Department of Civil & Environmental Engineering, Colorado State University, Fort Collins, CO 80523-1372, United States.
Department of Civil & Environmental Engineering, Colorado State University, Fort Collins, CO 80523-1372, United States.
Water Res. 2016 Jan 1;88:458-466. doi: 10.1016/j.watres.2015.10.031. Epub 2015 Oct 21.
The potential impact of rapid development of unconventional oil and natural gas resources using hydraulic fracturing and horizontal drilling on regional groundwater quality has received significant attention. Major concerns are methane or oil/gas related hydrocarbon (such as TPHs, BTEX including benzene, toluene, ethybenzene and xylene) leaks into the aquifer due to the failure of casing and/or stray gas migration. Previously, we investigated the relationship between oil and gas activity and dissolved methane concentration in a drinking water aquifer with the major finding being the presence of thermogenic methane contamination, but did not find detectable concentrations of TPHs or BTEX. To understand if aqueous and gas phases from the producing formation were transported concurrently to drinking water aquifers without the presence of oil/gas related hydrocarbons, the ionic composition of three water groups was studied: (1) uncontaminated deep confined aquifer, (2) suspected contaminated groundwater - deep confined aquifer containing thermogenic methane, and (3) produced water from nearby oil and gas wells that would represent aqueous phase contaminants. On the basis of quantitative and spatial analysis, we identified that the "thermogenic methane contaminated" groundwater did not have similarities to produced water in terms of ionic character (e.g. Cl/TDS ratio), but rather to the "uncontaminated" groundwater. The analysis indicates that aquifer wells with demonstrated gas phase contamination have not been contacted by an aqueous phase from oil and gas operations according to the methodology we use in this study and the current groundwater quality data from COGCC. However, the research does not prove conclusively that this the case. The results may provide insight on contamination mechanisms since improperly sealed well casing may result in stray gas but not aqueous phase transport.
水力压裂和水平钻井技术的快速发展对非常规油气资源的开发,可能会对区域地下水质量产生重大影响。人们主要关注的是,由于套管失效和/或游离气迁移,甲烷或与油气相关的碳氢化合物(如总石油烃、苯系物,包括苯、甲苯、乙苯和二甲苯)泄漏到含水层中。此前,我们研究了油气活动与饮用水含水层中溶解甲烷浓度之间的关系,主要发现是存在热成因甲烷污染,但未检测到总石油烃或苯系物的浓度。为了了解在没有与油气相关的碳氢化合物存在的情况下,来自生产地层的水相和气相是否同时迁移到饮用水含水层,研究了三组水样的离子组成:(1)未受污染的深部承压含水层,(2)含有热成因甲烷的疑似受污染地下水-深部承压含水层,以及(3)来自附近油气井的产出水,这将代表水相污染物。基于定量和空间分析,我们确定,就离子特征(如 Cl/TDS 比值)而言,“热成因甲烷污染”地下水与产出水没有相似性,而是与“未受污染”地下水相似。分析表明,根据我们在本研究中使用的方法和 COGCC 目前的地下水质量数据,已经证明存在气相污染的含水层井并未与油气作业产生的水相接触。然而,该研究并不能确凿地证明这一点。研究结果可能为污染机制提供一些启示,因为密封不当的井套管可能导致游离气泄漏,但不会导致水相迁移。