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Dissolved organic carbon riverine

Mantoura, R.F.C. and Woodward, E.M.S., 1983. Conservative behaviour of riverine dissolved organic carbon in the Severn estuary chemical and geochemical... [Pg.51]

D. Prediction of Soil Solution and Riverine Dissolved Organic Carbon Flux Using Watershed Soil Properties... [Pg.58]

Moran, M. A., W. M. Sheldon, and J. E. Sheldon. 1999. Biodegradation of riverine dissolved organic carbon in five estuaries of the southeastern United States. Estuaries 22 55-64. [Pg.261]

Stolte W, Panosso R, Gisselson LA, Graneli E (2002) Utilization effidency of nitrogen assodated with riverine dissolved organic carbon (>1 kDa) by two toxin-producing phytoplankton species. Aquat Microb Ecol 29 97-105... [Pg.200]

Guyot, J. L., and J. G. Wasson. 1994. Regional pattern of riverine dissolved organic carbon in the Bolivian Amazonian drainage basin. Limnology and Oceanography 39 452-458. [Pg.206]

Meyer, J. L. 1990. Production and utilization of dissolved organic carbon in riverine ecosystems. In Organic Acids in Aquatic Ecosystems, eds. E. M. Perdue, and E. T. Gjessing (John Wiley Sons, Ltd., Dahlem Konferenzen), pp. 281-299. [Pg.207]

Carbon is transported into the Amazon River/ocean mixing zone in numerous forms including dissolved inorganic carbon (DIC), dissolved organic carbon (DOC), and particulate organic carbon (POC). The average DIC, DOC, and POC concentrations in Amazon River water are 460, 275, and 180 pmol L-1 (Richey et al. 1991), which indicates that DOC supply exceeds POC supply and that DIC is the most abundant form of carbon in the river. Sholkovitz et al. (1978) noted that most riverine dissolved... [Pg.334]

Nevertheless, it seems reasonable to infer that aquatic humic substance concentrations in estuaries are intermediate between those of rivers and those of the open ocean, as would be expected from a mixture of river water and seawater. The concentrations of humic acids at intermediate salinities do not correspond, in a linear fashion, to the relative proportions of river water and seawater (Fig. 2), primarily because of a removal from solution of a portion of the riverine contribution. This behavior is in contrast to that of total dissolved organic carbon (DOC) which generally does show linear mixing lines when plotted versus salinity (Sholkovitz et al., 1978 Moore et al., 1979 Laane, 1980 Fox, 1983a Mantoura and Woodward, 1983). [Pg.214]


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