{"title":"Measurement of the radon-222 content of soil gas by liquid scintillation counting","authors":"David P. Genereux, Harold F. Hemond","doi":"10.1016/0168-9622(91)90025-R","DOIUrl":null,"url":null,"abstract":"<div><p>A method is described for measuring the <sup>222</sup>Rn content of soil gas using a conventional liquid scintillation counter. Gas samples, collected in wetted ground-glass syringes, are equilibrated with a scintillation cocktail which is then expelled into a scintillation vial and counted. The method is straightforward and relatively fast (5–6 min. of operator's time per sample), and yields results having 95% confidence limits of ∼ ± 10% for samples containing ≥ 2·10<sup>4</sup> Bq m<sup>−3</sup> of <sup>222</sup>Rn. The method is applied to a watershed near Bickford Reservoir in Massachusetts, U.S.A., where soil-gas <sup>22</sup>Rn content is found to be reasonably constant horizontally, but strongly and systematically increasing with depth, to > 5·10<sup>4</sup> Bq m<sup>−3</sup> at soil depths of ∼ 1 m.</p></div>","PeriodicalId":100231,"journal":{"name":"Chemical Geology: Isotope Geoscience section","volume":"87 3","pages":"Pages 265-275"},"PeriodicalIF":0.0000,"publicationDate":"1991-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0168-9622(91)90025-R","citationCount":"5","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemical Geology: Isotope Geoscience section","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/016896229190025R","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 5
Abstract
A method is described for measuring the 222Rn content of soil gas using a conventional liquid scintillation counter. Gas samples, collected in wetted ground-glass syringes, are equilibrated with a scintillation cocktail which is then expelled into a scintillation vial and counted. The method is straightforward and relatively fast (5–6 min. of operator's time per sample), and yields results having 95% confidence limits of ∼ ± 10% for samples containing ≥ 2·104 Bq m−3 of 222Rn. The method is applied to a watershed near Bickford Reservoir in Massachusetts, U.S.A., where soil-gas 22Rn content is found to be reasonably constant horizontally, but strongly and systematically increasing with depth, to > 5·104 Bq m−3 at soil depths of ∼ 1 m.