2015
DOI: 10.1016/j.jeurceramsoc.2014.10.035
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Effects of particle size distribution and starting phase composition in Na-feldspar/kaolinite system at high temperature

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Cited by 12 publications
(5 citation statements)
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“…Most likely SiO 2 needed for the formation of dicalcium silicate derived from small invisible quartz particles that are more reactive than the larger ones due to their larger surface area. Such a grains size effect was also reported for feldspar by Diella and co-workers, who studying the effect of particle size distribution in Na-feldspar/kaolinite system [75] and is consistent with Oswald ripening that is described by the Ostwald-Freundlich equation [76] in which surface tension causes small particles to dissolve and larger ones to grow. With increasing time (Section 3.2) or temperature (Section 3.3) dicalcium silicate rims have grown around larger quartz grains (Figures 13 and 16).…”
Section: In Situ Observations Of the Migration Of Solid-solid Reactiosupporting
confidence: 83%
“…Most likely SiO 2 needed for the formation of dicalcium silicate derived from small invisible quartz particles that are more reactive than the larger ones due to their larger surface area. Such a grains size effect was also reported for feldspar by Diella and co-workers, who studying the effect of particle size distribution in Na-feldspar/kaolinite system [75] and is consistent with Oswald ripening that is described by the Ostwald-Freundlich equation [76] in which surface tension causes small particles to dissolve and larger ones to grow. With increasing time (Section 3.2) or temperature (Section 3.3) dicalcium silicate rims have grown around larger quartz grains (Figures 13 and 16).…”
Section: In Situ Observations Of the Migration Of Solid-solid Reactiosupporting
confidence: 83%
“…Endmember proportions can also be described from the occupancy of the cavity cation sites alone (Equations (10) and 12- (14)), which give the same values as Equations (3)- (6). Equation (11) provides another estimate of the total excess silica proportion (Q cav2 ) based on the total cations.…”
Section: Ne-qz Solid Solution Seriesmentioning
confidence: 99%
“…The most probable alteration mineral would be cancrinite, which has a hexagonal structure with six-rings of tetrahedra similar to those of nepheline, although the linkages of these units are different in the two mineral groups. The general formula for the cancrinite group is (Na,K) 6 O. This is chemically similar to nepheline but is structurally different with the extra Na, Ca and large anions occupying "cancrinite cages" and large continuous channels (Deer et al 2004, their Figure 245) [51]; also see [52]).…”
Section: Ne-qz Solid Solution Seriesmentioning
confidence: 99%
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“…demir oksitler, kaolin, mika, vermükülit, quartz ve az miktarda feldispatlardan oluşmaktadır [4]. Quartz sinterlenen cisimlerin deformasyon ve büzülmesini dengelerken, sodyumca zengin feldispatlar sinterlenen cismin sağlamlaşmasını sağlayan ve porozitesini belirleyen yarı sıvı fazı oluştururlar [5][6][7].…”
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