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Distribution of ~(222)Rn in groundwater and estimation of resulting radiation dose to different age groups: A case study from Bangalore City

机译:〜(222)Rn在地下水中的分布以及不同年龄段的辐射剂量估算:以班加罗尔市为例

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摘要

Ingesting waters holding high levels of natural occurring radioactive element like Radon would contribute to increase in the effective dose received by people followed by an increased prevalence of cancer. The current study is an attempt to describe the extent of contribution of Rn-222 to natural background radiation and the resultant effective dose to public of different age groups. In order to do so, 65 groundwater samples from selected parts of Bangalore city were collected and analyzed for radon activity using RAD7 radon monitor coupled with RAD H2O accessories. The radon activity was in the range of 3.05-696 Bq/L (mean: 91.39 Bq/L) and 92.31% of the groundwater samples recorded elevated radon concentration above the United States environmental protection agency (USEPA's) Maximum Contaminant Level (MCL) value of 300 pCi/L, corresponding to 11.1 Bq/L. The mean annual effective dose contribution of people falling under different age groups (viz., infants, children, teens: males and females, adults: males and females, pregnant and lactating women) due to ingestion of water-borne Rn-222 ranged from 0.082 to 0.444mSv/y and was found to be higher in all the age groups of males compared to respective female age groups, but well within the United Nations Scientific Committee on the Effects of Atomic Radiation (UNSCEAR) and World Health Organization (WHO) proposed limit of 1mSv/y.
机译:摄入含有高水平自然发生的放射性元素(如water)的水将有助于人们增加有效剂量,继而增加癌症的患病率。当前的研究试图描述Rn-222对自然本底辐射的贡献程度以及由此产生的对不同年龄段公众的有效剂量。为此,收集了班加罗尔市部分地区的65个地下水样品,并使用RAD7 don监测仪和RAD H2O附件对analyzed活动进行了分析。 activity活度在3.05-696 Bq / L(平均:91.39 Bq / L)的范围内,且92.31%的地下水样品记录到的elevated气浓度高于美国环境保护署(USEPA)的最大污染物水平(MCL)值300 pCi / L,相当于11.1 Bq / L。摄入水源性Rn-222引起的不同年龄组(即婴儿,儿童,青少年:男性和女性,成人:男性和女性,孕妇和哺乳期妇女)的年平均有效剂量贡献范围为0.082至0.444mSv / y,并且在所有年龄段的男性中均高于女性年龄段,但在联合国原子辐射影响科学委员会(UNSCEAR)和世界卫生组织(WHO)范围内建议的限制为1mSv / y。

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