Fertilizer management for global ammonia emission reduction

Peng Xu, Geng Li, Yi Zheng, Jimmy C.H. Fung, Anping Chen, Zhenzhong Zeng, Huizhong Shen, Min Hu, Jiafu Mao, Yan Zheng, Xiaoqing Cui, Zhilin Guo, Yilin Chen, Lian Feng, Shaokun He, Xuguo Zhang, Alexis K.H. Lau, Shu Tao, Benjamin Z. Houlton

Research output: Contribution to journalArticlepeer-review

58 Scopus citations

Abstract

Crop production is a large source of atmospheric ammonia (NH3), which poses risks to air quality, human health and ecosystems1–5. However, estimating global NH3 emissions from croplands is subject to uncertainties because of data limitations, thereby limiting the accurate identification of mitigation options and efficacy4,5. Here we develop a machine learning model for generating crop-specific and spatially explicit NH3 emission factors globally (5-arcmin resolution) based on a compiled dataset of field observations. We show that global NH3 emissions from rice, wheat and maize fields in 2018 were 4.3 ± 1.0 Tg N yr−1, lower than previous estimates that did not fully consider fertilizer management practices6–9. Furthermore, spatially optimizing fertilizer management, as guided by the machine learning model, has the potential to reduce the NH3 emissions by about 38% (1.6 ± 0.4 Tg N yr−1) without altering total fertilizer nitrogen inputs. Specifically, we estimate potential NH3 emissions reductions of 47% (44–56%) for rice, 27% (24–28%) for maize and 26% (20–28%) for wheat cultivation, respectively. Under future climate change scenarios, we estimate that NH3 emissions could increase by 4.0 ± 2.7% under SSP1–2.6 and 5.5 ± 5.7% under SSP5–8.5 by 2030–2060. However, targeted fertilizer management has the potential to mitigate these increases.

Original languageEnglish
Pages (from-to)792-798
Number of pages7
JournalNature
Volume626
Issue number8000
DOIs
StatePublished - Feb 22 2024

Funding

This study was supported by the National Natural Science Foundation of China (grant nos. 42325702 to Yi Zheng, 42277086 to P.X. and 42321004 to Yan Zheng), the Natural Science Foundation of Guangdong Province (grant no. 2023A1515012280 to P.X.) and the Research Grants Council of the Hong Kong Special Administrative Region, China (grant no. 16302220 to J.C.H.F.), the Earth and Environmental Systems Sciences Division of the Biological and Environmental Research Office in the Office of Science of the US Department of Energy (DOE) (the Terrestrial Ecosystem Science Scientific Focus Area project and the Reducing Uncertainties in Biogeochemical Interactions through Synthesis and Computing Scientific Focus Area project to J.M.). Oak Ridge National Laboratory is supported by the Office of Science of the DOE under contract DE-AC05-00OR22725. We thank C. P. Ti of the Institute of Soil Science, Chinese Academy of Sciences; S. W. Liu of the Nanjing Agricultural University; and X. Y. Zhan of the Chinese Academy of Agricultural Sciences for providing us with data. This study was supported by the National Natural Science Foundation of China (grant nos. 42325702 to Yi Zheng, 42277086 to P.X. and 42321004 to Yan Zheng), the Natural Science Foundation of Guangdong Province (grant no. 2023A1515012280 to P.X.) and the Research Grants Council of the Hong Kong Special Administrative Region, China (grant no. 16302220 to J.C.H.F.), the Earth and Environmental Systems Sciences Division of the Biological and Environmental Research Office in the Office of Science of the US Department of Energy (DOE) (the Terrestrial Ecosystem Science Scientific Focus Area project and the Reducing Uncertainties in Biogeochemical Interactions through Synthesis and Computing Scientific Focus Area project to J.M.). Oak Ridge National Laboratory is supported by the Office of Science of the DOE under contract DE-AC05-00OR22725. We thank C. P. Ti of the Institute of Soil Science, Chinese Academy of Sciences; S. W. Liu of the Nanjing Agricultural University; and X. Y. Zhan of the Chinese Academy of Agricultural Sciences for providing us with data.

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