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Vacancy infilling during the crystallization of Fe-deficient hematite: An in situ synchrotron X-ray diffraction study of non-classical crystal growth

  • Si Athena Chen ORCID logo , Peter J. Heaney , Jeffrey E. Post , Peter J. Eng and Joanne E. Stubbs
Published/Copyright: August 31, 2023
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Abstract

The crystallization of hematite from precursor ferrihydrite was studied using time-resolved, angle-dispersive synchrotron X-ray difraction in aqueous solutions at pH 10 and 11 and at temperatures ranging from 80 to 170 °C. Rietveld analyses revealed a non-classical crystallization pathway involving vacancy infilling by Fe as defective hematite nanocrystals evolved. At 90 °C and pH 11, incipient hematite particles exhibited an Fe site occupancy as low as 0.68(2), and after 30 min, Fe occupancy plateaued at 0.84(1), achieving a metastable steady state with a composition corresponding to “hydrohematite.” During crystal growth, unit-cell volume increased with an increase in Fe occupancy. The increase in Fe occupancy in hydrohematite was accomplished by deprotonation, resulting in a shortening of the long Fe-O(H) bonds and decreased distortion of the octahedral sites. Once the occupancy stabilized, the unit-cell volume contracted following further nanoparticle growth. Our study documented various synthetic routes to the formation of “hydrohematite” with an Fe vacancy of 10–20 mol% in the final product.

The structure refined for synthetic hydrohematite at 90 °C and pH 11 closely matched that of natural hydrohematite from Salisbury, Connecticut, with a refined Fe occupancy of 0.83(2). Dry heating this natural hydrohematite generated anhydrous, stoichiometric hematite, again by continuous infilling of vacancies. The transformation initiated at 150 °C and was complete at 700 °C, and it was accompanied by the formation of a minor amorphous phase that served as a reservoir for Fe during the inoculation of the defective crystalline phase.

Funding statement: Funding for this research was provided by National Science Foundation Grant EAR-1552211 and EAR-1925903, the Pennsylvania State University Biogeochemistry dual-title Ph.D. program, and the Hiroshi and Koya Ohmoto Graduate Fellowship of Pennsylvania State University Geosciences Department. Synchrotron XRD was performed at GSECARS (University of Chicago) Beamline 13-BM-C at the APS. GSECARS is supported by NSF EAR-1634415 and DOE GeoSciences DE-FG02-94ER14466. A.P.S. is operated under DOE Contract No. DE-AC02-06CH11357.

Acknowledgments

We thank Nancy Lazarz at GSECARS BM-13 for her invaluable assistance in arranging for data collection at the beamline. We thank three anonymous reviewers and the associate editor who handled this paper for their helpful suggestions and comments.

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Received: 2021-11-05
Accepted: 2022-10-18
Published Online: 2023-08-31
Published in Print: 2023-09-26

© 2023 by Mineralogical Society of America

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