Variabilité spatio-temporelle de la composition isotopique de l'eau (18O, 2H) dans le continuum sol-plante-atmosphère 2. Approche en conditions naturelles-Reference-Cited by-同舟云学术

Variabilité spatio-temporelle de la composition isotopique de l'eau (18O, 2H) dans le continuum sol-plante-atmosphère 2. Approche en conditions naturelles

Published:1994-08 Issue:3-4 Volume:115 Page:317-333
ISSN:0009-2541
Container-title:Chemical Geology
language:fr
Short-container-title:Chemical Geology

Author:

Bariac T,Gonzalez-Dunia J,Katerji N,Béthenod O,Bertolini J.M,Mariotti A

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference44 articles.

1. The relationship between deuterium and oxygen-18 delta values in leaves water;Allison;Chem. Geol. (Isot. Geosci. Sect.),1985

2. La plante comme système fractionnant (18O) dans le transfert de l'eau à l'interface sol-atmosphère;Bariac,1980

3. Les isotopes stables (18O, 2H) de l'eau dans le continuum sol-plante-atmosphère: conséquence pour la vapeur d'eau atmosphérique;Bariac,1988

4. A routine method for 18O analysis of water vapor;Bariac;Int. J. Appl. Radiat. Isot.,1982

5. Évolution de la composition isotopique de l'eau (18O) dans le continuum sol-plante-atmosphère (exemple d'une parcelle cultivée en blé, Versailles, France, juin 1984);Bariac;Catena,1987

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