inorganic papers
i44
Marten G. Barkeret al. Sr4OI6 DOI: 101107/S1600536801006626 Acta Cryst.(2001). E57, i44±i45 Acta Crystallographica Section EStructure Reports Online
ISSN 1600-5368
Strontium oxide iodide
Marten G. Barker,² M. Grazia Francesconi, Thomas H. Shutt and Claire Wilson*
School of Chemistry, University of Nottingham, Nottingham NG7 2RD, England
² Deceased.
Correspondence e-mail: [email protected]
Key indicators Single-crystal X-ray study T= 150 K
Mean(Sr±O) = 0.01 AÊ Rfactor = 0.030 wRfactor = 0.055
Data-to-parameter ratio = 28.8
For details of how these key indicators were automatically derived from the article, see http://journals.iucr.org/e.
#2001 International Union of Crystallography Printed in Great Britain ± all rights reserved
Strontium oxide iodide, Sr4OI6, has been prepared by a
solid-state reaction and shown to be isostructural with bothA4OCl6,
whereAis Ba or Sr, and Ba4OI6.
Comment
Alkaline earth oxide chlorides and oxide bromides, of general formulaA4OX6(A= alkaline earth;X= Clÿ, Brÿ) are known
for their luminescence properties, when the alkaline earth site is doped with small amounts of Eu2+or Pb2+(Schipperet al.,
1992). This family has now been extended to the strontium oxide iodide compounds Sr4OI6. Sr4OI6 was prepared by a
solid-state reaction and is isostructural with Sr4OCl6
(Hage-mannet al., 1996), Ba4OCl6(Bergerhoff & Goost, 1970) and
Ba4OI6(Barkeret al., 2001). The oxygen is four-coordinated
by Sr cations, the iodine is four- and ®ve-coordinated by Sr cations, and the Sr is eight-coordinated by one oxygen and seven iodine anions at one site and seven-coordinated by one oxygen and six iodine anions at the other (Fig. 1). shows the overall structure and ®gures for the isostructural Ba4OI6given
in Barkeret al.(2001) show the coordination at each of these sites.
Experimental
SrO and SrI2powders were mixed in stoichiometric proportions and
placed in a nickel crucible. The mixture was then heated at 1273 K for 24 h in a silica tube, under ¯owing nitrogen. The product was cooled to room temperature at a rate of 1 K hÿ1.
Received 13 February 2001 Accepted 20 April 2001 Online 22 May 2001
Figure 1
[001] projection of the Sr4OI6structure showing the Iÿanions (blue) and
Crystal data
Sr4OI6
Mr= 1127.88
Hexagonal,P63mc
a= 10.747 (1) AÊ
c= 7.8678 (9) AÊ
V= 787.0 (3) AÊ3
Z= 2
Dx= 4.760 Mg mÿ3
MoKradiation Cell parameters from 841
re¯ections
= 5.9±27.6
= 25.21 mmÿ1
T= 150 (2) K Block, colourless 0.050.040.04 mm
Data collection
Bruker SMART1000 CCD area-detector diffractometer
!scans
Absorption correction: multi-scan (SADABS; Bruker, 1996)
Tmin= 0.272,Tmax= 0.365
3527 measured re¯ections 776 independent re¯ections
586 re¯ections withI> 2(I)
Rint= 0.054
max= 27.6
h=ÿ13!6
k=ÿ10!4
l=ÿ9!10 Intensity decay: none
Re®nement
Re®nement onF2
R[F2> 2(F2)] = 0.030
wR(F2) = 0.055
S= 0.94 721 re¯ections 25 parameters
w= 1/[2(F
o2) + (0.0206P)2]
whereP= (Fo2+ 2Fc2)/3
(/)max< 0.001
max= 1.27 e AÊÿ3
min=ÿ0.99 e AÊÿ3
Absolute structure: Flack (1983) Flack parameter = 0.064 (18)
Table 1
Selected bond lengths (AÊ).
Sr1ÐO 2.37 (2)
Sr1ÐI1i 3.366 (2)
Sr1ÐI2ii 3.830 (2)
Sr2ÐO 2.393 (6)
Sr2ÐI2iii 3.392 (2)
Sr2ÐI1iv 3.3947 (18)
Sr2ÐI2v 3.5567 (19)
Sr2ÐI1vi 3.5967 (17)
OÐSr2iv 2.393 (6)
OÐSr2vii 2.393 (6)
Symmetry codes: (i) 1ÿy;1xÿy;1z; (ii)y;1ÿxy;1
2z; (iii)xÿy;x;12z; (iv)ÿxy;1ÿx;z; (v)ÿy;xÿy;z; (vi) 1ÿx;1ÿy;1
2z; (vii) 1ÿy;1xÿy;z.
The origin was ®xed by application of a ¯oating origin restraint which effectively ®xes the centre of gravity of the structure in the polar-axis direction. This leads to smaller correlations than ®xing a single atom in structures with no dominant heavy atom (Flack & Schwarzenbach 1988).
Data collection:SMART(Bruker, 1998); cell re®nement:SAINT
(Bruker, 2000); data reduction:SAINTandSHELXL97 (Sheldrick, 1997); program(s) used to solve structure: SIR97 (Altomare et al., 1999); program(s) used to re®ne structure:SHELXL97 andWINGX
(Farrugia, 1999); molecular graphics: ATOMS (Dowty, 1998) and
ORTEP-3 (Farrugia, 1997); software used to prepare material for publication:SHELXL97 andPLATON(Spek, 2001).
References
Altomare, A., Burla, M. C., Camalli, M., Cascarano, G, Giacovazzo, C., Guagliardi, A., Moliterni, A. G. G., Polidori, G. & Spagna, R. (1999).J. Appl. Cryst.32, 115±119.
Barker, M. G., Francesconi, M. G., & Wilson, C. (2001).Acta Cryst.E57, i41± 43.
Bergerhoff, G. & Goost, L. (1970).Acta Cryst.B26, 19±23.
Bruker (1996).SADABS. Bruker AXS Inc., Madison, Wisconsin, USA. Bruker (1998). SMART Area-Detector Software Package. Version 5.054.
Bruker AXS Inc., Madison, Wisconsin, USA.
Bruker (2000). SAINT Frame Integration Software. Version 6.02a. Bruker AXS Inc., Madison, Wisconsin, USA.
Dowty, E. (1998).ATOMS. Version 4.1. Shape Software, 521 Hidden Valley Road, Kingsport, TN 37663, USA.
Farrugia, L. J. (1997).J. Appl. Cryst.30, 565. Farrugia, L. J. (1999).J. Appl. Cryst.32, 837±838. Flack, H. D. (1983).Acta Cryst.A39, 876±881.
Flack, H. D & Schwarzenbach, D. (1988).Acta Cryst.A44, 499±506. Hagemann, H., Kubel, F. & Bill, H. (1996).Eur. J. Solid State Inorg. Chem.33,
1101±1109.
Schipper, W. J., Vroon, Z. A. E. P., Blasse, G. & Schleid, T. (1992).Chem. Mater.4, 688±692.
supporting information
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Acta Cryst. (2001). E57, i44–i45
supporting information
Acta Cryst. (2001). E57, i44–i45 [https://doi.org/10.1107/S1600536801006626]
Strontium oxide iodide
Marten G. Barker, M. Grazia Francesconi, Thomas H. Shutt and Claire Wilson
(I)
Crystal data
Sr4OI6 Mr = 1127.88 Hexagonal, P63mc a = 10.747 (1) Å
c = 7.8678 (9) Å
V = 787.0 (3) Å3 Z = 2
F(000) = 956
Dx = 4.760 Mg m−3
Mo Kα radiation, λ = 0.71069 Å Cell parameters from 841 reflections
θ = 5.9–27.6°
µ = 25.21 mm−1 T = 150 K Block, colourless 0.05 × 0.04 × 0.04 mm
Data collection
Bruker SMART1000 CCD area-detector diffractometer
Radiation source: fine-focus sealed tube Graphite monochromator
ω scans
Absorption correction: multi-scan (SADABS; Bruker, 1996)
Tmin = 0.272, Tmax = 0.365
3527 measured reflections 776 independent reflections 586 reflections with I > 2σ(I)
Rint = 0.054
θmax = 27.6°, θmin = 5.9° h = −13→6
k = −10→4
l = −9→10
Refinement
Refinement on F2
Least-squares matrix: full
R[F2 > 2σ(F2)] = 0.030 wR(F2) = 0.055 S = 0.94 721 reflections 25 parameters 1 restraint
Primary atom site location: structure-invariant direct methods
Secondary atom site location: difference Fourier map
w = 1/[σ2(F
o2) + (0.0206P)2]
where P = (Fo2 + 2Fc2)/3
(Δ/σ)max < 0.001
Δρmax = 1.27 e Å−3
Δρmin = −0.99 e Å−3
Absolute structure: Flack (1983) Absolute structure parameter: 0.064 (18)
Special details
Refinement. Refinement of F2 against ALL reflections. The weighted R-factor wR and goodness of fit S are based on F2,
conventional R-factors R are based on F, with F set to zero for negative F2. The threshold expression of F2 > σ(F2) is used
only for calculating R-factors(gt) etc. and is not relevant to the choice of reflections for refinement. R-factors based on F2
are statistically about twice as large as those based on F, and R- factors based on ALL data will be even larger.
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2)
x y z Uiso*/Ueq
Sr1 0.3333 0.6667 0.8847 (3) 0.0290 (6)
Sr2 0.21157 (7) 0.42313 (14) 0.48599 (16) 0.0172 (3) I1 0.46542 (5) 0.53458 (5) 0.17690 (10) 0.0174 (2) I2 0.25533 (9) 0.12766 (5) 0.36865 (10) 0.0175 (2)
O 0.3333 0.6667 0.584 (3) 0.031 (5)
Atomic displacement parameters (Å2)
U11 U22 U33 U12 U13 U23
Sr1 0.0391 (10) 0.0391 (10) 0.0088 (12) 0.0196 (5) 0.000 0.000 Sr2 0.0181 (5) 0.0200 (7) 0.0142 (7) 0.0100 (4) −0.0004 (3) −0.0008 (6) I1 0.0187 (3) 0.0187 (3) 0.0129 (4) 0.0078 (4) 0.0015 (2) −0.0015 (2) I2 0.0195 (5) 0.0166 (3) 0.0174 (5) 0.0098 (2) 0.0008 (5) 0.0004 (2) O 0.027 (7) 0.027 (7) 0.038 (12) 0.014 (4) 0.000 0.000
Geometric parameters (Å, º)
Sr1—O 2.37 (2) Sr2—I2 3.5567 (19)
Sr1—I1i 3.366 (2) Sr2—I1vi 3.5967 (17)
Sr1—I1ii 3.366 (2) Sr2—I1v 3.5967 (17)
Sr1—I1iii 3.366 (2) Sr2—Sr2viii 3.926 (3)
Sr1—I2iv 3.830 (2) Sr2—Sr2vii 3.926 (3)
Sr1—I2v 3.830 (2) I1—Sr1x 3.366 (2)
Sr1—I2vi 3.830 (2) I1—Sr2viii 3.3947 (18)
Sr1—Sr2vii 3.870 (3) I1—Sr2xi 3.5967 (17)
Sr1—Sr2 3.870 (3) I1—Sr2xii 3.5967 (17)
Sr1—Sr2viii 3.870 (3) I2—Sr2xi 3.392 (2)
Sr2—O 2.393 (6) I2—Sr2xiii 3.5567 (19)
Sr2—I2v 3.392 (2) I2—Sr1xii 3.830 (2)
Sr2—I1vii 3.3947 (18) O—Sr2vii 2.393 (6)
Sr2—I1 3.3947 (18) O—Sr2viii 2.393 (6)
Sr2—I2ix 3.5567 (19)
O—Sr1—I1i 133.08 (4) I2v—Sr2—I1vi 71.32 (3)
O—Sr1—I1ii 133.08 (4) I1vii—Sr2—I1vi 146.26 (4)
I1i—Sr1—I1ii 78.48 (6) I1—Sr2—I1vi 72.54 (4)
O—Sr1—I1iii 133.08 (4) I2ix—Sr2—I1vi 135.64 (4)
I1i—Sr1—I1iii 78.48 (6) I2—Sr2—I1vi 70.80 (3)
I1ii—Sr1—I1iii 78.48 (6) O—Sr2—I1v 76.25 (17)
supporting information
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Acta Cryst. (2001). E57, i44–i45
I1i—Sr1—I2iv 69.97 (2) I1vii—Sr2—I1v 72.54 (4)
I1ii—Sr1—I2iv 69.97 (2) I1—Sr2—I1v 146.26 (4)
I1iii—Sr1—I2iv 138.80 (8) I2ix—Sr2—I1v 70.80 (3)
O—Sr1—I2v 88.11 (4) I2—Sr2—I1v 135.64 (4)
I1i—Sr1—I2v 138.80 (8) I1vi—Sr2—I1v 128.84 (6)
I1ii—Sr1—I2v 69.97 (2) O—Sr2—Sr1 35.4 (5)
I1iii—Sr1—I2v 69.97 (2) I2v—Sr2—Sr1 63.27 (5)
I2iv—Sr1—I2v 119.893 (5) I1vii—Sr2—Sr1 113.68 (5)
O—Sr1—I2vi 88.11 (4) I1—Sr2—Sr1 113.68 (5)
I1i—Sr1—I2vi 69.97 (2) I2ix—Sr2—Sr1 131.55 (3)
I1ii—Sr1—I2vi 138.80 (8) I2—Sr2—Sr1 131.55 (3)
I1iii—Sr1—I2vi 69.97 (2) I1vi—Sr2—Sr1 66.26 (3)
I2iv—Sr1—I2vi 119.893 (5) I1v—Sr2—Sr1 66.26 (3)
I2v—Sr1—I2vi 119.893 (5) O—Sr2—Sr2viii 34.9 (2)
O—Sr1—Sr2vii 35.85 (4) I2v—Sr2—Sr2viii 113.50 (3)
I1i—Sr1—Sr2vii 109.86 (4) I1vii—Sr2—Sr2viii 92.81 (2)
I1ii—Sr1—Sr2vii 109.86 (4) I1—Sr2—Sr2viii 54.67 (3)
I1iii—Sr1—Sr2vii 168.93 (6) I2ix—Sr2—Sr2viii 163.52 (2)
I2iv—Sr1—Sr2vii 52.26 (3) I2—Sr2—Sr2viii 112.351 (18)
I2v—Sr1—Sr2vii 105.43 (5) I1vi—Sr2—Sr2viii 56.92 (2)
I2vi—Sr1—Sr2vii 105.43 (5) I1v—Sr2—Sr2viii 110.87 (2)
O—Sr1—Sr2 35.85 (4) Sr1—Sr2—Sr2viii 59.52 (3)
I1i—Sr1—Sr2 168.93 (6) O—Sr2—Sr2vii 34.9 (2)
I1ii—Sr1—Sr2 109.86 (4) I2v—Sr2—Sr2vii 113.50 (3)
I1iii—Sr1—Sr2 109.86 (4) I1vii—Sr2—Sr2vii 54.67 (3)
I2iv—Sr1—Sr2 105.43 (5) I1—Sr2—Sr2vii 92.81 (2)
I2v—Sr1—Sr2 52.26 (3) I2ix—Sr2—Sr2vii 112.351 (18)
I2vi—Sr1—Sr2 105.43 (5) I2—Sr2—Sr2vii 163.52 (2)
Sr2vii—Sr1—Sr2 60.96 (6) I1vi—Sr2—Sr2vii 110.87 (2)
O—Sr1—Sr2viii 35.85 (4) I1v—Sr2—Sr2vii 56.92 (2)
I1i—Sr1—Sr2viii 109.86 (4) Sr1—Sr2—Sr2vii 59.52 (3)
I1ii—Sr1—Sr2viii 168.93 (6) Sr2viii—Sr2—Sr2vii 60.0
I1iii—Sr1—Sr2viii 109.86 (4) Sr1x—I1—Sr2viii 101.78 (5)
I2iv—Sr1—Sr2viii 105.43 (5) Sr1x—I1—Sr2 101.78 (5)
I2v—Sr1—Sr2viii 105.43 (5) Sr2viii—I1—Sr2 70.65 (6)
I2vi—Sr1—Sr2viii 52.26 (3) Sr1x—I1—Sr2xi 104.20 (5)
Sr2vii—Sr1—Sr2viii 60.96 (6) Sr2viii—I1—Sr2xi 153.95 (4)
Sr2—Sr1—Sr2viii 60.96 (6) Sr2—I1—Sr2xi 105.50 (4)
O—Sr2—I2v 98.7 (5) Sr1x—I1—Sr2xii 104.20 (5)
O—Sr2—I1vii 86.6 (4) Sr2viii—I1—Sr2xii 105.50 (4)
I2v—Sr2—I1vii 140.95 (3) Sr2—I1—Sr2xii 153.95 (4)
O—Sr2—I1 86.6 (4) Sr2xi—I1—Sr2xii 66.15 (4)
I2v—Sr2—I1 140.95 (3) Sr2xi—I2—Sr2 106.45 (2)
I1vii—Sr2—I1 77.69 (5) Sr2xi—I2—Sr2xiii 106.45 (2)
O—Sr2—I2ix 144.645 (17) Sr2—I2—Sr2xiii 147.04 (5)
I2v—Sr2—I2ix 82.78 (4) Sr2xi—I2—Sr1xii 64.47 (5)
I1vii—Sr2—I2ix 71.78 (3) Sr2—I2—Sr1xii 96.08 (2)
O—Sr2—I2 144.645 (18) Sr1—O—Sr2vii 108.7 (5)
I2v—Sr2—I2 82.78 (4) Sr1—O—Sr2 108.7 (5)
I1vii—Sr2—I2 114.41 (5) Sr2vii—O—Sr2 110.2 (4)
I1—Sr2—I2 71.78 (3) Sr1—O—Sr2viii 108.7 (5)
I2ix—Sr2—I2 70.71 (3) Sr2vii—O—Sr2viii 110.2 (4)
O—Sr2—I1vi 76.25 (17) Sr2—O—Sr2viii 110.2 (4)