Key Laboratory for Water and Sediment Science of Ministry of Education, School of Environment, Beijing Normal University, Beijing 100875, China.
Chemosphere. 2013 Feb;90(6):2020-6. doi: 10.1016/j.chemosphere.2012.10.079. Epub 2012 Nov 28.
Historical profiles and sources of PAHs at two typical sediment cores (i.e., the shipping route site and the shoal site) were fully compared to probe the controlling factors, specifically the water currents, for the PAHs deposition processes in the Yangtze River Estuary. Compared with ocean water currents, river runoff affected by the water impoundment of the Three Gorges Dam greatly affected the PAHs levels and percent contribution of PAHs sources in the two cores. River runoff hindered the PAHs deposition in shoal site, while a contrary phenomenon was observed for the shipping route site. Though the PAHs in the estuary were mainly from river catchment, only low ring PAHs in the shipping route site were mainly from the upper reach of the river. Coarse sediments with higher organic carbon content also accounted for the higher deposition levels of PAHs in the shipping route site.
对两个典型沉积物岩芯(即航道区和浅滩区)中的多环芳烃的历史分布特征和来源进行了充分的对比,以探究多环芳烃在长江口沉积过程的控制因素,特别是水流的作用。与海洋水流相比,受三峡大坝蓄水影响的河川径流对两个岩芯中的多环芳烃水平和多环芳烃来源的百分比贡献有很大影响。河川径流阻碍了浅滩区的多环芳烃沉积,而在航道区则观察到了相反的现象。尽管河口的多环芳烃主要来自河流流域,但航道区仅低环多环芳烃主要来自河流上游。高有机碳含量的粗沉积物也是航道区多环芳烃沉积水平较高的原因之一。