Texas lignite fly ash has been thermally treated at 1000-1200 degrees C in
air, and the products analyzed by X-ray diffraction (XRD), Fourier transfor
m infrared spectroscopy (FT-IR) and scanning electron microscopy (SEM). The
main crystalline phases found are mullite, hematite, quartz and cristobali
te. Cristobalite, which is present in small amounts on the untreated sample
s, has been interpreted to form preferentially in the outer regions of the
ash particles on thermal treatments of greater than or equal to 900 degrees
C. A model for its formation is presented and placed in perspective to fly
ash formation mechanisms along with supporting XRD, FT-IR and SEM results.
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