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Synthetic Imogolite Paracrystals

Published online by Cambridge University Press:  25 February 2011

Jeffrey C. Huling
Affiliation:
UNM/NSF Center for Micro-Engineered Ceramics, University of New Mexico, Albuquerque, NM 87131
C. Jeffrey Brinker
Affiliation:
UNM/NSF Center for Micro-Engineered Ceramics, University of New Mexico, Albuquerque, NM 87131 Sandia National Laboratories, Ceramic Synthesis and Inorganic Chemistry Department, Albuquerque, NM 87185
William C. Ackerman
Affiliation:
UNM/NSF Center for Micro-Engineered Ceramics, University of New Mexico, Albuquerque, NM 87131
Douglas M. Smith
Affiliation:
UNM/NSF Center for Micro-Engineered Ceramics, University of New Mexico, Albuquerque, NM 87131
Joseph K. Bailey
Affiliation:
Sandia National Laboratories, Ceramic Synthesis and Inorganic Chemistry Department, Albuquerque, NM 87185
Janos Farkas
Affiliation:
UNM/NSF Center for Micro-Engineered Ceramics, University of New Mexico, Albuquerque, NM 87131
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Abstract

Imogolite is a structurally microporous tubular clay comprising one-dimensional pore channels that are ∼1 nm in diameter. In addition to its novel tubular morphology, a notable structural characteristic of imogolite is its occurrence in paracrystalline tube bundles in which the individual tubes are close-packed with their axes in parallel alignment. We have developed a technique that aligns and tightly packs the tube bundles over macroscopic dimensions, in a manner analogous to the alignment and packing of the individual imogolite tubes within the bundles. This extends the range of imogolite paracrystallinity, effectively eliminating mesoporosity and nontubular phases.

Type
Research Article
Copyright
Copyright © Materials Research Society 1993

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References

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