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22 nd Salt Water Intrusion Meeting: Salt Water Intrusion in Aquifers: Challenges and Perspectivesdifferent equivalent concentrations, is resulting in brine with an enriched and a depletedcomponent of this pair. In principle mixing of this brine with the pristine groundwater canlead to further precipitation of the same mineral, wherever in the aquifer mixing occurs.REFERENCESBauer-Gottwein, P., T. Langer, H. Prommer, P. Wolski, and Kinzelbach, W., 2007. OkavangoDelta islands: Interaction between density-driven flow and geochemical reactions underevapo-concentration. J. Hydrol., 335, 389– 405.Freedman, V., & Ibaraki, M., 2002. Effects of chemical reactions on density-dependent fluidflow: On the numerical formulation and the development of instabilities. Adv. WaterResour., 25, 439–453.Langevin, C. D., & Guo, W., 2006. MODFLOW/MT3DMS-based simulation of variabledensityground water flow and transport. Ground Water, 44(3), 339–351.Mao, X., Prommer, H., Barry, D. A., Langevin, C. D., Panteleit, B., & Li, L. 2006. Threedimensionalmodel for multi-component reactive transport with variable densitygroundwater flow. Environ. Modell. Software, 21, 615– 628.Millero, F.J. 2001. Speciation of metals in natural waters. Abstracts of Papers of theAmerican Chemical Society, 221(1). U533-U533.Post, V.E.A., & Prommer, H., 2007. Reactive multicomponent transport simulation of theElder problem: Effects of chemical reactions on salt plume development. WaterResources Research. 43(10), W10404.Sanford, W. E., & Konikow, L. F., 1989. Simulation of calcite dissolution and porositychanges in saltwater mixing zones in coastal aquifers. Water Resour. Res., 25(4), 655–667.Sanford, W.E., & Wood, W.W., 1991. Brine evolution and mineral deposition inhydrologically open evaporite basins. Am J Sci 291 (7), 687–710.Wigley, T. M. L., & Plummer, L. N., 1976. Mixing of carbonate waters. Geochim.Cosmochim. Acta, 40, 989– 995.Yechieli, Y., & Wood, W.W., 2002. Hydrogeologic processes in saline systems: playas,sabkhas, and saline lakes. Earth-Science Reviews 58 (3–4), 343–365.182