1. Modeling Riverine N2O Sources, Fates, and Emission Factors in a Typical River Network of Eastern China
- Author
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Hu, Minpeng, Li, Bingqing, Wu, Kaibin, Zhang, Yufu, Wu, Hao, Zhou, Jia, and Chen, Dingjiang
- Abstract
Estimates of riverine N2O emission contain great uncertainty because of the lack of quantitative knowledge concerning riverine N2O sources and fates. Using a 3.5-year record of monthly N2O measurements from the Yongan River network of eastern China, we developed a mass-balance model to address the riverine N2O source and sink processes. We achieved reasonable model efficacies (R2= 0.44–0.84, Nash–Sutcliffe coefficients = 0.40–0.80) across three tributaries and the entire river system. Estimated riverine N2O loads originated from groundwater (38–88%), surface runoff (3–26%), and in-stream production (4–48%). Estimated in-stream losses via atmospheric release + complete denitrification accounted for 76, 95, 25, and 89% of riverine N2O fate for the agricultural, residential, forest, and entire river system, respectively. Considering limited complete denitrification, the model estimated an upper-bound riverine N2O emission rate of 2.65 ton N2O–N km–2year–1for the entire river system. Riverine N2O emission estimates were of comparable magnitude to those estimated with a power-law scaling model. Riverine N2O emissions using the IPCC default emission factor (0.26%) overestimated emissions by 3–15 times, whereas the dissolved N2O concentration-based emission factor overestimated or underestimated emissions. This study highlights the importance of combining comprehensive information on N2O sources and fates to achieve accurate riverine N2O emission estimates.
- Published
- 2021
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