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Mapping of Uranium-238 Deposit and its Contribution to Indoor Radon Gas in Ota, Ogun State, Nigeria

机译:铀-238矿床沉积物的测绘及其对Ota,Ogun州,尼日利亚的室内氡气的贡献

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In the present study, the distribution of uranium-238 was mapped from the background radiation of the area of study in order to determine its contribution to the concentration of indoor radon. The background radiation was studied using the handheld gamma spectrometer (RS 125) while the indoor radon concentration was measured with a Durridge RAD7 instrument. The results obtained showed variation in the distribution of 238U, 232Th and 40K in the study area with values ranging between 17.9 ± 0.3 and 58.05 ± 0.3, 2848 ± 10541 ± 0.8 and 3.25 ± 0.2 and 11.48 Bq/kg respectively. Furthermore, the indoor radon concentration was determined for the office on the ground floor, the result obtained was noted to be between 20 and 160 Bqm~(-3) which is far higher than the result obtained for the office on the first floor which is BDL-19 Bqm~(-3). In each cases, the results are lower than the international recommended safe limit of 200 Bqm~(-3). Therefore, it can be concluded that the background radiation from the soil in the premises and under the building contributes to the high concentration of indoor radiation in the office.
机译:在本研究中,铀-238的分布,以确定其对室内氡的浓度贡献从研究的区域的背景辐射映射。使用手持式伽马光谱仪(RS 125)研究了背景辐射,同时用DRIDGE RAD7仪器测量室内氡浓度。得到的结果显示了研究区域中238U,232和40K的分布的变化,其值分别值17.9±0.3和58.05±0.3,2848±10541±0.8和3.25±0.2和11.48 BQ / kg。此外,在底板上测定室内氡浓度,所得到的结果介于20至160bqm〜(-3)之间,远远高于在第一层上为办公室获得的结果BDL-19 BQM〜(-3)。在每种情况下,结果低于国际建议的200 bqm〜(-3)的安全限额。因此,可以得出结论,房屋和建筑物下的土壤中的背景辐射有助于办公室的高浓度室内辐射。

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