2016
DOI: 10.1021/acs.inorgchem.5b02984
|View full text |Cite
|
Sign up to set email alerts
|

High-Pressure Synthesis, Crystal Structure, and Magnetic Properties of Sr2MnO3F: A New Member of Layered Perovskite Oxyfluorides

Abstract: We have successfully synthesized Sr2MnO3F, a new layered perovskite oxyfluoride with a n = 1 Ruddlesden-Popper-type structure using a high-pressure, high-temperature method. Structural refinements against synchrotron X-ray diffraction data collected from manganese oxyfluoride demonstrated that it crystallizes in a tetragonal cell with the space group I4/mmm, in which the Mn cation is located at the octahedral center position. This is in stark contrast to the related oxyhalides that have square-pyramidal coordi… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

1
19
0

Year Published

2016
2016
2023
2023

Publication Types

Select...
7
2
1

Relationship

0
10

Authors

Journals

citations
Cited by 27 publications
(20 citation statements)
references
References 58 publications
1
19
0
Order By: Relevance
“…In terms of lattice mismatch, F occupancy of equatorial X 1 sites might be expected (giving perovskite blocks of a similar width to the [Bi 2 O 2 ] 2+ layers) but tilting of the Ti X 6 octahedra, about in-plane and out-of-plane axes, can also reduce this interfacial mismatch while maintaining satisfactory Ti– X bond lengths. The bond valence sum analysis and our understanding of strain suggest that F occupancy of equatorial X 1 sites is certainly possible in Bi 2 TiO 4 F 2 and is consistent with the conclusions of Needs et al 39 However, this contrasts with several other n = 1 Aurivillius and Ruddlesden-Popper oxyfluorides including Bi 2 NbO 5 F, 54 Sr 2 ScO 3 F, 67 and Sr 2 MnO 3 F, 68 which are reported to have F occupancy of apical anion sites despite similar arguments involving stacking strain between [Bi 2 O 2 ] 2+ and Nb(O,F) 2 layers ( a p = 3.95 Å and a p = 4.08 Å for F – in equatorial X 1 or apical X 2 sites, respectively) or between SrO and Mn(O,F) 2 layers (ideal a SrO ≈ 3.65 Å; for Sr 2 ScO 3 F a p = 4.12 Å and a p = 4.19 Å for F – in equatorial or apical sites, respectively; for Sr 2 MnO 3 F a p = 3.86 Å and a p = 3.99 Å for F – in equatorial or apical sites, respectively). It is striking that Bi 2 TiO 4 F 2 has relatively small stacking strain compared to these examples, suggesting the possibility that anion distribution might be tuned by strain engineering, for example.…”
Section: Discussionsupporting
confidence: 87%
“…In terms of lattice mismatch, F occupancy of equatorial X 1 sites might be expected (giving perovskite blocks of a similar width to the [Bi 2 O 2 ] 2+ layers) but tilting of the Ti X 6 octahedra, about in-plane and out-of-plane axes, can also reduce this interfacial mismatch while maintaining satisfactory Ti– X bond lengths. The bond valence sum analysis and our understanding of strain suggest that F occupancy of equatorial X 1 sites is certainly possible in Bi 2 TiO 4 F 2 and is consistent with the conclusions of Needs et al 39 However, this contrasts with several other n = 1 Aurivillius and Ruddlesden-Popper oxyfluorides including Bi 2 NbO 5 F, 54 Sr 2 ScO 3 F, 67 and Sr 2 MnO 3 F, 68 which are reported to have F occupancy of apical anion sites despite similar arguments involving stacking strain between [Bi 2 O 2 ] 2+ and Nb(O,F) 2 layers ( a p = 3.95 Å and a p = 4.08 Å for F – in equatorial X 1 or apical X 2 sites, respectively) or between SrO and Mn(O,F) 2 layers (ideal a SrO ≈ 3.65 Å; for Sr 2 ScO 3 F a p = 4.12 Å and a p = 4.19 Å for F – in equatorial or apical sites, respectively; for Sr 2 MnO 3 F a p = 3.86 Å and a p = 3.99 Å for F – in equatorial or apical sites, respectively). It is striking that Bi 2 TiO 4 F 2 has relatively small stacking strain compared to these examples, suggesting the possibility that anion distribution might be tuned by strain engineering, for example.…”
Section: Discussionsupporting
confidence: 87%
“…49 Given the similarity in cation-anion coordination in Figure 3(a), it becomes clear that an opportunity arises to form V analogs of the more numerous magneticallysquare-planar Mn fluorides, for example to produce NaRb 2 V 3 F 12 , Sr 2 VO 3 F, or LiVF 4 •H 2 O (corresponding to Mn-based ICSD codes 83871, 291640, and 417512, respectively). [50][51][52] Similar logic can be applied to the landscape around Rb 2 CrCl 2 I 2 , which is the only such compound in the Cr-I system. 53 Searching for hexagonal/kagomé ordering (metalmetal-metal angle 55 • -65 • ) again shows a high prevalence for oxides in Figure 6(b).…”
Section: B Uncovering Unconventional Compoundsmentioning
confidence: 99%
“…For simple perovskites oxyfluorides, O 2¹ and F ¹ are disordered; SrFeO 2 F, 3) BaFeO 2 F 4) PbScO 2 F 5) BaScO 2 F 6) AgFeOF 2 7) BaInO 2 F 8) and AgTiO 2 F 9) adopt the cubic or nearly cubic perovskite structure, in which O 2¹ and F ¹ occupy the same crystallographic sites and are randomly distributed. However, in a variety of RuddlesdenPopper type layered perovskites such as Sr 2 CuO 2 F 2 , 10) Sr 2 FeO 3 F, 11),12) Ba 2 InO 3 F, 13) Ba 2 ScO 3 F, 14) Sr 2 MnO 3 F, 15) Sr 3 Fe 2 O 5¹x F y 11), 16) and the others, 17) the F ¹ ions occupy selectively the interlayer site. This manner leads O/F order, but their degrees of ordering are different.…”
Section: Introductionmentioning
confidence: 99%