波特兰岩
去壳
无定形固体
化学工程
材料科学
多孔性
水泥
无定形二氧化硅
离子
化学
矿物学
核化学
复合材料
有机化学
硅酸盐水泥
植物
工程类
生物
作者
Qijun Yu,Kazuki Sawayama,Shuichi Sugita,Masami Shoya,Y Isojima
标识
DOI:10.1016/s0008-8846(98)00172-0
摘要
In this study it was confirmed that, at temperatures around 40°C and in the presence of water, the amorphous silica contained in rice husk ash (RHA) can react with Ca(OH)2 to form one kind of C-S-H gel (Ca1.5SiO3.5· xH2O). The C-S-H gel looks like flocs in morphology, with a porous structure and large specific surface. The average particle diameter of the reaction product, ranging from 4.8 to 7.9 μm, varies slightly with the condition under which the reaction occurs. When the product is heated, it gradually loses the water that exists in it, but it maintains an amorphous form up to 750°C. Above 780°C it begins to transform to crystalline CaSiO3. One of the main reasons for the improvement of concrete properties upon addition of RHA possibly may be attributed to the formation of more C-S-H gel and less portlandite in concrete due to the reaction occurring between RHA and the Ca2+, OH− ions, or Ca(OH)2 in hydrating cement.
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