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矿物对金属离子的竞争吸附实验研究 被引量:43

EXPERIMENT ON THE COMPETETION ADSORPTIONS OF METAL IONS ONTO MINERALS
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摘要 CaCO_3、石英、针铁矿、三水铝矿、高岭土、蒙脱石、水云母等矿物对Ag+、Cu2+、Zn2+、Ni2+、Cd2+、Pb2+和Cr3+金属离子的竞争吸附实验研究表明,在近中性低离子强度溶液中,矿物单位表面积吸附金属离子的大小顺序是:CaCO3>石英>水云母>高岭土>蒙脱石>针铁矿>三水铝矿。这些矿物可分成3组:第一组的矿物有石英、针铁矿和高岭土等1:1层硅酸盐矿物及其他氧化物;第二组为三水铝矿、水镁石和蒙脱石等2:1层硅酸盐矿物;第三组是碳酸盐、硫酸盐、磷酸盐等含氧盐矿物。它们对于金属离子的吸附反应;>SO-+Mn+=>SOM(n-1)+(n=1,2,3)有如下的显平衡常数KM与矿物介电常数ε的关系式:(1)lgk1M=7.813-26.15/ε(2)lgK2M-9.030-26.15/ε(3)lgK3M=11.65-26. The study on the competetion adsorptions shows that the order of metal ions adsorbed onto oxide and silicate minerals in near-neutral solution with low ionic strength are as follows (in mol /nm2): CaCO3 > quartz> hydromuscovite > kaolinite > Ca-montmorillonite> goethite> gibbsite. These minerals can be divided into three groups according to their appearance equilibrium constants KM of the adsorption reaction, which are the function of the dielectric constants ε of the absorbent absorbent mierals.The relationships between the constants KM and the ninteral dielectric constants ε are as follows: lgk1M= 7.813-26.15/εlgK2M-9.030-26.15/εlgK3M=11.65-26.15/εfor the adsorption reaction: > SO-+ Mn+=> SOM(n-1)+(n=1,2,3)The first group includes quartz, goethite, 1:1 Phyllosilicates and other oxide minerals;the second group comtains gibbsite,bruite and 2:1 phyllosilicates, the third group includes carbonate, sulphurate and phosphorate minerals. The appearance reaction constants have a variation of magnitute±0.5 for different metal ions with same mineral.
出处 《地球化学》 CAS CSCD 北大核心 1997年第6期25-32,共8页 Geochimica
基金 国家自然科学基金!49572091
关键词 矿物 金属离子 平衡常数 吸附实验 minerals, competetion adsorption, metal ions, equilibrium constants
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