Plot of dD vs. d 18 O values showing the meteoric water line

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David GÓMEZ-GRAS, Secretary of Department

Applicability of d-excess and 17O-excess as groundwater tracers for determination of recharge area

Applicability of d-excess and 17O-excess as groundwater tracers for determination of recharge area

Médard THIRY, Senior Researcher, Ph D (habilitation)

The δD vs. δ 18 O values of precipitation in the upper and middle

a) δ 18 O vs. δD diagram for the studied waters. Global Meteoric Water

Plot of δ¹⁸O versus δD and LMWLs in comparison with the GMWL. Circles

Hydrochemical and isotopic baselines for understanding hydrological processes across Macquarie Island

Plot of δD vs. δ 18 O for precipitation samples. LMWL represents the

δD vs. δ 18 O plots of water samples. The solid line is Meteoric Water

David GÓMEZ-GRAS, Secretary of Department

David GÓMEZ-GRAS, Secretary of Department

Isotope Hydrology

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