Characterization of denitrification activity in zones of groundwater exfiltration within a riparian wetland ecosystem

Movement of agricultural nitrogen (N) into riparian buffers often occurs within discrete seepage or upwelling zones which can limit the ability of the ecosystem to process the nutrient delivered by exfiltrating groundwater. Characterization of the biogeochemical processing of N within these zones is important in assessing the effectiveness of riparian buffers for mitigating nutrient loading of surface waters. The biogeochemical potential for denitrification in zones of exfiltration within a riparian buffer wetland dominated by high-carbon mucky soils was found to be highly stratified by profile depth with substantially higher activity in the surface layer of soil. The denitrification enzyme activity (DEA) within these zones was partly related to the population size of denitrifying microorganisms as measured by the most probable number (MPN) as well as the general microbial population as measured by substrate-induced respiration. The addition of glucose to the DEA assay stimulated enzyme activity indicating that carbon substrate was limiting activity. The stratification patterns of microbial populations and DEA are consistent with new carbon inputs to the ecosystem being most important driver of biogeochemical reactions such as denitrification in this high-carbon environment. A survey of carbon inputs to the ecosystem under study identified two major sources that contribute most of the annual biomass carbon inputs to the wetland: skunk cabbage in early summer and tree leaf litter in the fall. Tests of the ability of annually deposited wetland plant residues to stimulate denitrification and microbial respiration indicated that the degree of stimulation was inversely related to the C/N ratio of these carbon sources.