土耳其西南部Muğla省宣塔地质氡势地质统计模拟

Mutlu Zeybek, Alican Kop
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摘要

氡(222Rn)是一种惰性放射性气体,来源于铀(238U)系列,从地层(土壤、岩石)(Qg)、断层(Qf)和建筑材料(Qm)中释放出来,不能被五种感官检测到。氡在建筑物中积聚过多(>200 Bq/m3),对人们的健康产生负面影响(如肺癌)。本研究的目的是测量在Muğla省(土耳其西南部)靠近断层或可能断层的建筑物(本研究的目的是清真寺尖塔)中构成总氡气浓度(Qt)的各组分(Qg, Qf, Qm)的氡排放浓度,并对其大小进行排序。利用便携式RadonEye设备(韩国产)测量了Muğla省841座宣讲塔的室内氡浓度(IRC)。使用便携式Markus 10装置(瑞典制造)垂直于14座尖塔附近的断层线进行了至少5次土壤氡浓度(SRC)测量。在841座尖塔中,约有10%被发现高于欧洲室内氡参考值(EIRRV) (200 Bq/m3)。根据13个区进行评价,841个尖塔中IRC最高的是马尔马里斯(Çetibeli镇,2809 Bq/m3),最低的是乌拉(armutuk镇,217 Bq/m3)。在Marmaris地区(Çetibeli镇,2809 Bq/m3)的一个火山岩尖塔内测量到最高的IRC。SRC最低的是datalada区(Kızlan镇,5830 Bq/m3),出露蛇纹岩;最高的是Bodrum区(g rece镇,120000 Bq/m3),出露火山岩。确定了靠近断层的尖塔与可能的断层影响Qt的因子(Qg、Qf、Qm)的大小存在Qf>Qg>Qm的关系。因此,有关机构应定期和定期地对人们居住的所有建筑物进行IRC测量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geological and Geostatistical Modeling of Geogenic Radon Potential of Minarets in Muğla Province (SW Turkey)
Radon (222Rn), derived from the Uranium (238U) series and emitted from Geological Formation (soil, rock) (Qg), Fault (Qf) and Construction Material (Qm), which cannot be detected by the five senses, is an inert radioactive gas. Radon negatively affects people's health (such as lung cancer) as a result of excessive (>200 Bq/m3) accumulation in buildings. The aim of this study is to measure the radon emission concentrations of the components (Qg, Qf, Qm) that make up the Total Radon Gas Concentration (Qt) in the building (for the purpose of this study, mosque minarets) close to the fault or the possible fault in Muğla province (SW Turkey) and order their sizes. The Indoor Radon Concentration (IRC) of 841 minarets in Muğla province was measured with a portable RadonEye device (made in South Korea). At least 5 Soil Radon Concentration (SRC) measurements were made perpendicular to the fault lines near 14 minarets with a portable Markus 10 device (made in Sweden). About 10% of the 841 minarets were found to be above the European Indoor Radon Reference Value (EIRRV) (200 Bq/m3). When evaluated according to the 13 districts, it is seen that the district with the highest IRC in the 841 minarets is Marmaris (Çetibeli town, 2809 Bq/m3), and the district with the lowest is Ula (Armutçuk town, 217 Bq/m3). The highest IRC was measured inside a minaret made of volcanic rocks in the Marmaris district (Çetibeli town, 2809 Bq/m3). The lowest SRC was obtained in Datça district (Kızlan town, 5830 Bq/m3) where serpentinites outcropped, and the highest SRC was found in Bodrum district (Gürece town, 120000 Bq/m3) where volcanic rocks outcropped. It has been determined that there is a Qf>Qg>Qm relationship between the magnitudes of the factors (Qg, Qf, Qm) affecting Qt in the minarets close to the fault and possible faults. As a result, IRC measurements in all buildings where people live should be done periodically and regularly by the relevant institutions.
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