Mineralogical transformations of spodumene concentrate from Greenbushes, Western Australia. Part 1: Conventional heating
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文摘

Evidence of mineralogical transformations is presented in unprecedented level of detail.

β-Spodumene formation results in increased surface area and reduced particle size and SG.

XRD spectra provide evidence of γ-spodumene formation between 950 °C and 1100 °C.

Structural change first observed at 950 °C after 30 min are completed at 1100 °C in 10 min.

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