Abstract
Heavy metal contamination and their distribution in different size fractions of the surficial sediment in Haihe River, China have been investigated. These results reveal that the heavy metal contamination of Haihe River is closely related to the contaminating sources along the river and has the order: Cd > Cu > Pb > Cr. The contents of these heavy metals in the sediment of Haihe River are at least two times higher than their background values and the highest contaminating metal, Cd, is 15.5 times higher than its background value and determined in the urban area of Tianjin city. The surficial sediments of Haihe River, with 70% particles smaller than 20 μm, belong to sandy clay containing about 28% clay and 42% silt. Electron micrographs and x-ray analysis show that the concentrations of heavy metals depend on the particle size of sediments. The highest concentrations for most metals exist in fine-grained sediments, which are mainly composed of silicates, oxides, and hydroxides of Si, Fe, and Al. In contrast, lower levels of heavy metals are usually found in the coarse sandy sediments, which are composed of quartz, feldspar, and other rocky substances. Based on the results in the present study of the surficial sediments of Haihe River, the contents of Cr, Cu, Pd, and Cd in finer sediments are 2.4, 3.9, 2.8, and 3.6 times higher than those in coarse sandy sediments, respectively. Obviously, because of rapid industrial development in this area during the last few decades, the surficial sediments of Haihe River, especially those finer fractions, have been seriously contaminated by heavy metals.
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Acknowledgements
The authors appreciate China National Basic Research Program for the funding of this research (no. 2003CB415007 and 2004CB418501). We are also grateful to Dr. S. Zhao, Department of Environmental Analysis, China National Environmental Monitoring Center for her valuable comments and suggestions.
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Liu, L., Li, F., Xiong, D. et al. Heavy metal contamination and their distribution in different size fractions of the surficial sediment of Haihe River, China. Environ Geol 50, 431–438 (2006). https://doi.org/10.1007/s00254-006-0226-0
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DOI: https://doi.org/10.1007/s00254-006-0226-0