摘要
采用高温电炉对块状菱镁矿进行煅烧,研究了块状菱镁矿烧结末期(1600~1800℃)方镁石晶粒长大和致密化行为。结果表明:在烧结末期,随着温度升高,晶界快速移动,气孔"汇聚-排除"的速率和晶界向曲率中心的移动的速率增加,致使颗粒致密化迅速,方镁石晶粒长大明显。温度在1600~1700℃期间,晶界扩散是控制烧结致密化的主导机制,晶粒生长活化能为1.382×103k J·mol-1,晶粒以结晶长大方式为主;温度在1700~1800℃期间,体积扩散是控制烧结致密化的主导机制,晶粒生长活化能为1.164×103k J·mol-1,晶粒以聚晶长大方式为主。随温度的升高,晶粒长大活化能逐渐减小,晶粒长大速率增加。
The block magnesite was calcined using high temperature electric furnace. The grains growth and densification behavior of periclase at last sintering stage of block magnesite( 1600-1800 ℃) were investigated. The results show that with the temperature increasing,the grain boundary moves rapidly,the rate of pore " convergence-exclusion" and the moving speed of the grain boundaries to the curvature center increase,which cause particles densification rapidly and periclase grains grow significantly.During 1600-1700 ℃,grain boundary diffusion is the dominant mechanism of controlling densification,the activation energy of grain growth is 1. 382 × 103 k J · mol- 1and crystallization is the main way of grains growth; At the period of 1700-1800 ℃,volume diffusion is the dominant mechanism of controlling densification,the activation energy of grain growth is 1. 164 × 103 k J·mol- 1and glomerocryst grow is the main way of grains growth. Accompanying temperature increases,the activation energy of grain growth decreases,and the rate of grain growth increases.
引文
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