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长江口及其邻近水域硅酸盐的公布变化特征
潘胜军,沈志良
1.中国科学院海洋研究所海洋生态与环境科学重点实验室,中国科学院研究生院;2.中国科学院海洋研究所
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基金项目:国家重点自然科学基金项目,中国科学院知识创新工程方向项目,国务院三峡工程建设委员会资助项目
Distribution and variation of silicate in the Changjiang estuary and its adjacent waters
Pan Shengjun1,2, Shen Ziliang3
1.Key laboratory of Marine Ecology and Environmental Science,Institute of Oceanology,Chinese ,Academy of Sciences;2.Graduate University of Chinese Academy of Sciences;3.Key laboratory of Marine Ecology and Environmental Science,Institute of Oceanology,Chinese ,Academy of Sciences
Abstract:
Based on the data obtained from quarterly investigations in the Changjiang estuary and its adjacent sea areas in 2004,the distributions and variations of SiO3-Si are discussed. The reslts show that the concentrations of SiO3-Si were higher near the changjiang estuary and lower outside ghe sea.Generally,the concentrations of SiO3-Si were higher in the surface than in the buttomin shore;the opposite distributions off shore.The SiO3-Si concentrations both inside and outside the mouth in summer and autumn were higher than those in spring and winter.Distributions of SiO3-Si varied with increase and decrease of runlff and with enlarge and reduce of the extent of Changjiang dilution water.The concentrations of SiO3-Siin May were relatively less because of phytoplankton blooming. The seasonal variations of SiO3-Si/DIN and SiO3-Si/PO4-P ratios were mainly controlled by the variations of SiO3-Siconcentrations. Compared with the data of 1985-1986, the concentrations of SiO3-Sihave inereased2.3 times,both SiO3-Si DIN and SiO3-Si/PO 4-P ratios have ascended 1.6 and2.5 times respectively, which depended on the increasing of the SiO3-Si concentrations,May is the fitting season of phytoplankton blooming compared with other seasons,in which it is the relaively least that SiO3-Si/DIN and SiO3-Si/PO 4-P ratios departure from Redfield ratios. The removals of SiO3-Siin the estuary showed that aside from biological removal, there was a main effect coming from seawater dilution.
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