垃圾填埋有色溶解性有机质与铜络合机制

Complexation Between Copper(Ⅱ) and Colored Dissolved Organic Matter from Municipal Solid Waste Landfill

为了阐明填埋场中重金属的形态演变机制,采用三维荧光光谱、荧光猝灭滴定技术及平行因子分析,研究了不同填埋年限垃圾中有色溶解性有机物(colored dissolved organic matter,CDOM)与Cu(Ⅱ)的络合过程.结果表明,填埋垃圾CDOM中含有类蛋白、类富里酸及类胡敏酸物质,随着填埋时间的延伸,类蛋白物质含量呈下降趋势,而类富里酸和类胡敏酸含量呈上升趋势.填埋垃圾CDOM中类蛋白物质对Cu(Ⅱ)络合能力和参与络合的荧光基团比例存在差异,络合的条件稳定常数在4.00~5.75之间,参与络合的荧光基团比例在22.78%~95.30%之间;而类腐殖质与Cu(Ⅱ)作用的条件稳定常数和参与络合的荧光基团比例变化较小,类胡敏酸物质与Cu(Ⅱ)络合的条件稳定常数在4.71~5.54之间,参与络合的荧光基团比例在42.35%~61.46%之间,类富里酸物质与Cu(Ⅱ)络合的条件稳定常数在4.44~5.25之间,参与络合的荧光基团比例在46.14%~57.22%之间.类富里酸和类胡敏酸与Cu(Ⅱ)的结合能力都随着填埋年限的增加而降低,但参与络合的荧光基团比例增加,并且类胡敏酸物质与重金属的结合能力强于类富里酸,但参与配位的官能团较类富里酸少.

In order to elucidate the evolution mechanism of heavy metal species in landfill cells, three-dimensional excitation emission matrix fluorescence spectroscopy （3DEEM）, fluorescence quenching titration and parallel factor analysis （PARAFAC） were employed to study the complexation process between Cu（Ⅱ） and colored dissolved organic matter （CDOM） from landfill with different ages. The experimental results indicated that the landfilled CDOM comprised protein-like, humic-like and fuvic-like matter. The relative content of protein-like matter decreased during the landfill process, whereas the humic-like and fuvic-like matter increased during the process. The range of the conditional stability constants and the percentage of fluorophores participated the complextion between Cu（Ⅱ） and protein-like matter with different ages were 4.00-5.75 and 22.78%-95.30%, respectively. Those parameters changed slightly for humic-like matter with different ages, which ranged from 4.71 to 5.54 and from 42.35% to 61.46%, respectively. As regard to fulvic-like matter, those parameters were 4.44-5.25 and 46.14%-57.22%, respectively. The complexation ability of humic-like substances with Cu（Ⅱ） decreased during the landfill process, though the percentage of fluorophores participated the complexation increased. The complexation ability of humic-like substances with Cu（Ⅱ） was stronger than that of fulvic-like matter, though the percentage of fluorophores participated the complexation in humic-like matter was low compared with fulvic-like matter.