Abstract. Nitrous oxide (N2O) emissions from a nitrifying
biofilm reactor were investigated with N2O isotopocules. The nitrogen
isotopomer site preference of N2O (15N-SP) indicated the
contribution of producing and consuming pathways in response to changes in
oxygenation level (from 0 % to 21 % O2 in the gas mix), temperature
(from 13.5 to 22.3 ∘C) and ammonium concentrations (from 6.2 to
62.1 mg N L−1). Nitrite reduction, either nitrifier denitrification or
heterotrophic denitrification, was the main N2O-producing pathway under
the tested conditions. Difference between oxidative and reductive rates of
nitrite consumption was discussed in relation to NO2-
concentrations and N2O emissions. Hence, nitrite oxidation rates seem
to decrease as compared to ammonium oxidation rates at temperatures above 20 ∘C and under oxygen-depleted atmosphere, increasing N2O
production by the nitrite reduction pathway. Below 20 ∘C, a
difference in temperature sensitivity between hydroxylamine and ammonium
oxidation rates is most likely responsible for an increase in N2O
production via the hydroxylamine oxidation pathway (nitrification). A
negative correlation between the reaction kinetics and the apparent isotope
fractionation was additionally shown from the variations of δ15N and δ18O values of N2O produced from ammonium.
The approach and results obtained here, for a nitrifying biofilm reactor
under variable environmental conditions, should allow for application and
extrapolation of N2O emissions from other systems such as lakes, soils
and sediments.