inorganic papers
Acta Cryst.(2007). E63, i19–i21 doi:10.1107/S1600536806054936 Rief and Kubel Sr
3Al10SiO20
i19
Acta Crystallographica Section E
Structure Reports
Online
ISSN 1600-5368
Sr
3Al
10SiO
20from single-crystal data
Andreas Rief* and Frank Kubel
Vienna University of Technology, Institute for Chemical Technologies and Analytics, Getreidemarkt 9/164-SC, Vienna A-1160, Austria
Correspondence e-mail: [email protected]
Key indicators
Single-crystal X-ray study
T= 298 K
Mean(Al–O) = 0.002 A˚ Disorder in main residue
Rfactor = 0.036
wRfactor = 0.032
Data-to-parameter ratio = 11.9
For details of how these key indicators were automatically derived from the article, see http://journals.iucr.org/e.
Received 15 November 2006 Accepted 18 December 2006
#2007 International Union of Crystallography All rights reserved
Single crystals of tristrontium decaaluminum silicon icosa-oxide were synthesized by local flux growth with H3BO3as mineralizer. Lattice parameters and refinement data indicate no significant incorporation of B in the structure. Pairs of AlO6octahedra are located between layers of edge-linked Al/ Si–O4 tetrahedra. The Sr1 (2/msymmetry) and Sr2 (mirror plane) sites are orientated in layers perpendicular to the layers of Al/Si–O polyhedra.
Comment
Recently, Sr3Al10SiO20 doped with Tb, Eu or Eu/Ho was discovered to be a blue-emitting long-lasting phosphor for optical applications, such as TFT screens and LEDs (Kuanget al. 2005, 2006;Kubota & Shimada, 2002; Kubotaet al., 2002). Sr3Al10SiO20is isostructural with Pb3Al10GeO20(monoclinic,
C2/m; Vinek et al., 1970). The first structure refinement of Sr3Al10SiO20 was performed by Kubota et al. (2001) using powder diffraction data by Rietveld refinement based on Pb3Al10GeO20by replacing Pb sites with Sr. In order to obtain a more precise structure determination, we synthesized single crystals of Sr3Al10SiO20 (SR3). The published results from powder data agree very well with our single-crystal
measure-Figure 1
[image:1.610.209.456.444.708.2]ments. The lattice parameters of the single crystal (seeCrystal data) agree with the literature [a = 15.1416 (18), b = 11.1843 (12), c = 4.9026 (13) A˚ , = 108.117 (5) and V =
789.06 (16) A˚3; Kubota et al. 2001]. Capron et al. (2002) puplished a powder diffraction study with a refinement in space group I2/m [a = 14.394 (2), b = 11.189 (2), c = 4.904 (1) A˚ ,= 90.793 (1),V= 789.74 A˚3]. The refinement of the structure model against single-crystal data was performed usingXtal3.2 (Hallet al., 1992) to a finalR= 0.036. The good correlation between the powder and single-crystal data excludes any incorporation of B, even in small amounts. B tends to replace the tetravalent or octahedral Al position, and at least a reduction of the unit cell in thea-axis direction (due to deformations of the octahedral chains in this direction) should be observed.
A detailed description of the structure was reported by Kubotaet al.(2001). The matrix is composed of corner-linked Al/Si tetrahedra arranged in layers along thecaxis, connected to isolated pairs of edge-linked Al octahedra (see Fig. 1). These octahedra show distortion in all bond lengths and angles. Selected bond distances are given in Table 1. The averaged Al/Si—O bond distances are almost the same for both tetrahedral Al/Si positions [Al1/Si1—O 1.745 (6), Al2/ Si2—O 1.737 (6) A˚ ] and an identical substitution ratio is assumed. The occupancy factor for Si1,2 refined to 0.125 (subsequently set at this value) and is the same as is given in the literature. In the original Pb3Al10GeO20compound, all Al sites were substituted by a small amount (s.o.f. 0.091) of Ge.
Remarkable in this structure is the short distance between Sr1 and O5 of only 2.392 (3) A˚ ; the sum of ionic radii for Sr2+ and O2–is 2.58 A˚ (Shannon, 1976). Capronet al.(2002) report an even shorter Sr—O distance of 2.388 (8) A˚ . For Sr1, CN 12 and for Sr2, CN (4 + 4 + 4) is observed. The other Sr—O distances (Table 2) are within or longer than the range expected from the atomic radii [Sr(x)—O(y) > 2.68 A˚ ].
Experimental
Single crystals were synthesized from well ground analytical SrCO3, Al(OH)3(both Merck) and SiO2(Fluka) by adding 10% by weight of H3BO3(Aldrich). The carefully homogenized mixture of educts was pressed into pellets and fired at 1723 K (180 K h1) in a corundum crucible for 24 h. The samples were slowly cooled down to room temperature with a cooling rate of 180 K h1. To improve yield and crystal growth, samples were crushed, refired and repelleted after 12 h of heating. The hard sintered pellets were crushed carefully in a mortar into smaller fragments. Under polarized light, microscopic crystals showing homogeneous extinction were separated and prepared for single-crystal measurements.
Crystal data
Sr3Al10SiO20
Mr= 880.75
Monoclinic,C2=m a= 15.1438 (18) A˚ b= 11.1858 (13) A˚ c= 4.9018 (6) A˚
Z= 2
Dx= 3.707 Mg m
3
MoKradiation
= 10.86 mm1
T= 298 K Splinter, colourless
Data collection
Siemens SMART APEX diffractometer
!scans
Absorption correction: spherical (Tibballs, 1982)
Tmin= 0.302,Tmax= 0.318
4207 measured reflections 1261 independent reflections 1022 reflections withI> 3(I) Rint= 0.033
max= 30.5
Refinement
Refinement onF R[F2> 2(F2)] = 0.036
wR(F2) = 0.032 S= 1.70 1022 reflections
86 parameters (/)max= 0.001
max= 1.66 e A˚
3
min=1.15 e A˚
3
Table 1
Selected bond lengths (A˚ ).
Sr1i—O5i 2.3932 (17) Sr1i —O2i 2.6832 (18) Sr1i —O3ii 2.7018 (15) Sr1i —O4iii 2.8420 (16) Sr1i —O2ii 3.1967 (18) Sr1i —O6i 3.410 (3)
Sr1i—O1i 3.4812 (14) Sr2iv —O6i 2.527 (2) Sr2iv —O3v 2.6781 (16) Sr2iv —O6vi 3.158 (3) Sr2i —O1vii 3.5126 (14)
Symmetry codes: (i)xþ1 2;yþ
1 2;z; (ii)xþ
1 2;yþ
1
2;zþ1; (iii)xþ1;y;zþ1; (iv)
xþ1;y;zþ1; (v) xþ3 2;yþ
1
2;zþ1; (vi) xþ 1 2;yþ
1
2;zþ1; (vii)
xþ1 2;yþ
3 2;z.
The highest peak is located 0.00 A˚ from atom Sr2 and the deepest hole is located 1.02 A˚ from atom O5.
Data collection:SMART(Bruker, 2001); cell refinement:SAINT
(Bruker, 1999); data reduction:Xtal3.2 (Hallet al., 1992); program(s) used to solve structure:Xtal3.2; program(s) used to refine structure:
Xtal3.2; molecular graphics:Xtal3.2; software used to prepare mate-rial for publication:Xtal3.2.
References
[image:2.610.316.563.71.217.2]Bruker (1999).SAINT(Version 6.02a). Bruker AXS Inc., Madison, Wisconsin, USA.
Figure 2
Coordination environments for Sr1 and Sr2. Symmetry codes: (i)1 2+x, 1
2+y,z; (ii) 1 2+x,
1
2y,z; (iii) 1 2+x,
1
2y, 1 +z; (iv) 1 2+x,
1
2+y, 1 +z; (v)
1x,y, 1z; (vi) 1x, 1y, 1z; (vii)3 2x,
1
2+y, 2z; (viii) 3 2x, 1
2y, 1z; (ix) 3 2x,
1
2+y, 1z; (x) 1 2+x,
3
2y,z; (xi) 1 2x,
3 2y,-z;
(xii) 1 2 x,
1
2 + y,-z. Displacement ellipsoids are drawn at the 50%
Capron, M., Fayon, F., Coutures, J., Massiot, D. & Douy, A. (2002).J. Solid State Chem.169, 53–59.
Hall, S. R., Flack, H. D. & Stewart, J. M. (1992). Editors.Xtal3.2.Universities of Western Australia, Australia, Geneva, Switzerland, and Maryland, USA. Kuang, J. Y., Liu, Y. L. & Zhang, J. X. (2006).J. Mater. Sci.41, 5500–5503. Kuang, J. Y., Liu, Y. L., Zhang, J. X., Huang, L., Rong, J. & Yuan, D. (2005).
Solid State Commun.136, 6–10.
Kubota, S. & Shimada, M. (2002).Appl. Phys. Lett.15, 2749–2751. Kubota, S., Yamane, H. & Shimada, M. (2001).Acta Cryst.E57, i60–i61. Kubota, S., Yamane, H. & Shimada, M. (2002).Chem. Mater.14, 4015–4016. Shannon, R. D. (1976).Acta Cryst.A32, 751–767.
Tibballs, J. E. (1982).Acta Cryst.A38, 161–163.
Vinek, H., Voellenkle, H. & Nowotny, H. (1970).Monatsh. Chem.101, 275– 284.
inorganic papers
Acta Cryst.(2007). E63, i19–i21 Rief and Kubel Sr
supporting information
Acta Cryst. (2007). E63, i19–i21 [https://doi.org/10.1107/S1600536806054936]
Sr
3Al
10SiO
20from single-crystal data
Andreas Rief and Frank Kubel
tristrontium decaaluminum silicon icosaoxide
Crystal data
Sr3Al10SiO20
Mr = 880.75 Monoclinic, C2/m
Hall symbol: -C 2y
a = 15.1438 (18) Å
b = 11.1858 (13) Å
c = 4.9018 (6) Å
β = 108.137 (2)°
V = 789.09 (16) Å3
Z = 2
F(000) = 836
Dx = 3.707 Mg m−3
Mo Kα radiation, λ = 0.71073 Å Cell parameters from 4207 reflections
θ = 2.3–30.5°
µ = 10.86 mm−1
T = 298 K
Splinter, colourless
0.14 × 0.11 × 0.09 × 0.11 (radius) mm
Data collection
Siemens SMART APEX diffractometer
Detector resolution: 512 pixels mm-1
ω scans
Absorption correction: spherical (Tibballs, 1982)
Tmin = 0.302, Tmax = 0.318 4207 measured reflections
1261 independent reflections 1022 reflections with I > 3σ(I)
Rint = 0.033
θmax = 30.5°, θmin = 2.3°
h = −21→21
k = −15→15
l = −6→5
Refinement
Refinement on F
Least-squares matrix: full
R[F2 > 2σ(F2)] = 0.036
wR(F2) = 0.032
S = 1.70 1022 reflections 86 parameters
0 restraints 18 constraints
(Δ/σ)max = 0.001 Δρmax = 1.66 e Å−3 Δρmin = −1.15 e Å−3
Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2)
x y z Uiso*/Ueq Occ. (<1)
Sr1 0.21635 (2) 0.00000 0.73858 (8) 0.00000
Sr2 0.00000 0.50000 0.00000 0.00000
supporting information
sup-2
Acta Cryst. (2007). E63, i19–i21
Al3 0.00000 0.12868 (8) 0.50000 0.00000
Al4 0.00000 0.00000 0.00000 0.00000
O1 0.08364 (10) 0.24773 (13) 0.4294 (3) 0.00000 O2 0.24036 (10) 0.14101 (14) 0.3245 (4) 0.00000 O3 0.35984 (10) 0.14704 (14) −0.0061 (3) 0.00000 O4 0.42704 (9) 0.37941 (13) 0.1108 (3) 0.00000 O5 0.06564 (13) 0.00000 0.3873 (4) 0.00000 O6 0.40080 (14) 0.00000 0.4793 (5) 0.00000
Atomic displacement parameters (Å2)
U11 U22 U33 U12 U13 U23
Sr1 0.01130 (15) 0.01460 (18) 0.0185 (2) 0.00000 −0.00227 (13) 0.00000 Sr2 0.0118 (2) 0.0189 (3) 0.0135 (3) 0.00000 0.00093 (17) 0.00000 Al1 0.0075 (3) 0.0082 (3) 0.0067 (3) −0.0003 (2) 0.0030 (2) −0.0006 (3) Si1 0.0075 (3) 0.0082 (3) 0.0067 (3) −0.0003 (2) 0.0030 (2) −0.0006 (3) Al2 0.0081 (3) 0.0072 (3) 0.0073 (3) −0.0007 (3) 0.0024 (2) −0.0006 (3) Si2 0.0081 (3) 0.0072 (3) 0.0073 (3) −0.0007 (3) 0.0024 (2) −0.0006 (3) Al3 0.0076 (4) 0.0077 (5) 0.0059 (5) 0.00000 0.0032 (4) 0.00000 Al4 0.0077 (6) 0.0078 (6) 0.0063 (7) 0.00000 0.0027 (5) 0.00000 O1 0.0096 (7) 0.0097 (8) 0.0108 (8) −0.0011 (6) 0.0031 (6) −0.0007 (7) O2 0.0083 (7) 0.0122 (8) 0.0201 (10) −0.0021 (6) 0.0029 (7) −0.0002 (7) O3 0.0171 (8) 0.0105 (8) 0.0096 (9) −0.0022 (6) 0.0052 (6) −0.0013 (7) O4 0.0090 (7) 0.0087 (8) 0.0083 (8) −0.0027 (6) 0.0015 (6) −0.0000 (6) O5 0.0068 (9) 0.0084 (11) 0.0050 (11) 0.00000 0.0012 (8) 0.00000 O6 0.0151 (11) 0.0097 (11) 0.0126 (13) 0.00000 0.0005 (9) 0.00000
Geometric parameters (Å, º)
Sr1i—O5i 2.3932 (17) Al3i—O4 1.8856 (14) Sr1i—O2ii 2.6832 (18) Al3i—O4 1.8856 (14) Sr1i—O2i 2.6832 (18) Al3i—O5i 1.9253 (17) Sr1i—O3 2.7018 (15) Al3i—O5 1.9253 (17) Sr1i—O3 2.7018 (15) Al3i—O1 1.9417 (17) Sr1i—O4 2.8420 (16) Al3i—O1i 1.9417 (17)
Sr1i—O4 2.8420 (16) Al4—O5 1.849 (2)
Sr1i—O2 3.1967 (18) Al4—O5 1.849 (2)
Sr1i—O2 3.1967 (18) Al4—O4 1.9259 (16)
Sr1i—O6i 3.410 (3) Al4—O4 1.9259 (16)
Sr1i—O1ii 3.4812 (14) Al4—O4 1.9259 (16)
Sr1i—O1i 3.4812 (14) Al4—O4 1.9259 (16)
Sr2—O6i 2.527 (2) O1i—O4 2.712 (2)
Sr2—O6 2.527 (2) O1i—O3 2.744 (3)
Sr2—O3 2.6781 (16) O1i—O5i 2.7858 (15)
Sr2—O3 2.6781 (16) O1i—O4 2.7893 (19)
Sr2—O3 2.6781 (16) O1i—O1 2.826 (2)
Sr2—O3 2.6781 (16) O1i—O2i 2.843 (2)
Sr2—O6 3.158 (3) O1i—O6 2.8553 (15)
Sr2i—O1 3.5126 (14) O1i—O3 2.933 (2)
Sr2i—O1 3.5126 (14) O1i—O4 2.966 (2)
Sr2i—O1iii 3.5126 (14) O2i—O4 2.7685 (18) Sr2i—O1i 3.5126 (14) O2i—O3i 2.780 (3) Al1i—O4 1.7226 (15) O2i—O6i 2.796 (2) Al1i—O2i 1.7267 (15) O2i—O2 2.946 (2)
Al1i—O3 1.7595 (17) O2i—O3 2.981 (2)
Al1i—O1i 1.773 (2) O2i—O2ii 3.155 (2) Al1i—O5i 2.9537 (16) O2i—O5i 3.177 (2)
Si1i—O4 1.7226 (15) O2i—O3 3.217 (2)
Si1i—O2i 1.7267 (15) O3—O4 2.785 (2)
Si1i—O3 1.7595 (17) O3—O6 2.799 (2)
Si1i—O1i 1.773 (2) O3—O6i 3.229 (3)
Si1i—O5i 2.9537 (16) O3—O3 3.289 (2)
Al2—O2 1.7141 (17) O4—O5 2.508 (2)
Al2—O6 1.7327 (11) O4—O4 2.698 (2)
Al2—O3 1.741 (2) O4—O4 2.749 (2)
Al2—O1i 1.7587 (15) O4—O5i 2.777 (3)
Si2—O2 1.7141 (17) O4—O5 2.822 (3)
Si2—O6 1.7327 (11) O5i—O5 2.557 (3)
Si2—O3 1.741 (2) O6—O6 2.948 (3)
Si2—O1i 1.7587 (15)
O5i—Sr1i—O2ii 77.25 (5) Sr1i—O3—O3 52.50 (4) O5i—Sr1i—O2i 77.25 (5) O1—O3—O2 149.76 (7) O5i—Sr1i—O3 141.50 (3) O1—O3—O4 64.87 (6) O5i—Sr1i—O3 141.50 (3) O1—O3—O6 148.90 (8) O5i—Sr1i—O4 63.40 (6) O1—O3—O1 119.37 (7) O5i—Sr1i—O4 63.40 (6) O1—O3—O2 59.38 (6) O5i—Sr1i—O2 117.56 (5) O1—O3—O2i 56.39 (5) O5i—Sr1i—O2 117.56 (5) O1—O3—O6i 56.41 (5) O2ii—Sr1i—O2i 72.01 (5) O1—O3—O3 115.40 (7) O2ii—Sr1i—O3 73.37 (5) O2—O3—O4 99.50 (7) O2ii—Sr1i—O3 115.43 (5) O2—O3—O6 60.16 (7) O2ii—Sr1i—O4 102.23 (5) O2—O3—O1 59.71 (6) O2ii—Sr1i—O4 140.34 (4) O2—O3—O2 90.40 (7) O2ii—Sr1i—O2 112.66 (5) O2—O3—O2i 109.43 (6) O2ii—Sr1i—O2 164.89 (4) O2—O3—O6i 139.56 (7) O2i—Sr1i—O3 115.43 (5) O2—O3—O3 88.61 (6) O2i—Sr1i—O3 73.37 (5) O4—O3—O6 113.79 (6) O2i—Sr1i—O4 140.34 (4) O4—O3—O1 56.55 (5) O2i—Sr1i—O4 102.23 (5) O4—O3—O2 57.27 (5) O2i—Sr1i—O2 164.89 (4) O4—O3—O2i 106.43 (6) O2i—Sr1i—O2 112.66 (5) O4—O3—O6i 119.30 (8)
O3—Sr1i—O3 75.00 (5) O4—O3—O3 158.95 (6)
O3—Sr1i—O4 99.21 (5) O6—O3—O1 59.70 (5)
supporting information
sup-4
Acta Cryst. (2007). E63, i19–i21
O3—Sr1i—O2 55.48 (5) O6—O3—O2i 139.49 (7) O3—Sr1i—O2 91.95 (4) O6—O3—O6i 108.61 (6) O3—Sr1i—O4 137.55 (5) O6—O3—O3 54.01 (5)
O3—Sr1i—O4 99.21 (5) O1—O3—O2 97.68 (6)
O3—Sr1i—O2 91.95 (4) O1—O3—O2i 153.41 (7) O3—Sr1i—O2 55.48 (5) O1—O3—O6i 152.61 (7)
O4—Sr1i—O4 56.67 (4) O1—O3—O3 113.66 (6)
O4—Sr1i—O2 54.19 (4) O2—O3—O2i 56.60 (5) O4—Sr1i—O2 83.30 (4) O2—O3—O6i 100.74 (6)
O4—Sr1i—O2 83.30 (4) O2—O3—O3 142.69 (6)
O4—Sr1i—O2 54.19 (4) O2i—O3—O6i 51.42 (5) O2—Sr1i—O2 59.13 (4) O2i—O3—O3 88.80 (5) O6i—Sr2—O6 180.0000 O6i—O3—O3 59.38 (5) O6i—Sr2—O3 103.37 (6) Al1—O4—Al3 140.10 (9) O6i—Sr2—O3 103.37 (6) Al1—O4—Al4 115.20 (9) O6i—Sr2—O3 76.63 (5) Al1—O4—O5 155.40 (11) O6i—Sr2—O3 76.63 (5) Al1—O4—O4 126.59 (7) O6i—Sr2—O6 118.72 (7) Al1—O4—O1ii 99.91 (7) O6i—Sr2—O6 61.28 (7) Al1—O4—O4 90.67 (8) O6—Sr2—O3 76.63 (6) Al1—O4—O5i 146.98 (10)
O6—Sr2—O3 76.63 (6) Al1—O4—O1 107.50 (7)
O6—Sr2—O3 103.37 (5) Al1—O4—O5 76.88 (6)
O6—Sr2—O3 103.37 (5) Al1—O4—Sr1i 101.63 (6)
O6—Sr2—O6 61.28 (7) Al3—O4—Al4 96.43 (6)
O6—Sr2—O6 118.72 (7) Al3—O4—O5 49.53 (6)
O3—Sr2—O3 75.78 (5) Al3—O4—O4 92.75 (7)
O3—Sr2—O3 104.22 (5) Al3—O4—O1ii 45.73 (5)
O3—Sr2—O3 180.0000 Al3—O4—O4 96.31 (6)
O3—Sr2—O6 123.41 (4) Al3—O4—O2 152.06 (9)
O3—Sr2—O6 56.59 (4) Al3—O4—O5i 43.78 (5)
O3—Sr2—O3 180.0000 Al3—O4—O3 103.00 (7)
O3—Sr2—O3 104.22 (5) Al3—O4—O1 44.01 (5)
O3—Sr2—O6 123.41 (5) Al3—O4—O5 136.87 (8)
O3—Sr2—O6 56.59 (4) Al3—O4—Sr1i 90.83 (6)
O3—Sr2—O3 75.78 (5) Al3—O4—O1 137.07 (8)
O3—Sr2—O6 56.59 (4) Al4—O4—O5 47.05 (5)
O3—Sr2—O6 123.41 (4) Al4—O4—O4 45.54 (5)
O3—Sr2—O6 56.59 (4) Al4—O4—O1ii 142.15 (7)
O3—Sr2—O6 123.41 (4) Al4—O4—O4 44.46 (5)
O6—Sr2—O6 180.0000 Al4—O4—O2 107.97 (7)
O3—Al1i—O5i 161.33 (7) O5—O4—O2 150.73 (7) O1i—Al1i—O5i 66.91 (6) O5—O4—O5i 57.60 (7) O4—Si1i—O2i 106.76 (8) O5—O4—O3 143.49 (6) O4—Si1i—O3 106.23 (8) O5—O4—O1 63.19 (5) O4—Si1i—O1i 116.10 (8) O5—O4—O5 87.64 (7) O4—Si1i—O5i 68.51 (7) O5—O4—Sr1i 100.54 (7) O2i—Si1i—O3 117.52 (8) O5—O4—O1 122.97 (9) O2i—Si1i—O1i 108.66 (8) O4—O4—O1ii 121.63 (8) O2i—Si1i—O5i 80.89 (7) O4—O4—O4 90.00 (7) O3—Si1i—O1i 101.96 (8) O4—O4—O2 94.73 (6) O3—Si1i—O5i 161.33 (7) O4—O4—O5i 60.94 (5) O1i—Si1i—O5i 66.91 (6) O4—O4—O3 158.95 (7)
O2—Al2—O6 108.44 (10) O4—O4—O1 120.66 (6)
O2—Al2—O3 107.15 (8) O4—O4—O5 61.45 (5)
O2—Al2—O1i 110.13 (9) O4—O4—Sr1i 61.67 (5)
O6—Al2—O3 107.35 (10) O4—O4—O1 118.66 (7)
O6—Al2—O1i 109.73 (8) O1ii—O4—O4 126.27 (7) O3—Al2—O1i 113.87 (8) O1ii—O4—O2 108.67 (7) O2—Si2—O6 108.44 (10) O1ii—O4—O5i 60.99 (5) O2—Si2—O3 107.15 (8) O1ii—O4—O3 64.47 (6) O2—Si2—O1i 110.13 (9) O1ii—O4—O1 61.81 (6) O6—Si2—O3 107.35 (10) O1ii—O4—O5 176.70 (7) O6—Si2—O1i 109.73 (8) O1ii—O4—Sr1i 77.59 (6) O3—Si2—O1i 113.87 (8) O1ii—O4—O1 119.32 (7) O4—Al3i—O4 174.50 (8) O4—O4—O2 110.56 (7) O4—Al3i—O5i 82.31 (7) O4—O4—O5i 122.32 (7)
O4—Al3i—O5 93.56 (8) O4—O4—O3 101.88 (7)
O4—Al3i—O1 90.22 (6) O4—O4—O1 64.75 (6)
O4—Al3i—O1i 93.56 (7) O4—O4—O5 53.49 (6) O4—Al3i—O5i 93.56 (8) O4—O4—Sr1i 151.13 (7)
O4—Al3i—O5 82.31 (7) O4—O4—O1 58.28 (5)
O4—Al3i—O1 93.56 (7) O2—O4—O5i 119.82 (8) O4—Al3i—O1i 90.22 (7) O2—O4—O3 64.92 (5) O5i—Al3i—O5 83.23 (8) O2—O4—O1 143.55 (7) O5i—Al3i—O1 170.94 (7) O2—O4—O5 69.25 (6) O5i—Al3i—O1i 92.18 (7) O2—O4—Sr1i 69.45 (5)
O5—Al3i—O1 92.18 (7) O2—O4—O1 59.32 (5)
O5—Al3i—O1i 170.94 (6) O5i—O4—O3 123.15 (8) O1—Al3i—O1i 93.40 (8) O5i—O4—O1 87.66 (6)
O5—Al4—O5 180.0000 O5i—O4—O5 122.20 (6)
O5—Al4—O4 96.75 (6) O5i—O4—Sr1i 50.40 (5)
O5—Al4—O4 83.25 (6) O5i—O4—O1 179.12 (8)
O5—Al4—O4 83.25 (6) O3—O4—O1 80.32 (6)
O5—Al4—O4 96.75 (6) O3—O4—O5 112.23 (7)
O5—Al4—O4 83.25 (6) O3—O4—Sr1i 103.69 (6)
O5—Al4—O4 96.75 (6) O3—O4—O1 56.90 (6)
O5—Al4—O4 96.75 (6) O1—O4—O5 118.20 (8)
supporting information
sup-6
Acta Cryst. (2007). E63, i19–i21
O4—Al4—O4 91.09 (7) O1—O4—O1 93.21 (6)
O4—Al4—O4 180.0000 O5—O4—Sr1i 103.70 (6)
O4—Al4—O4 88.91 (7) O5—O4—O1 57.48 (5)
supporting information
sup-8
Acta Cryst. (2007). E63, i19–i21
supporting information
sup-10
Acta Cryst. (2007). E63, i19–i21
O3—O2i—O3 123.40 (7) Sr2i—O6—O3 53.79 (5) O2ii—O2i—O5i 60.23 (5) Sr2i—O6—O3 53.79 (5) O2ii—O2i—Sr1 60.43 (4) O2—O6—O2 68.68 (7) O2ii—O2i—O3 91.20 (6) O2—O6—O3 59.59 (6) O5i—O2i—Sr1 88.67 (5) O2—O6—O3 99.03 (7) O5i—O2i—O3 97.61 (7) O2—O6—O1 128.49 (8) Sr1—O2i—O3 142.87 (6) O2—O6—O1i 60.49 (5)
Al2—O3—Al1 120.08 (10) O2—O6—O6 143.09 (6)
Al2—O3—Sr2 103.07 (6) O2—O6—Sr2 111.87 (7)
Al2—O3—Sr1i 98.46 (7) O2—O6—O3 64.07 (6)
Al2—O3—O1 152.63 (8) O2—O6—O3 97.89 (9)
Al2—O3—O2 36.09 (5) O2—O6—O3 99.03 (7)
Al2—O3—O4 88.70 (7) O2—O6—O3 59.59 (6)
Al2—O3—O6 36.23 (5) O2—O6—O1 60.49 (5)
Al2—O3—O1 33.26 (5) O2—O6—O1i 128.49 (8)
Al2—O3—O2 113.20 (8) O2—O6—O6 143.09 (6)
Al2—O3—O2i 145.24 (8) O2—O6—Sr2 111.87 (7)
Al2—O3—O6i 144.59 (8) O2—O6—O3 97.89 (9)
Al2—O3—O3 86.55 (7) O2—O6—O3 64.07 (6)
Al1—O3—Sr2 114.72 (8) O3—O6—O3 71.99 (7)
Al1—O3—Sr1i 118.33 (7) O3—O6—O1 134.40 (9)
Al1—O3—O1 39.19 (6) O3—O6—O1i 62.49 (5)
Al1—O3—O2 113.19 (8) O3—O6—O6 90.57 (8)
Al1—O3—O4 36.43 (5) O3—O6—Sr2 53.02 (6)
Al1—O3—O6 150.18 (8) O3—O6—O3 108.61 (5)
Al1—O3—O1 91.28 (7) O3—O6—O3 156.61 (9)
Al1—O3—O2 30.91 (4) O3—O6—O1 62.49 (5)
Al1—O3—O2i 70.05 (6) O3—O6—O1i 134.40 (9)
Al1—O3—O6i 94.18 (8) O3—O6—O6 90.57 (8)
Al1—O3—O3 153.35 (10) O3—O6—Sr2 53.02 (6)
Sr2—O3—Sr1i 98.72 (5) O3—O6—O3 156.61 (9)
Sr2—O3—O1 80.74 (6) O3—O6—O3 108.61 (5)
Sr2—O3—O2 129.49 (7) O1—O6—O1i 162.44 (9)
Sr2—O3—O4 109.47 (6) O1—O6—O6 87.51 (5)
Sr2—O3—O6 70.39 (6) O1—O6—Sr2 94.67 (6)
Sr2—O3—O1 104.08 (5) O1—O6—O3 114.05 (9)
Sr2—O3—O2 140.07 (8) O1—O6—O3 53.19 (5)
Sr2—O3—O2i 100.99 (6) O1i—O6—O6 87.51 (5) Sr2—O3—O6i 49.58 (4) O1i—O6—Sr2 94.67 (6)
Sr2—O3—O3 52.11 (4) O1i—O6—O3 53.19 (5)
Sr1i—O3—O1 107.82 (6) O1i—O6—O3 114.05 (9) Sr1i—O3—O2 71.33 (5) O6—O6—Sr2 48.74 (6) Sr1i—O3—O4 148.55 (6) O6—O6—O3 112.69 (7)
Sr1i—O3—O6 88.25 (6) O6—O6—O3 112.69 (7)
Sr1i—O3—O2i 53.05 (4) O3—O6—O3 61.24 (6) Sr1i—O3—O6i 69.54 (5)