Abstract
Materials representing common interstratified clay minerals are shown to be composed of aggregates of fundamental particles. Transmission electron microscopy and x-ray diffraction demonstrate that the x-ray diffraction characteristics of a wide range of interstratification can be modeled experimentally by utilizing materials containing only three types of particles. The data have been incorporated into a new model that regards interstratified clay minerals as populations of fundamental particles whose x-ray diffraction patterns result from interparticle diffraction.
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Dates
Type | When |
---|---|
Created | 18 years, 10 months ago (Oct. 5, 2006, 3:41 p.m.) |
Deposited | 1 year, 7 months ago (Jan. 12, 2024, 3:21 a.m.) |
Indexed | 4 months, 3 weeks ago (April 1, 2025, 12:45 a.m.) |
Issued | 40 years, 11 months ago (Aug. 31, 1984) |
Published | 40 years, 11 months ago (Aug. 31, 1984) |
Published Print | 40 years, 11 months ago (Aug. 31, 1984) |
@article{Nadeau_1984, title={Interstratified Clays as Fundamental Particles}, volume={225}, ISSN={1095-9203}, url={http://dx.doi.org/10.1126/science.225.4665.923}, DOI={10.1126/science.225.4665.923}, number={4665}, journal={Science}, publisher={American Association for the Advancement of Science (AAAS)}, author={Nadeau, P. H. and Wilson, M. J. and McHardy, W. J. and Tait, J. M.}, year={1984}, month=aug, pages={923–925} }