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Diffusive and Convective Transport of Disposed CO_2 in Porous Media: A Numerical Approach

机译:多孔介质中CO_2的扩散和对流传输:一种数值方法

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Geologic Carbon Storage (GCS) is one the most promising methods for stabilizing the atmospheric CO_2 concentration, and one challenging problem at this point is the prediction of the long-term transport phenomena of disposed CO2 in the geologic time scale. While small pore size of sealing formations overlying a CO_2-injected layer hinders CO_2 movement in a liquid or supercritical phase, CO_2 dissolved in an aqueous phase will be transported by diffusion and convective flow in porous media. This study explores the diffusive and convective transport of dissolved CO_2 in porous media. Governing equations for modeling two-dimensional CO_2 transport problems were reviewed, and the system of equations was solved using Finite Element (FE) method. Our FE model was validated with published Hele-Shaw experiment results, and the transport of dissolved CO_2 in porous media was well captured with our numerical model. Additional different cases were simulated to examine the effects of CO_2 concentration profile at the interface between CO_2 and pore water. In addition, the effect of the heterogeneity in permeability, the initiation time of convection, and the dissolution rate of CO_2 were discussed.
机译:地质碳储量(GCS)是稳定大气中CO_2浓度的最有前途的方法之一,此时一个具有挑战性的问题是在地质时间尺度上预测已处置CO2的长期迁移现象。尽管覆盖在CO_2注入层上的密封结构的小孔径阻碍了CO_2在液相或超临界相中的移动,但溶解在水相中的CO_2将通过在多孔介质中的扩散和对流流动而被输送。这项研究探索了多孔介质中溶解的CO_2的扩散和对流传输。审查了建模二维CO_2输运问题的控制方程,并使用有限元(FE)方法求解方程组。我们的有限元模型已通过已发表的Hele-Shaw实验结果进行了验证,并且我们的数值模型很好地捕获了多孔介质中溶解的CO_2的传输。模拟了其他不同的情况,以检查CO_2和孔隙水之间的界面处CO_2浓度分布的影响。此外,还讨论了非均质性对渗透率,对流引发时间和CO_2溶解速率的影响。

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