Oriented overgrowth of acicular maghemite crystals on quartz
Keyword(s):
X Ray
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AbstractMaghemite with acicular morphology occurs as an oriented growth on fresh quartz surfaces in the magnetic sandy fraction of the B horizon of a Typic Rhodoxeralf from southern Portugal. The maghemite was characterized by Mössbauer spectroscopy, X-ray diffraction and electron microscopy (scanning and transmission), and on the basis of a structural similarity between quartz and maghemite, a mechanism has been proposed for the formation of the oriented overgrowth. Correlation with an interpretative chemical model is discussed, assuming active sites over quartz surfaces. Infrared absorption data agree with the proposed models.
2013 ◽
Vol 743-744
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pp. 83-87
1974 ◽
Vol 32
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pp. 506-507
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Keyword(s):
1982 ◽
Vol 40
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pp. 722-723
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1984 ◽
Vol 42
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pp. 288-289
1992 ◽
Vol 50
(2)
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pp. 1322-1323