research papers
Point-defect-induced forbidden reflections in resonant X-ray scattering†
aA. V. Shubnikov Institute of Crystallography, 119333 Moscow, Russia, and bPhysical Department of Moscow State University, 119899 Moscow, Russia
*Correspondence e-mail: eno@simmetry.phys.msu.ru
Point defects in crystals cause displacements of neighbouring atoms and hence become the source of an additional anisotropy of the X-ray
amplitude. This anisotropy can induce `forbidden' Bragg reflections near absorption edges, called point-defect-induced (PDI) reflections, which are absent in non-resonant X-ray scattering and in resonant X-ray scattering by perfect crystals. The deformation of external electron shells is the physical reason for this phenomenon. Some examples of crystals are considered in which the PDI reflections could be observed.Keywords: resonant X-ray diffraction; forbidden reflections; point defects.
1. Introduction
In resonant X-ray diffraction, forbidden Bragg reflections can occur near absorption edges owing to the anisotropy of X-ray susceptibility, induced by an asymmetric environment of resonant atoms (Templeton & Templeton, 1980; Dmitrienko, 1983, 1984). The asymmetric environment disturbs the valence electronic shells of atoms and causes the mentioned anisotropy. The asymmetry of a local atomic position can be an intrinsic property of a crystal, or it can be induced by different factors like magnetic interactions, thermal vibrations, point defects etc. Thus the forbidden reflections provide a tool for studying distortions in electronic states induced by different anisotropic factors.
The physical reason behind the forbidden reflections is that just near absorption edges the fij, depending on the symmetry of the resonant atom site (Dmitrienko, 1983; Blume, 1994). Under non-resonant conditions, at X-ray wavelengths far from absorption edges, these reflections are strictly forbidden by the extinction rules corresponding to screw axes and glide planes (Hahn, 1996). Therefore synchrotron radiation is needed to observe them. The dipole transition E1 usually provides the main contribution to the [see the review by Hodeau et al. (2001)]. Sometimes, however, the dipole resonant transition does not violate the extinction rules. Then, forbidden reflections can appear owing to the dipole–quadrupole (Templeton & Templeton, 1994), quadrupole (Finkelstein et al., 1992) transitions, thermal vibrations, point defects (Dmitrienko, Ovchinnikova & Ishida, 1999; Dmitrienko & Ovchinnikova, 2000) or by local of atomic positions (Dmitrienko & Ovchinnikova, 2001).
becomes a tensorUp to now, forbidden Bragg reflections, caused exclusively by the natural asymmetry of local atomic positions, have been studied in many crystals (see, for example, Templeton & Templeton, 1985; Finkelstein et al., 1992; Templeton, 1994; Kirfel et al., 1995; Nagano et al., 1996; Kokubun et al., 1998; Hagiwara et al., 1999; Garcia et al., 2000; Collins et al., 2001).
A survey of earlier works on the subject was given by Belyakov & Dmitrienko (1989). Magnetic reflections were also justified theoretically and observed experimentally (Blume, 1985; Hannon et al., 1988; Gibbs et al., 1985). Recently, forbidden reflections that appear due to thermal vibrations were observed in a wide temperature interval (Kokubun et al., 2001; Kirfel et al., 2002)
In the present paper we consider some details concerning point-defect-induced (PDI) reflections, which are absent in perfect crystals, and describe new structures suitable for experimental observation.
2. Resonant X-ray scattering by crystals with point defects
The influence of point defects on the X-ray diffraction pattern far from absorption edges was studied in detail a long time ago (Krivoglaz, 1983). Those defects, together with accompanying atomic displacements, cause the appearance of diffuse scattering and influence the position and intensity of the structural peaks.
Below we consider a special case of point defects: namely the impurities, which substitute the host atoms without violation of the local ), minimal concentrations of the impurities necessary to provide sufficient intensities of the forbidden reflections should be about 0.01–0.001, depending on the considered.
We also suppose that the concentration of defects is small, so that they do not influence each other. According to our evaluations (Dmitrienko & Ovchinnikova, 2000The atomic displacements caused by defects violate the ). We see that if the defect appears in the closest neighbourhood of the sth atom it changes its and influences the atomic factor fijs (s enumerates atoms inside one crystallographic position). The resonant corresponding to the diffraction vector H is equal to
of each neighbouring atom (Fig. 1In the absence of the defects, fij s is invariant under the transformations, where is an element of the G s describing the symmetry of the sth atomic site, = , = , l = , enumerates atoms around the considered one. Hence we write fijs = .
In the presence of the defect we have = , = , = , where is the displacement of the lth atom owing to the th impurity. The scattering amplitude of the sth resonant atom becomes equal to
where the first term is invariant over the Gl group, and tensor describes the additional contribution of the defect to the amplitude compared with the perfect crystal. Tensor is invariant under the of the G s which corresponds to the direction between the resonant atom and the impurity . Supposing that the displacements of all atoms is small, we can write the following expression for the tensor describing the PDI reflections (hence we suppose that the contribution of fijs is zero),
where gijn = . It is easy to see that the term is invariant under the Gl symmetry group; hence it gives no contribution to the discussed reflections. The main contribution from the point defects to the forbidden reflection in the dipole resonant transition can be written as
Below we shall consider several structures which allow the appearance of forbidden reflections of this type.
3. Crystals with Fd3¯m symmetry
Some examples of the structures with space symmetry (impurities in Ge and intermetallides with C-15 structure RFe2), which allow the existence of PDI reflections, were discussed previously (Dmitrienko & Ovchinnikova, 2000). Let us consider the forbidden reflections 0kl, k+l = 4n+2, in the Ge crystal where atoms with different orientations, 1 and 2, are in the (000) and positions, respectively. The corresponding is equal to F(0kl,k+l = 4n+2) = 4( f1-f2). Taking into account that these atoms are connected by inversion, we can write f 01 = f 02, fij1 = fij2, fijk1 = -fijk2, = . The impurity substitutes the Ge atoms and the neighbouring atoms are displaced along the directions. In this case the gij tensors are invariant under the group 3m and they are characterized by two eigenvalues g1 and g2. We obtain that the contribution, induced by the defects to the is equal to
where Cimp is the impurity concentration. This expression coincides with that given in our previous paper (Dmitrienko & Ovchinnikova, 2000) if the displacements are small.
4. Forbidden reflections in A-15 intermetallides
Intermetallides with A-15 structure are described by the A3B (Nb3Ge, V3Co etc.). B-type atoms are in the 2(a) position with symmetry; A-type atoms occupy the 6(d) position with symmetry.
and correspond to the chemical formulaNo forbidden reflections appear in the dipole transition near the B atom because its is cubic, . Point defects cannot induce any reflection, because all tensors in equation (3) vanish after averaging over the point-defect positions. Thus, in the considered approximation there are no PDI reflections near the of the B atom.
of theNear the A atom we can find the following forbidden reflections, induced by the dipole resonant transition: hkl with h+k+l = 2n+1 excepting h = 2n+1, k = 4n, l = 4n+2 (they are allowed) and h = 2n+1, k = , l = . For these reflections the is equal to
of thewhere atoms are enumerated in correspondence with the International Tables for Crystallography (Hahn, 1996). Odd and even atoms are connected by inversion, hence for the dipole transition f2n = f2n+1 and the reflection vanishes.
Let us suppose that there are impurities in the B position. They provide a correction to the tensor scattering amplitudes and the displacements of the A atoms in the first coordination sphere. For example, the impurity at the (000) point causes the appearance of the tensor factor on the third atom in the position and a corresponding displacement towards the point (000). Because these two atoms are in the mirror plane my, = (ux, 0,uz), is invariant over the group my. For each atom we must average the term over all possible positions of impurity around the sth atom (i.e. over the group ). After the summation over all atoms inside the position 6(d), the tensor of the forbidden reflection is equal to
where g11 = gyy-gxx. This reflection is forbidden far from the of an A element and in the dipole transition, but it is allowed for the dipole–quadrupole scattering. In the latter case, without any impurities, the tensor can be calculated as = , where fijks and fijka are the symmetric and antisymmetric parts of the third-rank tensor invariant over the = . According to the tables of Sirotin & Shaskolskaya (1975), fijks has two independent components and fijka has one component. Hence the dipole–quadrupole transition gives the following contribution to the considered reflections,
We see that the tensor structure of the PDI contribution (7) takes the same form as the symmetric part of the dipole–quadrupole contribution (8). This is rather obvious, because the transformation properties of the production ukfij are similar to the properties of a third-rank tensor. To separate the PDI contribution we would have to measure the dependence of the PDI forbidden reflections on the impurities concentration.
5. Crystals with Ia3¯d symmetry
In this section we consider ferrites with the garnet structure, which are widely used in magnetic devices because of their useful magnetic properties. It is known that the substitution of Fe atoms or rare-earth atoms essentially influences the magnetic properties of these structures (Smit & Wijn, 1959). The study of forbidden reflections induced by impurities provides information about the influence of defects on the valence electron states, which can be useful for the description of the magnetic properties.
Below we shall consider as an example the yttrium–iron garnet (YIG; Y3Fe5O12). In the pure YIG, magnetic ions Fe3+ occupy two sites: octahedral, 16(a), with and tetrahedral, 24(d), with symmetry. Y3+ ions occupy the 24(c) position with 222 O atoms are in 96(e) positions.
In the dipole resonant transition near the K-edge of Fe (7.1 keV), forbidden reflections can occur, which are induced separately by the 16(a) and 24(d) positions of iron. Near the of yttrium (the K-edge, 17.04 keV) we can find forbidden refections induced by yttrium in the 24(c) position. The 16(a) position provides the following set of forbidden reflections: h = 2n+1, k = , l = 0 and h = k = 2n+1, l = (plus permutations), for example, 110. The 24(d) and 24(c) sites yield forbidden reflections with h = k = 4n, l = (for example, 002). We can also find reflections which are forbidden for one of the positions and allowed for another. For example, h = 2n+1, k = , h+k+l = 4n reflections are allowed for the 24(d) position and forbidden for 16(a). The reflections h = k = 4n+2, l = still remain forbidden for both positions.
All these reflections occur exclusively owing to anisotropy induced by asymmetric atomic environment. Purely magnetic reflections are absent, because the magnetic moments inside each position are parallel. Forbidden reflections similar to the considered ones have been studied theoretically and observed experimentally in Mössbauer nuclear diffraction (Winkler et al., 1983; Rüffer et al., 1989).
Let us suppose that Me3+ ions are substituted for Fe ions. They can both be in the 16(a) and 24(d) positions. Then the 110 and 200 reflections will appear near the absorption edges of both Fe and Me. In the garnets, where yttrium atoms are substituted by atoms of another element M, the 002 reflection can be observed near the absorption edges of yttrium and M, but the 110 reflection remains forbidden.
Let us consider the hkl reflections with h = k = 4n+2, l = near the absorption edges of iron. For clarity we shall perform all the calculations for the 226 reflection. The 16(a) position of iron will not contribute to the forbidden reflection because its forbids the existence of both the symmetric and antisymmetric parts of a third-rank tensor. The symmetry of the 24(d) position allows the symmetric third-rank tensor with four independent components. The calculation similar to that made above for the group shows that Fe atoms of the 24(d) position give the following contribution to the forbidden reflection,
where gxy = gyzuy+gxzux, gxz = gxzux+3gyzuy, gyz = 3gxzux+gyzuy. Similarly we can show that the 24(d) Fe position in the presence of defects will contribute to the reflections corresponding to the 16(a) position in the absence of defects, for example, into the 110 reflection. PDI forbidden reflections 110 can also appear near the of yttrium. However, the term iHkuk gij cannot explain the appearance of the PDI forbidden reflections from the 16(a) position to the reflections 002. Atoms of the 16(a) position also cannot induce forbidden reflections in a perfect crystal owing to the dipole–quadrupole resonant transition or the thermal vibrations. Nevertheless, the contribution from the 16(a) position was observed in the purely nuclear 002 reflection in the Mössbauer diffraction pattern (Labushkin et al., 1995). To explain this we have to take into account the magnetic structure of YIG. The experiment was carried out at room temperature, and the magnetic moments in the single-crystal film of YIG were aligned along the [001] direction. Because the magnetic moments are time-reversible but not space-reversible, they violate the of atomic sites. In the case of the 16(a) position, the magnetic interaction violates the As a result, effects induced by the third-rank tensors can appear.
It follows from the above consideration that the forbidden reflections near the absorption edges of Fe, Y, M and Me would allow the concentrations of M and Me atoms to be found in all crystallographic positions and the displacements and the distortions of electronic states of the atoms to be studied.
6. Conclusions
Point defects violate the
of atomic environments and provide an additional anisotropy of This anisotropy, together with the defect-induced atomic displacements, causes the appearance of forbidden reflections, which are absent far from absorption edges and in perfect crystals. Of course, the discussed PDI reflections can, but not necessarily will, be observed and their experimental observation is a challenge for the future. To meet this challenge, the use of synchrotron radiation is certainly indispensable.Various crystals, considered in the present paper, provide examples of structures which allow the appearance of forbidden reflections of this type. It was shown that such reflections are accompanied by the contributions from a dipole–quadrupole resonant transition and from thermal vibrations. These contributions can be separated because only the PDI forbidden reflections depend on the defect concentration. Note that point defects can also create some corrections to the vibration modes, because a local vibration mode can occur. This may be essential for the study of thermal-motion-induced reflections near the
of the impurity.Sometimes the study of the PDI forbidden reflections can allow the concentration of impurities to be measured in different crystallographic positions. Such a situation exists in garnets with symmetry, where different forbidden reflections originate from different iron positions.
Footnotes
†Presented at the `XIV Russian Synchrotron Radiation Conference SR2002', held at Novosibirsk, Russia, on 15–19 July 2002.
Acknowledgements
This work is partly supported by the grant INTAS 01-0822. The authors are grateful to the organizers of SR2002 for financial support.
References
Belyakov, V. A. & Dmitrienko, V. E. (1989). Sov. Phys. Usp. 32, 697–719. CrossRef Google Scholar
Blume, M. (1985). J. Appl. Phys. 57, 3615–3618. CrossRef CAS Web of Science Google Scholar
Blume, M. (1994). Resonant Anomalous X-ray Scattering, edited by G. Materlik, C. J. Spark & K. Fisher, pp. 495–515. Amsterdam: North-Holland. Google Scholar
Collins, S. P., Laundy, D. & Stunault, A. (2001). J. Phys. Condens. Matter, 13, 1891–1905. Web of Science CrossRef CAS Google Scholar
Dmitrienko, V. E. (1983). Acta Cryst. A39, 29–37. CrossRef CAS Web of Science IUCr Journals Google Scholar
Dmitrienko, V. E. (1984). Acta Cryst. A40, 89–95. CSD CrossRef CAS Web of Science IUCr Journals Google Scholar
Dmitrienko, V. E. & Ovchinnikova, E. N. (2000). Acta Cryst. A56, 340–347. Web of Science CrossRef CAS IUCr Journals Google Scholar
Dmitrienko, V. E. & Ovchinnikova, E. N. (2001). Acta Cryst. A57, 642–648. Web of Science CrossRef CAS IUCr Journals Google Scholar
Dmitrienko, V. E., Ovchinnikova, E. N. & Ishida, K. (1999). Pis'ma Zh. Eksp. Teor. Fiz. 50, 153–156; JETP Lett. 50, 171–174 (English translation). Google Scholar
Finkelstein, K. D., Shen, Q. & Shastri, S. (1992). Phys. Rev. Lett. 69, 1612–1615. CrossRef PubMed CAS Web of Science Google Scholar
Garcia, J., Subias, G., Proietti, M. G., Renirier, H., Joly, Y., Hodeau, J. L., Blasco, J., Sanchez, M. C. & Berar, J. F. (2000). Phys. Rev. Lett. 85, 578–581. Web of Science CrossRef PubMed CAS Google Scholar
Gibbs, D., Moncton, D. E. & D'Amico, K. L. (1985). J. Appl. Phys. 57, 3619–3622. CrossRef CAS Web of Science Google Scholar
Hagiwara, K., Kanazawa, M., Horie, K., Kokubun, J. & Ishida, K. (1999). J. Phys. Soc. Jpn, 68, 1592–1597. Web of Science CrossRef CAS Google Scholar
Hahn, T. (1996). Editor. International Tables for Crystallography, Vol. A. Dordrecht: Kluwer. Google Scholar
Hannon, J. P., Trammell, G. T., Blume, M. & Gibbs, D. (1988). Phys. Rev. Lett. 61, 1245–1248. CrossRef PubMed CAS Web of Science Google Scholar
Hodeau, J.-L., Favre-Nicolin, V., Bos, S., Renivier, H., Lorenzo, E. & Berar, J.-F. (2001). Chem. Rev. 101, 1843–1867. Web of Science CrossRef PubMed CAS Google Scholar
Kirfel, A., Grybous, J. & Dmitrienko, V. E. (2002). Phys. Rev. B, 66, 165202-1–165202-7. Google Scholar
Kirfel, A., Lippmann, T. & Krane, H.-G. (1995). HASYLAB Annual Report, pp. 371–372. HASYLAB, Hamburg, Germany. Google Scholar
Kokubun, J., Kanazawa, M., Ishida, K. & Dmitrienko, V. E. (2001). Phys. Rev. B, 64, 073203-1–073203-4. Google Scholar
Kokubun, J., Nagano, T., Kuribayashi, M. & Ishida, K. (1998). J. Phys. Soc. Jpn, 67, 3114–3118. Web of Science CrossRef CAS Google Scholar
Krivoglaz, M. A. (1983). Theory of X-rays and Neutrons in Non-Ideal Crystals. Kiev: Naukova Dumka. (In Russian.) Google Scholar
Labushkin, V. G., Ovchinnikova, E. H., Smirnov, E. V. Sarkisov, E. R. & Uspensky, M. N. (1995). Kristallografija, 40, 900–905. CAS Google Scholar
Nagano, T., Kokubun, J., Yazawa, I., Kurasawa, T., Kuribayashi, M., Tsuji, E., Ishida, K., Sasaki, S., Mori, T., Kishimoto, S. & Murakami, Y. (1996). J. Phys. Soc. Jpn, 65, 3060–3067. CrossRef CAS Web of Science Google Scholar
Rüffer, R., Gerdau, E., Rüter, H. D., Sturhahn, W., Hollatz, R. & Schneider, A. (1989). Phys. Rev. Lett. 63, 2677–2679. CrossRef PubMed CAS Web of Science Google Scholar
Sirotin, Yu. I. & Shaskolskaya, M. P. (1975). Osn. Kristallofiz. Moskva: Nauka. (In Russian); Sirotine Y. & Chaskolskaia, M. (1984). Fondements de la Physique des Cristaux. Moscou: MIR. (In French.) Google Scholar
Smit, J. & Wijn, H. P. J. (1959). Ferrites. Eindhoven: Philips Technical Library. Google Scholar
Templeton, D. H. (1994). Resonant Anomalous X-ray Scattering, edited by G. Materlik, C. J. Spark & K. Fisher, pp. 1–7. Amsterdam: North-Holland. Google Scholar
Templeton, D. H. & Templeton, L. K. (1980). Acta Cryst. A36, 237–241. CrossRef CAS IUCr Journals Web of Science Google Scholar
Templeton, D. H. & Templeton, L. K. (1985). Acta Cryst. A41, 133–142. CrossRef CAS Web of Science IUCr Journals Google Scholar
Templeton, D. H. & Templeton, L. K. (1994). Phys. Rev. B, 49, 14850–14853. CrossRef CAS Web of Science Google Scholar
Winkler, H., Eisberg, R., Alp, E., Rüffer, R., Gerdau, E., Lauer, S., Trawtwein, A. X., Grodzicki, V. & Vera, A. (1983). Z. Phys. B, 49, 331–341. CrossRef CAS Google Scholar
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