Removal and Mass Balance of Phosphorus and Silica in the Turbidity Maximum Zone of the Changjiang Estuary
Abstract
The concentration of suspended particulate matter (SPM), sedimentation flux and various forms of phosphorus and silica in turbidity maximum zone (TMZ) in the Changjiang (Yangtze) estuary was studied. Based on the budget of P and Si, their mass balances in the TMZ were calculated. Research results show that the variation in concentration of dissolved inorganic silicon (DISi) was mainly controlled by sea water dilution in the Changjiang estuary, while that of dissolved inorganic phosphorus (DIP) was considerably affected by the buffering of suspended matter and sediment. The sedimentation fluxes of suspended particulate matter and particulate inorganic phosphorus (PIP), total particulate phosphorus (TPP), particulate inorganic silicon (PISi) and biological silicon (BSi) in the TMZ were 238.4 g m−2 d−1 and 28.3, 43.1, 79.0, 63.0 mg m−2 d−1, respectively. In addition, a simple method to estimate the ratio of resuspension of sediment in the TMZ was established, indicating that the sediment resuspension in the TMZ influenced significantly the mass balances of P and Si. Particulate-adsorbed P (60.8%) and 35.5% of TPP discharged from the river were filtered and then deposited in the TMZ. The input flux of PIP from the river mouth was 55.9% of that of DIP, being important as biologically available P, while that of PISi was only 3.5% of DISi, showing that particulate-adsorbed Si was much less important than particulate-adsorbed P.
Keywords
Phosphorus Silica Suspended particulate matter Transport Turbidity maximum zone Changjiang (Yangtze) estuaryReferences
- Allen, G. P., Salomon, J. C., Bassoullet, P., Du Penhoat, Y., & De GrandPre, C. (1980). Effects of tides on mixing and suspended sediment transport in macrotidal estuaries. Sedimentary Geology, 26, 69–90.CrossRefGoogle Scholar
- Bloesch, J., & Burns, N. M. (1980). A critical review of sedimentation trap technique. Schweizerische Zeitschrift fuer Hydrologie, 42, 15–55.Google Scholar
- Bowes, M. J., & House, W. A. (2001). Phosphorus and dissolved silicon dynamics in the River Swale catchment, UK: A mass-balance approach. Hydrological Processes, 15, 261–280.CrossRefGoogle Scholar
- Calmano, W. (1981). Potentially bioavailable phosphorus in sediments of the Weser estuary. Environmental Technology Letters, 2, 443–448.CrossRefGoogle Scholar
- Chambers, R. M., Fourqurean, J. W., Hollibaugh, J. T., & Vink, S. M. (1995). Importance of terrestrially-derived, particulate phosphorus to phosphorus dynamics in a west-coast estuary. Estuaries, 18, 518–526.CrossRefGoogle Scholar
- Chen, S. L., Zhang, G. A., Yang, S. L., & Yu, Z. Y. (2004). Temporal and spatial changes of suspended sediment concentration and resuspension in the Yangtze River Estuary and its adjacent waters. Acta Geographica Sinica, 59, 260–266. (in Chinese with English abstract).Google Scholar
- Conley, D. J., Smith, W. M., Cornwell, J. C., & Fisher, T. R. (1995). Transformation of particle-bound phosphorus at the land-sea interface. Estuarine, Coastal and Shelf Science, 40, 161–176.CrossRefGoogle Scholar
- Edmond, J. M., Boyle, E. A., Grant, B., & Stallard, R. F. (1981). The chemical mass balance in the Amazon plume. 1: The nutrients. Deep-Sea Research, 28, 1339–1374.CrossRefGoogle Scholar
- Edmond, J. M., Spivack, A., Grant, B. C., Hu, M. H., Chen, X., Cheng, S., et al. (1985). Chemical dynamics of the Changjiang estuary. Continental Shelf Research, 4, 17–36.CrossRefGoogle Scholar
- Fang, T. H. (2000). Partitioning and behaviour of different forms of phosphorus in the Tanshui estuary and one of its tributaries, Northern Taiwan. Estuarine, Coastal and Shelf Science, 50, 689–701.CrossRefGoogle Scholar
- Fanning, K. A., & Pilson, M. E. Q. (1973). The lack of inorganic removal of dissolved silica during river-ocean mixing. Geochimica et Cosmochimica Acta, 37, 2405–2415.CrossRefGoogle Scholar
- Fisher, T. R., Harding, L. W., Jr., Stanley, D. W., & Ward, L. G. (1988). Phytoplankton, nutrients, and turbidity in the Chesapeake, Delaware, and Hudson estuaries. Estuarine, Coastal and Shelf Science, 27, 61–93.CrossRefGoogle Scholar
- Fox, L. E., Sager, S. L., & Wofsy, S. C. (1985). Factors controlling the concentrations of soluble phosphorus in the Mississippi estuary. Limnology and Oceanography, 30, 826–832.CrossRefGoogle Scholar
- Fox, L. E., Sager, S. L., & Wofsy, S. C. (1986). The chemical control of soluble phosphorus in the Amazon estuary. Geochimica et Cosmochimica Acta, 50, 783–794.CrossRefGoogle Scholar
- Fox, L. E., Lipschultz, F., Kerkhof, L., & Wofsy, S. C. (1987). A chemical survey of the Mississippi estuary. Estuaries, 10, 1–12.CrossRefGoogle Scholar
- 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, 649–668.Google Scholar
- Gebhardt, A. C., Schoster, F., Gaye-Haake, B., Beeskow, B., Rachold, V., Unger, D., et al. (2005). The turbidity maximum zone of the Yenisei River (Siberia) and its impact on organic and inorganic proxies. Estuarine, Coastal and Shelf Science, 65, 61–73.CrossRefGoogle Scholar
- Hamblin, P. F. (1989). Observations and model of sediment transport near the turbidity maximum of the upper Saint Lawrence estuary. Journal of Geophysical Research, 94, 14419–14428.CrossRefGoogle Scholar
- He, S. L., & Sun, J. M. (1996). Characteristics of suspended sediment transport in the turbidity maximum of the Changjiang river estuary. Oceanologia et Limnologia Sinica, 27, 60–66. (in Chinese with English abstract).Google Scholar
- Herman, P. M. J., & Heip, C. H. R. (1999). Biogeochemistry of the MAximum TURbidity Zone of Estuaries (MATURE): Some conclusions. Journal of Marine Systems, 22, 89–104.CrossRefGoogle Scholar
- Hou, L. J., Lu, J. J., Liu, M., & Xu, S. Y. (2006). Species and bioavailability of phosphorus in surface sediments from the shoals in the Yangtze estuary. Acta Scientiae Circumstantiae, 26, 488–494. (in Chinese with English abstract).Google Scholar
- Jiufa, L., & Chen, Z. (1998). Sediment resuspension and implications for turbidity maximum in the Changjiang estuary. Marine Geology, 148, 117–124.CrossRefGoogle Scholar
- Kaul, L. W., & Froelich, P. N. (1984). Modeling estuarine nutrient geochemistry in a simple system. Geochimica et Cosmochimica Acta, 48, 1417–1433.CrossRefGoogle Scholar
- Koroleff, F., & Grasshoff, K. (1976). Determination of nutrients. In K. Grasshoff (Ed.), Methods of seawater analysis (pp. 117–181). Weinheim: Verlag Chemie.Google Scholar
- Krone, R. B. (1962). Flume studies of the transport in estuarine shoaling processes (p. 110). Berkeley, CA: Hydraulic Engineering Laboratory, University of Berkeley.Google Scholar
- Lebo, M. E. (1991). Particle-bound phosphorus along an urbanized coastal plain estuary. Marine Chemistry, 34, 225–246.CrossRefGoogle Scholar
- Lisitsyn, A. P. (1995). The marginal filter of the ocean. Oceanology, 34, 671–682.Google Scholar
- Mackenzie, F. T., & Garrels, R. M. (1965). Silicates reactivity with seawater. Science, 150, 57–58.CrossRefGoogle Scholar
- Martin, J. M., & Meybeck, M. (1979). Elemental mass-balance of material carried by major world rivers. Marine Chemistry, 7, 173–206.CrossRefGoogle Scholar
- Mayer, L. M., & Gloss, S. P. (1980). Buffering of silica and phosphate in a turbid river. Limnology and Oceanography, 25, 12–22.CrossRefGoogle Scholar
- Milliman, J. D., Shen, H. T., Yang, Z. S., & Meade, R. H. (1985). Transport and deposition of river sediment in the Changjiang estuary and adjacent continental shelf. Continental Shelf Research, 4, 37–45.CrossRefGoogle Scholar
- Muylaert, K., & Sabbe, K. (1999). Spring phytoplankton assemblages in and around the maximum turbidity zone of the estuaries of the Elbe (Germany), the Schelde (Belgium/The Netherlands) and the Gironde (France). Journal of Marine Systems, 22, 133–149.CrossRefGoogle Scholar
- Pan, D. A., Shen, H. T., & Mao, Z. C. (1999). Formation mechanism and features of the turbidity maximum in the Changjiang river estuary. Acta Oceanologica Sinica, 21(4), 62–69. (in Chinese with English abstract).Google Scholar
- Rehm, E. (1985). The distribution of phosphorus in the Weser river estuary. Environmental Technology Letters, 6, 53–64.CrossRefGoogle Scholar
- Salomons, W., & Gerritse, R. G. (1981). Some observations on the occurrence of phosphorus in recent sediments from western Europe. Science of the Total Environment, 17, 37–49.CrossRefGoogle Scholar
- Shen, Z. L. (1993a). The effects of the physic-chemical environment on the primary productivity in the Yangtze river estuary. Transactions of Oceanology and Limnology, 1, 47–51. (in Chinese with English abstract).Google Scholar
- Shen, Z. L. (1993b). A study on the relationships of the nutrients near the Changjiang river estuary with the flow of the Changjiang river water. Chinese Journal of Oceanology and Limnology, 11, 260–267. (in Chinese with English abstract).CrossRefGoogle Scholar
- Shen, H. T., & Pan, D. A. (2001). Turbidity maximum in the Changjiang estuary. Beijing: China Ocean Press. (in Chinese with English abstract).Google Scholar
- Shen, Z. L., Lu, J. P., Liu, X. J., & Diao, H. X. (1992). Distribution characters of the nutrients in the Changjiang river estuary and the effect of the Three Gorges project on it. Institute of Oceanology, Chinese Academy of Sciences. Studia Marina Sinica, 33, 109–129. Beijing: Science Press (in Chinese with English abstract).Google Scholar
- Sholkovitz, E. R., van Grieken, R., & Eisma, D. (1978). The major-element composition of suspended matter in the Zaire river and estuary. Netherlands Journal of Sea Research, 12, 407–413.CrossRefGoogle Scholar
- Siever, R., & Woodford, N. (1973). Sorption of silica by clay minerals. Geochimica et Cosmochimica Acta, 37, 1851–1880.CrossRefGoogle Scholar
- Smith, E. A., Mayfield, C. I., & Wong, P. T. S. (1977). Effects of phosphorus from apatite on development of freshwater communities. Journal of the Fisheries Research Board of Canada, 4, 2405–2409.CrossRefGoogle Scholar
- Smith, E. A., Mayfield, C. I., & Wong, P. T. S. (1978). Naturally occurring apatite as a source of orthophosphate for growth of bacteria and algae. Microbial Ecology, 4, 105–117.CrossRefGoogle Scholar
- Suzumura, M., Ueda, S., & Sumi, E. (2000). Control of phosphate concentration through adsorption and desorption processes in groundwater and seawater mixing at sandy beaches in Tokyo Bay, Japan. Journal of Oceanography, 56, 667–673.CrossRefGoogle Scholar
- Suzumura, M., Kokubun, H., & Arata, N. (2004). Distribution and characteristics of suspended particulate matter in a heavily eutrophic estuary, Tokyo Bay, Japan. Marine Pollution Bulletin, 49, 496–503.CrossRefGoogle Scholar
- Treguer, P., & Gueneley, S. (1988). Biogenic silica and particulate organic matter from the Indian sector of the Southern Ocean. Marine Chemistry, 23, 167–180.CrossRefGoogle Scholar
- Uncles, R. J., & Stephens, J. A. (1993). Nature of the turbidity maximum in the Tamar Estuary, U.K. Estuarine, Coastal and Shelf Science, 36, 413–431.CrossRefGoogle Scholar
- van Bennekom, A. J., Berger, G. W., Helder, W., & de Vries, R. T. P. (1978). Nutrient distribution in the Zaire estuary and river plume. Netherlands Journal of Sea Research, 12, 296–323.CrossRefGoogle Scholar
- Wolanski, E., King, B., & Galloway, D. (1995). Dynamics of the turbidity maximum in the Fly river estuary, Papua New Guinea. Estuarine, Coastal and Shelf Science, 40, 321–337.CrossRefGoogle Scholar
- Yang, G. F., Wu, J. Y., Gao, M. D., Zhou, T. C., Li, Y. Z., & Han, Y. S. (1992). Effects of the Three Gorges project on depositional structure and geochemistry characters of the Changjiang river estuary. Institute of Oceanology, Chinese Academy of Sciences. Studia Marina Sinica, 33, 69–108. Beijing: Science Press (in Chinese with English abstract).Google Scholar
- Zhang, Y. S., Zhang, F. J., Guo, X. W., & Zhang, M. P. (2004). Vertical flux of the settling particulate matter in the watercolumn of the yellow sea in summer. Oceanologia et Limnologia Sinica, 35, 231–238. (in Chinese with English abstract).Google Scholar