The D/H ratio and the evolution of water in the terrestrial planets

Mathematics – Logic

Scientific paper

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Biological Evolution, Deuterium, Ground Water, Hydrogen Atoms, Terrestrial Planets, Earth Surface, Liquid Phases, Planetary Atmospheres

Scientific paper

Unique models have yet to be devised for water evolution in the terrestrial planets, despite recent evidence of a Martian D/H ratio which is higher than terrestrial. One of the major uncertainties is the role of external impacts, especially those of comets, as additional sources of water; this places a high value on future observations' accurate determination of such isotopic ratios as O-17/O-16 and O-18/O-16 in both CO2 and water. In the case of Mars, it would be very useful to measure the D/H ratio in the nonexchanging polar ice.

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