1967
DOI: 10.1107/s0365110x6700386x
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Determination of particle size and strain in cold-worked magnesium by the method of variance

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1968
1968
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Cited by 11 publications
(14 citation statements)
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“…The use of the variance-range function is a powerful method for investigating crystal imperfections (Misra & Mitra, 1967;Criado, GonzS.lez, Gonz;ilez & Real, 1982;Criado, Gonzfilez & Real, 1986), and the determination of quantities D and (e2) 1/2 is straightforward from the values of W0h, kh, W0g and kg. However, some errors can be introduced in the data-processing stage that influence the magnitude of the derived parameters.…”
Section: Introductionmentioning
confidence: 99%
“…The use of the variance-range function is a powerful method for investigating crystal imperfections (Misra & Mitra, 1967;Criado, GonzS.lez, Gonz;ilez & Real, 1982;Criado, Gonzfilez & Real, 1986), and the determination of quantities D and (e2) 1/2 is straightforward from the values of W0h, kh, W0g and kg. However, some errors can be introduced in the data-processing stage that influence the magnitude of the derived parameters.…”
Section: Introductionmentioning
confidence: 99%
“…Similar study seems to be necessary for the Warren-Averbach method as well and the present work aims at achieving this. The present work also aims at examining the validity of some variants of the Warren-Averbach method, such as the single-line technique due to Mitra & Misra (1967), and also to evolve a technique relatively free from the limitations imposed by the Warren-Averbach approximations.…”
Section: Introductionmentioning
confidence: 99%
“…It is seen that the formation of metakaolin and the collapse of the kaolinite structure is preceded and accompanied by a disordering of the basal planes so that the interlayer spacing is variable. Mitra (1958) and Brindiey & Nakahira (1959) have observed that basal reflexions from kaolinite become asymmetrical as a result of dehydration at the temperature at which metakaolin starts to form. The asymmetry of the intensity profiles has been attributed by Mitra (1958) to irregularities in the interlayer distances of the basal planes.…”
mentioning
confidence: 99%
“…Mitra (1958) and Brindiey & Nakahira (1959) have observed that basal reflexions from kaolinite become asymmetrical as a result of dehydration at the temperature at which metakaolin starts to form. The asymmetry of the intensity profiles has been attributed by Mitra (1958) to irregularities in the interlayer distances of the basal planes. Mitra (1963) observed that this disorder exists even in ordinary kaolinite not subject to any heat treatment and has developed a method for quantitative determination of g, the mean fractional change in interlayer spacing, and of y, the proportion of planes affected by such disorders.…”
mentioning
confidence: 99%
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