EGU22-2352, updated on 27 Mar 2022
https://doi.org/10.5194/egusphere-egu22-2352
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Tracing N2O formation in full-scale wastewater treatment with natural abundance isotopes

Joachim Mohn1, Wenzel Gruber2, Paul Magyar3, Kerstin Zeyer1, Luzia von Känel4, Eberhard Morgenroth2, Moritz F. Lehmann3, Daniel Braun4, and Adriano Joss2
Joachim Mohn et al.
  • 1Empa, Air Pollution / Environmental Technology, Dübendorf, Switzerland (joachim.mohn@empa.ch)
  • 2Eawag, Department Process Engineering, Dübendorf, Switzerland
  • 3University of Basel, Aquatic and Isotope Biogeochemistry, Basel, Switzerland
  • 4ETH, Department of Civil, Environmental and Geomatic Engineering, Zürich, Switzerland

Nitrous oxide (N2O) dominates greenhouse gas emissions in wastewater treatment plants (WWTPs). Formation of N2O occurs during biological nitrogen removal, involves multiple microbial pathways, and is typically very dynamic. Consequently, N2O mitigation strategies require an improved understanding of nitrogen transformation pathways and their modulating controls. Analyses of the nitrogen (N) and oxygen (O) isotopic composition of N2O and its substrates at natural abundance have been shown to provide valuable information on formation and reduction pathways in laboratory settings, but have never been applied to full-scale WWTPs.

Here we show that N-species isotope ratio measurements at natural abundance level, combined with long-term N2O monitoring, allow identification of the N2O production pathways in a full-scale plug-flow WWTP (Hofen, Switzerland). The proposed approach can also be applied to other activated sludge systems. Heterotrophic denitrification appears as the main N2O production pathway under all tested process conditions, while nitrifier denitrification was less important, and more variable. N2O production by hydroxylamine oxidation was not observed. Fractional N2O elimination by reduction to dinitrogen (N2) during anoxic conditions was clearly indicated by a concomitant increase in SP, δ18O(N2O) and δ15N(N2O). The extent of N2O reduction correlated with the availability of dissolved inorganic N and organic substrates, which explains the link between diurnal N2O emission dynamics and organic substrate fluctuations. Consequently, dosing ammonium-rich reject water under low-organic-substrate conditions is unfavourable, as it is very likely to cause high net N2O emissions.

Our results demonstrate that monitoring of the N2O isotopic composition holds a high potential to disentangle N2O formation mechanisms in engineered systems, such as full-scale WWTP. Our study serves as a starting point for advanced campaigns in the future combining isotopic technologies in WWTP with complementary approaches, such as mathematical modelling of N2O formation or microbial assays to develop efficient N2O mitigation strategies.

How to cite: Mohn, J., Gruber, W., Magyar, P., Zeyer, K., von Känel, L., Morgenroth, E., Lehmann, M. F., Braun, D., and Joss, A.: Tracing N2O formation in full-scale wastewater treatment with natural abundance isotopes, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-2352, https://doi.org/10.5194/egusphere-egu22-2352, 2022.

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