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Deformations of the α‐Fe 2 O 3 rhombohedral lattice across the Néel temperature
Author(s) -
Fabrykiewicz P.,
Stękiel M.,
Sosnowska I.,
Przeniosło R.
Publication year - 2017
Publication title -
acta crystallographica section b
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.604
H-Index - 33
ISSN - 2052-5206
DOI - 10.1107/s2052520616017935
Subject(s) - monoclinic crystal system , trigonal crystal system , materials science , anisotropy , lattice (music) , crystallography , condensed matter physics , diffraction , hexagonal crystal system , synchrotron radiation , hexagonal lattice , x ray crystallography , powder diffraction , crystal structure , physics , optics , chemistry , antiferromagnetism , acoustics
High‐resolution synchrotron radiation powder diffraction patterns of α‐Fe 2 O 3 measured between room temperature and 1100 K, i.e. above the Néel temperature T N = 950 K, have been analyzed. The integral breadths of the Bragg peaks show a hkl ‐dependent anisotropy, both below and above T N . This anisotropy can be quantitatively described by using a statistical peak‐broadening model [Stephens (1999). J. Appl. Cryst. 32 , 281]. Model calculations show that the rhombohedral α‐Fe 2 O 3 lattice is deformed and the deformation leads to a monoclinic lattice with the unique monoclinic axis along the hexagonal [110] direction both below and above T N . The monoclinic symmetry of bulk α‐Fe 2 O 3 is compatible with α‐Fe 2 O 3 nanowire growth along the [110] direction reported in Fu et al. [ Chem. Phys. Lett. (2001), 350 , 491].