (CO2) into carbonate formations. The study sustains a pivotal role in analyzing the possible wellbore instabilities for drilling deep injection wells. Besides, the developed model can be essentially used to evaluate the caprock integrity for long-term CO2 storage and provide the primary analytical assessment of fault slip potential. This paper describes the extensive construction of a geomechanical model to achieve three ultimate goals. A variety of petrophysical interpretations, shear wave velocity modeling, and Mogi-Coulomb failure criterion are initially established to deliver a safe drilling mud weight window for overpressure ramps in the Delaware basin, a sub-basin of the Permian. Using the dependable outputs of rock properties and strengths, top seal quality is subsequently determined by calculation of the brittleness index and critical pressure of tensile failure. Finally, pore pressure, shear stress, friction angle, and in-situ stresses are integrated to predict maximum sustainable injection pressures for preliminary fault slip analysis in deep aquifer carbonate rocks. Two distinct overpressured zones of Wolfcamp and Barnett Shale are identified for wellbore instability based on pore pressure and fracture gradient prediction. These pressure ramps have a lower compressive strength, which causes the collapse pressure to exceed the pore pressure and serve as the lower bound of drilling mud weight. The wellbore stability simulation also shows low brittleness indices and high threshold breakdown pressures for Woodford shale caprock. It implies that the caprock may be more resistant to fracture growth and failure, indicating an effective top seal above the injected reservoirs. Meanwhile, close observation may be purposefully monitored to assess the fault slip potential in Devonian and Silurian formations once the critical injected fluid pressure approaches the projected threshold from the analytical computation. The findings from this study will be useful in further understanding wellbore stability under drilling practices and CO2 sequestration. The appropriate application can support optimizing the casing and drilling mud weight design while also modifying the injection fluid pressure. Furthermore, the estimated rock properties, formation pressure, and principal stresses will be significant elements in building a hydrodynamic simulation of gas plume distributions after certain injection years.
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