The nature and extent of bomb tritium remaining in deep vadose zone: A synthesis and prognosis

Author:

Huang Yanan1,Evaristo Jaivime2ORCID,Li Zhi1,Chun Kwok P.3,Sutanudjaja Edwin H.4,Cardenas M. Bayani5,Bierkens Marc F. P.46,Kirchner James W.789,van Genuchten Martinus Th.1011ORCID

Affiliation:

1. College of Natural Resources and Environment Northwest A&F University Yangling China

2. Copernicus Institute of Sustainable Development Utrecht University Utrecht The Netherlands

3. Department of Geography and Environmental Management University of the West England Bristol UK

4. Department of Physical Geography, Faculty of Geosciences Utrecht University Utrecht The Netherlands

5. Geological Sciences The University of Texas at Austin Austin Texas USA

6. Unit Soil and Groundwater Systems Deltares Utrecht The Netherlands

7. Department of Environmental Systems Science ETH Zurich Zurich Switzerland

8. Department of Earth and Planetary Science University of California Berkeley California USA

9. Swiss Federal Research Institute WSL Birmensdorf Switzerland

10. Department of Earth Sciences Utrecht University Utrecht The Netherlands

11. Department of Nuclear Engineering Federal University of Rio de Janeiro Rio De Janeiro Brazil

Abstract

AbstractTritium present in deep vadose zones is a useful tracer for estimating groundwater recharge, but its full utility is constrained by not knowing where and for how long the tritium tracing method remains applicable. We obtained 44 tritium profiles from 17 globally distributed sites with vadose zone thicknesses of 12–624 m and used transport models to estimate the number of years that tritium may still be useful. Results show that the method may still be usable for 26 of 44 soil profiles surveyed, mainly in China, Australia, the United States, South Africa, and Senegal, with a remaining useful period of between 6 and 83 years. We also developed a statistical model that uses outputs from a hydrological model to predict the applicability of the tritium tracing method. Global implementation of the statistical model showed that the method remains usable at 20% of Earth's land mass (excluding Antarctica and Greenland) over the next few decades.

Funder

National Natural Science Foundation of China

Natural Science Foundation of Shaanxi Provincial Department of Education

Publisher

Wiley

Subject

Soil Science

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