Non‐Equilibrium Fractionation Factors for D/H and (18)O/(16)O During Oceanic Evaporation in the North‐West Atlantic Region

Ocean isotopic evaporation models, such as the Craig‐Gordon model, rely on the description of nonequilibrium fractionation factors that are, in general, poorly constrained. To date, only a few gradient‐diffusion type measurements have been performed in ocean settings to test the validity of the comm...

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Detalles Bibliográficos
Autores principales: Zannoni, D., Steen‐Larsen, H. C., Peters, A. J., Wahl, S., Sodemann, H., Sveinbjörnsdóttir, A. E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9786641/
https://www.ncbi.nlm.nih.gov/pubmed/36582456
http://dx.doi.org/10.1029/2022JD037076

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9786641/
https://www.ncbi.nlm.nih.gov/pubmed/36582456
http://dx.doi.org/10.1029/2022JD037076

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