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Adsorption of Soil-Derived Humic Acid by Seven Clay Minerals: A Systematic Study

粘土矿物 伊利石 高岭石 吸附 蒙脱石 化学 锂长石 海泡石 Zeta电位 离子强度 坡缕石 腐植酸 离子交换 阳离子交换容量 无机化学 化学工程 矿物学 水溶液 地质学 土壤水分 有机化学 土壤科学 离子 原材料 肥料 纳米颗粒 工程类
作者
Rebecca A. Chotzen,Tamara Polubesova,Benny Chefetz,Yael G. Mishael
出处
期刊:Clays and Clay Minerals [Cambridge University Press]
卷期号:64 (5): 628-638 被引量:73
标识
DOI:10.1346/ccmn.2016.064027
摘要

Abstract Humic acid (HA)-clay complexes are well known for their contribution to soil structure and environmental processes. Despite extensive research, the mechanisms governing HA adsorption are yet to be resolved. A systematic study was conducted to characterize the adsorption of a soil-derived HA to seven clay minerals. Clay surfaces affected HA adsorption directly due to structural differences and indirectly by altering solution pH. The following order of HA removal was obtained for the clay minerals at their natural pH: illite ≫ palygorskite > kaolinite > sepiolite > montmorillonite = hectorite ≫ talc. Removal of HA (precipitation and adsorption) by kaolinite and illite was attributed to the low pH they induce, resulting in protonation of the clay and HA surfaces. In spite of the low pH, the zeta potential for HA remained negative, which promoted HA adsorption to the protonated clay surfaces by ligand exchange. Ionic strength did not affect HA adsorption to clay minerals with low zeta potentials, indicating that charge screening is not a major mechanism of HA adsorption for these minerals, and supporting the suggestion that ligand exchange is the main adsorption mechanism to pH-dependent sites. The increase in ionic strength did, however, promote HA adsorption to clay minerals with high zeta potentials. At pH 8–9 the order of HA affinity for clay minerals was: palygorskite >>sepiolite > montmorillonite = hectorite > kaolinite > illite > talc, emphasizing strong HA interactions with the fibrous clays. This strong affinity was attributed to their large surface areas and to strong interactions with OH groups on these clay surfaces. Results indicated that HA did not enter the intracrystalline channels of the fibrous clays but suggested that their macro-fiber structure facilitates HA adsorption. The sorption of HA to kaolinite further increased in the presence of Cu 2+ , and the sorption of Cu 2+ increased in the presence of HA, due to a number of synergistic effects. This study emphasizes the diverse effects of clay structure and solution chemistry on HA adsorption.
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