2013
DOI: 10.1016/j.jssc.2012.12.010
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Structural and magnetic investigation of Fe3+ and Mg2+ substitution into the trigonal bipyramidal site of InGaCuO4

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Cited by 7 publications
(4 citation statements)
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“…Thus, we built small models including only the core atoms (i.e., Fe1, S Cys19 , S Cys17 , S1, and S2) in the presence and absence of the OH À and evaluated the total energy values of the models. The analysis revealed that the optimum spin states with the minimum total energies were composed of the high spin states of Fe ions, which is consistent with the previous experimental data [33].…”
Section: Exploration Of Spin Assignmentssupporting
confidence: 90%
“…Thus, we built small models including only the core atoms (i.e., Fe1, S Cys19 , S Cys17 , S1, and S2) in the presence and absence of the OH À and evaluated the total energy values of the models. The analysis revealed that the optimum spin states with the minimum total energies were composed of the high spin states of Fe ions, which is consistent with the previous experimental data [33].…”
Section: Exploration Of Spin Assignmentssupporting
confidence: 90%
“…Similar anisotropic lattice evolution was also documented previously for other YbFe 2 O 4 -type solid solutions, such as InFeMg 1−y Cu y O 4 , 25 InGaZn 1−y Cu y O 4 , 23 and InGaZn 1−y Co y O 4 . 22 The common chemical feature of these solid solutions is that the magnetic dopants (Cu 2+ and Co 2+ ) have a relatively lower electronegativity than those of the host cations (Mg 2+ and Zn 2+ ).…”
Section: Paper Dalton Transactionssupporting
confidence: 87%
“…Fe 2+/3+ ions in RFe 2 O 4 can be substituted by various combinations of divalent Cu 2+ , Co 2+ , Zn 2+ , and Mg 2+ with trivalent Ga 3+ and Al 3+ cations, forming a large family of RFe 2 O 4 -type oxides with the general chemical formula RM1 2+ M2 3+ O 4 . 7–9,21–27 These oxides show intriguing magnetic, optical, and dielectric properties. Herein, we use tetravalent Ge 4+ ions in combination with divalent M 2+ (M = Cu, Co, Zn, and Mg) ions to design a new oxide series of R 2 M 3 GeO 8 .…”
Section: Introductionmentioning
confidence: 99%
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