Structural Distortion and Chemical Bonding in TlFeO3: Comparison with AFeO3 (A=Rare Earth)
✍ Scribed by Seung-Joo Kim; Gérard Demazeau; Igor Presniakov; Jin-Ho Choy
- Book ID
- 102611224
- Publisher
- Elsevier Science
- Year
- 2001
- Tongue
- English
- Weight
- 444 KB
- Volume
- 161
- Category
- Article
- ISSN
- 0022-4596
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✦ Synopsis
The crystal structure and the magnetic properties for thallium orthoferrite, TlFeO 3 , were characterized and compared with those of rare earth orthoferrites, AFeO 3 (A ؍ rare earth). TlFeO 3 has a GdFeO 3 -type perovskite structure (a ؍ 5.3172(2) A s , b ؍ 5.4465(2) A s , and c ؍ 7.7927(3) A s ; space group, Pbnm). Its cell parameters and unit-cell volume considerably deviate from a trend observed in the rare earth orthoferrites, which are attributed to a speci5c coordination of Tl 3؉ ion. According to magnetization measurements, TlFeO 3 shows an antiferromagnetic behavior accompanied with weak ferromagnetism. The magnetic ordering temperature, T N (560 K), for TlFeO 3 is lower than that for any other orthoferrite while the Fe+O+Fe superexchange angle (144.03) in TlFeO 3 is comparable to that in ErFeO 3 . The MoK ssbauer spectrum reveals a single Fe 3 ؉ quadrupole doublet with an isomer shift ؍ 0.18 ؎ 0.02 mm/s and a quadrupole splitting value ؍ 0.47 ؎ 0.02 mm/s at 623 K (> T N ), whereas it shows a magnetic hyper5ne sextet with ؍ 0.47 mm/s and a hyper5ne 5eld H hf (Fe 3 ؉ ) ؍ 535 kOe at 80 K (< T N ). The magnetism and the MoK ssbauer results underline a signi5cant competing e4ect of the Tl+O bond with the covalency of the Fe+O one. Despite the anomalous character of TlFeO 3 in structure and magnetism, it is found that the T N values for all orthoferrites, including TlFeO 3 , are strongly correlated with their crystallographic axial ratio, c/(2a. Through this type of analysis, the electronic e4ects of A cation on structural distortion and magnetic behavior in perovskite are discussed.
📜 SIMILAR VOLUMES
An unknown oxygen atom fractional co-ordinate characteristic of the pyrochlore structure type has been determined for selected rare earth zirconate and titanate pyrochlores via a systematic row wide-angle CBED technique and shown to vary systematically with rare earth ion size. In the case of the ti