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Chapter 2.3 - Accuracy in X-Ray Diffraction

Published online by Cambridge University Press:  05 November 2011

Larry W. Finger
Affiliation:
Carnegie Institution of Washington
Hideo Aoki
Affiliation:
University of Tokyo
Yasuhiko Syono
Affiliation:
Tohoku University, Japan
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Summary

The career and achievements of Yoshito Matsui have emphasized the attainment of accuracy in experimental studies. To honor him, this contribution presents an analysis of several sources of systematic errors in powder-diffraction experiments and evaluates their effects on the results. In particular, the error arising from uncorrected axial divergence in an energy-dispersive experiment may be as large as 1%. Smaller errors of 0.3% may arise from sample positioning errors, and errors as large as 2% can arise from the effects of nonhydrostatic stress.

Introduction

Although an x-ray diffraction experiment may have very high precision, there are many factors that need to be controlled if an accurate result is to be obtained. This paper discusses the potential systematic errors arising from peak asymmetry that are due to axial divergence, sample positioning errors, and nonhydrostatic stress distributions.

Axial Divergence

Axial divergence, the effect that causes peak asymmetry for diffraction maxima near 0° or 180° 2θ in powder-diffraction patterns, arises from the elliptical shape of the intersection of diffraction cones with the cylinder that describes the opening of the detector as it is swept through 2θ. The description of this effect and a method for calculating the resulting profile have been presented by Finger et al. [1]. This correction can be applied directly for data measured with monochromatic radiation and a diffractometer. Axial divergence should not affect monochromatic powder patterns measured with flat-plate detectors, such as imaging plates or CCD detectors. Such patterns are usually processed to convert the circular rings on the flat two-dimensional detector into a pseudo-one-dimensional pattern by dividing the pattern into a number of wedges and integrating each piece [2].

Type
Chapter
Information
Physics Meets Mineralogy
Condensed Matter Physics in the Geosciences
, pp. 63 - 70
Publisher: Cambridge University Press
Print publication year: 2000

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