Arid Zone Research ›› 2025, Vol. 42 ›› Issue (5): 820-828.doi: 10.13866/j.azr.2025.05.05

• Land and Water Resources • Previous Articles     Next Articles

Estimation of soil NOX emissions in the deserts and surrounding areas of Northern China

ZHOU Fei1,2(), WANG Changyan1, WANG Fang3, WU Qiaoli4, SU Xiaoli2, ZHANG Daizhou5, WU Feng2()   

  1. 1. School of Geography and Environment, Baoji University of Arts and Sciences, Baoji 721013, Shaanxi, China
    2. State Key Laboratory of Loess Science, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, Shaanxi, China
    3. Inner Mongolia Environmental Monitoring Central StationHohhot 010010, Inner Mongolia, China
    4. Xi’an Institute for Innovative Earth Environment Research, Xi’an 710061, Shaanxi, China
    5. Faculty of Environmental and Symbiotic Sciences, Prefectural University of Kumamoto, Kumamoto 862-8502, Japan
  • Received:2024-12-27 Revised:2025-04-02 Online:2025-05-15 Published:2025-10-22
  • Contact: WU Feng E-mail:zhoufei655129@163.com;kurt_wf@ieecas.cn

Abstract:

Previous studies have demonstrated that notable amounts of nitrogen oxides (NOX) are emitted from desert surfaces, and these emissions likely play a crucial role in the atmospheric reactive nitrogen cycle within the desert regions. However, quantitative assessments of NOX emissions in these regions are scarce, which limits our understanding of the environmental consequences thereof. This study aimed to quantify the soil NOX emission fluxes in the deserts and surrounding areas of Northern China to provide a basis for understanding the ecological benefits of desert NOX emissions. Based on the law of conservation of mass, we utilized NO2 vertical column density (NO2VCD) data from the Tropospheric Monitoring Instrument (TROPOMI) onboard the Sentinel-5P satellite for the deserts and surrounding areas of Northern China. The study quantified the soil NOX emission fluxes by subtracting the effects of atmospheric horizontal transport, diffusion, chemical transformation, deposition, and anthropogenic emissions of regional NOX. The results revealed the following: (1) The mean soil NOX emission flux in the deserts and surrounding areas of Northern China is 17.6 ng·m-2·s-1, ranging from 0 to 85 ng·m-2·s-1. Lower emission fluxes were predominantly observed in the central regions of the desert, whereas the Gobi surrounding the desert exhibited higher emission fluxes. (2) Among the different desert areas studied, the Badain Jaran Desert and surrounding areas have a mean emission flux of 13.1 ng·m-2·s-1, which is significantly lower than the 26.0 ng·m-2·s-1 emission flux observed in the Tengger Desert and surrounding areas (P<0.0001). This study provides a robust estimation of the soil NOX emission fluxes in the deserts and surrounding areas of Northern China, thereby enhancing our understanding of how desert ecosystems contribute to atmospheric chemistry and laying a solid foundation for future research in desert atmospheric chemistry.

Key words: desert air, ozone, top-down approach, surface-atmosphere exchange