State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China; Department of Water Environment, China Institute of Water Resources and Hydropower Research, Beijing 100038, China.
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China; Department of Water Environment, China Institute of Water Resources and Hydropower Research, Beijing 100038, China.
Sci Total Environ. 2020 May 10;716:136914. doi: 10.1016/j.scitotenv.2020.136914. Epub 2020 Jan 27.
Cascade reservoirs facilitate the effective use of water resources and help to alleviate existing problems of water shortage in drought-prone regions. However, the geochemical behavior and controlling mechanisms of trace metals in response to the operation of cascade reservoirs are relatively unknown. Here, trace metals (As, Cr, Cu, Li, Ni, Pb and Zn) from thirty sediment cores from cascade reservoirs (Panjiakou and Daheiting Reservoirs) in China were evaluated. Multiple methods including geochemical baseline, geostatistical analysis, factor analysis (FA), and positive matrix factorization (PMF), were combined to assess pollution status, identify and quantify potential anthropogenic sources, and determine the influence of hydrodynamic conditions on trace metals distribution. The results indicate that minor enrichment of trace metals appeared in both cascade reservoirs. However, trace metal concentrations exhibited spatial heterogeneity between two cascade reservoirs, and diverse hotspots of different metals were unexpectedly observed. This can be explained by the following three aspects: (1) Metal hotspots were detected upstream of the cascade dams via geostatistical analysis and FA, particularly for naturally sourced metals (As and Li) where dam interception resulted in higher concentrations in the upstream reservoir. (2) PMF analysis identified agricultural, industrial, and natural sources to account for 23.44%, 41.61%, and 34.95%, respectively, to the metal concentrations in the downstream reservoir. Anthropogenic emissions were the dominant factors influencing the spatial variability of Cu, Pb, and Zn between the cascade reservoirs, with higher concentrations observed in the downstream reservoir. (3) The hydrological regime also influenced the redistribution of human-derived metals, where slower flow velocities at river bends resulted in higher deposition of metal-bearing particles. This study shed light on the spatial distribution of trace metals in response to the construction and operation of cascade reservoirs, and it suggests that trace metal hotspots should be monitored to prevent potential contamination in sediments.
梯级水库有利于水资源的有效利用,并有助于缓解干旱地区现有的水资源短缺问题。然而,对于梯级水库中痕量金属的地球化学行为和控制机制还知之甚少。本研究选取中国潘家口和大黑汀两座梯级水库的 30 个沉积物岩芯,评估了其中的痕量金属(As、Cr、Cu、Li、Ni、Pb 和 Zn)。综合运用地球化学基线、地统计分析、因子分析(FA)和正定矩阵因子分析(PMF)等多种方法,评估污染状况,识别和量化潜在人为污染源,并确定水动力条件对痕量金属分布的影响。结果表明,两座梯级水库均存在痕量金属的轻微富集。然而,两种金属的痕量金属浓度在两个梯级水库之间存在空间异质性,并且意外地观察到不同金属的不同热点。这可以通过以下三个方面来解释:(1)通过地统计分析和 FA,在梯级水坝的上游检测到金属热点,特别是对于自然来源的金属(As 和 Li),由于大坝拦截导致上游水库中的浓度更高。(2)PMF 分析确定了农业、工业和自然来源,分别占下游水库中金属浓度的 23.44%、41.61%和 34.95%。人为排放是影响两座梯级水库中 Cu、Pb 和 Zn 空间变异性的主要因素,下游水库中的浓度更高。(3)水文条件也影响人类衍生金属的再分配,河流弯道处的流速较慢导致携带金属颗粒的沉积增加。本研究揭示了梯级水库建设和运行过程中痕量金属的空间分布情况,表明应监测痕量金属热点,以防止沉积物中的潜在污染。