Abstract
The results of in situ synchrotron X-ray powder diffraction experiments conducted during the synthesis of iron-deficient Na+/H3O+ and K+/H3O+ jarosites at temperatures in the range 80 to 120 °C are presented. They demonstrate that samples can be prepared in which the iron-site vacancies are ordered. The ordering is accompanied by a lowering of symmetry, from rhombohedral, space group R3̅m, to monoclinic, C2/m. The implications for magnetic properties are discussed.
Keywords: Jarosites; iron-deficient jarosites; monoclinic jarosites; iron-site vacancy ordering in jarosites
Received: 2010-4-28
Accepted: 2010-5-27
Published Online: 2015-4-2
Published in Print: 2010-10-1
© 2015 by Walter de Gruyter Berlin/Boston
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Keywords for this article
Jarosites;
iron-deficient jarosites;
monoclinic jarosites;
iron-site vacancy ordering in jarosites
Articles in the same Issue
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- A new method for quantitative petrography based on image processing of chemical element maps: Part I. Mineral mapping applied to compacted bentonites
- A new method for quantitative petrography based on image processing of chemical element maps: Part II. Semi-quantitative porosity maps superimposed on mineral maps
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- Density and seismic velocities of chromitite body in oceanic mantle peridotite
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