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首页> 外文期刊>International Journal of Greenhouse Gas Control >Modeling brine leakage to shallow aquifer through an open wellbore using T2WELL/ECO2N.
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Modeling brine leakage to shallow aquifer through an open wellbore using T2WELL/ECO2N.

机译:使用T2WELL / ECO2N对盐水通过裸眼井筒向浅层含水层的渗漏进行建模。

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The efficiency and sustainability of CO2 storage in deep saline formations depends on the integrity of the overlying caprocks. Existing oil and gas wells, which penetrate the formations, are potential leakage pathways. In this paper, T2WELL/ECO2N, a coupled wellbore-reservoir flow simulator of carbon dioxide and brine, is employed to analyze the effects of salinity and excess pore pressure (EPP) on brine leakage from an injection reservoir to a shallow fresh aquifer. The effectiveness of the Equivalent Porous Media (EPM) approach, a widely used approximation of wellbore flow in wellbore-reservoir simulations, is also evaluated. A hypothetical model is built to create test cases with EPP of 0.1 MPa, 0.5 MPa and 1.5 MPa under low-, middle-, and high-salinity. The results show that a quasi-steady-state leakage rate will be quickly established if the EPP caused by CO2 injection is higher than the threshold EPP. However, the brine salinity has an important impact on the brine leakage rate including the threshold EPP below which no leakage occurs. The leakage rate decreases with the increase of the salinity whereas the threshold EPP increases with the increase of the salinity. For the same brine salinity, the quasi-steady-state leakage rate increases with the EPP nonlinearly. The leakage rate calculated by the EPM approach is very sensitive to the equivalent permeability of the wellbore, which however, is not an intrinsic parameter of a given wellbore-aquifer system. Although the EPM approach could reproduce the dynamic leakage rate reasonably well with a fitted permeability, it could over- or underestimates the leakage rate by orders in magnitude for the same system depending on whether the true leakage rate itself is smaller or larger than that of the fitting case due to changes in the salinity and/or the EPP through an abandoned well. The dependence of the equivalent permeability on the flow rate makes the EPM approach not to be a viable method for predicting wellbore leakage except for the cases with very small leakage rates.
机译:CO 2 在深层盐层中的封存效率和可持续性取决于上覆盖层的完整性。贯穿地层的现有油气井是潜在的泄漏途径。在本文中,T2WELL / ECO2N是二氧化碳和盐水耦合的井筒-储层流动模拟器,用于分析盐度和超孔隙压力(EPP)对注入水向浅层新鲜含水层的盐水渗漏的影响。还评估了等效多孔介质(EPM)方法的有效性,该方法是在井眼储层模拟中广泛使用的近似井眼流量。建立了一个假设模型来创建在低,中和高盐度下EPP为0.1 MPa,0.5 MPa和1.5 MPa的测试用例。结果表明,如果CO 2 注入引起的EPP高于阈值EPP,将很快建立准稳态泄漏率。然而,盐水盐度对盐水泄漏率具有重要影响,包括阈值EPP,低于该阈值则不会发生泄漏。泄漏率随盐度的增加而降低,而阈值EPP随盐度的增加而增加。对于相同的盐水盐度,准稳态泄漏率随EPP非线性增加。通过EPM方法计算的泄漏率对井眼的等效渗透率非常敏感,但是,这不是给定井眼-含水层系统的固有参数。尽管EPM方法可以在合适的渗透率下合理地再现动态泄漏率,但它可能会根据实际泄漏率本身小于还是大于真实泄漏率,高估或低估同一系统的泄漏率。由于盐度和/或EPP通过一口废弃井的变化而导致的情况。等效渗透率对流量的依赖性使得EPM方法不是预测井眼泄漏的可行方法,除非泄漏率非常小。

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