Uranium levels in Cypriot groundwater samples determined by ICP-MS and α-spectroscopy

The uranium concentration and the isotopic ratio 238U/234U have been determined in Cypriot groundwater samples by ICP-MS after ultrafiltration and acidification of the samples and α-spectroscopy after pre-concentration and separation of uranium by cation-exchange (Chelex 100 resin) and electro-deposition on stainless steel discs. The uranium concentration in the groundwater samples varies strongly between 0.1 and 40 μg l−1. The highest uranium concentrations are found in groundwater samples associated with sedimentary rock formations and the obtained isotopic ratio 238U/234U varies between 0.95 and 1.2 indicating basically the presence of natural uranium in the studied samples. The pH of the groundwater samples is neutral to weak alkaline (7 < pH < 8) and this is attributed to the carbonaceous content of the sedimentary rocks and the ophiolitic origin of the igneous rocks, which form the background geology in Cyprus. Generally, in groundwaters uranium concentration in solution increases with decreasing pH (7 < pH < 8) and this is attributed to the fact that at lower pH dissolution of soil minerals occurs, and uranium, which is adsorbed or forms solid solution with the geological matrix enters the aqueous phase. This is also corroborated by the strong correlation between the uranium concentration and the electrical conductivity (e.g. dissolved solids) measured in the groundwaters under investigation.

► Higher uranium levels in sedimentary groundwater systems.
► Groundwater associated with igneous rock formations present lower uranium levels.
► Uranium levels in groundwater are related to the concentrations of TDS and pH.
► Uranium levels in groundwater can exceed the levels proposed for drinking water.