铅共存对菲在土壤中的吸附行为的影响
首发时间:2010-12-28
摘要:本文以壤质黄土和皂土为研究对象,采用静态吸附的方法研究Pb2+存在下对菲的吸附等温线的影响。动力学实验发现菲在吸附过程中,溶液的pH有所升高。且通过降低土壤溶液初始pH,发现将有利于菲在黄土以及皂土上的吸附。因此,为了避免重金属离子带来的pH降低从而增加菲的吸附,我们特别将吸附实验初始pH固定在5.8±0.1。在此pH条件下,我们研究了Pb共存条件下菲的吸附等温线,结果表明:在研究的浓度范围,其吸附均为线性。重金属Pb的存在一定程度上促进了菲的吸附。重金属对黄土吸附菲的促进作用可能是由于铅降低了黄土中水溶性有机质(DOM)的浓度,使得其固相有机质的含量增加,从而促进了对菲的吸附。而通过烧灼减少黄土的有机质含量后,Pb对其吸附菲的强化作用更加显著,说明这种强化作用可能部分与土壤有机质无关。在皂土上发现的促进效果证明了这一推论;这可能是因为吸附的重金属与溶液中的菲形成阳离子-π键的缘故。
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Influence of the coexisting Pb2+ on the phenanthrene adsorption behavior in the soil
Abstract:The potential influences of coexisting heavy metal solutions on the phenanthrene adsorption capacity were studied by series of batch experiments, where a natural clayish soil and bentonite were tested. The adsorption kinetic experiments show that the solution pH increases during the phenanthrene adsorption. As a result, a low initial pH in the solution facilitates the phenanthrene adsorption. Therefore, to eliminate the influence of the pH decrease resulting from the added heavy metal solution, the initial pH of the adsorption experiments was all adjusted at 5.8±0.1. Under this pH condition, we found that the phenanthrene adsorption isotherm is all linear in the studied concentration range. The presence of Pb2+ all increases the adsorption capacity of phenanthrene to some extent. In the natural clayish soil, such an enhancement could be partly attributed to the decreased organic matter in solution and increased SOM. However, when part of SOM in the clayish soil was destroyed by heating over 550 oC, phenanthrene adsorption enhanced by Pb was more significant, indicating that the enhancement may be partly independent of SOM. That speculation is corroborated by the similar enhancement phenomenon observed on bentonite, which may be the results of the formation of cation-π bond between the adsorbed soft metal cations and aromatic ring of the phenanthrene in solution.
Keywords: Soil adsorption heavy metals poly aromatic compounds
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