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Structure and magnetism of the topotactically reduced oxychloride Sr4Mn3O(6.5)Cl2.

Abstract:
Reaction of the n = 3 Ruddlesden-Popper oxychloride Sr(4)Mn(3)O(7.5)Cl(2) with calcium hydride yields the topotactically reduced phase Sr(4)Mn(3)O(6.5)Cl(2). The deintercalation of oxide ions from the central MnO(1.5) layer of the starting phase is accompanied by a rearrangement of the anion lattice, resulting in a layer of composition MnO(0.5) in the reduced material, consisting of chains of MnO(4) tetrahedra connected by edge and corner sharing. Magnetization and low-temperature neutron diffraction data are consistent with antiferromagnetic coupling of manganese spins, but no long-range magnetic order is observed down to 5 K, presumably due to the large interlayer separation in the reduced phase. The influence of anion substitution on the structural selectivity of low-temperature reduction reactions is discussed.
Publication status:
Published

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Publisher copy:
10.1021/ic300258f

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Institution:
University of Oxford
Division:
MPLS
Department:
Chemistry
Sub department:
Inorganic Chemistry
Role:
Author


Journal:
Inorganic chemistry More from this journal
Volume:
51
Issue:
9
Pages:
5325-5331
Publication date:
2012-05-01
DOI:
EISSN:
1520-510X
ISSN:
0020-1669


Language:
English
Pubs id:
pubs:325218
UUID:
uuid:efc3a7f7-dbdd-4d49-8b77-4cd99552d4f9
Local pid:
pubs:325218
Source identifiers:
325218
Deposit date:
2012-12-19
ARK identifier:

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