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作 者:Lu Liu Mei-long Hu Chen-guang Bai Xue-wei Lü Yu-zhou Xu Qing-yu Deng
机构地区:[1]College of Materials Science and Engineering, Chongqing University
出 处:《International Journal of Minerals,Metallurgy and Materials》2014年第11期1052-1061,共10页矿物冶金与材料学报(英文版)
基 金:financially supported by the National Natural Science Foundation of China(No.51090383);the Fundamental Research Funds for the Central Universities of China(No.CDJZR12130049)
摘 要:The effect of cooling rate on the crystallization of perovskite in high Ti-bearing blast furnace(BF) slag was studied using confocal scanning laser microscopy(CSLM). Results showed that perovskite was the primary phase formed during the cooling of slag. On the slag surface, the growth of perovskite proceeded via the successive production of quasi-particles along straight lines, which further extended in certain directions. The morphology and structure of perovskite was found to vary as a function of cooling rate. At cooling rates of 10 and 30 K/min, the dendritic arms of perovskite crossed obliquely, while they were orthogonal at a cooling rate of 20 K/min and hexagonal at cooling rates of 40 and 50 K/min. These three crystal morphologies thus obtained at different cooling rates respectively corresponded to the orthorhombic, cubic and hexagonal crystal structures of perovskite. The observed change in the structure of perovskite could probably be attributed to the deficiency of O^2-, when Ti2O3 was involved in the formation of perovskite.The effect of cooling rate on the crystallization of perovskite in high Ti-bearing blast furnace(BF) slag was studied using confocal scanning laser microscopy(CSLM). Results showed that perovskite was the primary phase formed during the cooling of slag. On the slag surface, the growth of perovskite proceeded via the successive production of quasi-particles along straight lines, which further extended in certain directions. The morphology and structure of perovskite was found to vary as a function of cooling rate. At cooling rates of 10 and 30 K/min, the dendritic arms of perovskite crossed obliquely, while they were orthogonal at a cooling rate of 20 K/min and hexagonal at cooling rates of 40 and 50 K/min. These three crystal morphologies thus obtained at different cooling rates respectively corresponded to the orthorhombic, cubic and hexagonal crystal structures of perovskite. The observed change in the structure of perovskite could probably be attributed to the deficiency of O^2-, when Ti2O3 was involved in the formation of perovskite.
关 键 词:blast furnace slag perovskite crystallization cooling rate
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