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Leakage pathway estimation in geologic CO2 storage: application of inverse analysis to synthetic heterogeneous domains

机译:地质二氧化碳储存中的渗漏途径估算:反分析在合成非均质区域中的应用

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The purpose of this study is to examine the feasibility of inverse analysis to estimate a leakage pathway in a heterogeneous permeability field by using pressure anomalies from the intrusion of brine that is accompanied by gaseous CO2. To achieve this goal, the iTOUGH2 model is employed and applied to multiple brine reservoirs that are designed to realize pressure perturbations that are induced by leakage. Prior to inverse analysis, forward modeling with the TOUGH2 model illustrates brine and/or CO2 discharge through a leakage pathway that penetrates a caprock and the pressure anomalies in a permeable reservoir that overlies the caprock when CO2 is injected into a storage reservoir. The inverse modeling is applied to two types of heterogeneous permeability domains: (1) a renormalized model domain from the known heterogeneity and (2) a simplified model domain that consists of a few homogeneous sections with unknown heterogeneity. The inversion results from the simplified model domain are compared to those from the renormalized model domain to identify the applicability of the simplified model domain to detect a leakage pathway in complex heterogeneous permeability domains. This inverse modeling on the renormalized and simplified model domains examines the effect of the number of monitoring wells, monitoring periods and noises in measurements through 15 and 17 modeling scenarios, respectively. The accuracies of the inversions on the simplified model domain, which depend on the monitoring scenarios, are identical to those of the inverse modeling on the renormalized domain. Residual analysis illustrates that higher magnitude residuals in the storage formation should be weighted to match the residuals in the overlying formation to successfully estimate leakage pathways.
机译:这项研究的目的是通过利用盐水入侵并伴有气态CO2引起的压力异常,研究反演分析估计非均质渗透层渗漏途径的可行性。为了实现这一目标,采用了iTOUGH2模型并将其应用于多个盐水储层,这些盐水储层旨在实现泄漏引起的压力扰动。在进行逆分析之前,使用TOUGH2模型进行的正向建模说明了盐水和/或CO2是通过渗漏途径排放的,该渗漏途径穿透了盖层,并且在将CO2注入到一个储层中时,一个可渗透储层的压力异常覆盖了盖层。逆建模应用于两种类型的非均质渗透性域:(1)来自已知非均质性的归一化模型域;(2)简化模型域,该模型域由一些具有未知非均质性的同质截面组成。将简化模型域的反演结果与重新归一化模型域的反演结果进行比较,以识别简化模型域在复杂异质渗透性域中检测泄漏途径的适用性。在重新规范化和简化的模型域上进行的这种逆向建模分别通过15个和17个建模方案来检验监测井数量,监测周期和测量噪声的影响。取决于监视方案,简化模型域上的反演精度与重新归一化域上的反演模型相同。残差分析表明,应权衡存储地层中较高数量的残差以匹配上覆地层中的残差,以成功估算泄漏路径。

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