Organo-montmorillonite barrier layers formed by combustion: Nanostructure and permeability

James B. Fox, Preejith V. Ambuken, Holly A. Stretz, Roberta A. Peascoe, E. Andrew Payzant

Research output: Contribution to journalArticlepeer-review

7 Scopus citations

Abstract

Self-assembly of nanoparticles into barrier layers has been the most cited theoretical explanation for the significant reduction in flammability often noted for polymer/montmorillonite nanocomposites. Both mass and heat transport reductions have been credited for such improvements, and in most cases a coupled mechanism is expected. To provide validation for early transport models, the structure of model barrier layers was investigated, these being produced by combustion of a homologous series of organo-montmorillonites. One model barrier layer was subjected to novel permeability analysis to obtain a flux, which will be useful in the evaluation of transport models. The effects of compatibilizer structure, temperature and pressure on barrier layer structure were examined. XRD versus TGA results suggest that the onset of chemical degradation and the onset of physical collapse on heating are correlated. Addition of pressure as low as 7kPa affected the onset of structural collapse; for the case of a "two-tailed" dimethyl dialkyl quaternary ammonium ion compatibilized organo-montmorillonite this meant expansion of the basal spacing rather than the expected densification. Permeability of Ar through the ash was found to be a sensitive measure of structural change of high aspect ratio MMT nanoparticles. Actual fluxes ranged from 0.139 to 0.151mol (m2s)-1 for 0.5mm thick samples.

Original languageEnglish
Pages (from-to)213-223
Number of pages11
JournalApplied Clay Science
Volume49
Issue number3
DOIs
StatePublished - Jul 2010

Funding

Funding for this project was provided by the National Institute of Standards and Technologies Grant Number 70NANB7H6006 and the Tennessee Technological University Center for Energy Systems Research . We thank Southern Clay Products for donating materials for this project. The real-time high temperature X-ray diffraction measurements were conducted at the Oak Ridge National Laboratory's High Temperature Materials Laboratory which is sponsored by the U.S. Department of Energy, Office of Energy Efficiency and Renewable Energy, Vehicle Technologies Program. Other X-ray diffraction measurements were conducted courtesy of the Tennessee Technological University Center for Manufacturing Research.

Keywords

  • High temperature
  • Montmorillonite
  • Organo-montmorillonite
  • Permeability
  • X-ray diffraction

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