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Fate of Radium in Marcellus Shale Flowback Water

机译:马赛勒斯页岩返排水中的镭的命运

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Radium is naturally occurring radioactive element that is found in shale gas wastewater(flowback and produced water). Ra~(226) is the main isotope that is often found in Marcellus Shaleflowback water at activities ranging from 500-10,000 pCi/L. In comparison, the EPA maximumcontaminant level (MCL) for drinking water is 5pCi/L and the maximum radioactivity fordisposal in RCRA-D non-hazardous landfill is 25pCi/g. This study is designed to investigate thefate of Radium in flowback/produced water and sediments during storage in surfaceimpoundment and to evaluate potential environmental implications of different managementoptions.
机译:镭是页岩气废水中发现的天然放射性元素 (回流和采出水)。 Ra〜(226)是马塞勒斯页岩中经常发现的主要同位素 返水活动范围为500-10,000 pCi / L。相比之下,EPA最大值 饮用水的污染物水平(MCL)为5pCi / L,最大放射性为 RCRA-D无害垃圾填埋场的处置量为25pCi / g。这项研究旨在调查 地表储存过程中返排/产生的水和沉积物中的镭的命运 蓄水并评估不同管理方式对环境的潜在影响 选项。

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