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Zheng Jianlu,Lin Zhiqing,Chen Yang. 1989. A study on chemical forms of heavy metals in the sediments of Zhujiang River and its estuary. Acta Oceanologica Sinica, (2):223-235
A study on chemical forms of heavy metals in the sediments of Zhujiang River and its estuary
A study on chemical forms of heavy metals in the sediments of Zhujiang River and its estuary
Received:February 13, 1988  Revised:October 05, 1988
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Author NameAffiliation
Zheng Jianlu South China Sea Institute of Oceanology, Academia Sinica, Guangzhou, China 
Lin Zhiqing South China Sea Institute of Oceanology, Academia Sinica, Guangzhou, China 
Chen Yang Zhejiang University, Hangzhou, China 
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Abstract:
      The five chemical bound forms of Fe, Al and Mn in sediments in the main channel of the Zhujiang River.and its estuary, namely, exchangeable, carbonic, oxidative, organic and residual (in crystal) forms, were determined. The method of sequential extraction was used for separating the five bound forms.
The main chemical form of the three elements in the sediments of the Zhujiang River and its estuarine zone is the residual one. The exchangeable form exists only in a small fraction.
Correlationships between the concentration of a certain form of heavy metals and Eh. pH and salinity were discussed. The principles of geochemistry are used to explain the mechanism of heavy metal transport in the river.
It was also found that the distribution rule of the chemical forms of Fe, Al and Mn in sediments in the lower reaches of the Zhujiang River was similar to the one in the lower reaches of the Yamaska River.
中文摘要:
      The five chemical bound forms of Fe, Al and Mn in sediments in the main channel of the Zhujiang River.and its estuary, namely, exchangeable, carbonic, oxidative, organic and residual (in crystal) forms, were determined. The method of sequential extraction was used for separating the five bound forms.
The main chemical form of the three elements in the sediments of the Zhujiang River and its estuarine zone is the residual one. The exchangeable form exists only in a small fraction.
Correlationships between the concentration of a certain form of heavy metals and Eh. pH and salinity were discussed. The principles of geochemistry are used to explain the mechanism of heavy metal transport in the river.
It was also found that the distribution rule of the chemical forms of Fe, Al and Mn in sediments in the lower reaches of the Zhujiang River was similar to the one in the lower reaches of the Yamaska River.
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