Study of Iron-Bearing Dolomite Dissolution at Various Temperatures: Evidence for the Formation of Secondary Nanocrystalline Iron-Rich Phases on the Dolomite Surface-Reference-Cited by-同舟云学术

Study of Iron-Bearing Dolomite Dissolution at Various Temperatures: Evidence for the Formation of Secondary Nanocrystalline Iron-Rich Phases on the Dolomite Surface

Published:2017-08-16 Issue:7 Volume:1 Page:442-454
ISSN:2472-3452
Container-title:ACS Earth and Space Chemistry
language:en
Short-container-title:ACS Earth Space Chem.

Author:

Debure Mathieu¹^ORCID,Andreazza Pascal²,Canizarès Aurélien³,Grangeon Sylvain¹,Lerouge Catherine¹,Mack Paul⁴,Madé Benoît⁵,Simon Patrick³,Veron Emmanuel³,Warmont Fabienne²,Vayer Marylène²

Affiliation:

1. BRGM − French Geological Survey, Water, Environment and Ecotechnologies Division, Storage and Deep Geological Settings Unit 3 Avenue Claude Guillemin, BP 36009, 45060 Orléans Cedex 2, France

2. ICMN - UMR 7374 CNRS - Université d’Orléans, 1b rue de la Férollerie, CS 40059, 45071 Orléans cedex 2, France

3. CEMHTI, UPR 3079 CNRS - Université d’Orléans, CS90055, 45071 Orléans, France

4. Thermo Fisher Scientific, Imberhorne Lane, East Grinstead, West Sussex RH19 1UB, United Kingdom

5. Andra, 1−7 rue Jean Monnet, 92298 Châtenay-Malabry, France

Funder

Bureau de Recherches G?ologiques et Mini?res

Agence Nationale pour la Gestion des D?chets Radioactifs

Publisher

American Chemical Society (ACS)

Subject

Space and Planetary Science,Atmospheric Science,Geochemistry and Petrology

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