Nitrogen biogeochemistry of aquaculture ponds

Nitrogen (N) biogeochemistry of aquaculture ponds is dominated by biological transformations of N added to ponds in the form of inorganic or organic fertilizers and formulated feeds. Nitrogen application in excess of pond assimilatory capacity can lead to the deterioration of water quality through the accumulation of nitrogenous compounds (e.g., ammonia and nitrite) with toxicity to fish or shrimp. Principal sources of ammonia include fish excretion and sediment flux derived from the mineralization of organic matter and molecular diffusion from reduced sediment, although cyanobacterial nitrogen fixation and atmospheric deposition are occasionally important. Principal sinks for ammonia include phytoplankton uptake and nitrification. The magnitude of losses by ammonia volatilization and ammonium fixation to cation exchange sites is minor, but unknown. Interactions between pond sediment and water are important regulators of N biogeochemistry. Sediment represents a source of ammonia and a sink for nitrite and nitrate. The large volume of reduced sediment suggests that the potential for N removal by denitrification is high, although the magnitude of N removal by this mechanism is low because nitrification and denitrification are tightly coupled in aquatic sediments and sediment nitrification is limited by the depth of sediment oxygen penetration. Nitrogen biogeochemistry of aquaculture ponds is affected by feeds and feeding practices, water exchange and circulation, aeration, pond depth and other management procedures. Opportunities for management of N biogeochemistry are limited and goals are based largely on the intensity of fish production. (C) 1998 Published by Elsevier Science B.V. All rights reserved.