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首页> 外文期刊>Journal of Hydrology >A framework to determine sensitive inorganic monitoring indicators for tracing groundwater contamination by produced formation water from shale gas development in the Fuling Gasfield, SW China
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A framework to determine sensitive inorganic monitoring indicators for tracing groundwater contamination by produced formation water from shale gas development in the Fuling Gasfield, SW China

机译:由SW China涪陵气田的Saling Gas Failaply Sale Mail开发生产的地层水分追踪地下水污染敏感无机监测指标的框架

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Potential environmental impacts on shallow groundwater from shale gas development facilitated by horizontal drilling and hydraulic fracturing is a widely debated "hot topic". In terms of potential aqueous phase contamination (including flowback fluids and produced water), there is a large gap in knowledge of the indicators for routine monitoring and contamination tracing, which should be considered critical and should be prioritized for analysis. Since formation water from shale formations is the main source of flowback fluids and produced water, and there are significant differences in some specific inorganic geochemical and isotopic compositions between shallow groundwater and formation water, this study has provided a framework to determine sensitive monitoring and diagnostic indicators for tracing potential groundwater contamination from produced water using end-member analysis. The results from a case study of the Fuling Gasfield, Sichuan Basin, SW China as the first and largest commercial shale gas development site in China, shows that produced authentic formation water with similar Br/Cl and Na/Cl ratio with seawater and low delta H-2 and delta O-18 values compared to the evaporated seawater might originate from evaporated seawater modified by water-rock interactions and be mixed with fresh meteoric water. The inorganic geochemical and isotopic indicators, such as Ba, Li, Na, Cl, Br, Sr-87/Sr-86 (as epsilon(sw)(Sr)) and delta B-11 are sensitive to the detection of contamination of fresh shallow groundwater by produced formation water, even in very small fractions (0.05%). Meanwhile, we present a groundwater contamination case related to shale gas development in the Fuling Gasfield. The robust conservative geochemical (Cl and Br) and isotopic (delta B-11 and epsilon(sw)(Sr)) mass balances show that 0.2-0.9% of formation water entered the shallow groundwater causing contamination. The case has also confirmed the effectiveness of those indicators. Findings from this study may help to improve groundwater monitoring and environmental regulations in countries with shale gas exploration and development.
机译:通过水平钻井和液压压裂促进的页岩气化浅层地下水对浅层地下水的潜在环境影响是一个广泛争论的“热门话题”。就潜在的水相污染(包括回流流体和生产的水)而言,有一个很大的差距,了解常规监测和污染跟踪的指标,这应该被认为是至关重要的,应优先考虑进行分析。由于来自页岩形成的形成水是流动流体和产生的水的主要来源,并且在浅地下水和地层水之间存在一些特定的无机地球化学和同位素组合物存在显着差异,本研究提供了确定敏感监测和诊断指标的框架用于使用末端成员分析跟踪生产水的潜在地下水污染。涪陵气田,四川盆地,SW中国作为中国第一和最大的商业页岩气体开发现场的案例研究表明,具有类似BR / CL和NA / CL比与海水和低三角洲的正宗形成水与蒸发的海水相比,H-2和Delta O-18值可能来自水岩相互作用改性的蒸发海水,并与新鲜的陨石混合。无机地球化学和同位素指标,如Ba,Li,Na,Cl,Br,SR-87 / SR-86(作为ε(SW)(SR))和Delta B-11对新鲜污染的检测敏感浅地下水通过产生的形成水,即使在非常小的级分(0.05%)。与此同时,我们在涪陵气田中展示了与页岩气发展有关的地下水污染案。鲁棒保守地球化学(Cl和Br)和同位素(Delta B-11和ε(SW)(SR))质量平衡表明,0.2-0.9%的形成水进入浅层地下水导致污染。案件还确认了这些指标的有效性。本研究的调查结果可能有助于改善具有页岩气勘探和发展国家的地下水监测和环境法规。

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