Preliminary studies on soil radon activity at geothermal hotspot of Bakreswar-Tantloi

Arkajit Aich
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引用次数: 1

Abstract

Bakreswar-Tantloi region of India, besides being a geothermally active region, also harbours a high amount of Radon in soil-gas and groundwater of the region. Measurement of Radon-content across the region is an active area of research aimed to properly understand the geothermal potential of the region, the study of local geology and to determine the risks of Radon exposure in the area. In an aim to evaluate the Radon potential of this important geothermal hub, we have done a pilot study on the region by doing spot measurements of Soil-Radon activity in 41 specific geographic locations spread out across the region of interest which will act as groundwork for further in-depth analysis. The measurements showed that Radon activity varies widely in the region with the Radon activity ranging from 1 kBqm−3 to 52 kBqm−3 across the measured locations. Mean Radon activity across the measured locations was found to be 16 kBqm−3 with standard deviation of the sample set of 14 kBqm−3. Seven locations recorded Radon activity to be greater than standard deviation from average while four locations recorded Radon activity greater than twice the standard deviation from average.
Bakreswar-Tantloi地热热点土壤氡活性的初步研究
印度Bakreswar Tantloi地区除了是一个地热活动区外,该地区的土壤气体和地下水中也含有大量的氡。测量整个地区的氡含量是一个活跃的研究领域,旨在正确了解该地区的地热潜力,研究当地地质,并确定该地区氡暴露的风险。为了评估这一重要地热枢纽的氡潜力,我们对该地区进行了试点研究,对分布在感兴趣地区的41个特定地理位置的土壤氡活动进行了现场测量,这将为进一步深入分析奠定基础。测量结果表明,该地区的氡活性变化很大,测量位置的氡活性范围为1 kBqm−3至52 kBqmm−3。测量位置的平均氡活度为16 kBqm−3,样本集的标准偏差为14 kBqmm−3。七个地点记录的氡活动大于平均值的标准偏差,而四个地点的氡活动则大于平均值标准偏差的两倍。
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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