We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
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
An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content.
Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)
Article purchase
Temporarily unavailable
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 Processing1 (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., Wilson, M.J., McHardy, W.J. & Tait, J.M. (1984b). Interstratified clays as fundamental particles. Science225, 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