| 腐殖酸-高岭土复合体形成机制及对三氯乙烯的吸附 |
| 摘要点击 1728 全文点击 1216 投稿时间：2014-03-25 修订日期：2014-08-12 |
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| 中文关键词 有机-矿质复合体 腐殖酸 高岭土 三氯乙烯 吸附 |
| 英文关键词 organic-mineral complexes humic acid kaolin trichloroethylene adsorption |
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| 中文摘要 |
| 为探究土壤中有机组分与无机矿质组分相互作用的机制,以腐殖酸代表有机质、高岭土代表无机矿质,制备不同有机质含量的腐殖酸-高岭土复合体模拟样品,进行三氯乙烯的吸附实验研究. 结果表明,各吸附剂样品对三氯乙烯的吸附符合Freundlich等温模型,且吸附量的实际值与理论叠加值有明显差异,说明复合体样品中腐殖酸与高岭土之间存在相互作用. 结合红外光谱、比表面积孔分析等多类表征,推测腐殖酸与高岭土相互作用的机制为: 腐殖酸含量较低时,腐殖酸分子首先分布于高岭土表面的活性位点上,随着腐殖酸含量的增加(有机质-矿质质量比O/M为0.02~0.04),部分腐殖酸分子进入高岭土表面的孔隙,达到相对稳定后腐殖酸分子继续作用于高岭土表面形成第一层腐殖酸分子膜(O/M为0.04~0.08),随着腐殖酸含量继续增加(O/M为0.08~0.10),更多的腐殖酸分子通过与第一层腐殖酸膜相互作用而在高岭土表面进行第二层叠加,同时第一层被压缩,第二层叠加相对稳定后(O/M为0.10~0.16),仍有部分腐殖酸叠加至第二层之上进行第三层叠加,随后内层腐殖酸进一步被压缩(O/M为0.16~0.24),但可能仍有少量腐殖酸分子和聚集体继续下一层叠加. |
| 英文摘要 |
| The interaction between soil organic components and mineral components was explored in this study. Humic acid and kaolin were used for the preparation of organic-mineral complexes with different contents of organic matter, for experimental study of the adsorption of trichloroethylene. The results showed that the adsorption of trichlorethylene fitted the Freundlich isotherm model. The existence of interaction between humic acid and kaolin was indicated by the significant difference between the actual value and the theoretically overlaid value of the adsorption capacity. With various characterizations, such as FTIR and surface area & pore analysis, the mechanism of interaction between humic acid and kaolin was suggested as follows. When their contents were low, humic acid molecules firstly loaded on the surface binding sites of kaolin. Then with the content increased, as O/M(organic-mineral mass ratio) was 0.02-0.04, some surface pores of kaolin were filled by part of the molecules. After reaching a relatively stable stage, as O/M was 0.04-0.08, humic molecules continued to load on the surface of kaolin and formed the first humic molecule-layer. With humic acid content continued increasing, as O/M was 0.08-0.10, more humic molecules attached to kaolin surface through the interaction with the first layer of molecules and then formed the second layer. O/M was 0.10-0.16 as the whole second layer stage, meanwhile the first layer was compressed. Then when O/M was 0.16-0.24, there were still some humic loadings onto the second layer as the third layer, and further compressed the inner humic acid layers. Besides, some humic acid molecules or aggregates might go on attaching to form as further outer layer. |
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