C:N:P stoichiometry shapes N2O emission factors across an urban river-estuary continuum: the underappreciated role of phosphorus
编号:467 访问权限:仅限参会人 更新:2026-08-31 16:42:11 浏览:0次 张贴报告

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摘要
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.
 
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报告人
Sibo Zhang
Guangdong University of Technology

稿件作者
Sibo Zhang Guangdong University of Technology
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重要日期
  • 会议日期

    01月12日

    2027

    01月15日

    2027

  • 07月21日 2026

    初稿截稿日期

  • 01月15日 2027

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University (MEL)
Department of Earth Sciences, National Natural Science Foundation of China (NSFC)
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