Lei Kun, Han Xuejiao, Zhao Jian, Qiao Fei, Li Zicheng, Yu Tao
State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China.
Ecotoxicol Environ Saf. 2016 Jun;128:153-60. doi: 10.1016/j.ecoenv.2016.02.019. Epub 2016 Mar 1.
For an improved understanding of the metal behavior between the sediment and overlaying water of Taihu Lake, the technique of diffusive gradients in thin films (DGT) was used to characterize the DGT measured concentration in sediments and release kinetics of Cr, Ni, Cu, Zn, Cd and Pb in representative lake parts. Spatially, the DGT-measured concentration of heavy metals showed that Zn, Cu, Ni, Cr, and Pb had higher concentrations in the northern lake than in the eastern Lake Taihu. The order of the release flux for the studied metals from sediments to overlaying water was Zn>Cu>Ni, Cr>Pb>Cd (p<0.05). DGT devices were deployed over a series of time (0.5, 1, 2, 4, 8, 12, 24 and 48 h) in sediment cores from the two typical lake parts (northwest algae dominant area and southeast macrophyte dominant area) to explore the dynamics in the sediment/DGT system, and the best fitted regression model was selected to characterize the release of metals in the two lake parts. The fitted results showed that the equilibration time of the metal release was approximately 24h and Zn had a higher release capacity than other metals. Further analyses indicated that significant correlation existed between the DGT-measured metal concentrations in sediments and metal concentrations in lake organisms (r=0.943 and 0.996 for zoobenthos and coilia ectenes, p<0.05), suggesting that DGT technique is more effective to predict the metal bioavailability in lake sediments.
为了更好地理解太湖沉积物与上覆水之间的金属行为,采用薄膜扩散梯度技术(DGT)来表征沉积物中DGT测定浓度以及太湖代表性区域中铬、镍、铜、锌、镉和铅的释放动力学。在空间上,DGT测定的重金属浓度表明,北部湖区的锌、铜、镍、铬和铅浓度高于太湖东部。研究的金属从沉积物到上覆水的释放通量顺序为锌>铜>镍,铬>铅>镉(p<0.05)。在太湖两个典型区域(西北藻类主导区和东南大型植物主导区)的沉积物岩芯中,在一系列时间(0.5、1、2、4、8、12、24和48小时)内部署DGT装置,以探索沉积物/DGT系统中的动态变化,并选择最佳拟合回归模型来表征两个湖区金属的释放情况。拟合结果表明,金属释放的平衡时间约为24小时,锌的释放能力高于其他金属。进一步分析表明,沉积物中DGT测定的金属浓度与湖泊生物体内的金属浓度之间存在显著相关性(底栖动物和凤鲚的r分别为0.943和0.996,p<0.05),这表明DGT技术在预测湖泊沉积物中金属生物有效性方面更有效。