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Published in 2017 at "Chemical Geology"
DOI: 10.1016/j.chemgeo.2017.08.014
Abstract: Abstract Geochemical and isotopic tracers (δ18O, δ2H, 87Sr/86Sr and δ13CTDIC) were used to constrain origins and chemical evolution of groundwater in a Mediterranean karst system. The Lez spring is the main perennial outlet of this…
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Keywords:
groundwater;
compartment;
hydrodynamics;
lez spring ... See more keywords