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A Full-Trace Database for the Analysis of Clay Minerals

Published online by Cambridge University Press:  06 March 2019

D. K. Smith
Affiliation:
Department of Geosciences and Intercollege Materials Research Laboratory The Pennsylvania State University, University Park, PA 16802
G. G. Johnson Jr.
Affiliation:
Department of Geosciences and Intercollege Materials Research Laboratory The Pennsylvania State University, University Park, PA 16802
R. Jenkins
Affiliation:
International Centre for Diffraction Data, 12 Campus Boulevard, Newtown Square, PA 19073-3273
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Abstract

A file of digitized diffraction traces for clay minerals has been developed as a test for the usefulness of such traces in the analysis of clays and clay deposits. The kaolin, smectite, mica clay and chlorite groups are represented by patterns of the most common mineral species in the small crystallite size which is typical of their natural occurrences. Patterns are included for the oriented sample and for glycolated and heated samples when appropriate. This database may form a nucleus for an extensive collection of clay mineral traces in the same manner as the early Powder Diffraction File did for the modern PDE.

Type
II. Phase Analysis, Accuracy and Standards in Powder Diffraction
Copyright
Copyright © International Centre for Diffraction Data 1994

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References

1. Johnson, G. G. Jr. and Vand, . (1967) “A computerized powder diffraction identification system”, Ind. Eng. Chem. 59, 1831.Google Scholar
2. Jenkins, R. and Holomany, M. A. (1987) “PC-PDF - A search/display system utilizing the CD-ROM and the complete Powder Diffraction File”, Powder Diffraction, 11, 215219.Google Scholar
3. Smith, D. K., Johnson, G. G. Jr., Scheible, A., Wims, A. M., Johnson, S. L., and Ullrnan, G. (1987) “Quantitative X-ray powder diffraction method using the full diffraction pattern”, Powder Diffraction, 2, 7377.Google Scholar
4. Hill, R. J. and Howard, C. J. (1987) “Quantitative phase analysis from neutron powder diffraction data using the Rietveld method”, J. Appl. Cryst. 20, 467474.Google Scholar
5. Bish, D. L. and Howard, S. A. (1988) “Quantitative phase analysis using the Rietveld method”, J. Appl. Cryst. 21, 8691.Google Scholar
6. Taylor, J. C. and Pecover, S. R. (1988) “Quantitative analysis of phases in zeolite bearing rocks from full X-ray diffraction profiles”, Austr. J. Phys. 41, 323335.Google Scholar
7. JCAMP-DX, “A standard form for exchange of infra-red spectra in computer readable form”, Revision 4.23, February 20, 1987, Joint Committee on Atomic and Molecular Physical DataGoogle Scholar
8. Hall, S. R., Allen, F. M. and Brown, I. D. (1991) “The crystallographic information File (CIF): A new standard archive file for crystallography”, Acta Crystallogr. A47, 655685.Google Scholar
9. Brindley, G. W. and Brown, G. (1982) “Crystal structures of clay minerals and their X-ray identification”, Mineralogical Society, London, UK Google Scholar
10. Moore, D. M. and Reynolds, R. C. Jr. (1991) “X-ray diffraction and the identification and analysis of clay minerals”, Oxford University Press, New York, NY.Google Scholar
11. Dragoo, A. L. (1986) “Standard reference materials for X-ray diffraction, Part 1: Overview of current and future SRM's”, Powder Diffraction, 1, 294298.Google Scholar
12. Smith, D. K, Johnson, G. G. Jr., and Wims, A. M. (1988) “Use of full diffraction spectra, both experimental and calculated, in quantitative powder diffraction analysis”, Austr. J. Phys. 41, 311321.Google Scholar