4.7 Article

Effects of nitrogen addition on the combined global warming potential of three major soil greenhouse gases: A global meta-analysis

Journal

ENVIRONMENTAL POLLUTION
Volume 334, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.envpol.2023.121848

Keywords

N deposition; Carbon dioxide; Nitrous oxide; Methane; Global warming potential; Terrestrial ecosystems

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Increased nitrogen deposition has a significant impact on soil greenhouse gas emissions. This meta-analysis of 124 simultaneous measurements from 54 studies found that nitrogen addition leads to an increase in the combined global warming potential (CGWP) of CO2, CH4, and N2O. Wetlands are the most sensitive ecosystem to nitrogen addition, and CO2 contributes the most to the CGWP change.
Increased nitrogen (N) deposition has a great impact on soil greenhouse gas (GHG) emissions, and numerous studies have revealed the individual effects of N addition on three major GHGs (CO2, CH4, and N2O). Never-theless, quantitative evaluation of the effects of N addition on the global warming potential (GWP) of GHGs based on simultaneous measurements is needed not only to better understand the comprehensive effect of N deposition on GHGs but also for precise estimation of ecosystem GHG fluxes in response to N deposition. Here, we conducted a meta-analysis using a dataset with 124 simultaneous measurements of the three major GHGs from 54 studies to assess the effects of N addition on the combined global warming potential (CGWP) of these soil GHGs. The results showed that the relative sensitivity of the CGWP to N addition was 0.43%/kg N ha-1 yr-1, indicating an increase in the CGWP. Among the ecosystems studied, wetlands are considerable GHG sources with the highest relative sensitivity to N addition. Overall, CO2 contributed the most to the N addition-induced CGWP change (72.61%), followed by N2O (27.02%) and CH4 (0.37%), but the contributions of the three GHGs varied across ecosystems. Moreover, the effect size of the CGWP had a positive relationship with N addition rate and mean annual temperature and a negative relationship with mean annual precipitation. Our findings suggest that N deposition may influence global warming from the perspective of the CGWP of CO2, CH4, and N2O. Our results also provide reference values that may reduce uncertainties in future projections of the effects of N deposition on GHGs.

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