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Relationships between the mean area, volume and thickness for dispersed particles of kaolinites and micaceous clays and their application to surface area and ion exchange properties

Published online by Cambridge University Press:  09 July 2018

P.H. Nadeau
P.H. Nadeau*
Affiliation:
Department of Mineral Soils, Macaulay Land Use Research Institute, Craigiebuckler Aberdeen AB9 2QJ, Scotland
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Information
Clay Minerals , Volume 22 , Issue 3 , September 1987 , pp. 351 - 356
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1987

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References

Bates, T.F. (1971) The kaolin minerals. Pp. 109–157 in: The Electron-Optical Investigation of Clays (Gard, J. A., editor). Mineralogical Society, London.CrossRefGoogle Scholar
Bundy, W.F., Johns, W.D. & Murray, H.H. (1966) Interrelationships of physical and chemical properties. Clays Clay Miner. 14, 331–346.Google Scholar
Cases, J.M., Cunin, P., Grillet, Y., Poinsignon, C. & Yvon, J. (1986) Methods of analysing morphology of kaolinites: relation between crystallographic and morphological properties. Clay Miner. 21, 55–68.Google Scholar
Conley, R.F. (1966) Statistical distribution of particle size and shape in the Georgie kaolins. Clays Clay Miner. 14, 317–330.Google Scholar
Eberl, D.D., Srodon, J., Lee, M., Nadeau, P.H. & Northrop, H.R. (1987) Sericites from the Silverton Caldera, San Juan Mountains, Colorado. Clays Clay Miner. 35 (in press).Google Scholar
Lietard, O., Yvon, J., Delon, J.F. Mercier, R. & Cases, J.M. (1980) Determination of the basal and lateral surfaces of kaolins. Variation with types of crystalline defects. Pp. 558–582 in: Fine Particle Processing 1 (Somasundaran, P., editor). AIME, New York.Google Scholar
Nadeau, P.H. (1985) The physical dimensions of fundamental clay particles. Clay Miner. 20, 499–514.Google Scholar
Nadeau, P.H. & Bain, D.C. (1986) The composition of some smectites and diagenetic illitic clays and implications for their origin. Clays. Clay Miner. 34, 455–464.Google Scholar
Nadeau, P.H., Tait, J.M., McHardy, W.J. & Wilson, M.J. (1984a) Interstratified XRD characteristics of physical mixtures of elementary clay particles. Clay Miner. 19, 67–76.Google Scholar
Nadeau, P.H., Wilson, M.J., McHardy, W.J. & Tait, J.M. (1984b). Interstratified clays as fundamental particles. Science 225, 923–925.CrossRefGoogle ScholarPubMed
Nadeau, P.H., Wilson, M. J., McHardy, W.J. & Tait, J.M. (1984c) Interparticle diffraction: a new concept for interstratified clays. Clay Miner. 19, 757–769.Google Scholar
Nadeau, P.H., Wilson, M.J., McHardy, W.J. & Tait, J.M. (1985) The nature of some diagenetic illitic clays from bentonites and sandstones: implications for the conversion of smectite to illite during diagenesis. Mineral. Mag. 49, 393–400.Google Scholar
Robertson, R.H.S., Brindley, G.W. & Mackenzie, R.C. (1954) Mineralogy of kaolin clays from Pugu, Tanganyika. Am. Miner. 39, 118–139.Google Scholar
Schultz, L.G., Shepard, A.O., Blackman, P.D. & Starkey, H.C. (1971) Mixed-layer kaolinite montmorillonite from the Yucatan Peninsula, Mexico. Clays Clay Miner. 19, 137–150.CrossRefGoogle Scholar