A study of the Kalamos Springs in Greece with environmental isotopes

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Abstract
Variations in the stable isotopic composition of water were used to define the area of recharge to the Kalamos springs, issuing brackish water near the coast. The two possible areas of recharge differed in elevation, so that their stable isotope indices were different owing to the altitude effect, whereby the stable isotopic composition of precipitation contains less deuterium and 18O with an increase of elevation. The results of the study showed that the area of recharge is located in the Parnis system at elevations greater than 570 m.

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