1952
DOI: 10.1063/1.1702234
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The Separation of Cold-Work Distortion and Particle Size Broadening in X-Ray Patterns

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Cited by 567 publications
(215 citation statements)
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“…The scanning range for 2θ was set to 6-45°to cover all the significant diffraction peaks of sample crystallites with a scan speed of 3°/min. A single order method based on WarrenAverbach (Warren and Averbach 1952) Fourier theory was used to compute the crystallites size from the broadening of X-ray reflection. For this purpose, a known analytical function for crystal size distribution was used (Somashekarappa et al 1999;Singh et al 2006).…”
Section: X-ray Diffractometrymentioning
confidence: 99%
“…The scanning range for 2θ was set to 6-45°to cover all the significant diffraction peaks of sample crystallites with a scan speed of 3°/min. A single order method based on WarrenAverbach (Warren and Averbach 1952) Fourier theory was used to compute the crystallites size from the broadening of X-ray reflection. For this purpose, a known analytical function for crystal size distribution was used (Somashekarappa et al 1999;Singh et al 2006).…”
Section: X-ray Diffractometrymentioning
confidence: 99%
“…This is a simple method, but accurate only to the order of magnitude. However, since Scherrer's work, line profile analysis has made enormous progress 21,22,23,24,25,26,27,28,29,30 .…”
Section: Powder Patterns and Size Informationmentioning
confidence: 99%
“…From (5) and the order independence of AS(L), the WA analysis is derived from taking the logarithm on both sides of (2) (Warren & Averbach, 1952): …”
Section: A the Warren-averbach Analysismentioning
confidence: 99%