2002
DOI: 10.1007/s003390201842
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Crystal and magnetic structures of new layered oxides A 2 GaMnO 5+y (A=Ca, Sr)

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Cited by 10 publications
(9 citation statements)
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“…This type of structure has been previously reported in the Mn-rich compound, Sr 2 Al 0.78 Mn 1.22 O 5.2 . The other type of structure has been reported for Sr 2 GaMnO 5.52 (oxygen storage phase), in which MnO 6 octahedral layers and GaO 6 octahedral layers are alternately laminated and oxygen defects exist in the GaO 2 plane of the GaO 6 octahedra . In the oxygen release phase, the DP structure is Mn-rich owing to the presence of the SrAl 2 O 4 impurity.…”
Section: Resultssupporting
confidence: 67%
See 1 more Smart Citation
“…This type of structure has been previously reported in the Mn-rich compound, Sr 2 Al 0.78 Mn 1.22 O 5.2 . The other type of structure has been reported for Sr 2 GaMnO 5.52 (oxygen storage phase), in which MnO 6 octahedral layers and GaO 6 octahedral layers are alternately laminated and oxygen defects exist in the GaO 2 plane of the GaO 6 octahedra . In the oxygen release phase, the DP structure is Mn-rich owing to the presence of the SrAl 2 O 4 impurity.…”
Section: Resultssupporting
confidence: 67%
“…29 The other type of structure has been reported for Sr 2 GaMnO 5.52 (oxygen storage phase), in which MnO 6 octahedral layers and GaO 6 octahedral layers are alternately laminated and oxygen defects exist in the GaO 2 plane of the GaO 6 octahedra. 30 In the oxygen release phase, the DP structure is Mn-rich owing to the presence of the SrAl 2 O 4 impurity. Therefore, it is presumed to have the same structure as Sr 2 Al 0.78 Mn 1.22 O 5.2 .…”
Section: ■ Results and Discussionmentioning
confidence: 99%
“…This spin axis is determined from the data of Mo¨ssbauer spectroscopy for the tetrahedral site occupied by the Fe 3þ ions. Since in the Mn-based brownmillerites, containing a single magnetic ion, the same spin axis was observed in the octahedral site [8][9][10][11][12][13], a coupling between Fe and Mn is evidenced. In agreement with the previous data of Rietveld analysis [1], we show the wholly unmixed Fe, Mn cationic distribution over the tetrahedral and octahedral sites.…”
Section: Introductionmentioning
confidence: 89%
“…Similarly, a good number of brownmillerites show the random distribution of cations between chains and planes. However, recently a number of site-unmixed (Mn,Al) and (Mn,Ga)-based brownmillerites were synthesized, showing the strongest single-ion magnetocrystalline anisotropy axis oriented perpendicular to the planes [8][9][10][11][12][13]. In all these Mn-based brownmillerites containing no other magnetic ions, such as Sr 2 GaMnO 5 [8][9][10][11], Sr 2 Al 1þd Mn 1Àd O 5 [12], Ca 2 AlMnO 5 [8], SrCaGaMnO 5 [13], the Mn 3þ spins were reported to align normally to layers.…”
Section: Introductionmentioning
confidence: 99%
“…This value is lower than the average theoretical moment expected for a 1:1 ratio of Mn 3+ (d 4 ) and Mn 4+ (d 3 ) cations in Ca 3 GaMn 2 O 8 , which is 4.39 μB. However, low moments have been observed for Mn in other Ga-containing oxides such as Ca 2 GaMnO 5.045 (3.6 μB), SrCaMnGaO 5+δ (3.3 μB), and Sr 2 GaMnO 5.0 (3.2 μB). , …”
Section: Resultsmentioning
confidence: 70%