摘要
表面络合模式已广泛应用于研究矿物表面吸附和溶解反应，尤其是（氢）氧化物和层状铝硅酸盐矿物。表面官能团是矿物参与表面络合反应的基本单元，（氢）氧化物矿物只具有表面羟基，而层状铝硅酸盐矿物除表面羟基外还具有离子交换位。矿物的表面电荷由永久结构电荷、配位表面电荷和离解表面电荷组成，各种零表面电荷状态可由不同的零电荷点来表征。恒电容模式、双层模式和三层模式是３ 种最常用的表面络合模式，它们在双电层结构、表面反应（质子化反应和络合反应）、表面电荷与质量平衡方程及应用范围上存在着一些差异。
Surface complexation models(SCMs) have been widely used to study mineral surface adsorption and solution, especially for (hydr)oxide and phylloaluminosilicate minerals Surface functional groups are basic units of surface complexation reactions of minerals. (Hydr)oxide minerals possess surface hydroxyl groups only and phylloaluminosilicate minerals have ion bearing exchange sites in addition to surface hydroxyl groups. Surface charges on minerals consists of permanent structural charge, coordinative surface charge and dissociated surface charge. A variety of zero surface charge conditions could be presented with different types of points of zero charge. The constant capacitance model (CCM), the double layer model (DLM) and the triple layer model (TLM) are three most commonly used SCMs Among them, some differences existed in their electrical double layer structures, surface reactions (protolysis and surface complexation), surface charge and mass balance equations, and range of application.
出处
《地球科学进展》
CAS
CSCD
2000年第1期90-96,共7页
Advances in Earth Science
基金
国家自然科学基金!"污染沉积物-水界面作用的多样性及其矿物学机制研究"(编号:49773206)
广东省自然科学基金!"矿物界面
关键词
表面络合模式
矿物-水界面
表面电荷
表面离子化
Surface complexation model
Mineral/water interface
Surface functional groups
Surface charge
