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2005/10/28 | 磁赤铁矿[Maghemite]
类别(℃〖化学〗)
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发表于 19:54
The
anhydrous iron oxide
Fe
2
O
3
which has a defect spinel structure with a hematite stoichiometry. It also exists in the
Fe
2
O
3
polymorph. Maghemite has a cation vacancy, so its structure is more accurately written as Fe
3
(Fe
5
-O
12
. It is highly ferromagnetic, and does not lose its magnetism easily upon contact. However, it is weak enough to be fairly easily realigned. It is the coating used on floppy disks and cassettes. It forms when iron minerals rust.
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