addenda and errata
Correct interpretation of diffraction properties of quartz crystals for X-ray optics applications. Corrigendum
aAdvanced Photon Source, Argonne National Laboratory, 9700 South Cass Avenue, Argonne, Illinois 60439, USA, and bInstituto de Ciencias da Vida e da Natureza, Universidade Federal da Integracao Latino-Americana, 2044 Foz do Iguacu, Parana, 85867-970, Brazil
*Correspondence e-mail: xiahuang@aps.anl.gov
Errors about left-handed (laevorotatory) quartz and right-handed (dextrorotatory) quartz in the paper by Huang, Gog, Kim, Kasman, Said, Casa, Wieczorek, Hönnicke & Assoufid [J. Appl. Cryst. (2016), 51, 140–147] are corrected.
Keywords: X-ray optics; quartz; Bragg reflection; Darwin bandwidth; X-ray analyzers.
In the paper by Huang et al. (2016), the authors erroneously stated that the helical arrangement of the Si atoms in quartz is the same as the `optical handedness'. The authors are grateful to Professor A. M. Glazer at Physics Department, University of Oxford, for pointing out that this statement is incorrect (see also Glazer, 2018). In fact, the two types of handedness are opposite to each other (Glazer & Stadnicka, 1986). Therefore, in the right-handed hexagonal coordinate system, the with the three Si atoms located at (u, 0, 0), (−u, −u, 1/3) and (0, u, 2/3) and the six O atoms at (x, y, z), (y, x, 2/3 − z), (−y, x − y, 2/3 + z), (−x, y − x, 1/3 − z), (y − x, −x, 1/3 + z) and (x − y, −y, −z) corresponds to (space group P3221) with right-handed (dextrototation), although here the three Si atoms form a left-handed helix (or left-handed screw, LS). Accordingly, still in the right-handed hexagonal coordinate system, the with the Si atoms located at (u, u, −1/3), (−u, 0, 0) and (0, −u, 1/3) (forming a right-handed screw, RS) and the O atoms at (x, x − y, z − 1/3), (y, y − x, 1/3 − z), (−y, −x, 1/3 + z), (−x, −y, −z), (y − x, y, z) and (x − y, x, 2/3 − z) corresponds to left-handed quartz (space group P3121) with left-handed (laevorotation). Since the authors have adopted u = 0.4699, x = 0.4141, y = 0.2681 and z = 0.1188, (P3221) corresponds to the z(+) setting in the right-handed hexagonal coordinate system of Donnay & Le Page (1978), and left-handed quartz (P3121) corresponds to the z(−) setting in the right-handed hexagonal coordinate system. These settings correspond to the `reverse settings' (widely adopted in the X-ray community) so that reflection is stronger than , and is much stronger than .
In summary, except for the words `right- or left-handed hexagonal coordinate systems' and `left-handed helix', all the other words `left-handed' should be `right-handed' and the words `right-handed' should be `left-handed' in the original paper and the original supporting information. A revised version of the paper and the supporting information with all the corrections has been deposited as new supporting information to this paper.
Supporting information
A corrected version of the original article. DOI: https://doi.org/10.1107/S1600576718004363/te9028sup1.pdf
Corrected Supplementary Information [complete lists of strong back reflections of Si (Table S1) and quartz (Table S2) for photon energies less than 16 keV]. DOI: https://doi.org/10.1107/S1600576718004363/te9028sup2.pdf
References
Donnay, J. D. H. & Le Page, Y. (1978). Acta Cryst. A34, 584–594. CrossRef CAS IUCr Journals Web of Science Google Scholar
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Huang, X.-R., Gog, T., Kim, J., Kasman, E., Said, A. H., Casa, D. M., Wieczorek, M., Hönnicke, M. G. & Assoufid, L. (2018). J. Appl. Cryst. 51, 140–147. CrossRef CAS IUCr Journals Google Scholar
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