Barium isotope fractionation during the experimental transformation of aragonite to witherite and of gypsum to barite, and the effect of ion (de)solvation-Reference-Cited by-同舟云学术

Barium isotope fractionation during the experimental transformation of aragonite to witherite and of gypsum to barite, and the effect of ion (de)solvation

Published:2018-02-05 Issue:3 Volume:54 Page:324-335
ISSN:1025-6016
Container-title:Isotopes in Environmental and Health Studies
language:en
Short-container-title:Isotopes in Environmental and Health Studies

Author:

Böttcher Michael E.¹,Neubert Nadja¹²,von Allmen Katja³,Samankassou Elias³,Nägler Thomas F.²

Affiliation:

1. Geochemistry & Stable Isotope Biogeochemistry Group, Department Marine Geology, Leibniz Institute for Baltic Sea Research, Warnemünde, Germany

2. Institute of Geological Sciences, University of Bern, Bern, Switzerland

3. Section of Earth and Environmental Sciences, University of Geneva, Geneva, Switzerland

Funder

Swiss National Science Foundation

University of Fribourg

Publisher

Informa UK Limited

Subject

Inorganic Chemistry,General Environmental Science,Environmental Chemistry

Link

https://www.tandfonline.com/doi/pdf/10.1080/10256016.2018.1430692

Reference56 articles.

1. Johnson CA, Beard BL, Albarède F, editors. Geochemistry of non-traditional stable isotopes. Chantilly (VA): Mineralogical Society of America; 2004. p. 454. (Reviews in Mineralogy & Geochemistry; 55).

2. Stable Isotope Geochemistry

3. Non-Traditional Stable Isotopes

4. Barium isotope fractionation in the global barium cycle: First evidence from barium minerals and precipitation experiments

5. Barium isotope fractionation during experimental formation of the double carbonate BaMn[CO3]2at ambient temperature

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