Interstratified clays as fundamental particles

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Authors:Nadeau, P. H.; Wilson, M. J.; McHardy, W. J.; Tait, J. M.
Author Affiliations:Primary:
Macaulay Inst. Soil Res., Dep. Miner. Soils, Craigiebuckler, Aberdeen, United Kingdom
Volume Title:Science
Source:Science, 225(4665), p.923-925. Publisher: American Association for the Advancement of Science, Washington, DC, United States. ISSN: 0036-8075
Publication Date:1984
Note:In English. 24 refs.; illus.
Summary:TEM and XRD demonstrate that the XRD characteristics of a wide range of interstratification can be modelled experimentally by using materials containing only three types of particles. The data have been incorporated into a new model that regards interstratified clay minerals as aggregates of fundamental particles whose XRD patterns result from interparticle diffraction. [C.N.]
Subjects:Bentonite; Clastic rocks; Clay mineralogy; Clay minerals; Corrensite; Crystal growth; Diagenesis; Experimental studies; Materials; Minerals; Mixed-layer minerals; Montmorillonite; Natural materials; Particles; Saponite; Sedimentary rocks; Sheet silicates; Silicates; Smectite; TEM data; Thermodynamic properties; X-ray data
Abstract Numbers:85M/2263
86M/2812
Record ID:1985014121
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom
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