Nutrient characteristics in the Yangtze River Estuary and the adjacent East China Sea before and after impoundment of the Three Gorges Dam.

From November 2002 to 2006, five cruises were undertaken in the Yangtze River Estuary and the adjacent East China Sea to compare the nutrient concentrations, ratios and potential nutrient limitation of phytoplankton growth before and after impoundment (June 2003) of the Three Gorges Dam (TGD). Concentrations of dissolved inorganic nitrogen (DIN), soluble reactive phosphorus (SRP) and total nitrogen (TN) exhibited an increasing trend from 2002 to 2006. In contrast, total phosphorus (TP) concentration exhibited a decreasing trend. The mean concentrations of DIN, SRP, and TN in the total study area increased from 21.4 microM, 0.9 microM, and 41.8 microM in 2002 to 37.5 microM, 1.3 microM, and 82.2 microM in 2006, respectively, while TP decreased from 2.1 microM to 1.7 microM. The concentration of dissolved reactive silica (DRSi) had no major fluctuations and the differences were not significant. The mean concentration of DRSi in the total study area ranged from 52.5 to 92.3 microM. The Si:N ratio decreased significantly from 2.7 in 2002 to 1.3 in 2006, while TN:TP ratio increased from 22.1 to 80.3. The area of potential P limitation of phytoplankton growth expanded after 2003 and potential Si limitation appeared in 2005 and 2006. Potential P limitation mainly occurred in an area of salinity less than 30 after 2003, while potential Si limitation occurred where the salinity was greater than 30. By comparison with historical data, the concentrations of nitrate and SRP in this upper estuary during November 1980-2006 increased obviously after impoundment of TGD but DRSi decreased. Meanwhile, the ratios of N:P, Si:N and Si:P decreased obviously.

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

[2]  H. Barnes Apparatus and methods of oceanography , 1959 .

[3]  Yixin Yan,et al.  Sediment transport from the Yangtze River, China, into the sea over the Post-Three Gorge Dam Period : A discussion , 2008 .

[4]  Linda Hayden,et al.  Comment on “Reduction of primary production and changing of nutrient ratio in the East China Sea: Effect of the Three Gorges Dam?” by Gwo-Ching Gong et al. , 2007 .

[5]  Chen Zhang,et al.  Sediment resuspension and implications for turbidity maximum in the Changjiang Estuary , 1998 .

[6]  B. Wehrli,et al.  Is the Iron Gate I reservoir on the Danube River a sink for dissolved silica? , 2004 .

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

[8]  Christoph Humborg,et al.  Effect of Danube River dam on Black Sea biogeochemistry and ecosystem structure , 1997, Nature.

[9]  C. Turley The changing Mediterranean Sea — a sensitive ecosystem? , 1999 .

[10]  S. Gloss,et al.  Buffering of silica and phosphate in a turbid river1 , 1980 .

[11]  G. Gong,et al.  Reduction of primary production and changing of nutrient ratio in the East China Sea: Effect of the Three Gorges Dam? , 2006 .

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

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

[14]  Mingjiang Zhou,et al.  Responses of a coastal phytoplankton community to increased nutrient input from the Changjiang (Yangtze) River , 2008 .

[15]  Alfred Wüest,et al.  Disrupting biogeochemical cycles - Consequences of damming , 2002, Aquatic Sciences.

[16]  D. DeMaster,et al.  Phytoplankton biomass and productivity in the Amazon River plume: correlation with seasonal river discharge , 1996 .

[17]  Xiaoyong Shi,et al.  [Nutrient distribution and its relationship with occurrence of red tide in coastal area of East China Sea]. , 2003, Ying yong sheng tai xue bao = The journal of applied ecology.

[18]  Timothy R. Parsons,et al.  A manual of chemical and biological methods for seawater analysis , 1984 .

[19]  B. Wehrli,et al.  Retention of Sediments and Nutrients in the Iron Gate I Reservoir on the Danube River , 2005 .

[20]  G. Alory,et al.  TOPEX/Poseidonデータ及び線形モデル結果(1964~1999年)による,熱帯太平洋の経年的海水準変動と関連する質量輸送 , 2002 .

[21]  J. Milliman,et al.  Seasonal variations of sediment discharge from the Yangtze River before and after impoundment of the Three Gorges Dam , 2009 .

[22]  L. Ward,et al.  Phytoplankton, nutrients, and turbidity in the Chesapeake, Delaware, and Hudson estuaries , 1988 .

[23]  T. Parsons,et al.  A practical handbook of seawater analysis , 1968 .

[24]  Z. Shi Behaviour of fine suspended sediment at the North passage of the Changjiang Estuary, China , 2004 .

[25]  Terry E. Whitledge,et al.  Does nitrogen or silicon limit phytoplankton production in the Mississippi River plume and nearby regions , 1992 .

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

[27]  E. Stoermer,et al.  Modification of the biogeochemical cycle of silica with eutrophication , 1993 .

[28]  X. P. Huang,et al.  The characteristics of nutrients and eutrophication in the Pearl River estuary, South China. , 2003, Marine pollution bulletin.

[29]  R. Murtugudde,et al.  Sea surface salinity changes in the East China Sea during 1997–2001: Influence of the Yangtze River , 2002 .

[30]  Hongbin Liu,et al.  Interactions between nutrients, phytoplankton growth, and micro- and mesozooplankton grazing in the plume of the Mississippi River , 2003 .

[31]  Timothy D. Jickells,et al.  Nutrients and chlorophyll at two sites in the Thames plume and southern North Sea , 2001 .

[32]  Yan Bai,et al.  Ecological anomalies in the East China Sea: impacts of the Three Gorges Dam? , 2007, Water research.

[33]  J. P. Riley,et al.  Formation kinetics of the pink azo dye in the determination of nitrite in natural waters , 1990 .

[34]  N. Nielsen H. Barnes: Apparatus and Methods of Oceanography. Chemical. George Allen & Unwin. 334 s. Tabeller, diagrammer og fotos. 22 x 14 cm. London 1959. 40 sh. , 1959 .

[35]  D. Conley,et al.  The transport and retention of dissolved silicate by rivers in Sweden and Finland , 2000 .

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

[37]  J. Strickland A practical hand-book of seawater analysis , 1972 .

[38]  Jurgen Neuberg,et al.  Unprecedented pressure increase in deep magma reservoir triggered by lava‐dome collapse , 2006 .

[39]  P. Raimbault,et al.  The input of nutrients by the Rhône river into the Mediterranean Sea: recent observations and comparison with earlier data , 1998, Hydrobiologia.

[40]  P. Froelich Kinetic control of dissolved phosphate in natural rivers and estuaries: A primer on the phosphate buffer mechanism1 , 1988 .

[41]  C. M. Grant,et al.  THE EXCHANGE OF PHOSPHATE BETWEEN ESTUARINE WATER AND SEDIMENTS1 , 1965 .

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