Definition
Hydrogen (symbol, H; atomic mass, 1.00794) has three isotopes. Two are stable in the environment and are denoted as \( _1^1\mathrm{H} \) (protium) and \( _1^2\mathrm{H} \) (deuterium or D). The third isotope, \( _1^3\mathrm{H} \) (tritium or T), is unstable and decays to 3He with a half-life of 12.32±0.02 years. Being hydrogen one of the water-forming elements, the ratio of the stable isotopes D/H has been used for identifying the origin of water within the Solar system. The D/H ratio measured in carbonaceous chondrites and Antarctic micrometeorites (143–170 × 10−6; Robert 2001; Engrand et al. 1999) is closer to the value of the present-day ocean (155.7 × 10−6) than that measured in long-period and Jupiter family comets (298–530 × 10−6; e.g., Bockelée-Morvan et al. 1998; Altwegg et al. 2015).
References
Altwegg K et al (2015) 67P/Churyumov-Gerasimenko, a Jupiter family comet with a high D/H ratio. Science 347:1261952
Bockelée-Morvan D et al (1998) Deuterated water in Comet C/1996 B2 (Hyakutake) and its implications for the origin of Comets. Icarus 133:147–162
Engrand C, Deloule E, Robert F, Maurette M, Kurat G (1999) Extraterrestrial water in micrometeorites and cosmic spherules from Antarctica: an ion microprobe study. Meteorit Planet Sci 34:773–786
Robert F (2001) L’origine de l’eau dans le Système Solaire telle qu’elle est enregistrée par son rapport isotopique D/H. In: Gargaud M, Despois D, Parisot JP (eds) L’environnement de la Terre primitive. Presses Universitaires de Bordeaux
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Pinti, D.L. (2022). Hydrogen Isotopes. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_753-5
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DOI: https://doi.org/10.1007/978-3-642-27833-4_753-5
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Hydrogen Isotopes- Published:
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DOI: https://doi.org/10.1007/978-3-642-27833-4_753-5
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Hydrogen Isotopes- Published:
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DOI: https://doi.org/10.1007/978-3-642-27833-4_753-4