Short-lived natural radionuclides as tracers in hydrogeological studies - A review.
Autor: | Schubert M; Helmholtz Centre for Environmental Research GmbH - UFZ, Department Catchment Hydrology, Permoserstr. 15, 04318 Leipzig, Germany. Electronic address: michael.schubert@ufz.de., Lin M; State Key Laboratory of Isotope Geochemistry and CAS Center for Excellence in Deep Earth Science, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China., Clark JF; Department of Earth Science, University of California, Santa Barbara, CA 93106, USA., Kralik M; Department 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., Damatto S; Instituto de Pesquisas Energeticas e Nucleares (IPEN), Comissão Nacional de Energia Nuclear (CNEN), Av. Prof. Lineu Prestes, 2242 Cidade Universitaria, 05508-000 Sao Paulo, Brazil., Copia L; International Atomic Energy Agency, Department of Nuclear Sciences and Applications, Division of Physical and Chemical Sciences, Isotope Hydrology Section, Vienna International Centre, PO Box 100, 1400, Vienna, Austria., Terzer-Wassmuth S; International Atomic Energy Agency, Department of Nuclear Sciences and Applications, Division of Physical and Chemical Sciences, Isotope Hydrology Section, Vienna International Centre, PO Box 100, 1400, Vienna, Austria., Harjung A; International Atomic Energy Agency, Department of Nuclear Sciences and Applications, Division of Physical and Chemical Sciences, Isotope Hydrology Section, Vienna International Centre, PO Box 100, 1400, Vienna, Austria. |
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Jazyk: | angličtina |
Zdroj: | The Science of the total environment [Sci Total Environ] 2024 Apr 10; Vol. 920, pp. 170800. Date of Electronic Publication: 2024 Feb 09. |
DOI: | 10.1016/j.scitotenv.2024.170800 |
Abstrakt: | Fundamental approaches to the study of groundwater rely on investigating the spatial and temporal distribution of stable and radioactive isotopes and other anthropogenic compounds in natural waterbodies. The most often used tracers for estimating groundwater flow paths and residence times, groundwater/surface water interaction as well as tracing chemical (contamination) sources include stable isotopes of water (δ 18 O and δ 2 H), radiocarbon ( 14 C; t Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper. (Copyright © 2024 The Authors. Published by Elsevier B.V. All rights reserved.) |
Databáze: | MEDLINE |
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