Air Masses Origin and Isotopic Tracers: A Study Case of the Oceanic and Mediterranean Rainfall Southwest of France
Aquifers recharge mainly by local rainfall, which depend on the air mass humidity and orographic lifting, causing rain. The stable isotopes of the water molecule, i.e., oxygen-18 and deuterium, are useful tracers to determine the water source origin. Moreover, the calculation of the deuterium excess...
Main Authors: | , , |
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Format: | Article |
Language: | English |
Published: |
MDPI AG
2013-05-01
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Series: | Water |
Subjects: | |
Online Access: | http://www.mdpi.com/2073-4441/5/2/617 |