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Crystal chemistry of the MgAl (sub 2) O (sub 4) -MgMn (sub 2) O (sub 4) -MnMn (sub 2) O (sub 4) system; analysis of structural distortion in spinel- and hausmannite-type structures

Ferdinando Bosi, Ulf Halenius and Henrik Skogby
Crystal chemistry of the MgAl (sub 2) O (sub 4) -MgMn (sub 2) O (sub 4) -MnMn (sub 2) O (sub 4) system; analysis of structural distortion in spinel- and hausmannite-type structures
American Mineralogist (April 2010) 95 (4): 602-607

Abstract

Single crystals of spinel and hausmannite having seven different compositions in the MgAl (sub 2) O (sub 4) -MgMn (sub 2) O (sub 4) -MnMn (sub 2) O (sub 4) system were synthesized and structurally and chemically characterized by X-ray diffraction and electron microprobe techniques. As predicted, tetrahedral and octahedral bond lengths increase with increasing substitutions of Mn (super 2+) for Mg and Mn (super 3+) for Al, respectively. A transition from cubic to tetragonal symmetry occurs at a critical concentration of Mn (super 3+) >1.4 atoms per formula unit as a result of the Jahn-Teller distortion around octahedrally coordinated Mn (super 3+) . The present data in conjunction with data from the literature provide a basis for quantitative analyses of the cation polyhedral-distortion parameters and their variations in spinel- and hausmannite-type structures (Fd3m and I4 (sub 1) /amd, respectively). In contrast to the linear correlation between <lambda (sub M) > (octahedral quadratic elongation) and sigma (super 2) (sub M) (octahedral bond-angle variance) observed for many silicates and isomorphic structures, these two distortion parameters are not correlated in multiple oxides with spinel- and hausmannite-type structures. By using a model of multiple linear regression, it is demonstrated that <lambda (sub M) > varies as a function of both sigma (super 2) (sub M) and Delta (sub M) (octahedral bond-length distortion). The degree of octahedral distortion is significant in the spinel structures and is in fact comparable with that calculated for the hausmannite-type structures. The degree of octahedral distortion is related to steric effects in both spinel- and hausmannite-type structures, whereas the electronic effects caused by Mn (super 3+) account for the transition from cubic to tetragonal symmetry.


ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 95
Serial Issue: 4
Title: Crystal chemistry of the MgAl (sub 2) O (sub 4) -MgMn (sub 2) O (sub 4) -MnMn (sub 2) O (sub 4) system; analysis of structural distortion in spinel- and hausmannite-type structures
Affiliation: Sapienza Universita di Roma, Dipartimento di Scienze della Terra, Rome, Italy
Pages: 602-607
Published: 201004
Text Language: English
Publisher: Mineralogical Society of America, Washington, DC, United States
References: 22
Accession Number: 2010-039438
Categories: Mineralogy of non-silicates
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 4 tables
Secondary Affiliation: Swedish Museum of Natural History, SWE, Sweden
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, copyright, Mineralogical Society of America. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 201022

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