1999
DOI: 10.1016/s1387-1811(99)00079-7
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The mechanism of the sodalite-to-cancrinite phase transformation in synthetic spent Bayer liquor

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Cited by 132 publications
(100 citation statements)
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“…The x-ray diffraction (XRD) results confirmed that two of the most common phyllosilicates in the sediment, smectite and biotite, underwent dissolution, while clinochlore was resistant to weathering under these conditions (Qafoku et al 2003c). The XRD, scanning electron microscope (SEM), and energy-dispersive x-ray spectroscopy (EDS) analyses and measurements demonstrated the formation of aluminosilicate, such as NO 3 -cancrinite with a yarn-like morphology (Anthony et al 1995;Bickmore et al 2001), sodalite with a cotton-ball like morphology (Barnes et al 1999b), and zeophyllite (with a platy morphology). Zeophyllite was formed in the presence of high aluminum concentrations.…”
Section: 7mentioning
confidence: 99%
“…The x-ray diffraction (XRD) results confirmed that two of the most common phyllosilicates in the sediment, smectite and biotite, underwent dissolution, while clinochlore was resistant to weathering under these conditions (Qafoku et al 2003c). The XRD, scanning electron microscope (SEM), and energy-dispersive x-ray spectroscopy (EDS) analyses and measurements demonstrated the formation of aluminosilicate, such as NO 3 -cancrinite with a yarn-like morphology (Anthony et al 1995;Bickmore et al 2001), sodalite with a cotton-ball like morphology (Barnes et al 1999b), and zeophyllite (with a platy morphology). Zeophyllite was formed in the presence of high aluminum concentrations.…”
Section: 7mentioning
confidence: 99%
“…The aging of zeolites to their structurally related feldspathoid minerals, the sodalites and cancrinites, is also a well known and well-understood phenomena. 21,22 Ostwald's rule of successive transformation demonstrates that the products found at the longest times represent phases which are thermodynamically more stable under the synthesis conditions than their predecessors. 20 This is in agreement with the known fact that zeolites of the chabzite type (Al 2 O 3 :8SiO 2 ) are the stable phase in ~200% excess NaOH while the denser dewatered sodalites (Al 2 O 3 :2SiO 2 ) are the stable phase in ≥300% excess NaOH at temperatures ≤100°C.…”
Section: Zeolite Aging Mechanismsmentioning
confidence: 99%
“…This is independent of the route of formation of the gel. Whether the NAS gel forms from solution via a hydrogel process or whether it forms from a sol (solid particles in liquid) 16 via a sol-gel process, the aging sequence of the NAS gel to denser sodalite and still denser cancrinite type species will typically follow an aging path such as that shown in Figure 2 according to Barnes, Mensah and Gerson 17 and Gerson and Zheng. 18 Note that the densification of the phases agrees with the following literature:…”
Section: The Role Of Kinetics In Thermodynamic Modelingmentioning
confidence: 99%