158 D8. Minerals, Energy, Microbes, and Organics: Impacts on the Environment, Society and Health
Tuesday, 24 September 2019
8:00 AM - 12:00 PM
Room 132ABC, North Building
NOBLE GAS STABLE ISOTOPE RECONSTRUCTION OF BACKGROUND CLIMATOLOGICAL WATER TABLE DEPTHS: AN INDICATOR OF LITHIUM MINING IMPACTS
Paper number: 158-9
Program: Technical Sessions
Time: 9:50 AM – 10:05 AM
Authors
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Alan M. SeltzerUniversity of California-San Diego, La Jolla, CA
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Jeffrey P. SeveringhausUniversity of California-San Diego, La Jolla, CA
Abstract
We apply a recently developed tool to reconstruct past water table depths using the isotopic composition of noble gases dissolved in groundwater in the Salar de Atacama, Chile, and Salinas Grandes, Argentina. Gravitational settling in the unsaturated zone of soils causes the heavy-to-light ratio of xenon and krypton isotopes to increase linearly with depth.3 Gases dissolved in groundwater thus reflect the depth-dependent isotopic composition of the unsaturated zone air just above the water table, recording the signal of the water table depth.
This project has been developed in collaboration with local indigenous communities with the goal of evaluating conflicting hydrological models4,5 of basins in the Lithium Triangle and ultimately assessing potential lithium mining impacts to groundwater.
1) 4. Kay (2018) Investing News. 2) Corenthal, et al. (2016) Geophys. Res. Lett. 43. 3) Seltzer, et al. (2017) Water Resources Research 53: 2716-2732. 4) Boutt et al. (2016) Hydrological Processes 30: 4720-4740. 5) Marazuela et al. (2019) Science of the Total Environment 654: 1118-1131.
Geological Society of America Abstracts with Programs. Vol. 51, No. 5
doi: 10.1130/abs/2019AM-338123
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