| Autor: |
Liu Qizhen, Li Jiufa, Ying Ming, Li Daoji, Zuo Shuhua, Xie Jun |
| Předmět: |
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| Zdroj: |
Chinese Journal of Geochemistry; 2007, Vol. 26 Issue 1, p84-90, 7p, 3 Charts, 3 Graphs, 1 Map |
| Abstrakt: |
Dissolved inorganic nutrient elements were analyzed from the samples collected in the South Passage of the Changjiang (Yangtze River) Estuary in March 2003, including NH4 +, NO3 −, NO2 − and PO4 3−. The water samples were collected with a Niskin sampler hourly at the near-surface, middle and near-bottom depths at the three stations—A1, A2 and A3—during two complete tidal cycles of neap tide and spring tide. Results showed that 1) the concentrations of NH4 +, NO3 − and NO2 − were a little higher respectively during the neap tide than those during the spring tide, while PO4 3− showed an opposite trend, and each was higher in the ebb tide than in the flood tide, either for the neap tidal cycle or the spring tidal cycle; 2) higher stratification of the nutrients existed obviously in this area, with the concentrations of which increased from the bottom to the surface, especially for NH4 + and NO3 −; 3) the coefficient of variation (C.V.) values of all dissolved inorganic nutrients varied from 4.06% to 36.8% beyond different influences of the tidal current and Changjiang runoff; 4) with increasing suspended matter in the water column, the concentrations of PO4 3− became lower in the filtered water; and 5) the total transport of each tidal cycle was much more in the spring tide than in the neap tide, and the positive values indicated that the nutrients had been exported to the East China Sea. Studies on the variations and net transport of dissolved inorganic nutrients in the South Passage of the Changjiang Estuary will provide the scientific basis for the study of the mechanism of red tide in the East China Sea. [ABSTRACT FROM AUTHOR] |
| Databáze: |
Complementary Index |
| Externí odkaz: |
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