4.7 Article

Long-term variations in sediment heavy metals of a reservoir with changing trophic states: Implications for the impact of climate change

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 609, Issue -, Pages 242-250

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.scitotenv.2017.04.041

Keywords

Climate change; Reservoir sediments; Heavy metals; Risk assessment; Eutrophic states

Funding

  1. Major State Basic Research Development Program [2010CB951104]
  2. National Natural Science Foundation of China [51121003]

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Two dated sediment cores from the Miyun Reservoir of Beijing in China were analyzed to reconstruct the pollution history of heavy metals including cadmium (Cd), chromium (Cr), iron (Fe), nickel (Ni), and zinc (Zn) as well as phosphorus (P). Enrichment factor (EF) and geoaccumulation index (I-geo) were applied to assess the enrichment status of heavy metals. Average EF and I-geo values indicated that the studied heavy metals in the sediments mainly originated from non-point source pollution and soil-water erosion, showing low ecological risks. In addition, correlation analysis and principal component analysis (PCA) identified that Cd, Zn, and P were mainly from agricultural diffusion pollution caused by utilization of the phosphate fertilizer; Zn, Ni, and Cr originated from soil erosion. PCA analysis was further conducted to investigate the relationships among meteorological factors, algae dominant total organic carbon (TOC), and heavy metals. Results showed that algae-dominant TOC had strong positive correlation with temperature, which can be explained by that increased temperature accelerated the growth of algae. Meanwhile the opposite loadings between algae-dominant TOC and heavy metal suggested that primary production played an important role in migration and transformation of metals. Moreover, stepwise multiple regression models showed that Fe was sensitive to temperature, which accounted for approximately 39.0% and 40.1% of the variations in Fe of two sediment cores, respectively. Fe showed significant decreasing trends during the past 50 years. Reductive environment of water-sediment interface caused by increasing temperature probably contributed to the restoration of ferric iron, resulting in the release of soluble Fe to overlying waters. Future climate change with elevated temperature and extreme weather events will aggravate the ecological risk of heavy metals in water environment due to the enhanced leaching effect and non-point source pollution as well as the release of heavy metals from sediments to water environment. (C) 2017 Published by Elsevier B.V.

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