Definition
Hydrogen (symbol, H; atomic mass, 1.00794) has three isotopes. Two are stable in natural environments and are denoted as 11 H and 21 H (deuterium or D). The third isotope 31 H (tritium or T) is unstable and decays to 3He with a half-life of 12.32 years. Being hydrogen one of the water-forming elements, its isotopic ratio D/H has been used for identifying the origin of water within the Solar System. Particularly, the chondritic D/H ratio measured in meteorites and Antarctic micrometeorites (143–170 × 10−6) is closer to the value of the bulk Earth (149–153 × 10−6) and the present-day ocean (155.7 × 10−6) than the comets (298–324 × 10−6). This is the isotopic evidence often used for claiming that water on Earth has been delivered by chondritic planetesimals rather than comets.
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© 2014 Springer-Verlag Berlin Heidelberg
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Pinti, D.L. (2014). Hydrogen Isotopes. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_753-4
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DOI: https://doi.org/10.1007/978-3-642-27833-4_753-4
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Publisher Name: Springer, Berlin, Heidelberg
Online ISBN: 978-3-642-27833-4
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Latest
Hydrogen Isotopes- Published:
- 07 December 2021
DOI: https://doi.org/10.1007/978-3-642-27833-4_753-5
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Original
Hydrogen Isotopes- Published:
- 15 April 2015
DOI: https://doi.org/10.1007/978-3-642-27833-4_753-4