Articles | Volume 22, issue 12
Hydrol. Earth Syst. Sci., 22, 6323–6333, 2018
https://doi.org/10.5194/hess-22-6323-2018
Hydrol. Earth Syst. Sci., 22, 6323–6333, 2018
https://doi.org/10.5194/hess-22-6323-2018
Research article
06 Dec 2018
Research article | 06 Dec 2018

Managed aquifer recharge with reverse-osmosis desalinated seawater: modeling the spreading in groundwater using stable water isotopes

Yonatan Ganot et al.

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Cited articles

Al-Basheer, W., Al-Jalal, A., and Gasmi, K.: Variations in isotopic composition of desalinated water, Water Environ. J., 31, 209–214, https://doi.org/10.1111/wej.12232, 2017. 
Birnhack, L., Voutchkov, N., and Lahav, O.: Fundamental chemistry and engineering aspects of post-treatment processes for desalinated water – A review, Desalination, 273, 6–22, https://doi.org/10.1016/j.desal.2010.11.011, 2011. 
Boronina, A., Balderer, W., Renard, P., and Stichler, W.: Study of stable isotopes in the Kouris catchment (Cyprus) for the description of the regional groundwater flow, J. Hydrol., 308, 214–226, https://doi.org/10.1016/j.jhydrol.2004.11.001, 2005. 
Burnett R. D. and Frind E. O.: Simulation of contaminant transport in three dimensions: 2. Dimensionality effects, Water Resour. Res., 23, 695–705, https://doi.org/10.1029/WR023i004p00695, 1987. 
Carle, S. F.: T-PROGS: Transition probability geostatistical software, University of California, Davis, CA, 84, available at: http://gmsdocs.aquaveo.com/t-progs.pdf (last access: 15 August 2017), 1999. 
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In recent years, surpluses of desalinated seawater (DSW) are stored in the Israeli coastal aquifer. We monitor DSW spread in the aquifer using the difference between isotope composition of reverse-osmosis DSW and natural fresh water, which simplifies the system to two distinct end-members. A hydrogeological flow and transport model is used to demonstrate the robustness of this simplification, predict the future spread of DSW in the aquifer and mixing in wells, and estimate DSW recovery efficacy.