Capacity for Denitrification and Reduction of Nitrate to Ammonia in a Coastal Marine Sediment
AUTOR(ES)
Sørensen, Jan
RESUMO
The capacity for dissimilatory reduction of NO3− to N2 (N2O) and NH4+ was measured in 15NO3−-amended marine sediment. Incubation with acetylene (7 × 10−3 atmospheres [normal]) caused accumulation of N2O in the sediment. The rate of N2O production equaled the rate of N2 production in samples without acetylene. Complete inhibition of the reduction of N2O to N2 suggests that the “acetylene blockage technique” is applicable to assays for denitrification in marine sediments. The capacity for reduction of NO3− by denitrification decreased rapidly with depth in the sediment, whereas the capacity for reduction of NO3− to NH4+ was significant also in deeper layers. The data suggested that the latter process may be equally as significant as denitrification in the turnover of NO3− in marine sediments.
ACESSO AO ARTIGO
http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=242830Documentos Relacionados
- Denitrification, Nitrate Reduction, and Oxygen Consumption in Coastal and Estuarine Sediments
- Denitrification in Marine Sediment: Measurement of Capacity and Estimate of In Situ Rate
- The rates and players of denitrification, dissimilatory nitrate reduction to ammonia (DNRA) and anaerobic ammonia oxidation (anammox) in mangrove soils
- Reduction of Ferric Iron in Anaerobic, Marine Sediment and Interaction with Reduction of Nitrate and Sulfate
- Denitrification and Ammonia Formation in Anaerobic Coastal Sediments