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MINERALS AND SYNTHETIC COMPOUNDS, AmXn, IN WHICH X
ATOMS ARE |
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CLOSE PACKED AND A ATOMS OCCUPY OCTAHEDRAL INTERSTICES |
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ReO3 |
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click here to see a key to this data bar
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octa |
25% |
fcc |
chain |
6
vertices |
A-
6c, X- 2c/fcc |
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structure |
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The ReO3
structure is identical to perovskite except that there is only one species |
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of FCC packed X atoms. Also 1/4 of these
anions are eliminated instead of being |
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substituted for. This leaves large
unoccupied cuboctahedral shaped voids in the |
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structure with eight AX6 groups
coordinated around each. As with perovskite 25% of |
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the octahedral voids are occupied and the
occupied AX6 groups form vertex linked |
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chains parallel to the
[100] axis. |
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Ex. ReO3 ( Re - A , O - X ) |
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Crystal lattice |
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Modeled the same as
perovskite except that triangles are removed from the |
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regions of the lattice where the cuboctahedral
voids are located (in the centers of |
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the eight AX6 groups coordinated
around them). |
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Polyhedral framework |
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linking surfaces |
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Figure 103 - ReO3
polyhedral |
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framework model |
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(
64 T, 6 S, 96 pinges ) |
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6
vertices |
click image to enlarge |
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The polyhedral
framework model is similar to perovskite except that squares
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are used to brace the octahedra to indicate
there is a cuboctahedral void in the |
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center. |
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Isostructural minerals/compounds |
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MoF3, NbF3, TaF3,
WO3 (high temperature) |
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Page
66 - Structure matters - ReO3 |
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