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MINERALS AND SYNTHETIC COMPOUNDS, AmXn, IN WHICH X
ATOMS ARE |
CLOSE PACKED AND A ATOMS OCCUPY TETRAHEDRAL INTERSTICES |
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Zincblende |
click here to see a key to this data bar
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tetra |
50% |
fcc |
3-d |
4
vertices |
A-
4c, X- 4c/fcc |
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structure |
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The zincblende
structure has A atoms occupying fifty percent of the tetrahedral |
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interstices in each successive layer of
FCC
packed X atoms. This structure is also |
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called sphalerite. |
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Ex. ZnS ( zinc sulfide, zincblende ) -
low temperature polymorph ( Zn - A , S - X ) |
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Crystal lattice |
In the FCC lattice
model the AX4 groups of sulfur atoms that are tetrahedrally |
coordinated with zinc atoms residing in their
interstitial voids are colored differently |
than the tetrahedral or octahedral clusters of
sulfur atoms whose voids are |
unoccupied
(blue). |
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Figure 60 -
Zincblende lattice |
click image to enlarge |
structure |
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The lattice model shows
that the AX4 coordination groups of atoms are joined |
by their vertices only due to the fact
that only fifty percent of the tetrahedral voids |
of each layer are occupied. |
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Polyhedral framework |
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linking surfaces |
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Figure 61 -
Zincblende polyhedral |
framework model |
( 50 T, 60 pinges) |
4
vertices |
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The polyhedral
framework model clearly shows that 50% of the tetrahedrally |
coordinated groups of X atoms are occupied with
A atoms. The structure is built up |
by linking all the vertices of these tetrahedra
together. By convention only the |
occupied tetrahedra are modeled to highlight the
geometry and symmetry of these |
AX4 coordinated groups of cations and anions. |
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Isostructural minerals/compounds |
AgI,
AlAs, AlP, AlSb, BAs, BN, BP, BePo, BeS, BeSe, BeTe, CdPo, CdS, CdSe, CdTe, |
CuBr, CuCl, CuF, CuI,
GaAs, GaP, Cu2Fe2S4, Cu2FeSnS4,
GaSb, HgS, HgSe, HgTe, |
InAs,
InP,
InSb,
MnS, MnSe, SiC, ZnPo, ZnSe, ZnTe |
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Page
43 - Structure matters - Zincblende |
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