CrVI and Trace Element Contaminated Groundwater Systems Connected with Ophiolitic Rocks

The level and distribution of chromium (as total chromium and CrVI) and other trace elements were investigated from surface and groundwater samples collected over three periods (n = 155) from Mersin (Turkey) in terms of their origins and potential health risk. The maximum total chromium is 41 µg/L and some of the samples have CrVI contents above 5 µg/L, which is the maximum permissible level of CrVI under Italian regulations. The dominant water facies are Ca-HCO₃ and Mg-HCO₃ types based on the Piper diagram. The Ca-HCO₃ type waters originate mainly from interaction with carbonate rocks, and the Mg-HCO₃ type waters originate from serpentinite dissolution. Chromium contents are higher in Mg-HCO₃ water types and the highest concentrations are found in samples from ophiolitic rocks and industrial areas. The As, Fe, Pb, Al, and Ni contents of some samples are above the EU limits in industrial areas.