1995
DOI: 10.1016/s0167-2991(06)81220-6
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Hydrothermal decomposition of aluminosilicate zeolites and prediction of their long-term stability

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Cited by 25 publications
(19 citation statements)
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“…This phenomenon was checked in this series that utilizes the sodium and proton modifications of a FAU zeolite. Whereas the Na-modification is nearly unchanged up to its collapse above 513 K (Ehrhardt et al, 1995), the H-modification is decomposed beginning already at 403 K (Fig. 3).…”
Section: Resultsmentioning
confidence: 98%
See 1 more Smart Citation
“…This phenomenon was checked in this series that utilizes the sodium and proton modifications of a FAU zeolite. Whereas the Na-modification is nearly unchanged up to its collapse above 513 K (Ehrhardt et al, 1995), the H-modification is decomposed beginning already at 403 K (Fig. 3).…”
Section: Resultsmentioning
confidence: 98%
“…The function g(w) characterizes the influence of steam pressure in the system, and it is assumed that it can be defined as a n-th order dependency of normalized steam concentration (Ehrhardt et al, 1995) …”
Section: Modelingmentioning
confidence: 99%
“…Content of extraframework species in steamed DAY samples [77] amounted to 0.6-4.9% for the aluminosilicate ( ) and 4.3-14,7% for silica gel ( ). It has been shown [83,84] that the intensity of the peaks assigned to and at lowtemperature steaming could be reduced by successive chemical dissolution in hydrochloric acid and solution of potassium hydroxide. Acid treatment caused the decomposition of the Al aluminosilicate with formation of silica gel.…”
Section: Extraframework Species In Steamed Y Zeolitesmentioning
confidence: 99%
“…Then, with the rising temperature, carnegiiete and nepheline occur above 1123 K [4,10]. In water or steam of autogenous pressure, NaY is stable up to 513 K [83]. It will be decomposed into an amorphous phase followed by transformation into hydroxysodalite or zeolite P [89,90].…”
Section: Origin Of Siliceous Extraframework Species Zeolitementioning
confidence: 99%
“…Several studies have been carried out on the hydrothermal stability of zeolite LTA and FAU (Wolf et al 1967;Lutz et al 1983Lutz et al , 1988Lutz et al , 2005Richtermendau et al 1988;Fichtner-Schmittler et al 1992;Ehrhardt et al 1995;Buhl et al 2004;Dimitrijevic et al 2006). In these publications, a relation between the susceptibility of zeolites to hydrothermal damage and the Si/Al-ratio, as well as the dependency on the cation size in ion-exchanged zeolites was established (Buhl et al 2004;Fichtner-Schmittler et al 1992).…”
Section: Introductionmentioning
confidence: 99%