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ABSTRACT
The magnitude of N loss from nitrification-denitrification reactions in sediment-water columns of a freshwater lake of Louisiana Gulf Coast drainage basin receiving elevated N loading from agricultural runoff was determining using 15NO3 dilution. Isotope dilution using added labeled NO3 allowed for the simultaneous determination of nitrification and NO3 reduction in the sediment-water column. The contribution of internal NH4 pools in bottom sediment to NO3 content in water column through diffusion and nitrification was measured. Nitrate reduction averaged 134 µmol m–2 h–1 over a 50-d incubation period in the sediment-water columns. Nitrification averaged 90 µmol m–2 h–1, approximately 70% of the denitrification rate. Nitrification and ammonium assimilation were also determined in lake water using 15N-labeled NH4 as a tracer. The nitrification rate determined in the water (0.9–1.4 mmol N m–3 d–1) was less than the rates measured in the sediment-water columns (1.4–3.3 mmol N m–3 d–1) using 15NO3 dilution. The results presented and isotope dilution technique used are applicable for use in understanding the fate of N in sediment-water systems of other aquatic environments.
Key Words: water quality mineralization denitrification eutrophication Louisiana N loading
1 Contribution from Laboratory for Wetland Soils and Sediments, Center for Wetland Resources, Louisiana State Univ., Baton Rouge, LA 70803-7511.
2 Assistant Professors, Laboratory for Wetland Soils and Sediments, Louisiana State Univ., Baton Rouge, LA 70803-7511.
Received for publication October 24, 1986.
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