Low-temperature magnetic behavior of ferrihydrite

Two samples of six‐line ferrihydrite (5Fe2O3·9H2O) were precipitated from an Fe(III) solution. The purity of the samples was verified by X‐ray diffraction. Scanning electron microscope pictures indicate that the grains have good crystallinity and variable grain size (

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Bibliographic Details
Published in:Journal of Geophysical Research 2000-04, Vol.105 (B4), p.8297-8303
Main Authors: Zergenyi, R. S., Hirt, A. M., Zimmermann, S., Dobson, J. P., Lowrie, W.
Format: Article
Language:English
Subjects:
Earth sciences
Earth, ocean, space
Exact sciences and technology
Mineralogy
Non silicates
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Description
Summary:Two samples of six‐line ferrihydrite (5Fe2O3·9H2O) were precipitated from an Fe(III) solution. The purity of the samples was verified by X‐ray diffraction. Scanning electron microscope pictures indicate that the grains have good crystallinity and variable grain size (
ISSN:0148-0227
2156-2202
DOI:10.1029/1999JB900315