Nitrogen trace gas emissions from a riparian ecosystem in southern Appalachia
In this paper, we present two years of seasonal nitric oxide (NO), ammonia (NH 3 ), and nitrous oxide (N 2 O) trace gas fluxes measured in a recovering riparian zone with cattle excluded and adjacent riparian zone grazed by cattle. In the recovering riparian zone, average NO, NH 3 , and N 2 O fluxes were 5.8, 2.0, and 76.7 m -2 s -1 (1.83,0.63, and 24.19 kg N ha -1 y -1 ), respectively. Fluxes in the grazed riparian zone were larger, especially for NO and NH 3 , measuring 9.1, 4.3, and 77.6 ng N m -2 s -1 (2.87, 1.35, and 24.50 kg N ha -1 y -1 ) for NO, NH 3 , and N 2 O, respectively. On average, N 2 O accounted for greater than 85% of total trace gas flux in both the recovering and grazed riparian zones, though N 2 O fluxes were highly variable temporally. In the recovering riparian zone, variability in seasonal average fluxes was explained by variability in soil nitrogen (N) concentrations. Nitric oxide flux was positively correlated with soil ammonium (NH + 4 ) concentration, while N 2 O flux was positively correlated with soil nitrate (NO - 4 ) concentration. Ammonia flux was positively correlated with the ratio of NH + 4 to NO - 3 . In the grazed riparian zone, average NH 3 and N 2 O fluxes were not correlated with soil temperature, N concentrations, or moisture. This was likely due to high variability in soil microsite conditions related to cattle effects such as compaction and N input. Nitric oxide flux in the grazed riparian zone was positively correlated with soil temperature and NO - 3 concentration. Restoration appeared to significantly affect NO flux, which increased ~ 600% during the first year following restoration and decreased during the second year to levels encountered at the onset of restoration. By comparing the ratio of total trace gas flux to soil N concentration, we show that the restored riparian zone is likely more efficient than the grazed riparian zone at diverting upper-soil N from the receiving stream to the atmosphere. This is likely due to the recovery of microbiological communities following changes in soil physical characteristics.
Walker, John T.
Geron, Christopher D.
Vose, James M.
Swank, Wayne T.
Chemosphere 49 (2002) 1389-1398
Walker, John T.; Geron, Christopher D.; Vose, James M.; Swank, Wayne T. 2002. Nitrogen trace gas emissions from a riparian ecosystem in southern Appalachia. Chemosphere 49 (2002) 1389-1398