THE INDOOR RADON AND THORON CONCENTRATIONS IN SCHOOLS OF SKOPJE (REPUBLIC OF NORTH MACEDONIA) AND BANJA LUKA (REPUBLIC OF SRPSKA) CITIES MEASURED BY RADUET DETECTORS

Z. Stojanovska, Z. Curguz, P. Kolarž, Z. Žunić, I. Boev, B. Boev
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Abstract

Radon (222Rn) and thoron (220Rn) are natural radioactive gases, generated in the terrestrial materials. They are the main sources of public exposure to ionising radiation in any of indoor environment worldwide. Differences in half-lives of 222Rn (T1/2 = 3.8 d) and 220Rn (T1/2 = 55.6 s) lead to its different indoor behavior. Several studies of indoor 222Rn and 220Rn in Northern Macedonia have been performed, starting with measurements in dwellings in 2008 and continuing with measurements in schools during 2012. The surveys in the Republic of Srpska began later (in 2011) with the simultaneous 222Rn and 220Rn measurements in the dwellings and schools of Banja Luka cities. This paper, as a result of our cooperation, summarizes the results and general conclusions obtained from 222Rn and 220Rn measurements in schools of capitals. In both cities, the measurements were made using Raduet - nuclear track detectors; deployed at distances: >0.5m (Skopje) and 0.2m (Banja Luka); and exposed in a period: March 2012 - May 2012 (Skopje) and April 2011 - May 2012 (Banja Luka). Results for 222Rn and 220Rn concentrations in both cities have a log-normal distribution. The 222Rn geometric mean value of 71 Bq/m3 in Skopje is higher than in Banja Luka city (GM = 50 Bq/m3). Among different radon potential in the cities, this difference could be related to the different exposure time of detectors. Furthermore, the dispersion of the 222Rn results in each city expressed through geometric standard deviation is relatively low: GSD = 2.13 (Skopje) and GSD = 2.11 (Banja Luka) indicating relatively homogeneous data sets. The 220Rn concentrations in Banja Luka (GM = 51 Bq/m3) were higher than in Skopje (GM = 11 Bq/m3). It is obvious that in the case of 220Rn, the exposure period did not play a significant role. One of the reasons for this difference could be the position of the detectors as well as the different building materials in the schools. On the contrary, the dispersion of the 220Rn results in Skopje (GSD = 3.38) was greater than in Banja Luka (GSD = 2.07).
氡(222Rn)和钍(220Rn)是天然放射性气体,产生于陆地物质中。它们是全世界任何室内环境中公众暴露于电离辐射的主要来源。222Rn (T1/2 = 3.8 d)和220Rn (T1/2 = 55.6 s)的半衰期不同,导致其室内行为不同。在马其顿北部开展了几项关于室内222Rn和220Rn的研究,从2008年开始在住宅中进行测量,并在2012年继续在学校进行测量。斯普斯卡共和国的调查开始较晚(2011年),在巴尼亚卢卡城市的住宅和学校同时测量222Rn和220Rn。本文是我们合作的结果,总结了首都学校222Rn和220Rn测量的结果和一般结论。在这两个城市,测量是使用Raduet -核径迹探测器进行的;部署距离:>0.5米(斯科普里)和0.2米(巴尼亚卢卡);暴露时间为:2012年3月至2012年5月(斯科普里)和2011年4月至2012年5月(巴尼亚卢卡)。两市222Rn和220Rn浓度均呈对数正态分布。斯科普里的222Rn几何平均值为71 Bq/m3,高于巴尼亚卢卡市(GM = 50 Bq/m3)。不同城市氡势的差异可能与探测器暴露时间的不同有关。此外,通过几何标准偏差表示的222Rn结果在每个城市的离散度相对较低:斯科普里的GSD = 2.13,巴尼亚卢卡的GSD = 2.11表明数据集相对均匀。巴尼亚卢卡220Rn浓度(GM = 51 Bq/m3)高于斯科普里(GM = 11 Bq/m3)。很明显,在220Rn的情况下,暴露时间并没有起到显著的作用。造成这种差异的原因之一可能是探测器的位置以及学校建筑材料的不同。相反,斯科普里(GSD = 3.38) 220Rn结果的分散度大于巴尼亚卢卡(GSD = 2.07)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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