Physics
Scientific paper
Dec 1987
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987sci...238.1702g&link_type=abstract
Science (ISSN 0036-8075), vol. 238, Dec. 18, 1987, p. 1702-1704.
Physics
20
Abundance, Deuterium, Moisture Content, Venus (Planet), Venus, Deuterium, Hydrogen, Water, Abundance, Isotopic Ratios, History, Evolution, Escape, Theoretical Studies, Hypotheses, Source
Scientific paper
The ratio of deuterium to hydrogen on Venus has been accepted as proof of a wetter, more Earth-like past on that planet. However, the present-day water abundance and the nonthermal hydrogen escape flux on Venus imply that hydrogen is in a steady state and that a hydrogen source, most likely cometary infall, is present. An alternative interpretation of the D/H ratio is offered, in which the measured value is consistent with a steady-state evolution over the age of the solar system. No past water excess is required to explain the isotopic data.
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