Abstract
The general explanation of the observations previously described under the above heading1 probably follows, as stated there, from the well-known Laue equations connecting line-breadth with the size of a crystallite measured in a direction a1. I have recently become aware of a paper by R. Brill,2 in which this aspect of Laue's work first appears to have been demonstrated quantitatively, and I would like to add this to my former note in order to direct attention to that paper.
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Nature, of May 9.
Zeit. für Krist., 75, 217.
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WOOD, W. Anomalous X-ray Diffraction Intensities. Nature 128, 272 (1931). https://doi.org/10.1038/128272c0
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DOI: https://doi.org/10.1038/128272c0
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