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Simulation and Performance Assessment of Partitioning Tracer Tests in Heterogeneous Aquifers

机译:非均质含水层中分区示踪剂测试的模拟和性能评估

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Characterization of dense non-aqueous phase liquid (DNAPL) in heterogeneous media represents a major challenge in the remediation process due to the complexity of DNAPL distribution in the subsurface. The partitioning interwell tracer test (PITT), which evaluates the relative transport of DNAPL-phase partitioning and conservative (i.e., non-partitioning) tracers, has recently been promoted as a way to quantify entrapped DNAPL mass in source zones. In some cases, the technique has been successfully applied to sites where DNAPL is present primarily at residual saturations. However, the effects of the geologic heterogeneity and DNAPL architecture on the performance and reliability of this technique have not yet been thoroughly examined. A systematic two-dimensional simulation study was conducted to evaluate the influence of DNAPL vertical distribution, well location, and geologic heterogeneity on the performance of the PITT for a total of 60 stochastic aquifer realizations. The aquifer hydraulic conductivity (K) distribution was denned using three different geostatistical parameter values describing the variance of the log K (sigma_(ln k)~2 = [1.22, 0.75, 0.25]). A multiphase flow simulator was used to generate the source zone, allowing the DNAPL to distribute naturally. The tracer test simulations conducted using these various synthetic aquifers were specifically designed to quantify PITT performance for different degrees of heterogeneity. For cases where the aquifer is relatively heterogeneous and the DNAPL architecture is complex, PITT estimation efficiency averaged 48 percent (decreasing to 20 percent in certain scenarios) as a result of bypass flow and the limited tracer accessibility to lower hydraulic conductivity regions. While other studies have suggested the PITT technique may underestimate DNAPL saturation for these conditions, potential errors of this magnitude have not previously been reported. The results of this work underscore the importance of geological heterogeneity on PITT performance.
机译:由于表面下DNAPL分布的复杂性,在非均质介质中表征稠密非水相液体(DNAPL)代表了修复过程中的主要挑战。最近已经推广了分区间孔示踪剂测试(PITT),该方法评估了DNAPL相分区示踪剂和保守(即非分区)示踪剂的相对迁移,已成为量化源区中捕获的DNAPL量的一种方法。在某些情况下,该技术已成功应用于DNAPL主要以残留饱和度存在的位点。但是,地质异质性和DNAPL体系结构对该技术的性能和可靠性的影响尚未得到彻底检验。进行了系统的二维模拟研究,以评估DNAPL垂直分布,井位和地质异质性对总共60个随机含水层实现的PITT性能的影响。使用三个不同的地统计学参数值(描述log K的方差)(sigma_(ln k)〜2 = [1.22,0.75,0.25])来确定含水层的水力传导率(K)分布。使用多相流模拟器生成源区,从而使DNAPL能够自然分布。使用这些各种合成含水层进行的示踪剂测试模拟经过专门设计,可以针对不同程度的异质性量化PITT性能。对于含水层相对不均一且DNAPL结构复杂的情况,由于旁通流量和示踪剂对较低水力传导率区域的可及性有限,PITT估算效率平均为48%(在某些情况下降低至20%)。尽管其他研究表明PITT技术可能会低估这些条件下的DNAPL饱和度,但之前尚未报道过这种程度的潜在误差。这项工作的结果强调了地质异质性对PITT性能的重要性。

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