In order to check for the accuracy of X-ray diffracted data collected with an area-detector diffractometer (FAST-Nonius), we have carried out several data collections on a good-quality pyrope crystal (space group 1a3d; a = 11.479 Å) under different experimental settings and compared the results with those obtained with the same crystal mounted on a conventional Philips PW1100 diffractometer. Several parameters have been tested (detector gain, crystal-to-detector distance, frame width, integration time per image, beam intensity, shoebox size and re-measuring of overflow reflections), and four critical features of the system have been identified: the low thermal stability of the detector, its narrow dynamic range, the importance of the detector-to-crystal distance and the integration of the diffracted intensities. We are now able to select the best experimental settings in order to obtain a refinement from FAST diffraction data good as that from Philips data, in terms of Rsym, Robs and standard deviation of the refined parameters.

X-ray data collection from mineral crystals by means of a position-sensitive detector: Advantages and disadvantages / D. Prella, F. Camara. - In: ZEITSCHRIFT FUR KRISTALLOGRAPHIE. - ISSN 0044-2968. - 214:10(1999), pp. 646-651. [10.1524/zkri.1999.214.10.646]

X-ray data collection from mineral crystals by means of a position-sensitive detector: Advantages and disadvantages

F. Camara
Secondo
Writing – Original Draft Preparation
1999

Abstract

In order to check for the accuracy of X-ray diffracted data collected with an area-detector diffractometer (FAST-Nonius), we have carried out several data collections on a good-quality pyrope crystal (space group 1a3d; a = 11.479 Å) under different experimental settings and compared the results with those obtained with the same crystal mounted on a conventional Philips PW1100 diffractometer. Several parameters have been tested (detector gain, crystal-to-detector distance, frame width, integration time per image, beam intensity, shoebox size and re-measuring of overflow reflections), and four critical features of the system have been identified: the low thermal stability of the detector, its narrow dynamic range, the importance of the detector-to-crystal distance and the integration of the diffracted intensities. We are now able to select the best experimental settings in order to obtain a refinement from FAST diffraction data good as that from Philips data, in terms of Rsym, Robs and standard deviation of the refined parameters.
area
Settore GEO/06 - Mineralogia
1999
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/698311
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