三水铝石向α lpha -氧化铝转变温度与粒径的关系

Mohsen Nasiri Ahmadabadi, A. Nemati, K. Arzani, S. Baghshahi
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引用次数: 1

摘要

在1100 ~ 1300℃范围内,三水铝石转变为α-氧化铝。煅烧温度越高,晶粒越大,导致晶粒生长异常。本研究的主要目的是通过减小三水铝石的粒径来降低三水铝石向α-氧化铝的转变温度。研究中使用的三水铝石经盐酸洗涤,钠含量降至0.1%以下。然后在不同的环境条件下在快速磨粉机中研磨不同的时间,然后在不同的温度下煅烧。采用SEM、XRD、XRF、PSA和STA对样品的微观结构、粒径和热行为进行了表征。样品研磨180 min后,转变温度从1300℃左右下降到1150℃。随着煅烧温度的降低,α-氧化铝晶粒尺寸由77.16 nm减小到64.37 nm。
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The relation between particle size and transformation temperature of gibbsite to αLPHA-alumina
ABSTRACT The transformation of gibbsite to α-alumina occurs in the range 1100 to 1300°C. The higher the calcination temperature, the larger the crystallites and this leads to abnormal grain growth. The main goal of this research was to reduce the transformation temperature of gibbsite to α-alumina by reducing the gibbsite particles size. The sodium content of the gibbsite used in the study was reduced to less than 0.1% by washing it in HCl solution. It was then ground in a fast mill at ambient conditions for different times then calcined at different temperatures. The microstructure, particles size and thermal behaviour of the samples were examined with SEM, XRD, XRF, PSA and STA, respectively. In a sample ground for 180 min, the transformation temperature decreased from about 1300°C to 1150°C. The reduction in the calcination temperature led to a reduction in α-alumina crystallite size from about 77.16 nm to 64.37 nm.
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CiteScore
3.50
自引率
0.00%
发文量
6
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