1961
DOI: 10.1154/s0376030800001464
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The Determination of Crystallite Size and Size Distribution from Broadened X-Ray Diffraction Lines

Abstract: Magnesium oxide crystallites having mean dimensions in the range of 25–1000 A can be prepared by controlled thermal decomposition of the carbonate.Following some earlier investigations of Birks and Friedman, we have determined the mean size and size distribution of several such MgO samples from the broadened X-ray diffraction lines which they exhibit. Contrary to the procedure of the above investigators, the harmonic analysis due to Stokes has been used to correct for instrumental broadening and values of mean… Show more

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Cited by 3 publications
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“…Warren (1959) considered this possibility of little practical importance due to expansion of the experimental noise by the second derivative and problems with effective separation of the size and distortion coefficients. There are in the literature, however, examples of effective calculation of p(n) (Pielaszek et al, 1983;Quinn & Cherin, 1962;Sashital et al, 1977) and the concept is tempting. Typical errors of the Fourier coefficients are due to incorrect peak background estimation and are observed for small n as the so-called 'hook effect', causing the A n distribution to be concave downwards locally.…”
Section: Warren-averbach Methods and Background Estimationmentioning
confidence: 99%
See 1 more Smart Citation
“…Warren (1959) considered this possibility of little practical importance due to expansion of the experimental noise by the second derivative and problems with effective separation of the size and distortion coefficients. There are in the literature, however, examples of effective calculation of p(n) (Pielaszek et al, 1983;Quinn & Cherin, 1962;Sashital et al, 1977) and the concept is tempting. Typical errors of the Fourier coefficients are due to incorrect peak background estimation and are observed for small n as the so-called 'hook effect', causing the A n distribution to be concave downwards locally.…”
Section: Warren-averbach Methods and Background Estimationmentioning
confidence: 99%
“…The use of this method in its full original form is rather limited (e.g. Quinn & Cherin, 1962;Sashital et al, 1977;Pielaszek et al, 1983). The main difficulties in its application lay in the estimation of the diffraction pattern background intensity, especially for the overlapping peaks, determination of the correct instrumental function, and the need to measure several orders of the same reflection to separate strain and size effects.…”
Section: Introductionmentioning
confidence: 99%