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巴西东南部温泉地下水中溶解铀浓度及U/U活度比

The dissolved uranium concentration and U/U activity ratio in groundwaters from spas of southeastern Brazil.

作者信息

Bonotto Daniel Marcos

机构信息

Departamento de Petrologia e Metalogenia, IGCE-Instituto de Geociências e Ciências Exatas, UNESP-Universidade Estadual Paulista Júlio de Mesquita Filho, Av. 24-A, No. 1515, CP 178, CEP 13506-900, Rio Claro, SP, Brazil.

出版信息

J Environ Radioact. 2017 Jan;166(Pt 1):142-151. doi: 10.1016/j.jenvrad.2016.03.009. Epub 2016 Mar 24.

Abstract

This paper describes the natural radioactivity due to U and U in 75 water sources from spas located in 14 municipalities in São Paulo and Minas Gerais states, Brazil. These waters are extensively utilized for drinking in public places, bottling and bathing purposes, among other uses. The water samples were taken from springs and pumped tubular wells drilled into different aquifer systems in the Paraná and Southeastern Shield hydrogeological provinces. The measurements of alpha-emitting radionuclides were also accompanied by the monitoring of temperature, pH, Eh, electrical conductivity, dissolved gases (O, CO, HS, radon, thoron) and major constituents. The dissolved U concentration data were lognormally distributed. The median and mean values corresponded to 0.02 and 0.09 μg/L, respectively. Significant relationships were found among the U/U activity ratio (AR) of dissolved uranium, the total dissolved solids (TDS) and dissolved bicarbonate contents, and also between the AR and dissolution rate in the monitored sites. The logU versus AR diagram used for the hydrogeochemical prospecting of concealed U deposits indicated that the water sources were mainly from reduced environments. The possibility of using the reciprocal of the dissolved U concentration and AR data to determine mixing volumes of different groundwater masses was demonstrated. The highest dissolved U concentration (4.82 μg/L) was well below the maximum allowed by WHO.

摘要

本文描述了巴西圣保罗州和米纳斯吉拉斯州14个市温泉的75个水源中铀和钍的天然放射性。这些水广泛用于公共场所饮用、装瓶和洗浴等用途。水样取自泉水以及钻入巴拉那和东南地盾水文地质省不同含水层系统的抽水井。对发射α粒子的放射性核素的测量还伴随着对温度、pH值、氧化还原电位、电导率、溶解气体(氧气、二氧化碳、硫化氢、氡、钍射气)和主要成分的监测。溶解铀浓度数据呈对数正态分布。中位数和平均值分别为0.02和0.09微克/升。在监测点发现溶解铀的铀/钍活度比(AR)、总溶解固体(TDS)和溶解碳酸氢盐含量之间存在显著关系,AR与溶解速率之间也存在显著关系。用于隐蔽铀矿床水文地球化学勘查的logU与AR图表明,水源主要来自还原环境。证明了利用溶解铀浓度和AR数据的倒数来确定不同地下水体混合体积的可能性。最高溶解铀浓度(4.82微克/升)远低于世界卫生组织允许的最大值。

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