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Radon exhalation rate from soil samples of South Kumaun Lesser Himalayas, India

机译:印度南部小喜玛拉雅山土壤样品中ex的呼出率

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摘要

Ionizing radiation expoSUre experienced by the general population SU mainly due to the indoor radon. Major part of radon comes from the top layer of the earth. The radon emanation SU associated with radon in soil and sleepy back radium in the soil. Both field and laboratory meaSUrements were carried out for the instantaneous and integrated radon concentration in soil-gas. The radon exhalation rate from collected soil samples was meaSUred using LR-115 Type II plastic track detector. The soil-gas radon concentration was meaSUred with the help of radon Emanometry method. The effective radium content of the soil samples was also calculated. The correlation coefficient between radium contents in collected soil samples and soil-gas radon from the same locations was calculated as 0.1, while it SU 0.2 between radon exhalation rate and soil-gas radon concentration. The reSUlts show weak positive correlation due to the geological dSUturbance in the equilibrium conditions and high mobility of radon in the same geological medium.
机译:一般人群SU经历的电离辐射暴露主要是由于室内the。 ra的大部分来自地球的顶层。 soil散SU与土壤中的and和土壤中的sleep睡镭有关。对土壤气体中瞬时和综合for浓度均进行了现场和实验室测量。使用LR-115 II型塑料径迹检测器测量收集的土壤样品中的气呼出率。借助于E量热法测量土壤气中concentration的浓度。还计算了土壤样品的有效镭含量。取土样中镭含量与同一地点土壤气ra的相关系数经计算为0.1,ex析出率与土壤气ra浓度的相关系数为SU 0.2。由于平衡条件下的地质扰动和ra在同一地质介质中的高迁移率,结果显示出弱的正相关性。

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