Conclusions from an IAEA Meeting on the sample preparation and measurement of radio sulfur in natural water samples
- 1Department of Nuclear Sciences and Applications, Vienna International Centre, International Atomic Energy Agency, 1400 Vienna, Austria.
- 2Department Umweltgeowissenchaften, Division of Environmental Geosciences (EDGE) Center for Microbiology and Environmental Systems Science, University of Vienna, Josef-Holaubek-Platz 2, UZA II VIENNA A-1090,Austria.
- 3Instituto de Pesquisas Energeticas e Nucleares (IPEN), Comissão Nacional de Energia Nuclear (CNEN), Cidade Universitaria, 05508-000 SÃO PAULO, BRAZIL.
- 4Universitaetsklinikum Heidelberg, Im Neuenheimer Feld 672, HEIDELBERG 69120,GERMANY.
- 5Department of Analytical Chemistry, Helmholtz Centre for Environmental Research UFZ, Permoserstrasse 15, 04318 LEIPZIG, GERMANY.
- 6WasserCluster Lunz, Biologische Station GmbH, Dr. Carl Kupelwieser Promenade 5, 3293 LUNZ AM SEE, AUSTRIA.
- 7Centre National de l'Energie, des sciences et des Techniques Nucléaires (CNESTEN), B.P 1382 RABAT PRINCIPALE, 10001 11100 RABAT,MOROCCO.
- 8Lawrence Livermore National Laboratory, 7000 East Ave., Livermore, SAN DIEGO, CA 94550-9234 UNITED STATES OF AMERICA.
Research on groundwater residence times is essential for evaluating groundwater abstraction rates and aquifer vulnerabilities, and hence, for sustainable water resources management. Naturally occurring radionuclides are suitable tools for related investigations. While the applicability of several long-lived radionuclides for the investigation of long-term processes has been demonstrated frequently, tracer-based approaches for studying residence times of less than one year have not been fully exploited. That is due to the rather small number of applicable radionuclides that show adequately short half-lives. A promising approach for investigating sub-yearly residence times applies radioactive Sulphur (35S). Radio-Sulphur is naturally produced by high-energy cosmic radiation in the upper atmosphere from where it is transferred with precipitation to the groundwater. As soon as the meteoric water enters the subsurface its 35S activity concentration decreases with an 87.4-day half-life. This makes 35S suitable for investigating sub-yearly groundwater residence times. However, the low 35S activities in natural waters require sulphate pre-concentration for 35S detection by means of liquid scintillation counting. This is done by sulphate extraction from large water samples with anion-exchange resins or/and precipitation as BaSO4. The resulting samples are usually associated with background interferences and quenching. The presented experiments aim at (i) optimizing the sample preparation procedure by simplifying the pre-concentration of sulphate to make it applicable for field sampling and at (ii) reducing quench and background during measurement. We will discuss the different sample preparation methods and lessons learned for the detection and quantification of 35S pre-concentrated from natural water samples that contain a wide range of SO42− concentrations.
How to cite: Kamau, S., Mostafa Amghar, E., Bibby, R., Copia, L., Coulson, L., Damatto, S., Harjung, A., Kopitz, J., Kralik, M., McGuire, B., Schubert, M., and Terzer-Wassmuth, S.: Conclusions from an IAEA Meeting on the sample preparation and measurement of radio sulfur in natural water samples, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-20334, https://doi.org/10.5194/egusphere-egu24-20334, 2024.