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the samples, dolomite dissolution occurs in an open system with PCO2 between 10 ‐2 and 10 ‐3 bar. The study of trace elements distribution shows that during dolomite dissolution alkaline metals, alkaline earth elements larger than Ca and some transition metals are relatively enriched in the solutions while the solutions result to be depleted in Fe, Al, Y and REE.

Water-rock interactions and trace elements distribution in dolomite aquifers: The Sassolungo and Sella systems (Northern Italy)