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Vertical variation of phosphorus forms in surface sediments from Wuli Bay,Taihu Lake,China 被引量:5

Vertical variation of phosphorus forms in surface sediments from Wuli Bay,Taihu Lake,China
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摘要 In order to investigate the cycling of phosphorus in the Taihu Lake, a sequential extraction technique was used to separate different phosphorus forms in surficial sediments from the Wuli Bay of the Taihu Lake. The concentrations of total P are high in the sediments, with an average of {2.80} mg·g+{-1}, and a variation range between {4.02} and {2.05} mg·g+{-1}. Total P is composed mainly of inorganic P (70%-90%), a large portion (75%-85%) of which lies in the CDB-extractable iron oxide phase. The low Fe/P atomic ratios ({2.0}-{5.3}) indicate that the Fe compounds extracted with CDB have a lower proportion of relatively crystalline phases in all samples, and that the absorption between iron and phosphorus has probably reached certain equilibrium. Organic C/N atomic ratios ({8.8}-{10.6}) for most of the samples are lower, which suggests a lacustrine authigenic source of organic matter in the sediments. Moreover, organic C/P atomic ratios (135-320) are usually higher than the Redfield ratio (106∶1), showing that the organic phosphorus had been preferentially released via organic matter degradation during the early diagenesis process. In order to investigate the cycling of phosphorus in the Taihu Lake, a sequential extraction technique was used to separate different phosphorus forms in surficial sediments from the Wuli Bay of the Taihu Lake. The concentrations of total P are high in the sediments, with an average of 2.80 mg ·g^-1, and a variation range between 4.02 and 2.05 mg·g^ -1. Total P is composed mainly of inorganic P (70% -90% ) , a large portion (75% -85% ) of which lies in the CDB-extractable iron oxide phase. The low Fe/P atomic ratios ( 2.0 - 5.3) indicate that the Fe compounds extracted with CDB have a lower proportion of relatively crystalline phases in all samples, and that the absorption between iron and phosphorus has probably reached certain equilibrium. Organic C/N atomic ratios (8.8 - 10.6 ) for most of the samples are lower, which suggests a lacustrine authigenic source of organic matter in the sediments. Moreover, organic C/P atomic ratios ( 135 -320) are usually higher than the Redfield ratio ( 106 : 1 ) , showing that the organic phosphorus had been preferentially released via organic matter degradation during the early diagenesis process.
出处 《Chinese Journal Of Geochemistry》 EI CAS 2006年第3期279-284,共6页 中国地球化学学报
基金 SupportedbytheKnowledgeInnovationMajorProjectsofChineseA-cademyofSciences(Nos.KZCX1-SW-12andKZCX2-105).
关键词 太湖 连续性变化 沉积物 湖泊污染 sequential extraction phosphorus forms sediment Taihu Lake
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