ABSTRACT
A greenhouse experiment was conducted to assess the denitrifying capacity of Panicum hemitomon Schult. freshwater marsh soils. High rates (100, 200 and 300 kg N ha−1) of N-15 labelled NH4 +- and NO3 −-N were applied to the soil surfaces of marsh cores to simulate nutrient loading from anthropogenic sources. Direct gaseous flux of N2 and N2O resulting from nitrification-denitrification in the flooded soils were measured over 46 d after N addition. Dinitrogen and N2O emissions from the soil surface were significantly affected by rate and form of inorganic N applied. Denitrification of added labelled NO3-N began immediately after addition. The nitrification process resulted in a 9 d lag before any of the added labelled NH4 +-N was denitrified. Maximum N2 emissions measured from the marsh cores treated with 100, 200 and 300 kg N ha−1 were <15, 650, and 1, 080 for (NH4)2SO4 and 2,700 3,430 and 4,490 g ha−1 d−1 for the KNO3 treatments, respectively. Nitrous oxide flux ranged from nondetectable concentrations above control values to 1,980 g ha−1 d−1 for the 300 kg KNO3-N ha−1 treatment. This study demonstrates that the freshwater marsh soils have the potential to remove large inputs of inorganic N through denitrification.