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Measurement and cartography of clay matrix orientations by image analysis and grey-level diagram decomposition

Published online by Cambridge University Press:  09 July 2018

P. Dudoignon
Affiliation:
ESIP Matériaux de Construction, CNRS- UMR 6532, 86022 Poitiers Cedex, France
A. Pantet
Affiliation:
ESIP Matériaux de Construction, CNRS- UMR 6532, 86022 Poitiers Cedex, France

Abstract

The observation of clayey matrix on a thin-section under polarized transmitted light allows the analysis of the clay particle arrangements, the measurement of their orientations in 3-D, and finally the cartography of the different orientation modes by using a simple image analysis system connected to the optical microscope. The method is based on: (1) the analysis of the shape evolution of the grey-level diagram vs. the rotating stage angles; and (2) the mathematical decomposition of these grey-level diagrams into elementary gaussian curves. For each identified orientation mode, the standard deviation of the grey values gives the dispersion index of the oriented particles around the axial plane. The 3-D representation is performed on the Wulff stereonet. The horizontal orientations are measured by simple rotation of the revolving stage and the dip angles are deduced from the peak displacements along the abscissa of the grey-level diagram during the complete rotation of the revolving stage. The quantifications (percentage, isotropy and distribution index) are performed after a thresholding operation of each orientation mode.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1998

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References

Arch, J. & Maltman, A. (1990) Anisotropic permeability and tormosity of wet sediments. J. Geophys. Res. 95, B6, 90359045.CrossRefGoogle Scholar
Bai, X., Smart, P. & Leng, X. (1994) Polarizing microphotometric analysis. Geotechnique, 44, 175180.Google Scholar
Deer, W.A., Howie, R.A. & Zussmann, J. (1966) An Introduction to the Rock Forming Minerals. Longmans, London.Google Scholar
Diamond, S. (1971) Microstructure and pore structure of impact-compacted clays. Clays Clay Miner. 19, 239249.Google Scholar
Dragon, A., Cormery, F., Désoyer, T. & Halm, D. (1994) Localized failure analysis using damage models. Pp. 127–140 in: Localization and Bifurcation Theory for Soils and Rocks (Chambon, R. et al., editors). Balkema, The Netherlands.Google Scholar
Dragon, A., Pham, D., Charlez Ph. & Shao, J.F. (1993) A model of anisotropic damage by (micro) crack growth. Pp. 7l-78. in: Assessment and Prevention of Failure Phenomena in Rock Engineering (Pasamehmetoglu et al., editors). Balkema, The Netherlands.Google Scholar
Foster, R.H. & De, P.K. (1971) Optical and electron microscopic investigation of shear induced structures in lightly consolidated (soft) and heavily consolidated (hard) kaolinite. Clays Clay Miner. 19, 3147.Google Scholar
Gillot, J.E. (1969) Study of the fabric of fine-grained sediments with the scanning electron microscope. J. Sed. Pet. 39, 90105.Google Scholar
Grumberger, D., Djéran-Maigre, I., Velde, B. & Tessier, D. (1994) Mesure de la réorientation des particules de kaolinite lors de la compaction par observation directe. C. R. Acad. Sci. Paris, 318, II, 627-633.Google Scholar
Lanson, B. (1993) DECOMPXR, X-ray Decomposition Program. ERM (Sarl), Poitiers, France.Google Scholar
Lanson, B. & Besson, G. (1992) Characterization of the end of smectite to illite transformation: decomposition of X-ray patterns. Clays Clay Miner. 40, 4052.Google Scholar
Luo, X., Brigaud, F. & Vasseur, G. (1992) Compaction coefficient of argillaceous sediments: their implications, significance and determination. Norw. Petrol. Soc., 321-332, Elsevier.Google Scholar
McKyes, E. & Yong, R.N. (1971) Three techniques for fabric viewing as applied to shear distortion of a clay. Clays Clay Miner. 19, 289293 Google Scholar
Morgenstern, N. R. & Tchalenko, J. S. (1967) The optical determination of preferred orientation in clays and its application to the study of microstructure in consolidated kaolin. Proc. Royal Soc. A300, 218-250.Google Scholar
Roubault, M. (1963) Détermination des Minéraux des Roches au Microscope polarisant. Lamarre-Poinat Ed., Paris.Google Scholar
Schneider, F., Burrus, J., Bouteca, M. & Vasseur, G. (1994) Effective stress concept in sedimentary basin modelling. First Break, 12, 321326.CrossRefGoogle Scholar
Sloane, R.L. & Kell, T.R. (1966) The fabric of mechanically compacted kaolin. Clays Clay Miner. 14, 289295.CrossRefGoogle Scholar