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Preferred orientation of mineral grains in sample mounts for quantitative XRD measurements: How random are powder samples?

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Clays and Clay Minerals

Abstract

The degree of preferred orientation of mineral grains in powder X-ray diffraction (XRD) samples prepared by standard techniques has been evaluated by means of a correction model implemented in the Rietveld program, BGMN. It is demonstrated that neither front- nor side-loading of mineral powders obtained by wet grinding in a McCrone micronizing mill yield powder mounts with randomly oriented particles. Despite fine grinding, the primary sizes and shapes of mineral grains contained in multi-phase samples influence the degree of preferred orientation in XRD powder mounts. Two minerals, both of platy habit, were found to show different degrees of preferred orientation in front- and side-loaded samples. In contrast to these methods of sample preparation, the spray-drying technique yielded perfect randomness of the particles. The experiments on artificial mineral mixtures demonstrate that the model applied can effectively correct for preferred orientation allowing reliable Rietveld quantitative phase analysis of moderately textured samples prepared by standard techniques.

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References

  • Bergmann, J. and Kleeberg, R. (1998) Rietveld analysis of disordered layer silicates. Materials Science Forum, 278–281, 300–305.

    Article  Google Scholar 

  • Bergmann, J., Friedel, P., and Kleeberg, R. (1998) BGMN — a new fundamental parameters based Rietveld program for laboratory X-ray sources, its use in quantitative analysis and structure investigations. Commission of Powder Diffraction, International Union of Crystallography CPD Newsletter, 20, 5–8.

    Google Scholar 

  • Bergmann, J., Monecke, T., and Kleeberg, R. (2001) Alternative algorithm for the correction of preferred orientation in Rietveld analysis. Journal of Applied Crystallography, 34, 16–19.

    Article  Google Scholar 

  • Bish, D.L. and Reynolds, R.C., Jr. (1989) Sample preparation for X-ray diffraction. Pp. 73–99 in: Modern Powder Diffraction (D.L. Bish and J.E. Post, editors). Reviews in Mineralogy, 20. Mineralogical Society of America, Washington, D.C.

    Chapter  Google Scholar 

  • Blount, A.M. and Vassiliou, A.H. (1979) A new method of reducing preferred orientation in diffractometer samples. American Mineralogist, 64, 922–924.

    Google Scholar 

  • Brindley, G.W. and Kurtossy, S.S. (1961) Quantitative determination of kaolinite by X-ray diffraction. American Mineralogist, 46, 1205–1215.

    Google Scholar 

  • Cheetham, A.K., Fender, B.E.F., and Cooper, M.J. (1971) Defect structure of calcium fluoride containing excess anions: I. Bragg scattering. Journal of Physics C, 4, 3107–3121.

    Article  Google Scholar 

  • Dermatas, D., Chrysochoou, M., Pardali, S., and Grubb, D.G. (2007) Influence of X-ray diffraction sample preparation on quantitative mineralogy: Implications for Chromate waste treatment. Journal of Environmental Quality, 36, 487–497.

    Article  Google Scholar 

  • v. Engelhardt, W. (1955) Über die Möglichkeit der quantitativen Phasenanalyse von Tonen mit Röntgenstrahlen. Zeitschrift für Kristallographie, 106, 430–459.

    Google Scholar 

  • Ferrari, M. and Lutterotti, L. (1994) Method for the simultaneous determination of anisotropic residual stresses and texture by X-ray diffraction. Journal of Applied Physics, 76, 7246–7255.

    Article  Google Scholar 

  • Flörke, O.W. and Saalfeld, H. (1955) Ein Verfahren zur Herstellung texturfreier Röntgen-Pulverpräparate. Zeitschrift für Kristallographie, 106, 460–466.

    Google Scholar 

  • Güven, N. (1971) The crystal structures of 2M1 phengite and 2M1 muscovite. Zeitschrift für Kristallographie, 134, 196–212.

    Google Scholar 

  • Hillier, S. (1999) Use of an air brush to spray dry samples for X-ray powder diffraction. Clay Minerals, 34, 127–135.

    Article  Google Scholar 

  • Hillier, S. (2003) Quantitative analysis of clay and other minerals in sandstones by X-ray powder diffraction (XRPD). Special Publication of the International Association of Sedimentologists, 34, 213–251.

    Google Scholar 

  • Hughes, R. and Bohor, B. (1970) Random clay powders prepared by spray-drying. American Mineralogist, 55, 1780–1786.

    Google Scholar 

  • Järvinen, M. (1993) Application of symmetrized harmonics expansion to correction of the preferred orientation effect. Journal of Applied Crystallography, 26, 525–531.

    Article  Google Scholar 

  • Klug, H.P. and Alexander, L.E. (1954) X-ray diffraction procedures for polycrystalline and amorphous materials. John Wiley & Sons, New York, 716 pp.

    Google Scholar 

  • Monecke, T., Köhler, S., Kleeberg, R., Herzig, P.M., and Gemmell, J.B. (2001) Quantitative phase-analysis by the Rietveld method using X-ray powder-diffraction data: Application to the study of alteration halos associated with volcanic-rock-hosted massive sulfide deposits. The Canadian Mineralogist, 39, 1617–1633.

    Article  Google Scholar 

  • Moore, D.M. and Reynolds, R.C., Jr. (1997) X-ray Diffraction and the Identification and Analysis of Clay Minerals, 2nd edition, Oxford University Press, New York.

    Google Scholar 

  • Newnham, R.E. (1961) A refinement of the dickite structure and some remarks on polymorphism in kaolin minerals. Mineralogical Magazine, 32, 683–704.

    Article  Google Scholar 

  • O’Connor, B.H. and Chang, W.J. (1986) The amorphous character and particle size distributions of powders produced with the micronizing mill for quantitative X-ray powder diffractometry. X-ray Spectrometry, 15, 267–270.

    Article  Google Scholar 

  • Popa, N.C. (1992) Texture in Rietveld refinement. Journal of Applied Crystallography, 25, 611–616.

    Article  Google Scholar 

  • Reynolds, R.C., Jr. (1986) The Lorentz-Polarization factor and preferred orientation in oriented clay aggregates. Clays and Clay Minerals, 34, 359–367.

    Article  Google Scholar 

  • Reynolds, R.C., Jr. (1989) Principles and techniques of quantitative analysis of clay minerals by X-ray powder diffraction. Pp. 4–36 in: Quantitative Mineral Analysis of Clays (D.R. Pevear and F.A. Mumpton, editors). CMS workshop lectures 1, The Clay Minerals Society, Bloomington, Indiana.

    Google Scholar 

  • Środoń, J. (2002) Quantitative mineralogy of sedimentary rocks with emphasis on clays and with applications to K-Ar dating. Mineralogical Magazine, 66, 677–687.

    Article  Google Scholar 

  • Środoń, J. (2006) Identification and quantitative analysis of clay minerals. Pp. 765–787 in: Handbook of Clay Science (F. Bergaya, B.K.G. Theng, and G. Lagaly, editors). Developments in Clay Science, 1, Elsevier, Amsterdam.

    Chapter  Google Scholar 

  • Środoń, J., Drits, V.A., McCarty, D.K., Hsieh, J.C.C., and Eberl, D.D. (2001) Quantitative X-ray diffraction analysis of clay-bearing rocks from random preparations. Clays and Clay Minerals, 49, 514–528.

    Article  Google Scholar 

  • Taylor, R.M. and Norrish, K. (1966) The measurement of orientation distribution and its application to quantitative X-ray diffraction analysis. Clay Minerals, 6, 127–142.

    Article  Google Scholar 

  • Von Dreele, R.B. (1997) Quantitative texture analysis by Rietveld refinement. Journal of Applied Crystallography, 30, 517–525.

    Article  Google Scholar 

  • Williams, P.P. and Megaw, H.D. (1964) The crystal structures of low and high albites at — 180°C. Acta Crystallographica, 17, 882–890.

    Article  Google Scholar 

  • Young, R.A. and Post, B. (1962) Electron density and thermal effects in alpha quartz. Acta Crystallographica, 15, 337–346.

    Article  Google Scholar 

  • Zevin, L. and Viaene, W. (1990) Impact of clay particle orientation on quantitative clay diffractometry. Clay Minerals, 25, 401–418.

    Article  Google Scholar 

  • Zhang, G., Germaine, J.T, Martin, R.T., and Whittle, A.J. (2003) A simple sample-mounting method for random powder X-ray diffraction. Clays and Clay Minerals, 51, 218–225.

    Article  Google Scholar 

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Correspondence to Reinhard Kleeberg.

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Kleeberg, R., Monecke, T. & Hillier, S. Preferred orientation of mineral grains in sample mounts for quantitative XRD measurements: How random are powder samples?. Clays Clay Miner. 56, 404–415 (2008). https://doi.org/10.1346/CCMN.2008.0560402

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  • DOI: https://doi.org/10.1346/CCMN.2008.0560402

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