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[喀斯特地下河中多环芳烃的水-沉积物分配]

[Water-Sediment Partition of Polycyclic Aromatic Hydrocarbons in Karst Underground River].

作者信息

Lan Jia-cheng, Sun Yu-chuan, Xiao Shi-zhen

出版信息

Huan Jing Ke Xue. 2015 Nov;36(11):4081-7.

Abstract

Based on polycyclic aromatic hydrocarbons (PAHs) field data of dissolved phase and sediment phase, partition coefficient K(p) in sediment-water interface from Laolongdong underground river was obtained. The concentration of PAHs in water and sediment and partition coefficient K(p) in sediment-water interface were studied. The results showed PAHs concentrations were 81.5-8 089 ng x L(-1) with a mean value (1 439 ± 2 248) ng x L(-1) in water and 58.2-1 051 ng x g(-1) with an average (367.9 ± 342.6) ng x g(-1) in sediment. The dominant PAHs were 2-3 rings PAHs in water and sediment. However, high rings PAHs obviously enriched in the sediment. Partition coefficients varied from 55.74 to 46 067 L x kg(-1) in sediment-water interface, increasing with the rise of PAH compounds. All the organic carbon partition in sediment-water interface were higher than predicate values based on typical model of equilibrium distribution indicated that PAHs were strongly adsorbed in sediment. The linear free-energy relationship coefficient between K(oc) value and octanol-water partition coefficient K(ow) was 0.75, but the slope was lower than 1, indicating that sediment in Laolongdong underground river had weakly lipophilic characteristics and adsorption ability for PAHs.

摘要

基于多环芳烃(PAHs)溶解相和沉积物相的现场数据,获得了老龙洞地下河沉积物 - 水界面的分配系数K(p)。研究了水中和沉积物中PAHs的浓度以及沉积物 - 水界面的分配系数K(p)。结果表明,水中PAHs浓度为81.5 - 8089 ng x L(-1),平均值为(1439 ± 2248) ng x L(-1);沉积物中PAHs浓度为58.2 - 1051 ng x g(-1),平均值为(367.9 ± 342.6) ng x g(-1)。水中和沉积物中PAHs的主要成分是2 - 3环PAHs。然而,高环PAHs在沉积物中明显富集。沉积物 - 水界面的分配系数在55.74至46067 L x kg(-1)之间变化,随PAH化合物的增加而增大。沉积物 - 水界面的所有有机碳分配均高于基于典型平衡分布模型的预测值,表明PAHs在沉积物中强烈吸附。K(oc)值与正辛醇 - 水分配系数K(ow)之间的线性自由能关系系数为0.75,但斜率低于1,表明老龙洞地下河的沉积物对PAHs具有弱亲脂性特征和吸附能力。

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