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Estimating maximum sustainable injection pressure during geological sequestration of CO_2 using coupled fluid flow and geomechanical fault-slip analysis

机译:使用耦合流体流动和地质力学断层滑移分析估算CO_2地质隔离中的最大可持续注入压力

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This paper demonstrates the use of coupled fluid flow and geomechanical fault slip (fault reactivation) analysis to estimate the maximum sustainable injection pressure during geological sequestration of CO_2. Two numerical modeling approaches for analyzing fault-slip are applied, one using continuum stress-strain analysis and the other using discrete fault analysis. The results of these two approaches to numerical fault-slip analyses are compared to the results of a more conventional analytical fault-slip analysis that assumes simplified reservoir geometry. It is shown that the simplified analytical fault-slip analysis may lead to either overestimation or underestimation of the maximum sustainable injection pressure because it cannot resolve important geometrical factors associated with the injection-induced spatial evolution of fluid pressure and stress. We conclude that a fully coupled numerical analysis can more accurately account for the spatial evolution of both in situ stresses and fluid pressure, and therefore results in a more accurate estimation of the maximum sustainable CO_2 injection pressure.
机译:本文演示了使用耦合流体流动和地质力学断层滑动(断层再活化)分析来估计地质封存CO_2期间的最大可持续注入压力。应用了两种数值建模方法来分析断层滑动,一种是使用连续应力应变分析,另一种是使用离散故障分析。将这两种方法用于数值断层滑动分析的结果与假设储层几何形状简化的更常规的分析断层滑动分析的结果进行了比较。结果表明,简化的分析性断层滑动分析可能导致对最大可持续注入压力的估计过高或过低,因为它无法解决与注入引起的流体压力和应力的空间演化有关的重要几何因素。我们得出结论,完全耦合的数值分析可以更准确地说明原位应力和流体压力的空间演化,因此可以得出最大可持续CO_2注入压力的更准确估算。

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