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Assessment of interconnection between surface water and groundwater in Sawa Lake area, southern Iraq, using stable isotope technique

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Abstract

Interaction between surface water represented by the Euphrates River, natural springs, and Sawa Lake with groundwater (11 wells) in southern Iraq was investigated in this study. Water samples were collected for hydrochemistry and stable isotope (2H and 18O) analysis. Sampling of water from determined stations (10 stations along the Euphrates, 3 springs, and Sawa Lake) were carried out during two stages; the first was in October 2013(dry season) and the second one was in March 2014 (wet season). The aim of the research is to assess the interaction of groundwater–surface water, which includes Al-Atshan River (branch of the Euphrates River), Sawa Lake, and the groundwater in the study area by using hydrochemistry and stable isotope techniques. The results indicate that surface waters have a different type of water from that of groundwater. In δ 2H and δ 18O diagrams, all groundwater, springs, and Sawa Lake waters are plotted below the Global Meteoric Water Line (GMWL) and the local meteoric water line (LMWL) indicating the influence of evaporation processes and seasonal variation. The LMWL deviates by a d-excess about +13.71 toward the East Mediterranean meteoric water line (EMWL) indicating that the origin of the vapor source is the Mediterranean Sea. The river water has different isotopic compositions from that of groundwater, springs, and Sawa Lake. The final conclusion is that there is no clear influence of the groundwater on the river water while there is an intermixing between the groundwater in the different locations in the study area.

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Correspondence to K. K. Ali.

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This article is part of the Topical Collection on Water Resources in Arid Areas

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Ali, K.K., Ajeena, A.R. Assessment of interconnection between surface water and groundwater in Sawa Lake area, southern Iraq, using stable isotope technique. Arab J Geosci 9, 648 (2016). https://doi.org/10.1007/s12517-016-2673-6

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  • DOI: https://doi.org/10.1007/s12517-016-2673-6

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