| Reference Type | Journal (article/letter/editorial) |
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| Title | The development of porous microstructures during the dehydration of boehmite |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Wilson, S. J. | Author |
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| Year | 1979 (June) | Volume | 43 |
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| Issue | 326 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_43/43-326-301.pdf+ |
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| DOI | doi:10.1180/minmag.1979.043.326.14Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 3025 | Long-form Identifier | mindat:1:5:3025:4 |
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| GUID | 0 |
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| Full Reference | Wilson, S. J. (1979) The development of porous microstructures during the dehydration of boehmite. Mineralogical Magazine, 43 (326) 301-306 doi:10.1180/minmag.1979.043.326.14 |
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| Plain Text | Wilson, S. J. (1979) The development of porous microstructures during the dehydration of boehmite. Mineralogical Magazine, 43 (326) 301-306 doi:10.1180/minmag.1979.043.326.14 |
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| In | (1979, June) Mineralogical Magazine Vol. 43 (326) Mineralogical Society |
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| Abstract/Notes | SummaryElectron-microscope observations have been used to follow the low-temperature dehydration of boehmite, and show that a coherent skeleton of γ-Al2O3 with a porous texture is produced. For material fired in air the development of a number of pore systems is described. Of these the most important, as far as the dehydration process is concerned, is a lamellar pore system parallel to (001)γ and having a regular spacing of the order of 35–40. Å. A much faster dehydration process is induced by exposure to the electron beam and results in the formation of a more randomly oriented pore structure. The observed microstructure and the calculated internal surface area are compared with the results of previous adsorption studies. |
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