Nutrients in the Changjiang River

N, P and SiO3–Si in the Changjiang mainstream and its major tributaries and lakes were investigated in the dry season from November to December, 1997, and in the flood season in August and October, 1998. An even distribution of SiO3–Si was found along the Changjiang River. However, the concentrations of total nitrogen, total dissolved nitrogen, dissolved inorganic nitrogen, nitrate and total phosphorus, total particulate phosphorus increased notably in the upper reaches, which reflected an increasing impact from human activities. Those concentrations in the middle and lower reaches of the Changjiang River were relatively constant. Dissolved N was the major form of N and the particulate P was the major form of P in the Changjiang River. The molar ratio of dissolved N to dissolved P was extremely high (192.5–317.5), while that of the particulate form was low (5.6–37.7). High N/P ratio reflected a significant input of anthropogenic N such as N from precipitation and N lost from water and soil etc. Dissolved N and P was in a quasi-equilibrium state in the process from precipitate to the river. In the turbid river water, light limitation, rather than P limitation, seemed more likely to be a controlling factor for the growth of phytoplankton. A positive linear correlationship between the concentration of dissolved N and the river’s runoff was found, mainly in the upper reaches, which was related to the non-point sources of N. Over the past decades, N concentration has greatly increased, but the change of P concentration was not as significant as N. The nutrient fluxes of the Changjiang mainstream and tributaries were estimated, and the result showed that the nutrient fluxes were mainly controlled by the runoff, of which more than a half came from the tributaries. These investigations carried out before water storage of the Three Gorges Dam will supply a scientific base for studying the influences of the Three Gorges Dam on the ecology and environment of the Changjiang River and its estuary.

[1]  M. Meybeck Le groupe Eau du PIGB, une réponse à une préoccupation globale croissante = The IGBP Water Group, a response to a growing global concern , 2000 .

[2]  Regional nitrogen budgets and riverine N & P fluxes for the drainages to the North Atlantic Ocean: Natural and human influences , 1996 .

[3]  Y. Wu,et al.  Nutrients in the Changjiang and its tributaries , 2003 .

[4]  D. Vaulot,et al.  Standing stock and production of phytoplankton in the estuary of the Chang-jiang (Yangste River) and the adjacent East China Sea , 1988 .

[5]  B. Whitton,et al.  NITROGEN AND PHOSPHORUS IN EAST COAST BRITISH RIVERS: SPECIATION, SOURCES, AND BIOLOGICAL SIGNIFICANCE , 1998 .

[6]  S. Nixon Coastal marine eutrophication: A definition, social causes, and future concerns , 1995 .

[7]  R. E. Turner,et al.  Changes in Mississippi River Water Quality this CenturyImplications for coastal food webs , 1991 .

[8]  Manfred Ehrhardt,et al.  Methods of seawater analysis , 1999 .

[9]  M. Meybeck Carbon, nitrogen, and phosphorus transport by world rivers , 1982 .

[10]  N. Rabalais,et al.  Changes in nutrient structure of river-dominated coastal waters: stoichiometric nutrient balance and its consequences , 1995 .

[11]  S. M. Liu,et al.  Human impacts on the large world rivers: Would the Changjiang (Yangtze River) be an illustration? , 1999 .

[12]  Hans W. Paerl,et al.  Coastal eutrophication and harmful algal blooms: Importance of atmospheric deposition and groundwater as “new” nitrogen and other nutrient sources , 1997 .

[13]  Paul H. Whitfield,et al.  Seasonal and long-term variations in water quality of the Skeena River at Usk, British Columbia , 1997 .

[14]  B. Hicks,et al.  The atmospheric input of trace species to the world ocean , 1991 .

[15]  Jing Zhang,et al.  Nutrient elements in large Chinese estuaries , 1996 .

[16]  J. Edmond,et al.  Chemical dynamics of the Changjiang estuary , 1985 .

[17]  D. M. Nelson,et al.  The Silica Balance in the World Ocean: A Reestimate , 1995, Science.

[18]  Qun Liu,et al.  A Nitrogen Budget of the Changjiang River Catchment , 2003 .

[19]  Liu Xin CONCENTRATION VARIATION AND FLUX ESTIMATION OF DISSOLVED INORGANIC NUTRIENT FROM THE CHANGJIANG RIVER INTO ITS ESTUARY , 2002 .

[20]  Richard A. Smith,et al.  Streamflow-induced variations in nitrate flux in tributaries to the Atlantic Coastal Zone , 1996 .

[21]  G. Gong,et al.  ‘ Excess Nitrate ’ in the East China Sea , 1998 .

[22]  J. Valderrama,et al.  The simultaneous analysis of total nitrogen and total phosphorus in natural waters , 1981 .

[23]  M. Brzezinski,et al.  THE Si:C:N RATIO OF MARINE DIATOMS: INTERSPECIFIC VARIABILITY AND THE EFFECT OF SOME ENVIRONMENTAL VARIABLES 1 , 1985 .

[24]  C. Qu,et al.  Geochemistry of dissolved and particulate elements in the major rivers of China (The Huanghe, Changjiang, and Zhunjiang rivers) , 1993 .

[25]  H. Casey,et al.  The LOIS river monitoring network: strategy and implementation , 1997 .

[26]  M. McBride Environmental Chemistry of Soils , 1994 .

[27]  Zhi-liang Shen Historical changes in nutrient structure and its influences on phytoplantkon composition in Jiaozhou Bay , 2001 .

[28]  Duan Shui The Variations of Nitrogen and Phosphorus Concentrations in the Monitoring Stations of the Three Major Rivers in China , 1999 .

[29]  N. Rabalais,et al.  LSU Digital Commons LSU Digital Commons Coastal Eutrophication near the Mississippi River Delta Coastal Eutrophication near the Mississippi River Delta , 2022 .

[30]  Dennis P. Swaney,et al.  Regional nitrogen budgets and riverine N & P fluxes for the drainages to the North Atlantic Ocean: Natural and human influences , 1996 .

[31]  Shen Zhiliang A study on the relationships of the nutrients near the Changjiang River estuary with the flow of the Changjiang River water , 1993 .

[32]  J. Schnoor,et al.  Nitrogen fixation: Anthropogenic enhancement‐environmental response , 1995 .

[33]  Jack J. Middelburg,et al.  Hydrogeochemistry of the River Rhine: Long term and seasonal variability, elemental budgets, base levels and pollution , 1989 .

[34]  G. Baturin Phosphorites on the sea floor , 1982 .

[35]  T. Fisher Nutrient limitation of phytoplankton in Chesapeake Bay , 1992 .

[36]  S. Duan Concentrations of nitrogen and phosphorus and nutrient transport to Estuary of the Yangtze River , 2000 .

[37]  Chen-Tung Arthur Chen,et al.  The Three Gorges Dam: Reducing the upwelling and thus productivity in the East China Sea , 2000 .

[38]  C. Humborg,et al.  Nutrient land-sea fluxes in oligothrophic and pristine estuaries of the Gulf of Bothnia, Baltic Sea , 2003 .

[39]  Sepa Key The Characteristics of Nutrients Distribution in the Yangtze River Estuary , 2006 .

[40]  G. Berger,et al.  Nutrient distribution in the Zaire estuary and river plume , 1978 .

[41]  D. Conley,et al.  Annual cycle of dissolved silicate in Chesapeake bay: implications for the production and fate of phytoplankton biomass , 1992 .

[42]  D. DeMaster,et al.  Nutrient dynamics in Amazon shelf waters: results from AMASSEDS , 1996 .

[43]  Is precipitation the dominant controlling factor of high inorganic nitrogen content in the Changjiang River and its mouth? , 2003 .