{"title":"Radio-sulphur (35S) detection by LSC – How to deal with interfering natural radionuclides","authors":"Michael Schubert , Juergen Kopitz","doi":"10.1016/j.jenvrad.2025.107813","DOIUrl":null,"url":null,"abstract":"<div><div>Naturally occurring radio-sulphur (<sup>35</sup>S) is suitable as an aqueous environmental tracer for the dating of groundwater and surface waters with residence times of less than one year. As a β-decaying radionuclide, <sup>35</sup>S is detected using liquid scintillation counting (LSC). When extracting <sup>35</sup>S as sulphate from large-volume water samples, there is the possibility of unintentional co-extraction of other naturally occurring radionuclides, which interfere with the measurement of <sup>35</sup>S by LSC. The most important of these radionuclides are (i) <sup>226</sup>Ra, (ii) the short-lived progeny of <sup>222</sup>Rn, (iii) <sup>210</sup>Pb and its progeny and (iv) <sup>3</sup>H. In addition, <sup>14</sup>C, which might be present in scintillation cocktails or LSC plastic vials, and <sup>40</sup>K, which is likely to be present in LSC glass vials, can have a significant impact on the LSC detection result. There are a few publications that address sample preparation for <sup>35</sup>S detection with LSC. However, the published datasets do not contain sufficiently detailed information to pursue the issue of potential interferences of the said naturally occurring radionuclides with the <sup>35</sup>S signal. In our study, we measured standardized samples containing the said radionuclides by LSC, evaluated location, shape and overlap of the associated energy peaks, and assessed the possible influences of the individual nuclides on the <sup>35</sup>S detection results. The findings of our study show that when measuring <sup>35</sup>S obtained from a natural water sample, counts detected in the <sup>35</sup>S energy window cannot be unconditionally interpreted as actual <sup>35</sup>S counts. Interfering nuclides (especially <sup>3</sup>H, <sup>14</sup>C, <sup>40</sup>K, and <sup>210</sup>Pb) can lead to counts in the <sup>35</sup>S energy window and thus to an overestimation of the <sup>35</sup>S activity concentration of the water sample (and consequently to an underestimation of the water age). We therefore recommend generally a complete evaluation of the LSC spectrum in order (i) to be able to infer the potential presence of other radionuclides in the measured sample, and (ii) to evaluate the DPM counted in the <sup>35</sup>S energy window accordingly, as these may contain counts of the aforementioned interfering radionuclides.</div></div>","PeriodicalId":15667,"journal":{"name":"Journal of environmental radioactivity","volume":"290 ","pages":"Article 107813"},"PeriodicalIF":2.1000,"publicationDate":"2025-09-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of environmental radioactivity","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0265931X25002000","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Naturally occurring radio-sulphur (35S) is suitable as an aqueous environmental tracer for the dating of groundwater and surface waters with residence times of less than one year. As a β-decaying radionuclide, 35S is detected using liquid scintillation counting (LSC). When extracting 35S as sulphate from large-volume water samples, there is the possibility of unintentional co-extraction of other naturally occurring radionuclides, which interfere with the measurement of 35S by LSC. The most important of these radionuclides are (i) 226Ra, (ii) the short-lived progeny of 222Rn, (iii) 210Pb and its progeny and (iv) 3H. In addition, 14C, which might be present in scintillation cocktails or LSC plastic vials, and 40K, which is likely to be present in LSC glass vials, can have a significant impact on the LSC detection result. There are a few publications that address sample preparation for 35S detection with LSC. However, the published datasets do not contain sufficiently detailed information to pursue the issue of potential interferences of the said naturally occurring radionuclides with the 35S signal. In our study, we measured standardized samples containing the said radionuclides by LSC, evaluated location, shape and overlap of the associated energy peaks, and assessed the possible influences of the individual nuclides on the 35S detection results. The findings of our study show that when measuring 35S obtained from a natural water sample, counts detected in the 35S energy window cannot be unconditionally interpreted as actual 35S counts. Interfering nuclides (especially 3H, 14C, 40K, and 210Pb) can lead to counts in the 35S energy window and thus to an overestimation of the 35S activity concentration of the water sample (and consequently to an underestimation of the water age). We therefore recommend generally a complete evaluation of the LSC spectrum in order (i) to be able to infer the potential presence of other radionuclides in the measured sample, and (ii) to evaluate the DPM counted in the 35S energy window accordingly, as these may contain counts of the aforementioned interfering radionuclides.
期刊介绍:
The Journal of Environmental Radioactivity provides a coherent international forum for publication of original research or review papers on any aspect of the occurrence of radioactivity in natural systems.
Relevant subject areas range from applications of environmental radionuclides as mechanistic or timescale tracers of natural processes to assessments of the radioecological or radiological effects of ambient radioactivity. Papers deal with naturally occurring nuclides or with those created and released by man through nuclear weapons manufacture and testing, energy production, fuel-cycle technology, etc. Reports on radioactivity in the oceans, sediments, rivers, lakes, groundwaters, soils, atmosphere and all divisions of the biosphere are welcomed, but these should not simply be of a monitoring nature unless the data are particularly innovative.