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首页> 外文期刊>Journal of Environmental Radioactivity >Mobility indices and doses from Po-210 and Pb-210 activity concentrations data in Brazilian spas groundwaters
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Mobility indices and doses from Po-210 and Pb-210 activity concentrations data in Brazilian spas groundwaters

机译:巴西温泉地下水中Po-210和Pb-210活度浓度数据的迁移率指数和剂量

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摘要

Po-210 and (210)pb activity concentrations in spas groundwaters occurring at Sao Paulo (SP) and Minas Gerais (MG) states, Brazil, have been reported in this paper with a dual purpose: to compare different indices for evaluating the radionuclides mobility into waters and to evaluate the drinking water quality from dose calculations. The waters (75 sampling points) are extensively used for drinking in public places, bottling and bathing purposes, among other. The samples were taken from springs and wells drilled at different aquifer systems inserted in Parana and Southeastern Shield hydrogeological provinces. The WHO guideline reference value for Pb-210 and Po-210 of 0.1 Bq/L in drinking water was not reached for Pb-210 but the Po-210 levels were equal or above it in four spas groundwaters from MG State. The maximum WHO guidance dose level of 0.1 mSv/yr was also reached or surpassed in them. The Pb-210 "mobility index" taking into account the ratio of the weight of the dissolved Pb-210 per unit volume of solution to its weight per unit weight of the rock matrix yielded values in the range of 0.01-5.2 kg/m(3). Another "mobility index" (Preference Ratio) expressing the ratio of Pb-210 and U-238 in the waters divided by the ratio of Pb-210 and U-238 in the rock matrices provided values between 0.004 and 7994. The (210)pb-/U-238 activity ratios of some spas groundwaters suggested preferential U-238 transport relative to Pb-210 into the liquid phase, whereas the ratio of the Pb-210 to U-238 mobility indices indicated the opposite. Such finding showed a better usefulness of the mobility indices for evaluating processes affecting the radionuclides release into the liquid phase during the water/rock interactions. (C) 2017 Elsevier Ltd. All rights reserved.
机译:本文报道了巴西圣保罗(SP)和米纳斯吉拉斯州(MG)州温泉矿泉水中Po-210和(210)pb的活动浓度,其双重目的是:比较不同指标以评估放射性核素迁移率进入水中,并根据剂量计算评估饮用水质量。这些水(75个采样点)被广泛用于在公共场所饮用,装瓶和洗浴等用途。样品取自在巴拉那州和东南盾构水文地质省的不同含水层系统中钻出的弹簧和井。 Pb-210未达到WHO饮用水中Pb-210和Po-210的参考参考值0.1 Bq / L,但在MG State的四个温泉地下水中Po-210的水平等于或高于该水平。其中还达到或超过了WHO指导剂量的最高水平0.1 mSv / yr。考虑到每单位体积溶液中溶解的Pb-210的重量与其在岩石基质中每单位重量的重量之比,Pb-210的“迁移率指数”在0.01-5.2 kg / m( 3)。表示水体中Pb-210和U-238的比率除以岩石基质中Pb-210和U-238的比率的另一个“迁移率指数”(“ Preference Ratio”)提供的值介于0.004和7994之间。(210)一些温泉地下水的pb- / U-238活度比表明,相对于Pb-210,U-238优先进入液相,而Pb-210与U-238的迁移率之比却相反。这样的发现表明迁移率指数对于评估影响水/岩石相互作用过程中放射性核素释放到液相中的过程的更好的实用性。 (C)2017 Elsevier Ltd.保留所有权利。

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