微型多孔材料
菱镁矿
煅烧
材料科学
柯肯德尔效应
陶瓷
矿物学
微观结构
多孔性
化学工程
粒径
冶金
镁
复合材料
化学
催化作用
生物化学
工程类
作者
Qianlin Chen,Wen Yan,Junjie Yan,Stefan Schafföner,Zhe Chen,Sanbao Ma,Guangqiang Li
摘要
Abstract Seven microporous MgO–Al 2 O 3 ceramics with an Al 2 O 3 content of 15–90 wt% were prepared using Al(OH) 3 and calcined magnesite as raw materials. A wet mixing process was employed during sample preparation to transform the calcined magnesite with a larger particle size to smaller Mg(OH) 2 particles. The in situ decomposition synthesis method and the Kirkendall effect were utilized to produce and control the pore structure of the microporous MgO–Al 2 O 3 ceramics. There were two kinds of pores in the microporous MgO–Al 2 O 3 ceramics. The first one resulted from the in situ decomposition of Al(OH) 3 and Mg(OH) 2 particles, which were small and equally distributed. Another one originated from the position of the Mg(OH) 2 particles due to the Kirkendall effect caused by MgO diffusion. They were similar in size to the Mg(OH) 2 pseudomorph particles. Simultaneously, the Al 2 O 3 content affected the packing behavior and the spinel formation, which changed the characteristics of the pores and necks among the particles. These mechanisms also affected the strengths of the microporous MgO–Al 2 O 3 ceramics. Thus, when the Al 2 O 3 content was 45–90 wt%, the microporous MgO–Al 2 O 3 ceramics had a high compressive strength (10.0–18.3 MPa) and apparent porosity (52.2%–58.4%).
科研通智能强力驱动
Strongly Powered by AbleSci AI