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A Review of NORM/TENORM in Wastes and Waters Associated with Marcellus Shale Gas Development and Production

机译:与Marcellus页岩气开发和生产相关的废水和水中的NORM / TENORM综述

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Marine black shales have long been known to contain elevated concentrations of uranium, thorium, and associated daughter products, commonly known as Naturally-Occurring Radioactive Material (NORM). Because uranium and thorium are only marginally soluble in near-neutral groundwater and formation waters typically associated with black shales, dissolved concentrations of these elements in produced waters (technologically-enhanced NORM [TENORM]) have not been considered a serious environmental issue. In contrast, radium-226 (~(226)Ra) and radium-228 (~(228)Ra) are much more soluble, particularly in formation waters with high concentrations of total dissolved solids (TDS). Total radium activities in formation and produced waters typically range from 30 to 5,000 picocuries per liter (pCi/L). While total radium activities in waters produced from Marcellus Shale gas wells are commonly less than 5,000 pCi/L, activities as high as 16,000 pCi/L have been reported. When produced water reaches the land surface, changes in pressure and temperature affect the solubility of dissolved gases, and subsequently affect the solubility of calcite, gypsum, and other minerals. These minerals commonly precipitate and form scale and sludges, which can accumulate on the inside surfaces of pipes, tanks, and other water-handling equipment. Radium isotopes co-precipitate and concentrate in these mineral deposits, thereby forming a residue with higher radioactivity values than the original water. The general occurrence and speciation of radionuclides in shale samples, produced waters, scale, and sludges associated with Marcellus Shale are presented and discussed in this paper.
机译:长期以来,已知海洋黑页岩中铀,th和相关子产品的浓度较高,通常被称为天然放射性物质(NORM)。由于铀和th仅微溶于近中性地下水和通常与黑色页岩有关的地层水,因此这些元素在采出水中的溶解浓度(技术上提高的NORM [TENORM])尚未被认为是严重的环境问题。相反,镭226(〜(226)Ra)和镭228(〜(228)Ra)的溶解度要高得多,特别是在总溶解固体(TDS)浓度较高的地层水中。地层水和采出水中镭的总活度通常为每升30至5,000微居里(pCi / L)。尽管从马塞勒斯页岩气井生产的水中的总镭活性通常低于5,000 pCi / L,但据报道其活动高达16,000 pCi / L。当采出水到达陆地表面时,压力和温度的变化会影响溶解气体的溶解度,进而影响方解石,石膏和其他矿物质的溶解度。这些矿物质通常会沉淀并形成水垢和淤渣,它们会积聚在管道,水箱和其他水处理设备的内表面上。镭同位素在这些矿藏中共沉淀并富集,从而形成比原始水具有更高放射性值的残留物。本文介绍并讨论了与Marcellus页岩有关的页岩样品,采出水,水垢和污泥中放射性核素的普遍存在和形态。

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