Philipps-University of Marburg, Faculty of Geography, Working Group for Hydro- and Soil Geography, Deutschhausstr. 10, 35037 Marburg, Germany.
University of Koblenz-Landau, Institute for Integrated Natural Sciences, Geography Department, Universitätsstr. 1, 56070 Koblenz, Germany.
Sci Total Environ. 2018 Nov 1;640-641:1072-1081. doi: 10.1016/j.scitotenv.2018.05.295. Epub 2018 Jun 6.
The draining of a dam is a relatively rare event, however, it can have severe consequences for a watercourse connected to that reservoir. In order to understand the effects of the draining on the mobility of pollutants stored in the bottom sediments, the concentrations of heavy metals and arsenic were measured in pore water, river water, and sediments sampled from three emptied reservoirs in Germany. Two of these sites were analyzed immediately after the draining, while the third reservoir was studied one and a half years after the complete discharge of the stored water. Heavy metal and arsenic concentrations within the sediments varied among the studied dams as a result of different geological characteristics and the degree of anthropogenic impacts. Based on the analysis of pore water samples, the concentrations of heavy metals and arsenic were not significantly altered shortly after the draining. However, increased concentrations of As, Fe, Cd, Ni, and Zn were measured in pore water samples after a longer duration of sediment exposure, which altered the redox conditions and sediment properties. The changes in Cu, Cr, Mn, and Pb concentrations in pore water samples were less pronounced. As a result of the pore water drainage increased dissolved heavy metal concentrations were found in the discharge water immediately after draining. At the third site, which had been emptied for one and a half years, only for Mn, a concentration increase was detected in the reservoir discharge water, which emphasizes the strong temporal dynamic of the mobilization of the analyzed elements.
大坝排水是一个相对罕见的事件,但它会对与该水库相连的水道产生严重后果。为了了解排水对储存在底泥中的污染物迁移的影响,对从德国三个排空水库采集的孔隙水、河水和沉积物中的重金属和砷浓度进行了测量。其中两个地点在排水后立即进行了分析,而第三个水库在储存水完全排出一年半后进行了研究。由于不同的地质特征和人为影响程度,研究中的大坝沉积物中的重金属和砷浓度存在差异。基于孔隙水样本的分析,排水后不久重金属和砷的浓度并没有明显改变。然而,在更长时间的沉积物暴露后,在孔隙水样本中测量到了 As、Fe、Cd、Ni 和 Zn 的浓度增加,这改变了氧化还原条件和沉积物特性。Cu、Cr、Mn 和 Pb 浓度在孔隙水样本中的变化不太明显。由于孔隙水的排水,在排水后立即在排放水中发现了溶解态重金属浓度的增加。在已经排空一年半的第三个地点,只有 Mn 在水库排放水中检测到浓度增加,这强调了分析元素的迁移具有很强的时间动态性。