Geohazards Research Center, King Abdulaziz University, P.O. Box 80206, Jeddah, Saudi Arabia.
Nuclear Materials Authority, P.O. Box 530, El-Maadi, Cairo, Egypt.
Environ Monit Assess. 2021 Jan 26;193(2):87. doi: 10.1007/s10661-021-08883-9.
The Al Aziziah area is built on volcanic and granitic rocks. The igneous rocks always contain a high amount of naturally radioactive elements such as uranium, thorium and potassium, which produce gamma rays causing environmental hazards when exceeding the permissible limit. Radon gas is a result from the decomposition of uranium/thorium leaks into enclosed areas (e.g. homes or offices). This leakage is controlled by many conditions, and one of them is the underlining rock type. To work on such an environmental study, a gamma ray spectrometer survey was used. The uranium, thorium and potassium contents, as well as their ratios and the total radiation, were determined and mapped. The radiation dose rate was calculated and mapped in mSv/y and nGy/h units. The radiation contamination of groundwater is detected from the contour map of the dose rate over the artificial drainage lines of rains and floods which move this water to the groundwater wells. The main results are as follows: granitic rocks show an average dose rate of about 2.4 mSv/y, while the deposits of these rocks have an average dose rate of 1.2 mSv/y. A low average dose is recorded over the basalt. The average radiation dose recorded in the study area is 1.08 mSv/y, while its range is from 0.001 to 4.41 mSv/y. The estimated effective doses within the Al Aziziah area and vicinity area were higher than 1 mSv/y, which is the public exposure limit, and lower than the occupational exposure limit of 20 mSv/y. We recommend ventilating homes and offices in these places on an ongoing basis and constant radon measuring in closed places.
阿扎齐耶地区建在火山岩和花岗岩上。火成岩通常含有大量天然放射性元素,如铀、钍和钾,当超过允许限值时,这些元素会产生伽马射线,造成环境危害。氡气是铀/钍泄漏到封闭区域(如家庭或办公室)分解的结果。这种泄漏受许多条件控制,其中之一是基础岩石类型。为了进行这样的环境研究,使用了伽马射线光谱仪测量。测定并绘制了铀、钍和钾的含量及其比值以及总辐射。计算并绘制了 mSv/y 和 nGy/h 单位的辐射剂量率。通过在人工排水线(雨水和洪水将这些水带到地下水井)的剂量率等高线图上检测地下水的辐射污染。主要结果如下:花岗岩的平均剂量率约为 2.4 mSv/y,而这些岩石的沉积物的平均剂量率为 1.2 mSv/y。玄武岩的平均剂量率较低。研究区域记录的平均辐射剂量为 1.08 mSv/y,范围为 0.001 至 4.41 mSv/y。阿扎齐耶地区及其附近地区的估计有效剂量高于 1 mSv/y,这是公众的暴露限值,低于 20 mSv/y 的职业暴露限值。我们建议在这些地方持续通风家庭和办公室,并在封闭场所持续测量氡气。