Iron disilicide (FeSi2) is an intermetallic compound, a silicide of iron that occurs in nature as the rare mineral linzhiite. At room temperature it forms orthorhombic crystals (β phase), which convert into a tetragonal α phase upon heating to 970 °C.[3]

See also

References

  1. ^ a b c Haynes, William M., ed. (2016). CRC Handbook of Chemistry and Physics (97th ed.). CRC Press. p. 4.67. ISBN 9781498754293.
  2. ^ Rizzi, A.; Rösen, B. N. E.; Freundt, D.; Dieker, Ch.; Lüth, H.; Gerthsen, D. (1995). "Heteroepitaxy of β-FeSi2 on Si by gas-source MBE". Physical Review B. 51 (24): 17780–17794. Bibcode:1995PhRvB..5117780R. doi:10.1103/PhysRevB.51.17780. PMID 9978811.
  3. ^ a b Dusausoy, Y.; Protas, J.; Wandji, R.; Roques, B. (1971). "Structure cristalline du disiliciure de fer, FeSi2-β". Acta Crystallographica Section B: Structural Crystallography and Crystal Chemistry. 27 (6): 1209–1218. doi:10.1107/S0567740871003765.
Allikas: https://en.wikipedia.org/wiki/Iron_disilicide
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