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Determination of correction factor of self-absorption for lead-210 in environment samples using spike method

机译:用尖峰法测定环境样品中铅210的自吸收校正因子

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In environment radiation measurement, calculation the correction factors are critical, especially for low energy measurement because of self-absorption phenomena. In this work the main purpose is to determination the self-absorption correction factors of lead-210 (210Pb) energy (46.5keV) in various environment samples (7 sediments, 5 soil) using an experimental method called Spike Method. The samples were collecting from different places in Syrian. They were prepared according to the laboratory producers starting from collecting, cleaning, drying, grounding, hemogenic and calculating the appearance density. Low-energy gamma spectroscopy HPGe was used for radiation analysis which available at the laboratories of the Protection and Safety Department - Syrian Atomic Energy Commission – Syria. The spike method depends on adding a quantity of a standard solution with a known activity which contains lead isotope 210Pb and added to the studied samples. Self-absorption correction factors (CF) calculated by the ratio of the count rate or activity of spiked and unspiked samples. The CF for sediment samples were between 29% to 54% and for soil samples, the CFs were between 38% to 56% recording correction higher than sediment samples. The results showed a relatively high self-absorption and CFs values because of the chemical composition changeable between the spiked and unspiked samples. For that, it is better to adopt other methods less expensive, give results faster, higher accuracy and do not make change in the chemical composition. The results were also showed the density factor is the most influential factor in self-absorption phenomena.
机译:在环境辐射测量,计算校正因子是关键的,特别是对于因自吸收现象低能量的测量。在该工作的主要目的是确定自吸收校正铅-210(210Pb测)能量(46.5keV)的各种环境样品中使用称为穗方法的实验方法的因素(7个沉积物,土壤5)。样品从叙利亚不同的地方收集。它们根据从收集,清洗,干燥,接地,hemogenic和计算的外观密度开始实验室生产制备。低能量的伽玛能谱高纯锗用于辐射分析其提供的保护和安全部门的实验室 - 叙利亚原子能委员会 - 叙利亚。尖峰方法取决于添加标准溶液的量与已知的活性,其含有铅同位素210Pb测,并加入到所研究的样本。通过加标和未加标样品的计数率或活性的比率计算自吸收校正系数(CF)。对沉积物样品的CF分别为29%至54%,对于土壤样本,中心分别为56%记录比校正沉积物样品高38%之间。结果表明,因为加标和未加标样品之间的化学组成改变的相对高的自吸和CFS值。为此,最好是采取其他的方法更便宜,得出的结果更快,精度更高,不要使在化学成分变化。该结果也表明,密度系数是自吸收现象影响最大的因素。

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