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- W2014378826 abstract "Confocal and electron microscopic observations of willemite (α-Zn2SiO4) crystalline ware glaze, fired to 1270 °C and then aged at 1080 °C for 5 h, indicated the glaze decomposed as (Zn, Ti, Ca)-rich and (Si, Al, K, Na)-rich regions, from which willemite crystallites and amorphous droplets were formed, respectively. Under the constraint of the glaze thickness, the willemite crystallites further developed into plate-like spherulites, which consists of lath-like crystals growing at the order of [0001]⪢〈101̄0〉>〈21̄1̄0〉 and viable for coalescence over {21̄1̄0} habit plane. The impinged plate-like spherulites formed a flat interface at the early stage of crystallization, but irregular interface in late stage due to weaving, truncation and lateral coalescence of the crystals. The {21̄1̄0}-specific coalescence can be rationalized by Brownian-type motion/rotation of the crystals until parallel epitaxy is reached." @default.
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- W2014378826 date "2004-08-01" @default.
- W2014378826 modified "2023-10-01" @default.
- W2014378826 title "On the nucleation, growth and impingement of plate-like α-Zn2SiO4 spherulites in glaze layer: a confocal and electron microscopic study" @default.
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- W2014378826 doi "https://doi.org/10.1016/j.msea.2004.02.063" @default.
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