1980
DOI: 10.1007/bf00550379
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Energetics of formation of lamellar porous microstructures in ?-Al2O3

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1984
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Cited by 22 publications
(12 citation statements)
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“…No change in pore size with temperature was observed for the goethites of this study. Wilson et al (1980) observe a dependence of pore size with water-vapour pressure for boehmite but no change in size with temperature, and a similar relationship may be true for goethite. Although a change in microstructure may occur with Pn2o, thus affecting reaction rates, the transformation mechanism may remain the same.…”
Section: Tem and Xrdsupporting
confidence: 57%
“…No change in pore size with temperature was observed for the goethites of this study. Wilson et al (1980) observe a dependence of pore size with water-vapour pressure for boehmite but no change in size with temperature, and a similar relationship may be true for goethite. Although a change in microstructure may occur with Pn2o, thus affecting reaction rates, the transformation mechanism may remain the same.…”
Section: Tem and Xrdsupporting
confidence: 57%
“…In order to understand this variability, the structural rearrangements of bulk boehmite at low temperatures have been extensively studied. , Recently, theoretical calculations have developed new models for γ-alumina, documenting variations in the spinel structure as well as the non-spinel structure. Dehydration models based on both spinel and non-spinel γ-Al 2 O 3 report fine-scale structural changes and predict porosity around and below 1 nm. Porosity below 1 nm was also seen experimentally by SAXS analysis in dehydrated boehmite materials. , Further theoretical work has hypothesized that fine-scale porosity (around 1 nm in dimension) is characteristic of the γ-Al 2 O 3 crystal structure. , Despite intensive research, the distribution of vacancies and atomic structure of experimental γ-Al 2 O 3 remain the subjects of controversy.…”
Section: Introductionmentioning
confidence: 99%
“…The topotactic transformation of boehmite to γ-Al 2 O 3 produces a well-developed pore structure, resulting in a high surface area. The subsequent phase transformations to δ- and θ-Al 2 O 3 are also topotactic and are accompanied by changes in the porous microstructure such that each phase has a characteristic microstructure. Each subsequent phase has an increased mean pore size and decreased surface area.…”
Section: Introductionmentioning
confidence: 99%
“…It is logical that hydrogen, whether in the form of water, hydroxide, or isolated protons, is likely to be present in these regions. However, the lamellar porous microstructure of γ-Al 2 O 3 , with reported mean pore widths of 8−10 Å and spacing between 35 and 40 Å, creates ample surface for hydrogen species attachment. This can make it difficult to discern between surface hydrogen-containing species and possible hydrogen-containing species within the bulk.…”
Section: Introductionmentioning
confidence: 99%