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The relationship between deuterium and oxygen-18 concentrations in natural meteoric waters from many parts of the world has been determined with a mass spectrometer. The isotopic enrichments, relative to ocean water, display a linear correlation over the entire range for waters which have not undergone excessive evaporation.
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Harmon Craig (Fri,) studied this question.
synapsesocial.com/papers/69d8d25533ca018b39ae4267 — DOI: https://doi.org/10.1126/science.133.3465.1702
Harmon Craig
Scripps Institution of Oceanography
Science
University of California, San Diego
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