A positive and negative value connotes enrichment and depletion in the heavy isotope respectively relative to the standard. These values indicate biogenic origin and dominance of shallow water-soil interaction. Therefore, these stable isotopic ratios are useful in evaluating the precipitation source areas of recharge to an aquifer Mazor, Our sampling sites comprised of shallow groundwater wells mostly hand-dug and surface water located around and across the study area. The precision obtained was 0.
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