Soil GHG fluxes are altered by N deposition: New data indicate lower N stimulation of the N2O flux and greater stimulation of the calculated C pools

• Published in: Global change biology Vol. 26; no. 4; pp. 2613 - 2629
• Main Authors: Deng, Lei, Huang, Chunbo, Kim, Dong‐Gill, Shangguan, Zhouping, Wang, Kaibo, Song, Xinzhang, Peng, Changhui
• Format: Journal Article
• Language: English
• Published: Oxford Blackwell Publishing Ltd 01.04.2020
• Subjects: Agricultural land; Carbon dioxide; carbon sink; Climate change; Deposition; Ecosystems; Emissions; Environmental changes; Equivalence; Fluxes; Global warming; Grasslands; Greenhouse effect; greenhouse gas emissions; Greenhouse gases; Mathematical analysis; Meta-analysis; Methane; Nitrogen; Nitrogen enrichment; Nitrous oxide; Organic carbon; Organic soils; Pools; Soil; Soils; Stimulation; Terrestrial ecosystems; Terrestrial environments; Uptake
• ISSN: 1354-1013; 1365-2486
• DOI: 10.1111/gcb.14970

The effects of nitrogen (N) deposition on soil organic carbon (C) and greenhouse gas (GHG) emissions in terrestrial ecosystems are the main drivers affecting GHG budgets under global climate change. Although many studies have been conducted on this topic, we still have little understanding of how N deposition affects soil C pools and GHG budgets at the global scale. We synthesized a comprehensive dataset of 275 sites from multiple terrestrial ecosystems around the world and quantified the responses of the global soil C pool and GHG fluxes induced by N enrichment. The results showed that the soil organic C concentration and the soil CO2, CH4 and N2O emissions increased by an average of 3.7%, 0.3%, 24.3% and 91.3% under N enrichment, respectively, and that the soil CH4 uptake decreased by 6.0%. Furthermore, the percentage increase in N2O emissions (91.3%) was two times lower than that (215%) reported by Liu and Greaver (Ecology Letters, 2009, 12:1103–1117). There was also greater stimulation of soil C pools (15.70 kg C ha−1 year−1 per kg N ha−1 year−1) than previously reported under N deposition globally. The global N deposition results showed that croplands were the largest GHG sources (calculated as CO2 equivalents), followed by wetlands. However, forests and grasslands were two important GHG sinks. Globally, N deposition increased the terrestrial soil C sink by 6.34 Pg CO2/year. It also increased net soil GHG emissions by 10.20 Pg CO2‐Geq (CO2 equivalents)/year. Therefore, N deposition not only increased the size of the soil C pool but also increased global GHG emissions, as calculated by the global warming potential approach. The plants input more C into the soil, causing the ecosystem to become a net CO2 sink under the N enrichment (deposition), which negatively contributed to global warming. N enrichment (deposition) suppressed the CH4 uptake but stimulated CH4 emissions, which increased atmospheric CH4 and N enrichment (deposition) increased N2O emissions, which positively contributed to global warming. Globally, N deposition increased the terrestrial soil C sink by 6.34 Pg CO2/year. It also increased net soil GHG emissions by 10.20 Pg CO2‐Geq (CO2 equivalents)/year, as calculated by the global warming potential approach.