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Reciprocal lattice scan modes in single crystal diffractometry: a reexamination for cases of mineralogical interest

Published/Copyright: August 25, 2010
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Abstract

The choice of reciprocal lattice nodes scan mode (ω, ω/θ, ω/2θ) in single crystal automated diffractometry is examined from an operational point of view, for typical routine situations in mineralogy (Mo radiation, θ < 30°, monochromator). A critical reexamination of the literature (not always free from ambiguities) is attempted and experimental investigations on natural clinopyroxenes are reported. In the above specified conditions, unless extreme cases, what is really important is not primarily the chosen scan mode itself, but rather the size of the horizontal detector aperture in relation to scan mode. If this relationship is correctly chosen, the choice of scan mode itself can be somehow arbitrary and not relevant for refinement accuracy and precision. The criterion of “minimum detector aperture width”, largely emphasized in the literature, is of very limited operative relevance. Even a wrong choice of aperture-scan coupling affects precision but not accuracy of the final crystal chemical model (with the exception of thermal parameters underestimation). The different areas of reciprocal lattice sampled as background with different scan modes do not affect refinement results.

Published Online: 2010-08-25
Published in Print: 1989

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