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In situ high temperature X-ray diffraction study on high strength aluminous porcelain insulator with the Al2O3-SiO2-K2O-Na2O system
被引:20
|作者:
Meng, Yong
[1
,2
]
Gong, Guohong
[1
]
Wei, Dongtian
[1
,2
]
Xie, Yumin
[3
]
机构:
[1] Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang 550002, Guizhou, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Bijie Highland Porcelain Insulator Ltd Liabil Co, Bijie 551700, Guizhou, Peoples R China
关键词:
In situ high temperature;
XRD;
Porcelain insulator;
Mineral;
Reaction;
HIGH-VOLTAGE INSULATORS;
MULLITE FORMATION;
MICROSTRUCTURE;
KAOLINITE;
CLAYS;
CLASSIFICATION;
PRODUCT;
QUARTZ;
BODIES;
D O I:
10.1016/j.clay.2016.07.014
中图分类号:
O64 [物理化学(理论化学)、化学物理学];
学科分类号:
070304 ;
081704 ;
摘要:
The high strength aluminous porcelain insulator with a mineral composition of kaolinite, corundum, microcline, quartz, small amounts of albite and anatase was investigated by in situ high temperature XRD (HTXRD) from 25 degrees C to 1300 degrees C The amount change and reaction of minerals contained in the porcelain insulator were presented vividly. The full process occurred in successive stages: 1) kaolinite decomposed into amorphous metakaolinite in the temperature range of 500-600 degrees C; 2) metakaolinite kept amorphous form up to,about 1000 degrees C; 3) at about 1000 degrees C, amorphous metakaolinite generated primary mullite; 4) after bout 1200 degrees C, microcline began to melt, forming an alkaline liquid phase which facilitated the growth of primary mullite into secondary mullite; 5) the alkaline liquid phase could etch beta-quartz, resulting in the reflection intensity of beta-quartz decreasing; 6) corundum was very stable in the whole heating process. (C) 2016 Elsevier B.V. All rights reserved.
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页码:760 / 767
页数:8
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