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Titlebook: Expanded Clays and Other Microporous Solids; Mario L. Occelli,Harry E. Robson Book 1992 Springer Science+Business Media New York 1992 adso

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书目名称Expanded Clays and Other Microporous Solids
编辑Mario L. Occelli,Harry E. Robson
视频video
图书封面Titlebook: Expanded Clays and Other Microporous Solids;  Mario L. Occelli,Harry E. Robson Book 1992 Springer Science+Business Media New York 1992 adso
出版日期Book 1992
关键词adsorption; boron; catalysis; chemistry; design; information; organic compounds; oxidation; oxides; phosphate
版次1
doihttps://doi.org/10.1007/978-1-4615-3534-8
isbn_softcover978-1-4613-6568-6
isbn_ebook978-1-4615-3534-8
copyrightSpringer Science+Business Media New York 1992
The information of publication is updating

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Synthesis of Dioctahedral 2:1 Layered Silicates in an Acid and Fluoride Medium,fluoride medium. Their general formula is M.(Al.)(Si..Al.)O.((OH).F.). (for a half-unit cell) with x being a value between 0 and 0.9 and y a value between 0 and 2. The substitution of fluorine atoms for hydroxyl groups increases the thermal stability. These layer silicates are the first stage toward
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,Ein Gesamtmodell für Führung?,AI-pillared clays thermally stable up to 750°C have been prepared from easily available starting materials: a natural clay, namely the saponite, and a commercial aqueous solution of Chlorhydrol.
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Optimization of the Pillaring of a Saponite,AI-pillared clays thermally stable up to 750°C have been prepared from easily available starting materials: a natural clay, namely the saponite, and a commercial aqueous solution of Chlorhydrol.
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Intercalation Properties of Layered Metal (IV) Phosphates Towards Organic Bases, Metal Complexes anLayered materials continue to evince interest because their nonrigid structure permits the intercalation of host molecules or compounds, which give rise to new produCts with properties of great interest in several fields: catalysis, ionic conduction, gas absorption, etc.
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,Kurzzusammenfassung der Fälle,ercalates in which the interlayer thickness is substantially larger than the thickness of the host layer. Three general classes of hosts are considered, namely, 2:1 smectite clays,layered double hydroxides (LDHs), and layered silicic acids. The direct intercalation of metal oxide sol particles can b
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