4.8 Article

B-Cation Order Control of Magnetism in the 1322 Perovskite CaCu3Fe2Nb2O12

期刊

CHEMISTRY OF MATERIALS
卷 26, 期 16, 页码 4832-4837

出版社

AMER CHEMICAL SOC
DOI: 10.1021/cm502064b

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资金

  1. Ministry of Economy and Competitiveness (MINECO) [PIB2010JP-00181]
  2. Ministry of Education, Culture, Sports, Science and Technology (MEXT) of Japan
  3. JST CREST program
  4. EPSRC
  5. STFC
  6. Royal Society, U.K.
  7. Spanish MINECO [MAT2010-19837-C06-03]
  8. [19GS0207]
  9. [22740227]

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Cation ordering in the 1322 perovskite CaCu3Fe2Nb2O12 has been investigated by synchrotron X-ray diffraction structure analysis, high-resolution electron microscopy, and magnetic measurements. All of the samples have full 1:3 ordering of Ca and Cu cations at the perovskite A-sites, but the Fe and Nb cations at the B sites show different degrees of ordering depending on the synthesis conditions. A slow-cooled sample has almost complete rock-salt-type 1:1 cation ordering at the B sites, but a rapidly cooled sample has no long-range B-cation arrangement. The ordered compound shows a large saturated magnetization (5.7 mu B/formula unit (fu)) below 170 K due to the ferrimagnetism of the A'-site Cu2+ and B-site Fe3+ spins, whereas the B-site disordered form has a small magnetization (<1 mu B/fu at 5 K). The degree of B-site cation order thus controls the magnetic behavior of 1322 CaCu3Fe2Nb2O12 perovskites.

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