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Title: Sr{sub 4+n}Mn{super III}{sub 4}Mn{super IV}{sub n} O{sub 10+3n} : A new homologous series of oxygen vacancy-ordered perovskite compounds built from Mn{sup III}-O pyramids and Mn{sup IV}-O octahedra.

Journal Article · · Acta Crystallogr. B

A new homologous series of oxygen-vacancy-ordered perovskites with the formula Sr{sub 4+n}Mn{sub 4}{sup 3+}Mn{sub n}{sup 4+}O{sub 10+3n} is proposed based on the structural trends found for the recently described Sr{sub 4}Mn{sub 4}O{sub 10}, Sr{sub 5}Mn{sub 5}O{sub 13} and Sr{sub 7}Mn{sub 7}O{sub 19} compounds. These compounds correspond to n = 0 (Sr{sub 4}Mn{sub 4}{sup 3+}O{sub 10}), n = 1 (Sr{sub 5}Mn{sub 4}{sup 3+}Mn{sup 4+}O{sub 13}) and n = 3 (Sr{sub 7}Mn{sub 4}{sup 3+}Mn{sub 3}{sup 4+}O{sub 19}) members of the series. A linear set of four Mn{sup 3+}O{sub 5} pyramids placed on the ab plane and pointing along the +x, -y, +y, -x directions defines the n = 0 building block for the series. The nth members can be constructed from blocks containing four pyramids and n Mn{sup 4+}O{sub 6} octahedra with 2/m symmetry. Compounds in the related systems CaMnO{sub x} and LaCuO{sub x}, containing Mn{sup 3+} and Cu{sup 2+} pyramids and Mn{sup 4+} and Cu{sup 3+} octahedra have also been found to be members of the series. The size and charge of the A-site cation and the apical distortion of the pyramidally coordinated B-site cation are shown to be important factors in the stabilization of certain members of the series. A qualitative explanation for the absence of some of the possible members of the series is presented based on these factors.

Research Organization:
Argonne National Lab. (ANL), Argonne, IL (United States)
Sponsoring Organization:
USDOE Office of Science (SC); DOT
DOE Contract Number:
DE-AC02-06CH11357
OSTI ID:
992042
Report Number(s):
ANL/MSD/JA-59703; TRN: US201021%%372
Journal Information:
Acta Crystallogr. B, Vol. 64, Issue 2 ; 2008
Country of Publication:
United States
Language:
ENGLISH