Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China; University of Chinese Academy of Sciences, Beijing, 100049, China.
Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, 100085, China; Hangzhou Institute for Advanced Study, UCAS, Hangzhou, 310024, China; University of Chinese Academy of Sciences, Beijing, 100049, China.
Chemosphere. 2022 Jan;287(Pt 3):132265. doi: 10.1016/j.chemosphere.2021.132265. Epub 2021 Sep 15.
Spatial trends, partitioning behavior, and potential sources of polychlorinated naphthalenes (PCNs) in water-sediment system from the Yangtze River Delta (YRD) were investigated in this study. The total concentrations of 75 PCNs in water and sediment samples were 0.022-0.310 ng/L and 0.01-1.59 ng/g dry weight, respectively. The homolog patterns in the sediment and water samples were somewhat different. Di-to tetra-CNs made larger contributions in the sediment, while the mono-to tri-CNs were dominant homologs in the water. Overall, the low-chlorinated naphthalenes (mono-to tetra-CNs) were found to be the dominant homologs in the YRD water and sediment samples, and the homolog group contributions to the total PCNs concentrations decreased as the number of chlorine atoms increased. CN-5/7 and CN-24/14 were found at high concentrations in both the water and sediment. Partitioning and transfer of PCNs between water and sediment were assessed by calculating the partition coefficients and fugacity fractions. The partition coefficients showed that PCNs were not in equilibrium status in the water-sediment system, and hydrophobicity played an important role in PCNs partitioning. The fugacity fractions indicated that mono- to tri-CNs had stronger tendencies to escape from the sediment into the water, while the high-chlorinated naphthalenes close to equilibrium. Principal component analysis and correlation analysis indicated that industrial thermal processes and the use and disposal of products containing PCNs industrial products are sources of PCNs in the YRD water-sediment system.
本研究调查了长江三角洲(YRD)水-沉积物系统中多氯萘(PCNs)的空间分布趋势、分配行为和潜在来源。水和沉积物样品中 75 种 PCN 的总浓度分别为 0.022-0.310ng/L 和 0.01-1.59ng/g 干重。沉积物和水样中的同系物模式有些不同。二到四氯萘在沉积物中贡献较大,而一到三氯萘是水中的主要同系物。总体而言,低氯萘(一到四氯萘)是 YRD 水和沉积物样品中的主要同系物,同系物组对总 PCN 浓度的贡献随氯原子数的增加而降低。CN-5/7 和 CN-24/14 在水和沉积物中均有高浓度存在。通过计算分配系数和逸度分数评估了 PCNs 在水-沉积物之间的分配和转移。分配系数表明 PCNs 在水-沉积物系统中未达到平衡状态,疏水性在 PCNs 分配中起着重要作用。逸度分数表明一到三氯萘有更强的从沉积物进入水中的趋势,而高氯萘则接近平衡。主成分分析和相关分析表明,工业热过程以及使用和处置含 PCN 产品是 YRD 水-沉积物系统中 PCN 的来源。