摘要
本文研究了 Ca O—Mg O—Si O2 — H2 O体系的水热反应特性。结果表明 :在 Ca O— Mg O—Si O2 一 H2 O系统中 ,Ca O优先与 Si O2 反应生成水化硅酸钙 ,Mg O部分固溶于水化硅酸钙中 ,部分生成 Mg( OH) 2 ,部分与剩余的 Si O2 反应生成水化硅酸镁 ;Mg O固溶时 ,可促进托勃莫来石向硬硅钙石转化 ,不固溶 。
The reaction characteristics of CaO-MgO-SiO 2-H 2O system under hydrothermal condition were studied. The results show that, in the CaO-MgO-SiO 2-H 2O system, CaO firstly react with SiO 2 to form calcium silicate hydrates whilst, some of the MgO dissolve in the calcium silicate hydrates, some of the MgO form Mg(OH) 2, some of the MgO react with surplus SiO 2 to form magnesium silicate hydrates. The Presence of MgO can promote the change from tobermorite to xonotlite, without MgO, the temperature of the change increases.
出处
《西南工学院学报》
2000年第4期1-4,共4页
Journal of Southwest China Institute of Technology
基金
国家自然科学基金! (No.56974 0 3 4 )
国家建材局行业基金! (No.J-96-2 0 )资助项目
