沸石
硅酸铝
粉煤灰
热液循环
方解石
莫来石
铝土矿
石英
矿物学
吸热过程
阳离子交换容量
化学工程
化学
核化学
地质学
吸附
材料科学
冶金
有机化学
工程类
陶瓷
土壤科学
土壤水分
催化作用
物理化学
作者
Vadim Berkgaut,Arieh Singer
标识
DOI:10.1016/0169-1317(95)00033-x
摘要
During; hydrothermal treatment in NaOH medium coal fly ash partially transformed to zeolite P and/or hydroxysodalite, while quartz slowly dissolved and mullite remained stable. Residual coal favored the formation of zeolite P. The relative proportion of the two zeolites could be changed by seeding. During fusion of fly ash with NaOH an endothermic reaction at 170–180°C occurred, resulting in formation of an unreported Na aluminosilicate with approximate composition Na15Si4Al3020 and major XIRD reflections at 4.793, 3.828, 3.000, 2.854, 2.578, and 2.524 A. The product of fusion interacted with water giving aluminosilicate gel, which yielded zeolite P upon hydrothermal treatment at 100°C without aging and zeolite X after aging in water for 12 hours at room temperature. Cation exchange capacity was 420 and 400 meq/ 100 g for zeolite P and zeolite X respectively.
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