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ISSN: 2052-5206

X-ray structure of barium titanate – missed ­opportunities

aSchool of Physics, Madurai Kamaraj University, Madurai 625021, India
*Correspondence e-mail: [email protected]

(Received 21 June 2000; accepted 11 July 2000)

Anomalous X-ray scattering effects are quite extensive in the noncentrosymmetric ferroelectric structure of barium titanate, and typical estimates for three published X-ray diffraction experiments are computed. These data show that the Bijvoet pairs should not be averaged before least-squares refinement for this polar crystal with small atomic displacements from a higher symmetric space group.

In the tetragonal ferroelectric structure of barium titanate, the heavy atoms have the dispersive components fBa = −0.613, f′′Ba = 2.28, fTi =0.28 and f′′Ti = 0.446 (International Tables for X-­ray ­Crystallography, 1974) for Mo KMathematical equation X-rays used in three extensive structure analyses, namely Evans (1961[Evans, H. J. Jr (1961). Acta Cryst. 14, 1019-1026.]), Harada et al. (1970[Harada, J., Pederson, T. & Barnea, Z. (1970). Acta Cryst. A26, 336-344.]; HPB) and recently Buttner & Maslen (1992[Buttner, R. H. & Maslen, E. N. (1992). Acta Cryst. B48, 764-769.]; BM). For the point group 4mm, any reflection with l Mathematical equation 0 can exhibit a Bijvoet difference Mathematical equation = 0.5(IMathematical equation )/(I + Mathematical equation) between the intensities of inverse reflections.

In Table 1[link], our estimated dispersive effects for a few reflections are displayed for the above three reported structures. The structure magnitudes |F+|, |F|, the phase angles Mathematical equation+, Mathematical equation and the Mathematical equation values are listed along with |Fc| and Mathematical equation(Fo), as reported by the above three authors. Mathematical equation(Mathematical equation) can be up to four times larger than Mathematical equation(Fo) and therefore such dispersive scattering estimates should have been measurable.

Table 1
Our dispersion estimates for the three experiments

aOur dispersion estimates (Chandrasekaran & Mohanlal, 1965) applying an average isotropic Debye–Waller term, exp(−2Bsin2Mathematical equation/Mathematical equation2) for the intensities. See text. bEstimates for ambient room temperature.

  Evans (1961[Evans, H. J. Jr (1961). Acta Cryst. 14, 1019-1026.] Our dispersion estimates (1965)a HPB(1970) Our dispersionestimates for HPBb BM (1992) Our dispersion estimatesb for BM (1992)
hkl |Fc|;Mathematical equation(Fo) Mathematical equation% |Fc| |F+| |F−| Mathematical equation% |Fc|;Mathematical equation(Fo) |F+| |F−| Mathematical equation% Mathematical equation+ Mathematical equation
000 102 101.6 101.6 101.6 102 101.6 101.6    
003 21;0.32 8.4 N.M. 19.2 18.5 −7.4 19.1;0.06 17.6 18.4 8.9 13.9 −3.3
005 15.5;0.26 10.3 14.8 14.7 13.7 −13.8 13.8;0.1 11.9 13 17.6 18.9 −5.9
007 11.2;0.1 16 10.3 10.5 9.2 −25.9 9.2;0.13 7 8.3 34.5 25.7 −9.2
009 8.1;0.11 21.7 7.9 8.1 6.7 −36.8 N.M. 4.3 5.6 50 29.4 −10.2
207 10.4;0.07 15.1 9.9 9.9 8.6 −27.7 9;0.08 6.6 7.9 26.2 25.8 −8.8
307 18;0.05 16.7 17.9 16.7 18 15.4 14.8;0.27 13 11.6 −22.4 −7.2 20.3
407 9.3;0.09 17 8.2 8.4 7.1 −32.7 7.7;0.09 5.7 6.8 36.4 25.8 1.3
507 15;0.09 18.6 N.M. 13.7 15 17.6 11.9;0.27 10 8.9 −25.3 −6.1 20.4
108 18.2;0.06 0.55 9.7 9.9 8.8 −22.9 7.7;0.09 5.5 6.8 42 33.3 −16.2
208 17.4;0.1 1.08 17.3 18.1 18.7 5.7 14.8;0.2 14 13.3 −9.7 −1.4 13.6
308 9;0.08 0.66 8.2 8.9 7.9 −25.1 7.1;0.09 5.1 6.3 42 32.5 −14.7
408 15.2;0.08 1.28 15 15.9 16.4 6.5 N.M. 12.1 11.5 −10 −0.4 13.5
†N.M. – Not measured.

We have in fact computed the |F+|, |F| and Mathematical equation values at ambient temperature for all reflections up to Mathematical equation Å−1 for the BM (1992) structure. The trends are summarized in Table 2[link].

Table 2
Summary of compound dispersion values for ­reflections with sinMathematical equation/Mathematical equation Mathematical equation 1.4 Å−1

Description No. of reflections
Total up to 1.5 Å−1 for Mo KMathematical equation 912
With l = 0 index 112
With l Mathematical equation 0 and |F| Mathematical equation 4 electrons 735
|Mathematical equation| Mathematical equation 20% 268 (+ve = 181, −ve = 87)
|Mathematical equation| Mathematical equation 10% 187 (+ve = 94, −ve = 93)
|Mathematical equation| Mathematical equation 5% 145 (+ve = 68, −ve = 77)
|Mathematical equation| Mathematical equation 5% 312 (+ve = 108, −ve = 204)
Thus, the dispersive scattering effects are quite ­appreciable for a large number of reflections, with both positive and negative signs for Mathematical equation (negative, −ve for I Mathematical equation Mathematical equation).

Evans (1961[Evans, H. J. Jr (1961). Acta Cryst. 14, 1019-1026.]) measured approximately 350 h0l reflections using a Geiger counter fitted to a Weissenberg instrument and Mo KMathematical equation X-rays up to Mathematical equation Å−1. He reported an `impasse' in the structure determination, even with residuals as low as 0.03, owing to parameter interaction in the least-squares refinements with such a polar space group deviating by small atomic displacements from a higher symmetric space group. In a discussion we pointed out (Chandrasekaran & Mohanlal, 1965[Chandrasekaran, K. S. & Mohanlal, S. K. (1965). Acta Cryst. 19, 853.]) our estimates of the very appreciable Mathematical equation values for a large number of reflections. In a rejoinder Evans (1966[Evans, H. J. Jr (1966). Acta Cryst. 21, 182.]) stated that his raw expermental data for h0l, Mathematical equation 0l and h0Mathematical equation , Mathematical equation0Mathematical equation had not shown any such differences, which he attri­buted to `antiparallel twinning', with l+ and l intensities tending to average out. In HPB (1970) a single C domain crystal was used for the X-ray studies; dispersive scattering effects were noticed in that only the refinements using an l index of positive sign yielded the best standard errors for the parameters with low residuals.

BM (1992) recorded two independent sets of measurements on the same sample with Mathematical equation3500 data in each set, up to 1.08 Å−1 for Mo KMathematical equation. They stated that `Friedel pairs were averaged and merged even in case 3 (the correct noncentrosymmetric P4mm structure), because the effects of anomalous dispersion are very small (Buerger, 1960[Buerger, M. J. (1960). Crystal Structure Analysis. New York: John Wiley.])'. It is not clear to us from this quote whether they had sought to measure Bijvoet differences at all in their experiment or merely cited the text (Buerger, 1960[Buerger, M. J. (1960). Crystal Structure Analysis. New York: John Wiley.]) to justify their merging and averaging of the Friedel pairs. Also, BM (1992) had probably taken the magnitudes |f + f′ + if′′| for the atomic scattering factors, which procedure would eliminate any Mathematical equation values in the structure-factor calculations and, in addition, lead to large errors in the structure-factor magnitudes and phases. Furthermore, Buerger (1960[Buerger, M. J. (1960). Crystal Structure Analysis. New York: John Wiley.]) devotes four pages to anomalous scattering, with Argand diagrams for F+ and F, a table for f′ and f′′ for different targets and several examples of the actual experimental measurement of Bijvoet differences.

The least-squares and Fourier procedures for noncentrosymmetric structures with appreciable dispersive scattering have been extensively discussed in a previous review ­(Srinivasan, 1972[Srinivasan, R. (1972). Advances in Structure Research by Diffraction Methods, edited by W. Hoppe & R. Mason, pp. 105-197. Oxford: Pergamon Press.]) and an International Conference Report (Ramaseshan & Abrahams, 1974[Ramaseshan, S. & Abrahams, S. C. (1974). Anomalous Scattering Proc. Int. Congress Conference, Madrid. Copenhagen: Munksgaard.]). Here, therefore, we only cite Ibers & Hamilton (1964[Ibers, J. A. & Hamilton, W. C. (1964). Acta Cryst. 17, 781.]), who recommend that Friedel pairs should be treated independently in the least squares, using the actual observed values and corresponding calculated values |F+(H)| and |F(H)|. For the effects of domains in BaTiO3, tending to average out l+ and l intensities, the Flack ­enantiopole parameter (Flack, 1983[Flack, H. (1983). Acta Cryst. A39, 876-881.]), namely |F(Mathematical equation)|2 = (1 − x) |F(h)|2 + x|F(−h)|2, is called for to account for the intensities, with x as a parameter for refinement.

Footnotes

Present address: The Madura College, Madurai 615011, Tamil Nadu, India.

Acknowledgements

One of us (KSC) wishes to dedicate this work to the memory of the late Professor M. Buerger, with whom he had a pleasant personal acquaintance and another (RS) acknowledges the CSIR for financial assistance.

References

First citationBuerger, M. J. (1960). Crystal Structure Analysis. New York: John Wiley.  Google Scholar
First citationButtner, R. H. & Maslen, E. N. (1992). Acta Cryst. B48, 764–769.  CrossRef CAS Web of Science IUCr Journals Google Scholar
First citationChandrasekaran, K. S. & Mohanlal, S. K. (1965). Acta Cryst. 19, 853.  CrossRef IUCr Journals Web of Science Google Scholar
First citationEvans, H. J. Jr (1961). Acta Cryst. 14, 1019–1026.  CrossRef CAS IUCr Journals Web of Science Google Scholar
First citationEvans, H. J. Jr (1966). Acta Cryst. 21, 182.  CrossRef IUCr Journals Web of Science Google Scholar
First citationFlack, H. (1983). Acta Cryst. A39, 876–881.  CrossRef CAS Web of Science IUCr Journals Google Scholar
First citationHarada, J., Pederson, T. & Barnea, Z. (1970). Acta Cryst. A26, 336–344.  CrossRef CAS IUCr Journals Web of Science Google Scholar
First citationIbers, J. A. & Hamilton, W. C. (1964). Acta Cryst. 17, 781.  CrossRef IUCr Journals Web of Science Google Scholar
First citationRamaseshan, S. & Abrahams, S. C. (1974). Anomalous Scattering Proc. Int. Congress Conference, Madrid. Copenhagen: Munksgaard.  Google Scholar
First citationSrinivasan, R. (1972). Advances in Structure Research by Diffraction Methods, edited by W. Hoppe & R. Mason, pp. 105–197. Oxford: Pergamon Press.  Google Scholar

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