Centre for Atomic Molecular Physics and Quantum Optics, University of Douala, PO Box 8580, Douala, Cameroon.
Local Material Promotion Authority, PO BOX 2396, Yaoundé, Cameroon.
Radiat Environ Biophys. 2023 Nov;62(4):427-439. doi: 10.1007/s00411-023-01042-3. Epub 2023 Aug 3.
The radon-prone area of the Adamawa region in Cameroon is characterized by high natural radiation background resulting from the high concentrations of radium-226, thorium-232, and indoor radon. To produce a radon-risk map, radon measurements in soil were carried out in the city of Ngaoundere. The radon activity concentration in soil gas ranged from 256 to 166 kBq m with a mean of 80 kBq m and a standard deviation of 38 kBq m. The area is mostly classified as high risk (80%) according to the Swedish classification, and 20% as medium risk. A low-risk area was not observed. Granite-like geology sites were characterized by higher radon concentration. A ratio of about 295:1 was obtained for soil radon gas to indoor radon concentrations, with a positive correlation (R = 0.40), and a transfer factor of 3 per mil. These results demonstrate that in situ measurements of radon concentration in soil can provide accurate information on the level of indoor radon concentrations. Geostatistical and deterministic interpolation techniques have been used to obtain a radon map by comparing the suitability of ordinary kriging and inverse-distance-weighted (IDW) interpolation methods. It turned out that there is not much difference in the prediction errors of the two techniques (Root Mean Square Error = 34.4 for ordinary kriging and 34.3 for IDW). It is concluded that both methods give acceptable results. In situ measurements and geostatistical analysis allow assessment of expected indoor radon exposure in a given area at reduced costs and time required. However, for the investigated area, more research is needed to produce reliable radon-risk maps.
喀麦隆阿达马瓦地区的氡高发地区的特点是镭-226、钍-232 和室内氡的浓度高,导致天然辐射背景高。为了制作氡风险图,在 Ngaoundere 市进行了土壤中的氡测量。土壤气体中的氡活度浓度范围为 256 至 166 kBq/m,平均值为 80 kBq/m,标准偏差为 38 kBq/m。根据瑞典分类,该地区主要被归类为高风险(80%),20%为中风险。没有观察到低风险区。类花岗岩地质点的氡浓度较高。土壤氡气与室内氡浓度的比值约为 295:1,呈正相关(R = 0.40),转移因子为 3 毫拉德。这些结果表明,土壤中氡浓度的原位测量可以提供室内氡浓度水平的准确信息。使用地质统计学和确定性插值技术,通过比较普通克里金插值法和反距离加权插值法的适用性,获得了氡图。结果表明,两种技术的预测误差没有太大差异(普通克里金法的均方根误差为 34.4,反距离加权法为 34.3)。可以得出结论,两种方法都能给出可接受的结果。原位测量和地质统计学分析可以以较低的成本和所需时间评估给定区域内预期的室内氡暴露情况。然而,对于所研究的地区,需要进行更多的研究以生成可靠的氡风险图。