Thermally induced conversion of Mg2+ cation exchanged LTA, FAU, GIS and SOD zeolites: Syntheses and characterization of γ-cordierite, a new Mg2Al4Si5O18 polymorph
The thermal behaviours of fully Mg2+ cation exchanged LTA, FAU (X and Y species), GIS and SOD zeolites were investigated in the temperature range from ambient to 1400 °C. The initial zeolite frameworks collapsed into amorphous intermediate substances after air heating between 800-850 °C. Prolonged a...
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| Format: | Article |
| Language: | English |
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Serbian Chemical Society
2007-01-01
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| Series: | Journal of the Serbian Chemical Society |
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| Online Access: | http://www.doiserbia.nb.rs/img/doi/0352-5139/2007/0352-51390712351D.pdf |
| _version_ | 1818887996143828992 |
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| author | Dimitrijević Radovan Dondur Vera |
| author_facet | Dimitrijević Radovan Dondur Vera |
| author_sort | Dimitrijević Radovan |
| collection | DOAJ |
| description | The thermal behaviours of fully Mg2+ cation exchanged LTA, FAU (X and Y species), GIS and SOD zeolites were investigated in the temperature range from ambient to 1400 °C. The initial zeolite frameworks collapsed into amorphous intermediate substances after air heating between 800-850 °C. Prolonged annealing of these products above 850 °C induced recrystallization into sapphirine-like phases (Mg-LTA and Mg-FAUx zeolites) and µ-cordierite (Mg-FAUy and Mg-GIS zeolites) phases. These phases were unstable during further temperature/time treatment and between 1000-1100 °C they polymorphously transformed into γ-cordierite, a new Mg2Al4Si5O18 polymorph. γ-Cordierite was formed as a transformation product from the investigated zeolite precursors, except for the Mg-SOD zeolite. Structurally the γ-cordierite phase is a modulated, Mg-stuffed derivative of cristobalite with the approximate composition Mg2Al4Si5O18, which precedes the appearance of α-cordierite. The orthorhombic unit cell dimensions calculated from X-ray powder diffraction pattern are: a = 16.387(7) Å, b = 8.835(4) Å, c = 7.853(3) Å. γ-Cordierite has a narrow range of temperature stability (1100-1200 °C) and during prolonged temperature/time treatment, it is polymorphously transformed to the α-cordierite phase. |
| first_indexed | 2024-12-19T16:46:06Z |
| format | Article |
| id | doaj.art-68746d8f902648a9a657af33dcb848ee |
| institution | Directory Open Access Journal |
| issn | 0352-5139 1820-7421 |
| language | English |
| last_indexed | 2024-12-19T16:46:06Z |
| publishDate | 2007-01-01 |
| publisher | Serbian Chemical Society |
| record_format | Article |
| series | Journal of the Serbian Chemical Society |
| spelling | doaj.art-68746d8f902648a9a657af33dcb848ee2022-12-21T20:13:39ZengSerbian Chemical SocietyJournal of the Serbian Chemical Society0352-51391820-74212007-01-0172121351136210.2298/JSC0712351D0352-51390712351DThermally induced conversion of Mg2+ cation exchanged LTA, FAU, GIS and SOD zeolites: Syntheses and characterization of γ-cordierite, a new Mg2Al4Si5O18 polymorphDimitrijević Radovan0Dondur Vera1Rudarsko-geološki fakultet, Katedra za kristalografiju, BeogradFakultet za fizičku hemiju, BeogradThe thermal behaviours of fully Mg2+ cation exchanged LTA, FAU (X and Y species), GIS and SOD zeolites were investigated in the temperature range from ambient to 1400 °C. The initial zeolite frameworks collapsed into amorphous intermediate substances after air heating between 800-850 °C. Prolonged annealing of these products above 850 °C induced recrystallization into sapphirine-like phases (Mg-LTA and Mg-FAUx zeolites) and µ-cordierite (Mg-FAUy and Mg-GIS zeolites) phases. These phases were unstable during further temperature/time treatment and between 1000-1100 °C they polymorphously transformed into γ-cordierite, a new Mg2Al4Si5O18 polymorph. γ-Cordierite was formed as a transformation product from the investigated zeolite precursors, except for the Mg-SOD zeolite. Structurally the γ-cordierite phase is a modulated, Mg-stuffed derivative of cristobalite with the approximate composition Mg2Al4Si5O18, which precedes the appearance of α-cordierite. The orthorhombic unit cell dimensions calculated from X-ray powder diffraction pattern are: a = 16.387(7) Å, b = 8.835(4) Å, c = 7.853(3) Å. γ-Cordierite has a narrow range of temperature stability (1100-1200 °C) and during prolonged temperature/time treatment, it is polymorphously transformed to the α-cordierite phase.http://www.doiserbia.nb.rs/img/doi/0352-5139/2007/0352-51390712351D.pdfmg2+ cation exchanged zeolitesthermal conversionγ-cordierite newpolymorphphase stability |
| spellingShingle | Dimitrijević Radovan Dondur Vera Thermally induced conversion of Mg2+ cation exchanged LTA, FAU, GIS and SOD zeolites: Syntheses and characterization of γ-cordierite, a new Mg2Al4Si5O18 polymorph Journal of the Serbian Chemical Society mg2+ cation exchanged zeolites thermal conversion γ-cordierite newpolymorph phase stability |
| title | Thermally induced conversion of Mg2+ cation exchanged LTA, FAU, GIS and SOD zeolites: Syntheses and characterization of γ-cordierite, a new Mg2Al4Si5O18 polymorph |
| title_full | Thermally induced conversion of Mg2+ cation exchanged LTA, FAU, GIS and SOD zeolites: Syntheses and characterization of γ-cordierite, a new Mg2Al4Si5O18 polymorph |
| title_fullStr | Thermally induced conversion of Mg2+ cation exchanged LTA, FAU, GIS and SOD zeolites: Syntheses and characterization of γ-cordierite, a new Mg2Al4Si5O18 polymorph |
| title_full_unstemmed | Thermally induced conversion of Mg2+ cation exchanged LTA, FAU, GIS and SOD zeolites: Syntheses and characterization of γ-cordierite, a new Mg2Al4Si5O18 polymorph |
| title_short | Thermally induced conversion of Mg2+ cation exchanged LTA, FAU, GIS and SOD zeolites: Syntheses and characterization of γ-cordierite, a new Mg2Al4Si5O18 polymorph |
| title_sort | thermally induced conversion of mg2 cation exchanged lta fau gis and sod zeolites syntheses and characterization of γ cordierite a new mg2al4si5o18 polymorph |
| topic | mg2+ cation exchanged zeolites thermal conversion γ-cordierite newpolymorph phase stability |
| url | http://www.doiserbia.nb.rs/img/doi/0352-5139/2007/0352-51390712351D.pdf |
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