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Volume 64 
Part 9 
Page i65  
September 2008  

Received 16 July 2008
Accepted 16 August 2008
Online 30 August 2008

Key indicators
Single-crystal X-ray study
T = 298 K
Mean [sigma]() = 0.000 Å
Some non-H atoms missing,
Disorder in main residue
R = 0.041
wR = 0.104
Data-to-parameter ratio = 51.4
Details
Open access

Natural perovskite: (CaII0.95 (1)CeIII0.011 (2)NaI0.010 (4))(FeIII0.022 (2)TiIV0.98 (1))O3

aDepartment of Chemistry, Federal University of Minas Gerais, Av. Antônio Carlos 6627, 31270-901 Belo Horizonte, Brazil
Correspondence e-mail: ngfernandes@ufmg.br

A natural sample of perovskite (calcium caesium sodium iron titanium oxide) from the Tapira Alkaline Complex in southeastern Brazil was found by electron microprobe analysis to have the chemical formula (Ca2+0.95 (1)Ce3+0.011 (2)Na+0.010 (4))(Fe3+0.022 (2)Ti4+0.98 (1))O2-3 and by IR spectroscopy to be an anhydrous mineral. Oxygen anions are arranged around Ti4+ in an almost perfect octahedron and around Ca2+ in a distorted 12-fold polyhedron.

Related literature

For related literature, see: Banfield & Veblen (1992[Banfield, J. F. & Veblen, D. R. (1992). Am. Mineral. 77, 545-557.]); Beran et al. (1996[Beran, A., Libowittzky, E. & Armbruster, T. (1996). Can. Mineral. 34, 803-809.]); Chakhmouradian & Mitchell (1998[Chakhmouradian, A. R. & Mitchell, R. H. (1998). Can. Mineral. 36, 953-969.]); Haggerty & Mariano (1983[Haggerty, S. E. & Mariano, A. N. (1983). Contrib. Mineral. Petrol. 84, 365-381.]); Kay & Bailey (1957[Kay, H. F. & Bailey, P. C. (1957). Acta Cryst. 10, 219-226.]); Lloyd & Bailey (1991[Lloyd, F. E. & Bailey, D. K. (1991). 5th International Kimberlite Conference (Extended Abstracts), edited by O. H. Leonardos, H. O. A. Meyer & J. C. Gaspar, pp. 263-269. Araxá, Brazil, CPRM, Special Publication 3/91.]); Mariano & Mitchell (1991[Mariano, A. N. & Mitchell, R. H. (1991). Proceedings of the 5th International Conference, Araxa, Brazil, pp. 251-253. Extended Abstracts.]); Seer & Moraes (1988[Seer, H. J. & Moraes, L. C. (1988). Rev. Bras. Geo. 18, 134-140.]); Sgarbi & Gaspar (1995[Sgarbi, P. B. A. & Gaspar, J. C. (1995). 6th International Kimberlite Conference (Extended Abstracts), Novosibirsk, Rússia, pp. 498-499.]); Sgarbi & Valença (1994[Sgarbi, P. B. A. & Valença, J. G. (1994). International Symposium on the Physics and Chemistry of the Upper Mantle (Extended Abstracts), pp. 27-29. São Paulo, Brazil: CPRM/FAPESP.]); Soubies et al. (1991[Soubies, F., Melfi, A. J. & Autefage, F. (1991). Rev. Bras. Geo. 21, 3-16.]).

Experimental

Crystal data
  • Na0.01Ca0.96Fe0.02Ti0.98Ce0.01O3

  • Mr = 136.40

  • Orthorhombic, P b n m

  • a = 5.3818 (4) Å

  • b = 5.4431 (4) Å

  • c = 7.6450 (5) Å

  • V = 223.95 (3) Å3

  • Z = 4

  • Mo K[alpha] radiation

  • [mu] = 5.94 mm-1

  • T = 298 (2) K

  • 0.2 × 0.15 × 0.15 mm

Data collection
  • Siemens P4 diffractometer

  • Absorption correction: refined from [Delta]F (SHELXL97; Sheldrick, 2008[Sheldrick, G. M. (2008). Acta Cryst. A64, 112-122.]) Tmin = 0.356, Tmax = 0.409

  • 2383 measured reflections

  • 1594 independent reflections

  • 1527 reflections with I > 2s(I)

  • Rint = 0.033

  • 3 standard reflections every 197 reflections intensity decay: 0.8%

Refinement
  • R[F2 > 2[sigma](F2)] = 0.041

  • wR(F2) = 0.103

  • S = 1.25

  • 1594 reflections

  • 31 parameters

  • [Delta][rho]max = 2.01 e Å-3

  • [Delta][rho]min = -2.88 e Å-3

Table 1
Selected geometric parameters (Å ,° ), where A represents the Ca2+, Na+ and Ce3+ cations, on a 12-coordinated site and B represents Fe3+ and Ti4+ cations on an octahedral site

A-O1 2.359 (2) O1iv-A-O1iv 162.30 (6)
A-O1iv 2.481 (2) O2iv-A-O2viii 80.97 (4)
A-O1iv 3.027 (2) O1-A-O2vii 118.03 (2)
A-O1 3.052 (2) O2ii-A-O1iv 65.08 (3)
A-O2viii 2.378 (1)    
A-O2ii 2.620 (1)    
A-O2iv 2.667 (1)    
A-O2vi 3.233 (1)    
B-O1ii 1.9513 (3) O1-B-O1ii 180.0
B-O2vii 1.956 (1) O2-B-O2vii 89.41 (1)
B-O2v 1.959 (1) O1-B-O2 89.58 (6)
Symmetry code: (ii) [-x, -y, z + {\script{1\over 2}}]; (iii) [(x + {\script{1\over 2}}) -1, -y + {\script{1\over 2}}, -z]; (iv) [-x + {\script{1\over 2}}, (y + {\script{1\over 2}}) - 1, 1- (-z + {\script{1\over 2}})]; (v) -x, -y, -z; (vi) [x, y, 1 - (-z + {\script{1\over 2}})]; (vii) [-x + {\script{1\over 2}}, y + {\script{1\over 2}}, z]; (viii) [(x + {\script{1\over 2}}) - 1, -y + {\script{1\over 2}}, z + {\script{1\over 2}}]; (ix) [-x, -y + 1, (z + {\script{1\over 2}}) -1].

Data collection: XSCANS (Siemens, 1991[Siemens (1991). XSCANS User's Manual. Siemens Analytical X-ray Instruments Inc., Madison, Wisconsin, USA.]); cell refinement: XSCANS; data reduction: XSCANS; program(s) used to solve structure: SHELXS97 (Sheldrick, 2008[Sheldrick, G. M. (2008). Acta Cryst. A64, 112-122.]); program(s) used to refine structure: SHELXL97 (Sheldrick, 2008[Sheldrick, G. M. (2008). Acta Cryst. A64, 112-122.]); molecular graphics: CrystalMaker (CrystalMaker, 2007[CrystalMaker (2007). CrystalMaker for Windows. CrystalMaker Software Ltd, Yarnton, England.]); software used to prepare material for publication: WinGX (Farrugia, 1999[Farrugia, L. J. (1999). J. Appl. Cryst. 32, 837-838.]).


Supplementary data and figures for this paper are available from the IUCr electronic archives (Reference: MG2053 ).


Acknowledgements

The authors are grateful to Dr José Affonso Brod, University of Brasília, Brazil, for providing the perovskite samples, and to Mr William T. Soares for the microprobe analysis. This work was supported by the Minas Gerais Foundation for Research Development, FAPEMIG (Grant CEX 1123/90). EGG is grateful to the Brazilian Science Research Council, CNPq, for providing a graduate fellowship.

References

Banfield, J. F. & Veblen, D. R. (1992). Am. Mineral. 77, 545-557.  [ChemPort]
Beran, A., Libowittzky, E. & Armbruster, T. (1996). Can. Mineral. 34, 803-809.  [ChemPort]
Chakhmouradian, A. R. & Mitchell, R. H. (1998). Can. Mineral. 36, 953-969.  [ChemPort]
CrystalMaker (2007). CrystalMaker for Windows. CrystalMaker Software Ltd, Yarnton, England.
Farrugia, L. J. (1999). J. Appl. Cryst. 32, 837-838.  [CrossRef] [ChemPort] [details]
Haggerty, S. E. & Mariano, A. N. (1983). Contrib. Mineral. Petrol. 84, 365-381.  [CrossRef] [ChemPort]
Kay, H. F. & Bailey, P. C. (1957). Acta Cryst. 10, 219-226.  [CrossRef] [ChemPort] [details]
Lloyd, F. E. & Bailey, D. K. (1991). 5th International Kimberlite Conference (Extended Abstracts), edited by O. H. Leonardos, H. O. A. Meyer & J. C. Gaspar, pp. 263-269. Araxá, Brazil, CPRM, Special Publication 3/91.
Mariano, A. N. & Mitchell, R. H. (1991). Proceedings of the 5th International Conference, Araxa, Brazil, pp. 251-253. Extended Abstracts.
Seer, H. J. & Moraes, L. C. (1988). Rev. Bras. Geo. 18, 134-140.
Sgarbi, P. B. A. & Gaspar, J. C. (1995). 6th International Kimberlite Conference (Extended Abstracts), Novosibirsk, Rússia, pp. 498-499.
Sgarbi, P. B. A. & Valença, J. G. (1994). International Symposium on the Physics and Chemistry of the Upper Mantle (Extended Abstracts), pp. 27-29. São Paulo, Brazil: CPRM/FAPESP.
Sheldrick, G. M. (2008). Acta Cryst. A64, 112-122.  [CrossRef] [details]
Siemens (1991). XSCANS User's Manual. Siemens Analytical X-ray Instruments Inc., Madison, Wisconsin, USA.
Soubies, F., Melfi, A. J. & Autefage, F. (1991). Rev. Bras. Geo. 21, 3-16.


Acta Cryst (2008). E64, i65  [ doi:10.1107/S1600536808026421 ]

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