Journal of Rare Earths | 2019

Identification of ions present in LiF-DyF3 melts and the mechanism of Dy2O3 dissolution therein

 
 
 
 
 
 
 

Abstract


Abstract Herein, the present paper were attempted to identify ions in LiF-DyF3 melts according to the law of decreasing primary crystallization temperature and model analysis. Specifically, the primary crystallization temperatures of LiF-DyF3 and LiF-DyF3-Dy2O3 melts with various DyF3 and Dy2O3 contents were determined by differential scanning calorimetry (DSC), and reactions occurring in the above melts were investigated using ideal dilute solution (Temkin and Flood) models. Moreover, crystal phases produced by rapid solidification of LiF-DyF3, LiF-Dy2O3, DyF3-Dy2O3, and LiF-DyF3-Dy2O3 melts were identified by X-ray diffraction (XRD) analysis. The primary crystallization temperature of LiF-DyF3 melts exhibits an approximately linear decrease with increasing molar fraction of DyF3, and the general formula of complex ions in these melts is expressed as DyFx(3−x), e.g., DyF4−. Finally, we investigated the dissolution of Dy2O3 in LiF-DyF3 melts, showing that it was chemical in nature and afforded Dy1+xO3xF3–3x and DyOF.

Volume 37
Pages 211-217
DOI 10.1016/J.JRE.2018.05.014
Language English
Journal Journal of Rare Earths

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