1980
DOI: 10.1107/s0567739480001933
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Relationship between `observed' and `true' intensity; effect of various counting modes

Abstract: be neglected and the familiar formula for shortrange-order diffuse scattering (see e.g. Guinier, 1963, p. 269) is obtained. For values of a much greater than this many such diffuse curves corresponding to higher values of P must be included in the summation. Each of these will represent successively broader more diffuse peaks as r 2p approaches zero. The factor (k 2 t72)P/P! eventually goes to zero as P increases for any tr but for values of a ~_ 1 many terms must be included.References BARTLETT, M. S. (1967)… Show more

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“…First, for each pattern, the background was determined as a monotonically decreasing smoothed natural cubic spline function to approximate together the manually selected fragments of the pattern, and then the background was subtracted (as illustrated in Figure 5). After subtracting the background, each pattern was represented with the small step of diffraction angle as a natural cubic spline by applying optimal smoothing [65] with an error estimate derived from quantum count statistics of X-ray intensity measurements [66][67][68]. The optimal smoothing was performed so that the root-mean-square difference between the vector of measured background-corrected X-ray intensities and the vector of corresponding smoothing spline was equal to the root-mean-square estimate of the error in the experimental pattern.…”
Section: Xrd Characterization Of the Absorbents Testedmentioning
confidence: 99%
“…First, for each pattern, the background was determined as a monotonically decreasing smoothed natural cubic spline function to approximate together the manually selected fragments of the pattern, and then the background was subtracted (as illustrated in Figure 5). After subtracting the background, each pattern was represented with the small step of diffraction angle as a natural cubic spline by applying optimal smoothing [65] with an error estimate derived from quantum count statistics of X-ray intensity measurements [66][67][68]. The optimal smoothing was performed so that the root-mean-square difference between the vector of measured background-corrected X-ray intensities and the vector of corresponding smoothing spline was equal to the root-mean-square estimate of the error in the experimental pattern.…”
Section: Xrd Characterization Of the Absorbents Testedmentioning
confidence: 99%