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Published in J Environ Qual 23:965-972 (1994)
© 1994 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Carbon Flux between Sediment and Water Column of a Shallow, Subtropical, Hypereutrophic Lake

P. M. Gale* and K. R. Reddy

Soil and Water Science Dep., P.O. Box 110510, Univ. of Florida, Institute of Food and Agric. Science, Gainesville, FL 32611.

* Corresponding author.

ABSTRACT

Field and laboratory experiments were conducted to measure forms, storages, and flux of C in the water-sediment colunm of a shallow, subtropical, hypereutrophic lake. High gross primary productivity in the lake (1.4 ± 0.3 kg C m–2 yr–1) was not significantly correlated with any water chemistry parameters measured. This suggested that the phytoplankton community was functioning at maximum levels and under nutrient nonlimiting conditions. Major C input to the lake is through gross primary productivity, of which 90% is lost through heterotrophic and microbial respiration processes within the water column. Resuspension of the bottom sediments was a major input of C into the water column, contributing 720 g C m–2 yr–1. In comparison, diffusive flux of dissolved organic C from the sediment was minimal (1.2 g C m–2 yr–1), as were external inputs into the water column (20 g C m–2 yr–1). High productivity of this system has resulted in a net accumulation of C (as sediments) of 118 g C m–2 yr–1.


NOTES

Contribution of the Florida Agric. Exp. Stn. Journal Ser. no. R-03291.

Received for publication August 16, 1993.


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J. Song, Y. Luo, Q. Zhao, and P. Christie
Microcosm Studies on Anaerobic Phosphate Flux and Mineralization of Lake Sediment Organic Carbon
J. Environ. Qual., November 1, 2004; 33(6): 2353 - 2356.
[Abstract] [Full Text] [PDF]




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