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- W374449944 abstract "Structures with Fe^(3+) shared through oxo- or hydroxyl-groups have antiferromagneticinteractions. Such interactions result in enhanced intensity of the Fe^(3+) optical absorption bandswhich in some systems can be as great as a factor of 100 compared to isolated, octahedrallycoordinated Fe^(3+) ions. A comparison is presented between the intensity of the lowest energy crystal-fieldband of Fe^(3+) minerals and their magnetic moments which demonstrates the dependence ofoptical absorption intensity and antiferromagnetic interactions in the host phase. Hematite, which isusually responsible for the red color of geological materials, owes its intense color to these magneticinteractions." @default.
- W374449944 created "2016-06-24" @default.
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- W374449944 date "1996-01-01" @default.
- W374449944 modified "2023-09-24" @default.
- W374449944 title "Why hematite is red: Correlation of optical absorption intensities and magnetic moments of Fe^(3+) minerals" @default.
- W374449944 hasPublicationYear "1996" @default.
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