Fluorine insertion into the Ruddlesden-Popper phase La2BaFe2O7: the structure and magnetic properties of La2BaFe2O5F4
Fluorination of the n = 2 Ruddlesden-Popper phase La 2 BaFe 2 O 7 occurs at ∼300 °C in flowing 10% F 2 in N 2 to form La 2 BaFe 2 O 5 F 4 . This oxide fluoride contains 2F − ions in interstitial sites within the rocksalt regions and 2F − ions that have substituted for O 2− ions in apical sites withi...
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Veröffentlicht in: | Dalton transactions : an international journal of inorganic chemistry 2014-02, Vol.43 (5), p.238-243 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | Fluorination of the
n
= 2 Ruddlesden-Popper phase La
2
BaFe
2
O
7
occurs at ∼300 °C in flowing 10% F
2
in N
2
to form La
2
BaFe
2
O
5
F
4
. This oxide fluoride contains 2F
−
ions in interstitial sites within the rocksalt regions and 2F
−
ions that have substituted for O
2−
ions in apical sites within the rocksalt layers. The fluorination results in an expansion along
c
of 7.6% to yield a tetragonal unit cell of dimensions
a
= 3.96237(7) Å,
c
= 22.3972(5) Å. The structure and magnetic properties have been examined by Mössbauer spectroscopy, neutron powder diffraction and magnetic susceptibility measurements. La
2
BaFe
2
O
5
F
4
becomes antiferromagnetically ordered at temperatures below ∼500 K, and the magnetic order shows a striking resemblance to that observed in La
2
BaFe
2
O
7
. The magnetic moments on Fe
3+
are perpendicular to [001] and aligned along ±{100} directions above 300 K, but at temperatures below 200 K, they rotate by 45° to lie along ±{110}. Mössbauer spectroscopy suggests the presence of Fe
3+
within the primary phase, but also indicates that fluorination results in some particle fragmentation to form a paramagnetic component of the fluorinated material.
Fluorination of La
2
BaFe
2
O
7
occurs to form La
2
BaFe
2
O
5
F
4
containing both interstitial and substitutional fluoride ions. The Fe
3+
ions are not oxidised. |
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ISSN: | 1477-9226 1477-9234 |
DOI: | 10.1039/c3dt52769g |