C:N:P stoichiometry shapes N2O emission factors across an urban river-estuary continuum: the underappreciated role of phosphorus
ID:467
Poster Presentation
2027-01-15 18:45 (China Standard Time)
Session:Session 69 - The nitrogen cycle in a changing ocean: from the process level to basin scale
Abstract
The emission factor (EF5) approach is widely used to estimate N2O emissions from rivers and estuaries. However, current IPCC default EF5 values use fixed and identical factors for both systems (0.26%), without accounting for environmental variability or the substantial differences between these two systems. Here, we investigated EF5 variability and its controls along the urbanized Pearl River-estuary continuum using isotopocule analysis, metagenomics, and global data synthesis. By integrating our field measurements with compiled global datasets, we found that EF5 ranged from 0.0014% to 18.6% in rivers (n = 3,560) and from 0.01% to 12.81% in estuaries (n = 254). Across the continuum, isotopocule analysis suggested that denitrification dominated N2O production (>89%), while SHAP analysis identified nitrate as the strongest EF5 predictor. Lower EF5 under nitrate-rich conditions was associated with uneven denitrifier responses: higher nitrate increased nirS but not nirK abundance and was more strongly associated with upstream nitrate-reduction genes than with downstream N2O-producing genes. Phosphorus-related variables also explained substantial EF5 variation. Higher total phosphorus concentrations were associated with lower EF5 and greater potentials for assimilatory nitrate uptake and DNRA, indicating that more nitrate may have been consumed by non-N2O-producing pathways. Predictor importance was zone dependent: nitrate-related factors were more important in low-nitrate estuaries, whereas phosphorus-related factors became primary factors in rivers. In urbanized riverine reaches, TN:TP was positively associated with EF5, partly reflecting wastewater influence, where elevated TN:TP coincided with disproportionately greater dissolved N2O inputs relative to nitrate. Global synthesis further showed that estuarine EF5 was generally higher than riverine EF5, with high salinity inhibiting N2O reduction. These findings demonstrate that riverine and estuarine EF5 differ in both magnitude and dominant controls, providing a basis for system-specific prediction and refinement of aquatic N2O emission factors.
Speaker
Author
Important Dates
-
Jan 30
2026
Session / Event proposals open
-
Mar 31
2026
Session / Event proposals close
(Extended to April 7) -
Apr 30
2026
Session acceptance notifications
-
Apr 30
2026
Abstract submissions & registration open
-
Jun 30
2026
Abstract submissions close
(Extended to July 21) -
Aug 31
2026
Abstract acceptance notifications
-
Sep 15
2026
Scientific program released
-
Oct 15
2026
Early bird registration closes
-
Jan 12–15
2027
XMAS 2027
