University of Lyon, Université Claude Bernard Lyon 1, Institute of Analytical Sciences, UMR 5280, 5 rue de la Doua, F-69100, Villeurbanne, France; Irstea, UR MALY, 5 rue de la Doua, F-69100, Villeurbanne, France.
University of Strasbourg, Laboratoire Image Ville Environnement UMR 7362 CNRS/UdS/ENGEES, 3 rue de l'Argonne, F-67083, Strasbourg, France.
Sci Total Environ. 2015 Nov 1;532:80-90. doi: 10.1016/j.scitotenv.2015.05.057. Epub 2015 Jun 6.
In urbanized areas, small streams can be greatly damaged by urban inflows and combined sewer overflows. These polluted inputs can be several times higher than the natural stream flow over short time periods. Sound knowledge of the spatial distribution of the discharged pollutants in sediments is therefore crucial for designing monitoring strategies and suitable remediation operations. This field study combines geomorphic characterization, hydraulic conductivity measurement and pollutant assays in sediments of a small suburban river. The study site was divided up into geomorphic units: riffles, pools and runs. The last two were grouped into one class named "pool-runs" owing to their closely similar open channel flow hydraulics. Benthic and hyporheic sediments were sampled at 2m intervals. Conventional particulate pollutants (Cr, Pb, N(org), P(tot) & C(org)) were assayed in samples. The main result was: pollutants were not randomly distributed in the stream sediments, but their location showed clear concentration differences by geomorphic units, with preferential accumulation in the hyporheic zones of riffle units and a lesser one in the hyporheic zones of pools. A decrease in hydraulic conductivity was significantly correlated with an increase in pollutant concentration. This occurred mainly at the transition between riffles and pool units. The down-welling water fluxes in the sediment calculated using Darcy's formula reflect this slowdown. Our findings highlight the need to take into account the geomorphological and hydrological functioning of a stream to accurately locate the biogeochemical hotspots to be treated and thereby develop more relevant monitoring and remediation methodologies.
在城市化地区,小溪可能会受到城市流入物和合流污水溢流的严重破坏。这些受污染的输入物在短时间内可能是自然水流的数倍以上。因此,了解沉积物中排放污染物的空间分布对于设计监测策略和合适的修复操作至关重要。本现场研究结合了形态特征描述、水力传导率测量和沉积物中污染物分析,研究对象是一条小型郊区河流。研究点分为形态单元:急流、水池和流段。由于后两者具有相似的明渠流动水力学特性,因此将最后两个单元归为一类,称为“池流段”。在 2m 的间隔处采集底栖和地下河沉积物样本。对 Cr、Pb、N(org)、P(tot) 和 C(org) 等常规颗粒污染物进行了分析。主要结果是:污染物在溪流沉积物中不是随机分布的,而是根据形态单元位置显示出明显的浓度差异,优先在急流单元的地下河带中积累,而在水池的地下河带中积累较少。水力传导率的降低与污染物浓度的增加呈显著相关。这种情况主要发生在急流和水池单元之间的过渡区。使用达西公式计算的沉积物中的下渗水流通量反映了这种减速。我们的研究结果强调需要考虑溪流的地貌和水文功能,以准确确定需要处理的生物地球化学热点,并由此开发更相关的监测和修复方法。