Spectroscopic and magnetic studies of ferric iron hydroxy sulfates: Intensification of color in ferric iron clusters bridged by a single hydroxide ion
- Creators
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Rossman, George R.
Abstract
Optical and infrared spectroscopic data and magnetic susceptibility data are reported for the ferric hydroxy-sulfate minerals magnesiocopiapite and botryogen and the related mineral coquimbite. The physical properties of intensity of color, pleochroism, and magnetic susceptibility associated with the hydroxobridged Fe^(3+) dimer of magnesiocopiapite and with the hydroxobridged Fe^(3+) infinite chain of botryogen are compared to those of isolated Fe^(3+). The hydroxobridged minerals show strong pleochroism with intensity enhancement of the spin-forbidden ligand field absorption bands occurring when the electric vector of the incident light is oriented in the direction of the Fe-OH-Fe axis. The intensity enhancement and pleochroism are associated with antiferromagnetic exchange coupling of the Fe^(3+) ions.
Additional Information
© 1975 Mineralogical Society of America. Manuscript received January 20, 1975; accepted for publication, February 10, 1975. Contribution No. 2518, Division of Geological and Planetary Sciences, California Institute of Technology.Additional details
- Eprint ID
- 38174
- Resolver ID
- CaltechAUTHORS:20130430-082926010
- Created
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2013-04-30Created from EPrint's datestamp field
- Updated
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2019-11-26Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)
- Other Numbering System Name
- Caltech Division of Geological and Planetary Sciences
- Other Numbering System Identifier
- 2518