摘要
采用XRD、IR、XPS等测试方法 ,对锂改性蒙脱石矿物中锂的化学状态进行分析 ,发现锂改性过程中 ,Li+ 离子不仅与蒙脱石层间吸附阳离子进行交换 ,还能置换蒙脱石晶格八面体中的阳离子和进入间隙位置。Li+
The montmorillonite is an aluminosilicate mineral which has 21 type la yered structure. The cation exchange in interlayer is an important feature. The montmorillonite is treated by means of lithium exchange in this paper. The che mical states of lithium in lithium-exchanged montmorillonite are analyzed by X RD, IR and XPS etc. The results show that the lithium-exchange is different fro m the other cation-exchange in montmorillonite. Because of smaller ionic radius of Li-+ ion, Li-+ ions can not only exchange with the absorbed cations in mon tmorillonite interlayer, but also replace the cations in the octahedral sites an d enter into the interstitial positions of montmorillonite lattice. There are th ree chemical states of lithium existing in montmorillonite lattice structure. Among them, number of absorbed Li-+ ions in interlayer is more than that of Li-+ ions in the replacement and interstitial positions.
出处
《高校地质学报》
CAS
CSCD
2000年第2期322-326,共5页
Geological Journal of China Universities
关键词
锂改性
蒙脱石矿物
化学状态
锂离子
lithium-exchange
montmorillonite mineral
Li-+ ions
chemical state