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首页> 外文期刊>Applied radiation and isotopes: including data, instrumentation and methods for use in agriculture, industry and medicine >Distribution of natural and anthropogenic radionuclides in soil and beach sand samples of Kalpakkam (India) using hyper pure germanium (HPGe) gamma ray spectrometry.
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Distribution of natural and anthropogenic radionuclides in soil and beach sand samples of Kalpakkam (India) using hyper pure germanium (HPGe) gamma ray spectrometry.

机译:使用超纯锗(HPGe)γ射线光谱法在卡尔帕卡姆(印度)的土壤和海滩沙子样本中分布自然和人为放射性核素。

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摘要

Pre-operational survey at Kalpakkam coast, indicated elevated gamma background radiation levels in the range of 100-4000 nGy h(-1) over the large tracts of the coastal sands due to the presence of pockets of monazite mineral in beach sands. In view of the prevalence of monazite, a systematic gamma spectrometric study of distribution of natural radionuclides in soil and beach sand samples collected from the terrestrial and coastal environment of Kalpakkam was performed and concentrations of primordial radionuclides such as 238U, 232Th and 40K and anthropogenic radionuclide 137Cs were determined. The concentrations of 238U, 232Th and 40K in soil samples were 5-71, 15-776 and 200-854 Bq kg(-1) dry, respectively. In beach sand samples, 238U, 232Th and 40K contents varied in the range of 36-258, 352-3872 and 324-405 Bq kg(-1) dry, respectively. The total absorbed gamma dose rate in air due to the presence of 238U, 232Th and 40K in Kalpakkam soil samples varied between 24 and 556 nGy h(-1) with a mean of 103 nGy h(-1). The contribution to the total absorbed gamma dose rate in air in the decreasing order was due to the presence of 232Th (76.4%), followed by 40K (16.9%) and 238U (6.7%) in Kalpakkam soils. However, in beach areas of Kalpakkam, the presence of 232Th in beach sand contributed maximum (94.0%) to the total absorbed gamma dose rate in air followed by 238U (4.7%) and minimum contribution was by 40K (1.3%). 137Cs in Kalpakkam soils ranged from < or = 1.0 to 2.8 Bq kg(-1) dry, which was 1-3 order of magnitude less than the concentration of primordial radionuclides in soil.
机译:在卡尔帕卡姆海岸进行的作业前调查表明,由于海滩沙中存在独居石矿物,因此在大片沿海沙中,γ背景辐射水平升高,范围为100-4000 nGy h(-1)。鉴于独居石的普遍性,对从卡尔帕卡姆陆地和沿海环境收集的土壤和海滩沙子样品中的天然放射性核素分布进行了系统的伽马能谱研究,并对原始放射性核素(例如238U,232Th和40K和人为放射性核素)的浓度进行了研究。确定了137C。土壤样品中238U,232Th和40K的干重分别为5-71、15-776和200-854 Bq kg(-1)。在海滩沙样品中,238U,232Th和40K含量分别在36-258、352-872和324-405 Bq kg(-1)干燥范围内变化。卡尔帕卡姆土壤样品中由于存在238U,232Th和40K而在空气中吸收的总伽马剂量率在24至556 nGy h(-1)之间变化,平均值为103 nGy h(-1)。空气中总吸附伽马剂量率的降低顺序是由于存在232Th(76.4%),其后是卡尔帕卡姆土壤中的40K(16.9%)和238U(6.7%)。然而,在卡尔帕卡姆海滩地区,海滩沙子中232Th的存在对空气中总吸收伽马剂量率的贡献最大(94.0%),其次为238U(4.7%),最小贡献为40K(1.3%)。卡尔帕卡姆土壤中的137 Cs范围从<或= 1.0至2.8 Bq kg(-1)干,比土壤中原始放射性核素的浓度少1-3个数量级。

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