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The origin,historical variations,and distribution of heavy metals in the Qiongzhou Strait and nearby marine areas
Authors:Zhiqiang Zhang  Liang Chen  Weiping Wang  Tuanjie Li  Tingting Zu
Institution:1.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences: CAS Key Laboratory of Marginal Sea Geology,Guangzhou,P. R. China;2.South China Sea Branch of State Oceanic Administration,Guangzhou,P. R. China;3.South China Sea Branch Institute of Oceanology,Chinese Academy of Sciences,Guangzhou,P. R. China
Abstract:We analyzed heavy metal concentrations in a number of surface sediments and cores from the Qiongzhou Strait and surrounding marine areas. The areas of high concentrations are primarily outside the eastern mouth of the Qiongzhou Strait and on the west side of the Leizhou Peninsula, whereas the areas of low concentrations are located primarily in the eastern Qiongzhou Strait. The maximum Cd, Pb and Zn concentrations in the samples collected in our study do not exceed the official standards for marine sediments, whereas the concentrations of Cr and Cu slightly exceed the standards. Correlations exist between the concentrations of Cu, Pb, Zn, Cr and Cd, and the concentrations of these metals are positively correlated with the mean particle size (φ value), indicating that the finer sediments have adsorbed greater amounts of heavy metal elements than the coarser sediments. An evaluation of the potential environmental risks demonstrates that certain indices of heavy metal pollution and environmental risks are relatively low and may be assigned low risk levels, thereby indicating that, in terms of heavy metals, the marine sedimentary environment in this region is only mildly impacted. Our analysis of the contaminant origins shows that the heavy metals in this region primarily originate in the Pearl River Estuary and that a small amount of them is derived from local runoff. The elevated heavy metal concentrations from the upper sections of the cores started 130 years ago, which indicats that heavy metals in the surface sediments are primarily due to human activities associated with industrialization.
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