标准添加法测定粉末样品中的210Pb

C.John Bland
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引用次数: 7

摘要

标准添加法是化学中测定微量物质的一种众所周知的方法。用46.5 keV的γ射线在约4%的衰变中对210Pb的活度进行了放射性测定。将210Pb活度的标准添加物吸附在阴离子交换树脂上,然后与样品混合。该程序用于提取的面积的光峰从连续体上,它是叠加,是详细描述。210Pb活度的值是使用拟合计数率数据的最佳直线的斜率和截距来计算的。在四个标准矿石样品上获得的结果表明,该方法产生的结果与其他方法(如提示210Bi子矿的β-射线光谱法)的准确度相当。然而,这种方法避免了所需的繁琐的化学分离。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Radiometric determination of 210Pb in powder samples by the method of standard additions

The method of standard additions is a well known procedure in chemistry for the measurement of trace substances. The use of this method is described in the radiometric determination of 210Pb activity via the γ-ray at 46.5 keV emitted in about 4% of the decays. Standard additions of 210Pb activity are adsorbed on anion exchange resin which is then mixed with the sample. The procedure used to extract the area of the photopeak from the continuum on which it is superimposed, is described in detail. The value of the 210Pb activity is calculated using the slope and intercept of the best straight line fitting the count-rate data plotted against added activity. Results obtained on four standard ore samples indicate that this method yields results of comparable accuracy to other methods such as β-ray spectrometry of the prompt 210Bi daughter. This method, however, avoids the tedious chemical separations required.

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