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- W2356371378 abstract "：The materials recorded by Datong、Yushu and Shanghai hydrologic meteor ological observatories since late 50 years, including rainfall, flow, concentrat ions of dissolved silicate (Dsi)、DIN(NO3-)、DIP(P2O5) and silt discharge were a nalyzed. The results show a sharp decrease trend of Dsi flux in the Changjiang R iver since late 50 years; and 53.33μmol/L of the dissolved silicate concentrati on decreased from 1959 to 1984, which came mainly from the dam constructions and the eutrophication formed by industry and agriculture of fertilizer, pesticide, etc. The relation of Dsi flux with silt discharge is positive, but negative wit h DIN and DIP; and complex with flow and rainfall: positive as flow27 386 m3/s and rainfall 1210 mm/a but negative as they are greater respectively. It will l ead to the development of limiting factor of biologic nutrients in the Changjia ng River estuary and East China Sea from N limiting and P limiting to Si limitin g." @default.
- W2356371378 created "2016-06-24" @default.
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- W2356371378 date "2001-01-01" @default.
- W2356371378 modified "2023-09-26" @default.
- W2356371378 title "Changes of dissolved silicate flux from the Changjiang River into sea and its in fluence since late 50 years." @default.
- W2356371378 hasPublicationYear "2001" @default.
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