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Distribution of natural radionuclides in the soils and assessment of radiation hazards in the Khrami Late Variscan crystal massif (Georgia)

机译:土壤中天然放射性核素的分布以及Khrami晚Variscan晶体地块(乔治亚州)的辐射危害评估

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摘要

This study was performed to determine the distributions of radionuclides (238U, 232Th and 40K naturally occurring in Khrami Late Variscan crystal massif and soils overlapping its adjacent territory built by Neogene and Quaternary lava using a gamma-ray spectrometry with an HPGe detector. By identification of artificial radionuclide 137Cs concentration revealed the character of radioactive contamination of the area under investigation. Based on the obtained results, the radiological parameters (outdoor absorbed gamma dose rate, annual effective dose; radium equivalent activity) were estimated to assess radiation hazards caused by use of industrial materials. The difference was established between concentrations of radionuclides having emerged at the expense of Late Variscan crystal substrate and recently erupted lavas. The results were compared with similar studies conducted in different countries and with data and recommendations published by international organizations (UNSCEAR, ICRP).
机译:本研究旨在确定在Khrami晚Variscan晶体地块和土壤中自然产生的放射性核素( 238 U, 232 Th和 40 K通过使用HPGe探测器的伽马射线光谱法,将其与新近纪和第四纪熔岩建造的相邻区域重叠,通过鉴定人工放射性核素 137 Cs的浓度,揭示了该区域放射性污染的特征。根据获得的结果,估算放射学参数(室外吸收的伽马剂量率,年有效剂量;镭当量活性)以评估使用工业材料引起的辐射危害,从而确定了以放射性同位素的消耗为代价而出现的放射性核素浓度之间的差异。 Variscan晶体基底和最近喷出的熔岩,将结果与不同国家进行的类似研究进行了比较,并与国际组织(UNSCEAR,ICRP)。

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