Hydrothermal stability of NaBH4 enclathrated sodalites with aluminosilicate and gallosilicate framework

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • Josef Christian Buhl
  • Florian Stemme
  • Irma Poltz

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OriginalspracheEnglisch
Seiten (von - bis)276-282
Seitenumfang7
FachzeitschriftMicroporous and Mesoporous Materials
Jahrgang126
Ausgabenummer3
Frühes Online-Datum18 Juni 2009
PublikationsstatusVeröffentlicht - Dez. 2009

Abstract

The time dependent stability of tetrahydroborate sodalites with aluminosilicate- and gallosilicate framework was studied in water at room temperature and under hydrothermal conditions at 353 K. The experiments were carried out in different time intervals (4-48 h) using an excess of water according a solid:liquid mass ratio of 1:150. The kinetics of decomposition was followed by registration of weight loss, change of the pH-value and by X-ray powder diffraction as well as FT-IR spectroscopy. Both samples undergo remarkable time dependent decomposition. The decomposition rate is higher for the gallosilicate sodalite even though its crystal size is larger compare to the aluminosilicate sodalite. Besides formation of some X-ray amorphous material in both cases precipitation of crystalline aluminosilicate or gallosilicate was found, always connected with impurities of carbonate anions. FT-IR clearly showed that the remaining parts of sodalite structure of both samples were always pure tetrahydroborate sodalite. No borate species other than BH4- were detected. Thus, hydrolysis of the moisture sensitive BH4- anions by an entrance of water into intact cages can be excluded under the described experimental conditions.

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Hydrothermal stability of NaBH4 enclathrated sodalites with aluminosilicate and gallosilicate framework. / Buhl, Josef Christian; Stemme, Florian; Poltz, Irma.
in: Microporous and Mesoporous Materials, Jahrgang 126, Nr. 3, 12.2009, S. 276-282.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Buhl JC, Stemme F, Poltz I. Hydrothermal stability of NaBH4 enclathrated sodalites with aluminosilicate and gallosilicate framework. Microporous and Mesoporous Materials. 2009 Dez;126(3):276-282. Epub 2009 Jun 18. doi: 10.1016/j.micromeso.2009.06.018
Buhl, Josef Christian ; Stemme, Florian ; Poltz, Irma. / Hydrothermal stability of NaBH4 enclathrated sodalites with aluminosilicate and gallosilicate framework. in: Microporous and Mesoporous Materials. 2009 ; Jahrgang 126, Nr. 3. S. 276-282.
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abstract = "The time dependent stability of tetrahydroborate sodalites with aluminosilicate- and gallosilicate framework was studied in water at room temperature and under hydrothermal conditions at 353 K. The experiments were carried out in different time intervals (4-48 h) using an excess of water according a solid:liquid mass ratio of 1:150. The kinetics of decomposition was followed by registration of weight loss, change of the pH-value and by X-ray powder diffraction as well as FT-IR spectroscopy. Both samples undergo remarkable time dependent decomposition. The decomposition rate is higher for the gallosilicate sodalite even though its crystal size is larger compare to the aluminosilicate sodalite. Besides formation of some X-ray amorphous material in both cases precipitation of crystalline aluminosilicate or gallosilicate was found, always connected with impurities of carbonate anions. FT-IR clearly showed that the remaining parts of sodalite structure of both samples were always pure tetrahydroborate sodalite. No borate species other than BH4- were detected. Thus, hydrolysis of the moisture sensitive BH4- anions by an entrance of water into intact cages can be excluded under the described experimental conditions.",
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AU - Buhl, Josef Christian

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AU - Poltz, Irma

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N2 - The time dependent stability of tetrahydroborate sodalites with aluminosilicate- and gallosilicate framework was studied in water at room temperature and under hydrothermal conditions at 353 K. The experiments were carried out in different time intervals (4-48 h) using an excess of water according a solid:liquid mass ratio of 1:150. The kinetics of decomposition was followed by registration of weight loss, change of the pH-value and by X-ray powder diffraction as well as FT-IR spectroscopy. Both samples undergo remarkable time dependent decomposition. The decomposition rate is higher for the gallosilicate sodalite even though its crystal size is larger compare to the aluminosilicate sodalite. Besides formation of some X-ray amorphous material in both cases precipitation of crystalline aluminosilicate or gallosilicate was found, always connected with impurities of carbonate anions. FT-IR clearly showed that the remaining parts of sodalite structure of both samples were always pure tetrahydroborate sodalite. No borate species other than BH4- were detected. Thus, hydrolysis of the moisture sensitive BH4- anions by an entrance of water into intact cages can be excluded under the described experimental conditions.

AB - The time dependent stability of tetrahydroborate sodalites with aluminosilicate- and gallosilicate framework was studied in water at room temperature and under hydrothermal conditions at 353 K. The experiments were carried out in different time intervals (4-48 h) using an excess of water according a solid:liquid mass ratio of 1:150. The kinetics of decomposition was followed by registration of weight loss, change of the pH-value and by X-ray powder diffraction as well as FT-IR spectroscopy. Both samples undergo remarkable time dependent decomposition. The decomposition rate is higher for the gallosilicate sodalite even though its crystal size is larger compare to the aluminosilicate sodalite. Besides formation of some X-ray amorphous material in both cases precipitation of crystalline aluminosilicate or gallosilicate was found, always connected with impurities of carbonate anions. FT-IR clearly showed that the remaining parts of sodalite structure of both samples were always pure tetrahydroborate sodalite. No borate species other than BH4- were detected. Thus, hydrolysis of the moisture sensitive BH4- anions by an entrance of water into intact cages can be excluded under the described experimental conditions.

KW - Aluminosilicates

KW - Gallosilicates

KW - Hydrogen storage

KW - Hydrothermal stability

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