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首页> 外文期刊>Annals Of Geophysics >A study of radon and thoron concentration in the soils along the active fault of NW Himalayas in India
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A study of radon and thoron concentration in the soils along the active fault of NW Himalayas in India

机译:印度西北喜马拉雅山活动断裂带土壤中ra和tho的浓度研究

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The Study has been conducted to analyse the radon and thoron flux in the soils of Mandi district, Himachal Pradesh. The detectors have been rooted at seventy one lithological locations in the north-eastern part of the district.? The average values of radon concentration has been observed as 4541 Bq/m 3 with maximum of 19970 Bq/m 3 at location no 3 and minimum of 867 Bq/m 3 at location no 57 and the Thoron variation ranges from 37 to 6970 Bq/m 3 with an average value of 1778 Bq/m 3 . The radon liberation at different positions has been correlated to the presence of the active fault to reveal the contributory aspects for abnormal release of radon in the soils. The spatial distribution of Radon and Thoron gas along the lines passing through the fault zones have unveiled the variances connected to the local tectonic structures. Radon exhalation rates, radium contents and porosity of soil samples have been calculated and a correlation factor of 0.64 has been detected for the observed concentrations of thoron and the porosity of the soil.
机译:该研究已经进行了分析,以分析喜马al尔邦曼迪地区土壤中的ra和气通量。这些探测器植根于该地区东北部的71个岩性位置。 don浓度的平均值为4541 Bq / m 3,在3号位置的最大值为19970 Bq / m 3,在57号位置的最小值为867 Bq / m 3,而Thoron的变化范围为37至6970 Bq / m 3。 m 3,平均值为1778 Bq / m 3。 positions在不同位置的释放与活动断层的存在相关,揭示了abnormal在土壤中异常释放的原因。 on气和Thor气沿着穿过断裂带的线的空间分布揭示了与局部构造结构有关的变化。计算了samples气的出气率,镭含量和土壤样品的孔隙率,对于观测到的of浓度和土壤孔隙率,相关系数为0.64。

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