Université Lille 1, Laboratoire Géosystèmes, UMR CNRS 8217, CNRS - Université Lille 1, Avenue Paul Langevin, 59655 Villeneuve d'Ascq, France.
Vrije Universiteit, Brussel (VUB), Laboratory of Analytical and Environmental Chemistry (ANCH), Brussels, Belgium; IRSTEA, UR MALY, 5 rue de la Doua, CS 70077, 69626 Villeurbanne Cedex, France.
Sci Total Environ. 2014 Feb 1;470-471:600-7. doi: 10.1016/j.scitotenv.2013.10.015. Epub 2013 Oct 26.
Sediments in the Deûle River (northern France) are severely polluted by metals in the vicinity of several metallurgical plants. The aim of this paper is to identify the role played by the recurrent resuspension of these polluted sediments by boat traffic on the dissolved Pb and Zn concentrations in the river. For that purpose, several high-frequency on-line monitoring campaigns were performed. Our results clearly suggest that the resuspension of sedimentary particles into the overlying water significantly increased the dissolved electrolabile Pb and Zn contents. This increase does not persist for a long time because at night and during weekends and holidays, when the boat traffic strongly slows down, Pb and Zn concentrations drop again quickly. Our data also indicate that the biological processes (such as photosynthetic and respiration activities), diffusive and benthic fluxes, as well as dilution of pore water into the overlying water during sediment remobilization do not contribute significantly to the sharp increase of dissolved Pb and Zn concentrations in the river during the day. The good correlation between turbidity and electrolabile metal concentration allows us to discard slow AVS (Acid Volatile Sulfides) oxidation as well. Desorption of metals from sediment particles was clearly the most relevant process, responsible for the increase of dissolved Pb and Zn concentrations in the water column.
法国北部迪尔河的沉积物受到附近几家冶金厂金属的严重污染。本文的目的是确定船只交通反复搅动这些受污染沉积物对河流中溶解态 Pb 和 Zn 浓度的影响。为此,进行了多次高频在线监测。我们的结果清楚地表明,沉积物颗粒的再悬浮会显著增加可溶解的 Pb 和 Zn 含量。但这种增加不会持续很长时间,因为在夜间以及周末和节假日,船只交通大幅减速,Pb 和 Zn 浓度又会迅速下降。我们的数据还表明,生物过程(如光合作用和呼吸活动)、扩散和底栖通量,以及在沉积物再悬浮期间孔隙水向表层水的稀释,并没有显著促进河流中溶解态 Pb 和 Zn 浓度在白天的急剧增加。浊度和可溶解金属浓度之间的良好相关性也排除了缓慢的 AVS(酸可挥发硫)氧化。金属从沉积物颗粒上的解吸显然是最重要的过程,导致了水柱中溶解态 Pb 和 Zn 浓度的增加。