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熔盐辅助合成整体式钾地质聚合物陶瓷

Synthesis of Monolithic Potassium Geopolymer Ceramics Assisted by Molten Salt.

作者信息

Ai Tao, Hong Feng-Hua, Kang Yi-Na, Zhang Hao-Ran, Yan Xin

机构信息

School of Materials Science & Engineering, Chang'an University, Xi'an 710061, China.

Sinosteel Luoyang Institute of Refractories Research Co., Ltd., Luoyang 471039, China.

出版信息

Materials (Basel). 2019 Feb 2;12(3):461. doi: 10.3390/ma12030461.

Abstract

Potassium geopolymer (KGP) ceramics are synthesized by the molten salt method. Metakaolin changes to a potassium geopolymer through a reaction with potassium silicate at 80 °C/24 h. Potassium geopolymer, with a silicon to aluminum (Si/Al) molar ratio of 2, turns into a leucite ceramic in molten potassium salt (KCl) at 900 °C/6 h. X-Ray Diffraction analysis of the KGP treated by molten KCl salt shows the amorphous phase change to leucite crystal phase. A scanning electron microscope image of sintered KGP proves that the grain size of the leucite crystal decreases with soaking time. Compared with solid state sintering, liquid molten salt sintering KGP can be more easily formed into dense ceramics at lower temperatures.

摘要

钾地聚合物(KGP)陶瓷通过熔盐法合成。偏高岭土在80℃/24小时的条件下与硅酸钾反应转变为钾地聚合物。硅铝(Si/Al)摩尔比为2的钾地聚合物在900℃/6小时的熔融钾盐(KCl)中转变为白榴石陶瓷。经熔融KCl盐处理的KGP的X射线衍射分析表明非晶相转变为白榴石晶相。烧结KGP的扫描电子显微镜图像证明白榴石晶体的晶粒尺寸随浸泡时间减小。与固态烧结相比,液态熔盐烧结KGP在较低温度下更容易形成致密陶瓷。

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