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A Rietveld refinement using neutron powder diffraction data of a fully deuterated topaz, Al2SiO4(OD)2

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inorganic papers

Acta Cryst.(2005). E61, i253–i255 doi:10.1107/S1600536805034811 Jianrong Chenet al. Al

2SiO4(OD)2

i253

Acta Crystallographica Section E

Structure Reports Online

ISSN 1600-5368

A Rietveld refinement using neutron powder

diffraction data of a fully deuterated topaz,

Al

2

SiO

4

(OD)

2

Jianrong Chen,a* George A. Lager,aMartin Kunz,bThomas C. Hansencand Peter Ulmerd

aDepartment of Geography and Geosciences,

University of Louisville, Kentucky 40292, USA,

bLawrence-Berkeley Laboratory, Berkeley, CA

94720, USA,cInstitut Laue–Langevin, BP 156,

F-38042 Grenoble Cedex 9, France, and

d

Laboratorium fu¨r Kristallographie, ETH Zentrum, Sonneggstrasse 5, CH-8092 Zurich, Switzerland

Correspondence e-mail: [email protected]

Key indicators

Powder neutron study T= 295 K

Mean(Al–O) = 0.003 A˚ Disorder in main residue Rfactor = 0.037 wRfactor = 0.046

Data-to-parameter ratio = 106.9

For details of how these key indicators were automatically derived from the article, see http://journals.iucr.org/e.

#2005 International Union of Crystallography

Printed in Great Britain – all rights reserved

The structure of topaz-OD, dialuminium orthosilicate di-hydroxide, Al2SiO4(OD)2, was refined in the space group

Pbnm by Rietveld analysis of constant wavelength neutron powder diffraction data. Two non-equivalent half-occupied deuterium positions were located. Each D atom is character-ized by an irregular trifurcated hydrogen-bond geometry. The refined hydrogen-bond distances are in the ranges 2.038 (5)– 2.281 (6) and 2.280 (5)–2.524 (6) A˚ for the two D atoms. Hydrogen-bond angles range from 83.6 (4) to 151.9 (4).

Results indicate that it is feasible to characterize the hydrogen bonding in small-volume samples (25 mg) synthesized at high pressure and temperature.

Comment

This study was undertaken in order to provide more reliable information on the hydrogen-bonding geometry in a fully deuterated topaz (topaz-OD) and determine the feasibility of characterizing the hydrogen bonding in small-volume samples (Chenet al., 2004). A previous X-ray single-crystal refinement showed that H atoms are located in two non-equivalent half-occupied sites, leading to the reduction of symmetry from

Pbnm to Pbn21, at least locally (Northrup et al., 1994).

However, owing to the weak X-ray scattering power of hydrogen, the H-atom positions could not be determined with a high degree of accuracy. Neutron diffraction, on the other hand, is well suited to this investigation because of the large neutron scattering length of deuterium.

Topaz-OD is an orthosilicate consisting of chains of AlO6

octahedra linked by silicate tetrahedra. D atoms reside in a cavity, lying in the (010) plane, and are disordered over four sites, which occur in pairs related by mirror symmetry (Fig. 2). The trifurcated hydrogen-bond geometry differs slightly from the previously reported arrangement (Northrupet al., 1994.). D1 is hydrogen bonded to atoms O3, O2 and O4, whereas D2 is bonded to atoms O4, O1 and O2(x + 1

2, y 1 2, z+

1 2]

(Fig. 3), in contrast to the X-ray data with hydrogen bonds to atoms O4, O1 and O2(x+1

2,y 1 2,z+

1

2] [see Fig. 2 of the

original paper by Northrup et al. (1994); note also that the H1 O3 hydrogen bond is incorrectly represented in the original Fig. 2]. The weaker hydrogen bonds are associated with D2, resulting in shorter O—D2 bond length. The refined hydrogen-bond distances are in excellent agreement with the theoretical calculation and our experimental IR spectra (Churakov & Wunder, 2004; Lageret al., 2005).

Experimental

A polycrystalline sample (25 mg) of topaz-OD was prepared from SiO2,-Al2O3and D2O at 1023 K, 7.5 GPa, for 21 h using a rocking multi-anvil press.

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Crystal data

Al2SiO4(OD)2

Mr= 182.07 Orthorhombic,Pbnm a= 4.7282 (1) A˚ b= 8.9320 (2) A˚ c= 8.4309 (2) A˚ V= 356.06 (1) A˚3

Z= 4

Dx= 3.396 Mg m

3

Neutron radiation

Wavelength of incident radiation: 1.37404 A˚

T= 295 K White

Specimen shape: cylinder 444 mm

Particle morphology: equi-dimen-sional 10mm crystals

Data collection

PSD powder diffractometer D20, at ILL

Specimen mounting: loose powder in can

Specimen mounted in reflection mode

2min= 5.0231, 2max= 154.0119

Increment in 2= 0.025

Refinement

Rp= 0.0368

Rwp= 0.0464

Rexp= 0.0353

S= 1.32

2min= 15.0175, 2max= 154.0119

Excluded region(s): <15.0/2

CW profile function number 2 with 18 terms; profile coefficients for

Simpson’s rule integration of pseudo-Voigt function (Howard, 1982; Thompsonet al., 1987). 5560 reflections

52 parameters (/)max= 0.01

Preferred orientation correction: none

Table 1

Selected geometric parameters (A˚ ,).

Al—O1 1.974 (3)

Al—O2i

1.951 (3)

Al—O3ii 1.918 (3)

Al—O3iii

1.917 (3)

Al—O4 1.829 (3)

Al—O4iv

1.825 (3)

Si—O1v

1.631 (4)

Si—O2 1.666 (4)

Si—O3 1.656 (3)

Si—O3vi

1.656 (3)

D1—O4 0.971 (5)

D2—O4 0.941 (5)

Al—O4—D1 104.0 (3)

Al—O4—D2 111.3 (4)

Alvii

—O4—D1 101.7 (4)

Alvii

—O4—D2 107.1 (4)

Symmetry codes: (i) 3 2x;y

1

2;z; (ii) 1þx;y1;z; (iii) 1x;1y;z; (iv) 1

2þx; 1

2y;z; (v)x;1þy;z; (vi)x;y; 1

2z; (vii)x 1 2;

[image:2.610.47.298.68.229.2]

1 2y;z.

Table 2

Hydrogen-bonding geometry (A˚ ,).

D—H A D—H H A D A D—H A

O4—D1 O4vii 0.971 (5) 2.253 (6) 2.614 (2) 100.7 (4) O4—D1 O2viii

0.971 (5) 2.281 (6) 2.966 (2) 126.8 (4) O4—D1 O3ix

0.971 (5) 2.038 (5) 2.930 (2) 151.9 (4) O4—D2 O1 0.941 (5) 2.524 (6) 2.593 (2) 83.6 (4) O4—D2 O2viii

0.941 (5) 2.363 (6) 2.966 (2) 121.6 (4) O4—D2 O4vi

0.941 (5) 2.280 (5) 3.101 (2) 145.3 (4)

Symmetry codes: (vi) x;y;1

2z; (vii) x 1 2;

1

2y;z; (viii) 1 2x;y

1 2;

1 2z; (ix) x;y1;z.

Constant wavelength (CW) neutron diffraction data were collected for about 2 h on the D20 powder diffractometer at Institut Laue—Langevin, Grenoble, France. The 25 mg sample was contained in a vanadium can. Data were analysed by the Rietveld method using the programGSAS(Larson & Von Dreele, 2000). Neutron scattering lengths of 0.3349, 0.4149, 0.5803 and 0.66711012cm for Al, Si, O and D, respectively, were used (Rauch & Waschowski, 2003). The structure of topaz–OH (Northrup et al., 1994) was used as a trial model. Refinements were carried out in space groups Pbnm and

Pbn21. However, the refinement in Pbn21 did not converge,

inorganic papers

i254

Jianrong Chenet al. Al

[image:2.610.89.250.287.492.2]

2SiO4(OD)2 Acta Cryst.(2005). E61, i253–i255

Figure 3

(010) projection of the topaz-OD structure, showing the trifurcated hydrogen-bond arrangement.

Figure 1

Observed, calculated and difference neutron powder diffraction profiles for topaz-OD. Tick marks below the profile indicate the allowed Bragg reflections.

Figure 2

[image:2.610.316.565.534.607.2] [image:2.610.92.245.547.718.2]
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suggesting that the powder data cannot be used to resolve the possible symmetry reduction. Refined occupancies of D1 and D2 were within one s.u. of 0.5 and were fixed to this value in subsequent refinements. The 52 parameters in the refinement comprised a scale factor, six profile coefficients (Thompson–Cox–Hastings pseudo-Voigt function), 12 background coefficients (shifted Chebyshev function), the zero error, the unit-cell parameters, the atomic posi-tional parameters and isotropic displacement parameters.

Data collection:MAD(local program in D20 diffractometer); cell refinement: GSAS (Larson & Von Dreele, 2000); data reduction:

LAMP (Richardet al., 2004); program(s) used to refine structure:

GSAS; molecular graphics: DIAMOND(Brandenburg, 2005); soft-ware used to prepare material for publication: GSAS; program(s) used to solve structure: used coordinates from X-ray work.

This research was supported by the National Science Foundation through grant No. EAR-0337534.

References

Brandenburg, K. (2005).DIAMOND.Demo Version 3.0. Crystal Impact GbR, Bonn, Germany.

Chen, J. R., Lager, G. A., Kunz, M., Ulmer, P. & Hansen, T. (2004).Eos Trans. AGU, Vol. 85, No. 47.

Churakov, S. V. & Wunder, B. (2004).Phys Chem Miner.31, 131–141. Howard, C. J. (1982).J. Appl. Cryst.15, 615–620.

Lager, G. A., Chen, J. R., Liu, Z. X., Hu, J. Z. & Ulmer, P. (2005). GSAAbstr. Prog.Vol. 37, No. 7.

Larson, A. C. & Von Dreele, R. B. (2000).GSAS.Report No. LAUR 86–748. Los Alamos National Laboratory, New Mexico, USA.

Northrup, P. A., Leinenweber, K. & Parize, J. B. (1994).Am. Mineral.79, 401– 404.

Rauch, H. & Waschowski, W. (2003).Neutron Data Booklet, edited by A.-J. Dianoux & G. Lander. Philadelphia: Old City Publishing.

Richard, D., Ferrand, M. & Kearley, G. J. (2004).LAMP. Institut Laue-Langevin, Grenoble, France.

Thompson, P., Cox, D. E. & Hastings, J. B. (1987).J. Appl. Cryst.20, 79– 83.

inorganic papers

Acta Cryst.(2005). E61, i253–i255 Jianrong Chenet al. Al

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supporting information

sup-1

Acta Cryst. (2005). E61, i253–i255

supporting information

Acta Cryst. (2005). E61, i253–i255 [https://doi.org/10.1107/S1600536805034811]

A Rietveld refinement using neutron powder diffraction data of a fully

deuterated topaz, Al2SiO4(OD)2

Jianrong Chen, George A. Lager, Martin Kunz, Thomas C. Hansen and Peter Ulmer

Dialuminium orthosilicate dihydroxide

Crystal data

Al2SiO4(OD)2 Mr = 182.07

Orthorhombic, Pbnm a = 4.7282 (1) Å b = 8.9320 (2) Å c = 8.4309 (2) Å V = 356.06 (1) Å3 Z = 4

Dx = 3.396 Mg m−3

Neutron radiation, λ = 1.37404 Å T = 295 K

Particle morphology: equii-dimensional 10µm crystals

white

cylinder, 4 × 4 mm

Data collection

The PSD powder

diffractometer D20, at ILL Germanium monochromator

Specimen mounting: loose powder in can

Data collection mode: reflection Scan method: step

2θmin = 15.018°, 2θmax = 154.012°, 2θstep = 0.025°

Refinement

Least-squares matrix: full Rp = 0.037

Rwp = 0.046 Rexp = 0.035 R(F2) = 0.07382 5960 data points

Excluded region(s): <15.0 °/2θ

Profile function: CW Profile function number 2 with 18 terms Profile coefficients for Simpson's rule integration of pseudovoigt function (Howard, 1982; Thompson et al., 1987). #1(GU) = 217.007 #2(GV) = -511.054 #3(GW) = 407.749 #4(LX) = 2.951 #5(LY) = 0.000 #6(trns) = 7.080 #7(asym) = 18.0696 #8(shft) = 0.0000 #9(GP) = 0.000 #10(stec)= 0.00 #11(ptec)= 0.00 #12(sfec)= 0.00 #13(L11) = 0.000 #14(L22) = 0.000 #15(L33) = 0.000 #16(L12) = 0.000 #17(L13) = 0.000 #18(L23) = 0.000 Peak tails are ignored where the intensity is below 0.0010 times the peak Aniso.

broadening axis 0.0 0.0 1.0 52 parameters

0 restraints 0 constraints

(Δ/σ)max = 0.01

Background function: GSAS Background function number 1 with 12 terms. Shifted Chebyshev function of 1st kind 1: 15.5910 2: -1.30168 3: 1.59919 4: 1.754620E-02 5: -0.429047 6: -0.549426 7: 0.155696 8: 2.576300E-02 9: 0.372468 10: -0.107973 11: -0.172470 12: -0.149335

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supporting information

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Acta Cryst. (2005). E61, i253–i255

Fractional atomic coordinates and isotropic or equivalent isotropic displacement parameters (Å2)

x y z Uiso*/Ueq Occ. (<1)

Al 0.9071 (6) 0.1325 (3) 0.0779 (3) 0.0030 (4)

Si 0.4032 (6) 0.9404 (3) 0.25 0.0002 (5)

O1 0.7080 (5) 0.0260 (2) 0.25 0.0015 (4)

O2 0.4431 (4) 0.7551 (3) 0.25 0.0017 (5)

O3 0.2129 (3) 0.9922 (2) 0.0946 (2) 0.0031 (3)

O4 0.5917 (3) 0.2504 (2) 0.0661 (2) 0.0048 (3)

D1 0.440 (1) 0.1858 (5) 0.1031 (8) 0.045 (1) 0.5

D2 0.532 (1) 0.2811 (7) 0.1675 (6) 0.048 (1) 0.5

Geometric parameters (Å, º)

Al—O1 1.974 (3) Si—O1v 1.631 (4)

Al—O2i 1.951 (3) Si—O2 1.666 (4)

Al—O3ii 1.918 (3) Si—O3 1.656 (3)

Al—O3iii 1.917 (3) Si—O3vi 1.656 (3)

Al—O4 1.829 (3) D1—O4 0.971 (5)

Al—O4iv 1.825 (3) D2—O4 0.941 (5)

Al—O4—D1 104.0 (3) Alvii—O4—D1 101.7 (4)

Al—O4—D2 111.3 (4) Alvii—O4—D2 107.1 (4)

Symmetry codes: (i) −x+3/2, y−1/2, z; (ii) x+1, y−1, z; (iii) −x+1, −y+1, −z; (iv) x+1/2, −y+1/2, −z; (v) x, y+1, z; (vi) x, y, −z+1/2; (vii) x−1/2, −y+1/2, −z.

Hydrogen-bond geometry (Å, º)

D—H···A D—H H···A D···A D—H···A

O4—D1···O4vii 0.97 (1) 2.25 (1) 2.614 (2) 101 (1)

O4—D1···O2viii 0.97 (1) 2.28 (1) 2.966 (2) 127 (1)

O4—D1···O3ix 0.97 (1) 2.04 (1) 2.930 (2) 152 (1)

O4—D2···O1 0.94 (1) 2.52 (1) 2.593 (2) 84 (1)

O4—D2···O2viii 0.94 (1) 2.36 (1) 2.966 (2) 122 (1)

O4—D2···O4vi 0.94 (1) 2.28 (1) 3.101 (2) 145 (1)

Figure

Figure 1Observed, calculated and difference neutron powder diffraction profilesfor topaz-OD

References

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