PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
Tytuł artykułu

Change characteristics of DSi and nutrition structure at the Yangtze River Estuary after Three Gorges Project impounding and their ecological effect

Autorzy
Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The variation law of dissolved silica (DSi), dissolved inorganic nitrogen (DIN), dissolved inorganic phosphorus (DIP) and nutrition structure after the Three Gorges Project (TGP) impounding as well as their ecological effect were analyzed according to monitoring survey of the Yangtze River Estuary in spring (May) and summer (August) from 2004–2009. The results showed that after impounding, DSi and DIN concentration decreased and increased, respectively. During the study period, DSi decreased by about 63%, while DIN almost tripled. DIP concentration fluctuated slightly. With respect to nutrition structure, N:P increased, whereas Si:P and Si:N declined. According to chemometry standard of nutrient limits, nutrition structure tended to be imbalanced and the limiting factor of phytoplankton growth (P) was studied. Changes of nutrition structure have largely decreased diatom and caused different composition of dominant phytoplankton species. This may change ecosystem structure of the Yangtze River Estuary.
Rocznik
Strony
74--79
Opis fizyczny
Bibliogr. 30 poz., tab., wykr.
Twórcy
autor
  • East China Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, China
autor
  • East China Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, China
autor
  • East China Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, China
Bibliografia
  • [1]. Baodong, W. (2006). Culturaleutrophication in the Changjiang (Yangtze River) plume, History and perspective, 69, pp. 471-477.
  • [2]. Boitsov, V.D., Karsakov, A.L. & Trofimov, A.G. (2012). Atlantic water temperature 259 and climate in the Barents Sea, 2000-2009, Ices Journal of Marine Science, 69, pp. 833-840.
  • [3]. Carey, J.C. & Fulweiler, R.W. (2012). Human activities directly alter watershed dissolved silica fl uxes, Biogeochemistry, 111, pp. 125-138.
  • [4]. Cheng, H.Q. & Li, M.T. (2002). Dissolved silicate flux fluctuation from river into the sea: a case study in Changjiang, Resources and Environment in the Yangtze Basin, 10(6), pp. 558-563. (in Chinese)
  • [5]. Conley, D.J., Chelske, C.L. & Stoermer, E.F. (1993). Modification of the biogeochemical cycle of silica with eutrophication, Marine Ecology Progress Series, 101, pp. 179-192.
  • [6]. Edmond, J.M., Spivack, A., Grant, B.C., Hu, M.-H., Chen, Z., Chen, S. & Zeng, X. (1983). Chemical dynamics of the estuary of the Changjiang River, Proceeding of international symposium on sedimentation on the continental shelf with special reference to the East China Sea, 1, pp.251-262.
  • [7]. Friedl, G. & Wüest, A. (2002). Disrupting biogeochemical cycles consequences of damming, Aquatic Sciences-Research across boundaries, 64, pp. 55-65.
  • [8]. Froelich, P.N. (1988). Kinetic control of dissolved phosphate in natural rivers and estuaries: a primer on the phosphate buffer mechanism, Limnology and Oceanography, 33, pp. 649-668.
  • [9]. Gu, H., Yu, Z., Wang, G., Wang, J., Ju, Q., Yang, C. & Fan, C. (2015). Impact of climate change on hydrological extremes in the Yangtze River Basin, China, Stochastic Environmental Research & Risk Assessment, 29, pp. 693-707.
  • [10]. Humborg, C., Ittekkot, V., Cociasu, A. & Bodungen, B.V. (1997). Effect of Danube River dam on Black Sea biogeochemistry and ecosystem structure, Nature, 386, pp. 385-388.
  • [11]. Jeong, H.J., Yoo, Y.D., Lee, K.H., Kim, T.H., Seong, K.A., Kang, N.S., Lee, S.Y., Kim, J.S., Kim, S. & Yih, W.H. (2013). Red tides in Masan Bay, Korea in 2004-2005: I. daily variations in the abundance of red-tide organisms and environmental factors, Harmful Algae, 30, pp. 75-88.
  • [12]. Justic, D., Rabalais, N.N., Turner, R.E. & Dortch, Q. (1995). Changes in nutrient structure of river-dominated coastal waters: stoichiometric nutrient balance and its consequences, Estuarine, Coastal and Shelf Science, 40(3), pp. 339-356.
  • [13]. Kostecki, M. & Suschka, J. (2013). The successful results of Plawniowice reservoir (upper Silesia region-south of Poland) restoration by hypolimnetic withdrawal, Archives of Environmental Protection, 39, pp. 17-25.
  • [14]. Li, M.T. & Chen, H.Q. (2001). Changes of dissolved silicate flux from the Changjiang River into sea and its influence since late 50 years, China Environmental Science, 21, pp. 193-197. (in Chinese)
  • [15]. Li, X., Yang, L. & Yan, W. (2011). Model analysis of dissolved inorganic phosphorus exports from the Yangtze River to the estuary, Nutrient Cycling in Agroecosystems, 90, pp. 157-170.
  • [16]. Liu, R.Y. & Luo, B.Z. (1992). Impacts of the three gorges project on the ecology and environment of the Changjiang river estuary and adjacent waters, Studia Marina Sinica, 33,pp. 1-13. (in Chinese)
  • [17]. Medeiros, P.R.P., Knoppers, B.A., & Cavalcante, G.H. (2011). Changes in nutrient loads (N, P and Si) in the São Francisco estuary after the construction of dams, Brazilian Archives of Biology & Technology, 54, pp. 387-397.
  • [18]. Ning, X.R., Shi, J.X., Cai, Y.M. & Liu, C. (2004). Biological productivity front in the Changjiang Estuary and the Hangzhou Bay and its ecological effects, Acta Oceanologica Sinica, 26, pp. 96-106. (in Chinese)
  • [19]. Rantajärvi, E., Gran, V., Hällfors, S. & Olsonen, R. (1997). Effects of environmental factors on the phytoplankton community in the Gulf of Finland-unattended high frequency measurements and multivariate analyses, Hydrobiologia, 363, pp. 127-139.
  • [20]. Redfield, A.C., Ketchum, B.H. & Richards, F.A. (1963). The influence 296 of organisms on the composition of seawater, New York: John Wiley, Sea, pp. 26-77.
  • [21]. Sellner, K.G., Doucette, G.J. & Kirkpatrick, G.J. (2003). Harmful algal blooms: causes, impacts and detection. Journal of Industrial Microbiology & Biotechnology, 30, pp. 383-406.
  • [22]. Sharp, J.H. (2003). Long term nutrient trends and phytoplankton response in Delaware Estuary. USA. Dallas: Crown Press.
  • [23]. Smetacek, V. (1998). Biological oceanography: Diatoms and the silicate factor, Nature, 391, pp. 224-225.
  • [24]. Tarkowska-Kukuryk, M. (2013). Effect of phosphorous loadings on macrophytes structure and trophic state of dam reservoir on a small lowland river (Eastern Poland), Archives of Environmental Protection, 39, pp. 33-46.
  • [25]. Treguer, P., Nelson, D.M., Van Bennekom, A.J., DeMaster, D.J., Leynaert, A. & Quéguine, B.(1995). The silica balance in the world ocean: a reestimate, Science, 268,pp. 375-379.
  • [26]. Turner, R.E. & Rabalais, N.N. (1991). Changes in Mississippi River water quality this century: implications for coastal food webs, Bioscience, 41, pp. 140-147.
  • [27]. Vitousek, P.M., Aber, J.D., Howarth, R.W., Likens, G.E., Matson, P.A., Schindler, D.W., Schlesinger, W.H. & Tilman, D.G. (1997). Human alteration of the global nitrogen cycle: sources and consequences, Ecological applications, 7, pp. 737-750.
  • [28]. Yu, L.H., Li, D.J., Fang, T., Li, Y. & Gao, L. (2006). Distributions of DSi, DIN and changes of Si: N ratio on summer in Changjiang estuary before and after storage of Three Gorges Reservoir, Acta Ecologica Sinica, 26, pp. 2817-2826. (in Chinese)
  • [29]. Zhang, C., Wang, L., Zhang, S. & Li, X. (1998). Geochemistry of rare earth elements in the mainstream of the Yangtze River, China, Applied Geochemistry, 13, pp. 451-462.
  • [30]. Zhang, J., Wu, Y., Jennerjahn, T.C., Ittekkot, V. & He, Q. (2007). Distribution of organic matter in the Changjiang (Yangtze River) Estuary and their stable carbon and nitrogen isotopic ratios: Implications for source discrimination and sedimentary dynamics, Marine Chemistry, 106, pp. 111-126.
Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-ca80d5a0-f5f7-44e2-8b51-d800c55b3b39
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.