COMMENT ON "THE ROLE OF H3O+ IN THE CRYSTAL STRUCTURE OF ILLITE" BY F. NIETO, M. MELINI, AND I. ABAD

Vidal, Olivier and Dubacq, Benoit and Lanari, Pierre (2010) COMMENT ON "THE ROLE OF H3O+ IN THE CRYSTAL STRUCTURE OF ILLITE" BY F. NIETO, M. MELINI, AND I. ABAD. Clays and Clay Minerals, 58 (5). pp. 717-720. DOI 10.1346/CCMN.2010.0580510

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Abstract

The arguments of Nieto et al. (2010) in favor of the incorporation of H3O+ rather than H2O in interlayer positions of illite are disputable. Stoichiometric arguments suggest that the excess water in the Silver Hill illite is in the form of H2O. Moreover, recent thermodynamic models assuming the incorporation of interlayer H2O in illite provide reasonable estimates of temperature and water content using the AEM/TEM analyses of Nieto et al. (2010).

Item Type: Article
Uncontrolled Keywords: 2010AREP; IA62;
Subjects: 01 - Climate Change and Earth-Ocean Atmosphere Systems
Divisions: 01 - Climate Change and Earth-Ocean Atmosphere Systems
Journal or Publication Title: Clays and Clay Minerals
Volume: 58
Page Range: pp. 717-720
Identification Number: 10.1346/CCMN.2010.0580510
Depositing User: Sarah Humbert
Date Deposited: 04 Jun 2011 14:25
Last Modified: 23 Jul 2013 10:02
URI: http://eprints.esc.cam.ac.uk/id/eprint/2073

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