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Paleoclimatology (thesaurus)

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chemical process > deuterium excess

Terme préférentiel

deuterium excess  

Définition

  • The δ18O and δD measurements allow us to calculate the deuterium excess, which is defined as follows: d = δD−8*δ18O (Dansgaard, 1964). This second order parameter is mainly dependent on the climatic conditions in the precipitation source regions (Merlivat and Jouzel, 1979). (Adapted from: B. Stenni et al. (2007), The Holocene, 17(7), 1033-1039.)

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http://data.loterre.fr/ark:/67375/QX8-19NHGLXM-7

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