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内华达州地下水中的 210Po 及其与总α放射性的关系。

210Po in nevada groundwater and its relation to gross alpha radioactivity.

机构信息

U.S. Geological Survey, 2730 N Deer Run Road, Carson City, NV 89701, USA.

出版信息

Ground Water. 2011 Mar-Apr;49(2):160-71. doi: 10.1111/j.1745-6584.2010.00688.x.

Abstract

Polonium-210 ((210) Po) is a highly toxic alpha emitter that is rarely found in groundwater at activities exceeding 1 pCi/L. (210) Po activities in 63 domestic and public-supply wells in Lahontan Valley in Churchill County in northern Nevada, United States, ranged from 0.01 ± 0.005 to 178 ± 16 pCi/L with a median activity of 2.88 pCi/L. Wells with high (210) Po activities had low dissolved oxygen concentrations (less than 0.1 mg/L) and commonly had pH greater than 9. Lead-210 activities are low and aqueous (210) Po is unsupported by (210) Pb, indicating that the (210) Po is mobilized from aquifer sediments. The only significant contributors to alpha particle activity in Lahontan Valley groundwater are (234/238) U, (222) Rn, and (210) Po. Radon-222 activities were below 1000 pCi/L and were uncorrelated with (210) Po activity. The only applicable drinking water standard for (210) Po in the United States is the adjusted gross alpha radioactivity (GAR) standard of 15 pCi/L. (210) Po was not volatile in a Nevada well, but volatile (210) Po has been reported in a Florida well. Additional information on the volatility of (210) Po is needed because GAR is an inappropriate method to screen for volatile radionuclides. About 25% of the samples had (210) Po activities that exceed the level associated with a lifetime total cancer risk of 1× 10(-4) (1.1 pCi/L) without exceeding the GAR standard. In cases where the 72-h GAR exceeds the uranium activity by more than 5 to 10 pCi/L, an analysis to rule out the presence of (210) Po may be justified to protect human health even though the maximum contaminant level for adjusted GAR is not exceeded.

摘要

钋-210((210)Po) 是一种剧毒的α放射物,在地层水中的活度很少超过 1pCi/L。在美国内华达州北部丘吉尔县拉洪坦谷的 63 个家庭和公共供水井中,(210)Po 的活度范围为 0.01±0.005 至 178±16pCi/L,中位数为 2.88pCi/L。(210)Po 活度高的水井溶解氧浓度低(小于 0.1mg/L),pH 值通常大于 9。铅-210 的活度较低,水相(210)Po 不支持(210)Pb,表明(210)Po 从含水层沉积物中被迁移出来。拉洪坦谷地下水中α粒子活度的唯一重要贡献者是(234/238)U、(222)Rn 和(210)Po。氡-222 的活度低于 1000pCi/L,与(210)Po 活度无关。美国唯一适用于(210)Po 的饮用水标准是 15pCi/L 的调整总α放射性(GAR)标准。(210)Po 在一个内华达州的井中不挥发,但在一个佛罗里达州的井中报告了挥发性(210)Po。需要更多关于(210)Po 挥发性的信息,因为 GAR 是一种不适合筛选挥发性放射性核素的方法。大约 25%的样本的(210)Po 活度超过了终生总癌症风险为 1×10(-4)(1.1pCi/L)的水平,而没有超过 GAR 标准。在 72hGAR 超过铀活度 5 到 10pCi/L 以上的情况下,为了保护人类健康,可能需要进行分析以排除(210)Po 的存在,即使调整后的 GAR 的最大污染物水平没有超标。

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