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首页> 外文期刊>Journal of Hazardous Materials >Sorption And Desorption Of Cd, Cr, Cu, Ni, Pb And Zn By A Fibric Histosol And Its Organo-mineral Fraction
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Sorption And Desorption Of Cd, Cr, Cu, Ni, Pb And Zn By A Fibric Histosol And Its Organo-mineral Fraction

机译:纤维组织溶胶对Cd,Cr,Cu,Ni,Pb,Zn的吸附解吸及其有机矿物组分

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摘要

It has often been stated that the contribution of soil organic matter(OM) to the sorption of heavy metals can be evaluated using the surface horizon of a Histosol as typical of soil organic matter. However, components of Histosols other than organic matter, such as clay minerals and Fe or Mn oxides, can also sorb heavy metals. In this work we compared the heavy metal sorption and desorption behaviour of a Fibric Histosol H horizon with that of its organo-mineral fraction (OMF, defined as the fraction of wet particle size < 100 μm) in experiments in which Cd, Cr, Cu, Ni, Pb and Zn were sorbed simultaneously from solutions of various concentrations. The OMF sorbed the metals reversibly and apparently mainly at specific sites to each particular metal, in keeping with the good fit of Langmuir isotherms to the sorption data; greatest sorption capacity was for lead and copper. Whole H horizon appeared to include sites at which binding was less reversible and chromium competed with the other metals, especially copper. Organo-mineral fraction is suggested to evaluate the soil organic matter contribution to heavy metal fixation.
机译:经常有人指出,土壤有机质(OM)对重金属吸附的贡献可以通过使用作为土壤有机质典型特征的组织溶胶的表面层来评估。但是,除有机物以外的组织溶胶成分,例如粘土矿物和铁或锰的氧化物,也可以吸收重金属。在这项工作中,我们在实验中比较了Cd,Cr,Cu的实验结果,比较了纤维状组织溶胶H层和有机矿物部分(OMF,定义为湿粒径<100μm的部分)的重金属吸附和解吸行为。 ,Ni,Pb和Zn同时从各种浓度的溶液中吸附。 OMF可逆地吸附金属,显然主要是在每种特定金属的特定位置吸附金属,这与Langmuir等温线与吸附数据的良好拟合保持一致。铅和铜的最大吸附能力。整个H层似乎包括结合不可逆且铬与其他金属(尤其是铜)竞争的位点。建议使用有机矿物分数来评估土壤有机质对重金属固着的贡献。

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