Eutrophication characteristics and variation analysis of estuaries in China
LI Jun-long1,2, ZHENG Bing-hui2, ZHANG Ling-song1,2, JIN Xiao-wei1, HU Xu-peng3, LIU Fang1, SHAO Jun-bo3
1. State Environmental Protection Key Laboratory of Quality Control in Environmental Monitoring, China National Environmental Monitoring Center, Beijing 100012, China;
2. State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China;
3. Zhoushan Marine Ecological Environmental Monitoring Station, Zhoushan 316000, China
Eutrophication characteristics and variations were analyzed using four main statistical methods of box-plot analysis, cluster analysis, correlation analysis and principal component analysis, which were conducted based on natural geographic data and water quality monitoring data of 65 estuaries from 2007 to 2012 years in China. The results showed there was significant difference in eutrophication response indicators between the large-scale estuaries and small-scale estuaries. The eutrophication states of large-scale estuaries were more serious. It was also showed DIN, PO43--P and COD were the first principal component of eutrophication characteristics, followed as DO and Chl-a for second, and Depth, Tidal and Area for third. In addition, there was significant positive correlation between the Chl-a and TN input (P<0.01), DIN (P<0.01), PO43--P (P<0.05), inflow (P<0.01) and temperature (P<0.05), while there was significant negative correlation between chlorophyll a and tidal (P<0.05), salinity (P<0.01) and DO (P<0.01) in estuaries. It indicated the increase in nutrient input was the main factor which resulted in eutrophication symptoms. However, eutrophication state would be adjusted by typological factors and lead to different response characteristics among estuaries. The nutrient conversion efficiencies of estuarine tidal below 2.5m were higher than the ones above 2.5m. It is implied the eutrophication susceptibility to nutrient load could be regulated by changing water residence time, vertical mixing and light conditions. Furthermore, the Chl-a concentration were also influenced by water exchange with offshore area, biological predation and other nutrient forms supply in estuary. The differences and extent of eutrophication among estuaries were determined synthetically by nutrient inputs from human activities, as well as natural attributes of the estuary.
Hoyer M V, Frazer T K, Notestein S K., et al. Nutrient, chlorophyll, and water clarity relationships in Florida's nearshore coastal waters with comparisons to freshwater lakes[J]. Can. J. Fish. Aquat. Sci., 2002,59:1024-1031.
Zhou M J, Shen Z L, Yu R C. Responses of a coastal phytoplankton community to increased nutrient input from the Changjiang (Yangtze) River[J]. Cont. Shelf Res., 2008,28:1483-1489.
[8]
Fisher T R, Harding L W, Stanley D W, et al. Phytoplankton nutrients and turbidity in the Chesapeake, Delaware and Hudson Estuaries[J]. Estuarine Coastal Shelf Sci., 1988,27:61-93.
[9]
Wavar M V M, Corre P L, Birrien J L. Transport of carbon, nitrogen and phosphorus in a Brittany river, France[J]. Estuarine Coastal Shelf Sci., 1989,29:489-500.
Hao Y J, Tang D L, Yu L., et al. Nutrient and chlorophyll a anomaly in red-tide periods of 2003~2008 in Sishili Bay, China[J]. Chin. J. Oceanol. Limnol., 2011,29(3):664-673.
[13]
Durbin E G, Durbin A G, Beardsley R C. Springtime nutrient and chlorophyll a concentrations in the southwestern Gulf of Maine[J]. Cont. Shelf Res., 1995,15(4/5):433-450.
Fairbridge R W. 1980. The estuary:its definition and geochemical role[M]//Chemistry and Geochemistry of Estuaries (Olausson, E & Cato I, eds). New York:John Wiley. 1-35.
Cheng X Y, Li S J. Evolution process and characteristic analysis of Lake Eutrophication in the Yangtze River Delta[J]. Chin. Sci. Bull., 2006,51(7):848-855.
Uncles R J, Joint I R. Vertical mixing and its effects on phytoplankton growth in a turbid estuary[J]. Can. J. Fish. Aquat. Sci., 1983,40(Suppl 1):221-228.
[29]
Demers S L, Legendre J C, Therriaui T. Phytoplankton responses to vertical tidal mixing[M]. New York:Springer Verlag, 1986:1-40.
[30]
Abigail M G, Dionysios E R, Martin E, et al. A long-term chlorophyll data set reveals regime shift in North Sea phytoplankton biomass unconnected to nutrient trends[J]. Limnol. Oceanogr., 2007,52(2):635-648.
[31]
Kemp W M, Boynton W R, Adolf J E, et al. Eutrophication of Chesapeake Bay:historical trends and ecological interactions[J]. Mar. Ecol. Prog. Ser., 2005,303:1-29.
[32]
Hiebauer H J, Alexander V, Henrichs S M. A time-series study of the spring bloom at the Bering Sea ice edge I. Physical processes, chlorophyll and nutrient chemistry[J]. Cont. Shelf Res., 1995,15(15):1859-1877.
[33]
Yves Monbet. Control of Phytoplankton Biomass in Estuaries:A Comparative Analysis of Microtidal and Macrotidal Estuaries[J]. Estuaries Coasts, 1992,15(4):563-571.
[34]
Gong G C, Chen Y L L, Liu K K. Chemical hydrography and chlorophyll a distribution in the East China Sea in summer:implications in nutrient dynamics[J]. Cont. Shelf Res., 1996, 16(12):1561-1590.
[35]
Yin K D, Harrison P J. Influences of flood and ebb tides on nutrient fluxes and chlorophyll on an intertidal flat[J]. Mar. Ecol. Prog. Ser., 2000,196:75-85.
[36]
Shao X X, Wu M, Gu B H, et al. Nutrient retention in plant biomass and sediments from the salt marsh in Hangzhou Bay estuary, China[J]. Environ. Sci. Pollut. Res., 2013,20:6382-6391.
Davies P. Nutrient processes and chlorophyll in the estuaries and plume of the Gulf of Papua[J]. Cont. Shelf Res., 2004,24:2317-2341.
[41]
Souchu P, Bec B, Smith V H, et al. Patterns in nutrient limitation and chlorophyll a along an anthropogenic eutrophication gradient in French Mediterranean coastal lagoons[J]. Can. J. Fish. Aquat. Sci., 2010,67:743-753.
[42]
Thongdonphum B., Meksumpun S. and Meksumpun C. Nutrient loads and their impacts on chlorophyll a in the Mae Klong River and estuarine ecosystem:an approach for nutrient criteria development[J]. Water Sci. Technol., 2011,64(1):178-188.