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一种测定土壤气体中220Rn(钍射气)浓度的方法。

A method for determining soil gas 220Rn (thoron) concentrations.

作者信息

Hutter A R

机构信息

Environmental Measurements Laboratory, U.S. Department of Energy, New York, NY 10014-3621, USA.

出版信息

Health Phys. 1995 Jun;68(6):835-9. doi: 10.1097/00004032-199506000-00012.

Abstract

A technique has been developed to accurately, precisely, and quickly measure soil gas 220Rn using commercially available grab-sample scintillation detectors. The method requires two counting periods for each sample: a 1-min count as soon as the sample has been drawn into a scintillation cell, followed by a 5- or 10-min count at least 5 min after the soil gas sample has been obtained. The 222Rn concentration is determined from the second count. The counts in the first counting period (1-min) due to 222Rn and its progeny are calculated from the known 222Rn concentration and then subtracted from the total counts obtained in the first counting period. The remaining counts are due to 220Rn and its progeny and are used to calculate the 220Rn concentration. The overall uncertainty when using this method to measure typical soil gas 220Rn and 222Rn concentrations [> approximately 5 kBq m-3 (130 pCi L-1)] was determined to be 19.8% and 10.8% (90% confidence levels), respectively, from analyses of duplicate field measurements. The lowest 220Rn concentrations that can be measured using this technique while maintaining an overall error no greater than about 30% is approximately 500 Bq m-3 (13 pCi L-1), assuming an approximately equal 222Rn concentration. The 220Rn measurement uncertainty at this concentration level decreases to approximately +/- 20% if at least three measurements sampled in series are arithmetically averaged. The uncertainty in the 220Rn measurement at low levels is proportionately affected by the relative concentration of 222Rn present.

摘要

已开发出一种技术,可使用市售的抓取式闪烁探测器准确、精确且快速地测量土壤气体中的220Rn。该方法对每个样品需要两个计数周期:样品一旦被吸入闪烁池,立即进行1分钟计数,然后在获得土壤气体样品至少5分钟后进行5或10分钟计数。222Rn浓度由第二次计数确定。根据已知的222Rn浓度计算第一次计数周期(1分钟)中由222Rn及其子体产生的计数,然后从第一次计数周期获得的总计数中减去该值。剩余的计数归因于220Rn及其子体,并用于计算220Rn浓度。通过对重复现场测量的分析,使用该方法测量典型土壤气体220Rn和222Rn浓度[>约5 kBq m-3(130 pCi L-1)]时的总体不确定度分别确定为19.8%和10.8%(90%置信水平)。假设222Rn浓度大致相等,使用该技术在保持总体误差不大于约30%的情况下可测量的最低220Rn浓度约为500 Bq m-3(13 pCi L-1)。如果对至少三个串联采样的测量值进行算术平均,该浓度水平下的220Rn测量不确定度将降至约±20%。低水平220Rn测量的不确定度受存在的222Rn相对浓度的成比例影响。

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