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Fractionnement isotopique lors des changements d’état solide-vapeur et liquide-vapeur de l’eau à des températures inférieures à 0°C

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Merlivat, L., Nief, G.·1967·Tellus A: Dynamic Meteorology and Oceanography

Abstract

Measurements of the hydrogen isotopic composition of water in atmospheric precipitations make possible the study of their formation and evolution, since deuterium is a natural tracer for the water molecule.In a hydrologic cycle, each change of state is accompanied by an isotopic fractionation expressed in terms of a factor ?, which is a function of temperature. This fractionation is due to differences in the physical properties of the molecules H2O and HDO. In the work described in this paper we have measured α between −40°C and 0°C for the phase equilibrium ice-water vapor and between −15°C and 0°C for the equilibrium liquid-water vapor.The values obtained may be expressed in the relationslog ?solide-vapeur= αsolide-vapeur = −4.10 · 10−2 + 7.074/T2log ?liquide-vapeur= αliquide-vapeur = −4.34 · 10−2 + 6.520/T2.

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Metadata

Authors
Merlivat, L., & Nief, G.
Venue
Tellus A: Dynamic Meteorology and Oceanography
Published
1967-01-01
Volume
19
Issue
1
Pages
122
ISSN
  • 0280-6495 (ISSN-L)
  • 1600-0870
OpenAlex
W1979180024
Cited by
205
References
0
FWCI
6.95
Type
journal article
Language
fr
Open access
bronze

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CoChat. (2026). Citation check: Fractionnement isotopique lors des changements d’état solide-vapeur et liquide-vapeur de l’eau à des températures inférieures à 0°C. https://app.cochat.ai/papers/10.3402/tellusa.v19i1.9756
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Merlivat, L., & Nief, G. (1967). Fractionnement isotopique lors des changements d’état solide-vapeur et liquide-vapeur de l’eau à des températures inférieures à 0°C. Tellus A: Dynamic Meteorology and Oceanography. https://doi.org/10.3402/tellusa.v19i1.9756

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