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Löhnert, E. P., & Sonntag, C. (1981). Grundwasserversalzungen im Raum Hamburg im Licht neuer Isotopendaten. Zeitschrift der Deutschen Geologischen Gesellschaft, 132, 559–574.
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Lucia, M. D., Kempka, T., Jatnieks, J., & Kuhn, M. (2017). Integrating surrogate models into subsurface simulation framework allows computation of complex reactive transport scenarios. Energy Procedia, 125, 580–587.
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Demirak, A., Balci, A., Karaoğlu, H., & Tosmur, B. (2006). Chemical characteristics of rain water at an urban site of south western Turkey. Environmental monitoring and assessment, 123(1-3), 271–283.
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Herut, B., Starinsky, A., & Katz, A. (1993). Strontium in rainwater from Israel: sources, isotopes and chemistry. Earth and Planetary Science Letters, 120(1-2), 77–84.
Abstract: Eighteen ram samples from Israel have been analyzed for their chemical composmon and S7Sr/S6Sr ratios The Sr-Isotoplc rahos lie In the range 0 7078 and 0 7092, and the Sr concentrations vary from 1 × 10 -4 to 9 x 10 4 meq Sr/l.
Soluble salts in rainwater are inherited from three major natural sources, seaspray, Recent marine minerals and mineral dust eroded from rock outcrops and soft A mixing model is formulated to apply the chemical composmon of rain (CI and Sr 2+) and ~ts isotopic 87Sr/S6Sr ratio, for the identification and est~mahon of the Sr sources.
All the samples fall within the m~xing space predicted by the model for the three end members mentioned above The data indicate that the most important non-seaspray source contributing d~ssolved salts to the rams m Israel comprises a mixture of Senoman to Eocene chalk (and its weathering products) and Recent marine minerals, from local and imported sources.
Most of the samples (67%) contain 50% or more non-seaspray Sr 0 e, Sr dissolved from dust or Recent marine minerals), whereas 56% of the samples display 87Sr/86Sr ratios lower than 0 7090. The rest represent mixtures of seaspray and Recent marine minerals.
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Arslan*, H. (2012). Spatial and temporal mapping of groundwater salinity using ordinary krigingand indicator kriging: The case of Bafra Plain, Turkey. Agric. Water Manag., 113, 57–63.
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