DISTRIBUTION AND VARIATION OF SILICATE IN THE CHANGJIANG ESTUARY AND ITS ADJACENT WATERS
Shengjun Pan, Shen Zhi-liang
Abstract
Shengjun Pan, Shen Zhi-liang
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 SiO_3-Si are discussed.The results show that the concentrations of SiO_3-Si were higher near the Changjiang estuary and lower outside the sea.Generally,the concentrations of SiO_3-Si were higher in the surface than in the bottom in shore;the opposite distributions off shore.The SiO_3-Si concentrations both inside and outside the mouth in summer and autumn were higher than those in spring and winter. Distributions of SiO_3-Si varied with increase and decrease of runoff and with enlarge and reduce of the extent of Changjiang dilution water.The concentrations of SiO_3-Si in May were relatively less because of phytoplankton blooming.The seasonal variations of SiO_3-Si/ DIN and SiO_3-Si/PO_4-P ratios were mainly controlled by the variations of SiO_3-Si concentrations. Compared with the data of 1985-1986,the concentrations of SiO_3-Si have increased 2.3 times,both SiO_3-Si/DIN and SiO_3-Si/PO_4-P ratios have ascended 1.6 and 2.5 times respectively, which depended on the increasing of the SiO_3-Si concentrations.May is the fitting season of phytoplankton blooming compared with other seasons,in which it is the relatively least that SiO_3-Si/DIN and SiO_3-Si/PO_4-P ratios departure from Redfield ratios.The removals of SiO_3-Si in the estuary showed that aside from biological removal,there was a main effect coming from seawater dilution.
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Based on the data obtained from quarterly investigations in the Changjiang estuary and its adjacent sea areas in 2004,the distributions and variations of SiO_3-Si are discussed.The results show that the concentrations of SiO_3-Si were higher near the Changjiang estuary and lower outside the sea.Generally,the concentrations of SiO_3-Si were higher in the surface than in the bottom in shore;the opposite distributions off shore.The SiO_3-Si concentrations both inside and outside the mouth in summer and autumn were higher than those in spring and winter. Distributions of SiO_3-Si varied with increase and decrease of runoff and with enlarge and reduce of the extent of Changjiang dilution water.The concentrations of SiO_3-Si in May were relatively less because of phytoplankton blooming.The seasonal variations of SiO_3-Si/ DIN and SiO_3-Si/PO_4-P ratios were mainly controlled by the variations of SiO_3-Si concentrations. Compared with the data of 1985-1986,the concentrations of SiO_3-Si have increased 2.3 times,both SiO_3-Si/DIN and SiO_3-Si/PO_4-P ratios have ascended 1.6 and 2.5 times respectively, which depended on the increasing of the SiO_3-Si concentrations.May is the fitting season of phytoplankton blooming compared with other seasons,in which it is the relatively least that SiO_3-Si/DIN and SiO_3-Si/PO_4-P ratios departure from Redfield ratios.The removals of SiO_3-Si in the estuary showed that aside from biological removal,there was a main effect coming from seawater dilution.
Key concepts: Estuary, Phytoplankton, Silicate, Silicon, Mineralogy, Environmental science, Oceanography, Geology