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Increasing soil nitrous acid emissions driven by climate and fertilization change aggravate global ozone pollution
  • +5
  • Yanan Wang,
  • Qinyi Li,
  • Ivonne Trebs,
  • Yurun Wang,
  • Chuanhua Ren,
  • Alfonso Saiz-Lopez,
  • Likun Xue,
  • Tao Wang
Yanan Wang
Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University
Author Profile
Qinyi Li
Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Environment Research Institute, Shandong University
Ivonne Trebs
Department of Environmental Research and Innovation, Luxembourg Institute of Science and Technology
Yurun Wang
Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University
Chuanhua Ren
Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University, School of Atmospheric Sciences, Joint International Research Laboratory of Atmospheric and Earth System Sciences, Nanjing University
Alfonso Saiz-Lopez
Department of Atmospheric Chemistry and Climate, Institute of Physical Chemistry Blas Cabrera, Spanish National Research Council (CSIC)
Likun Xue
Environment Research Institute, Shandong University
Tao Wang
Department of Civil and Environmental Engineering, The Hong Kong Polytechnic University

Corresponding Author:

Abstract

Soil microbial nitrous acid (HONO) production has been identified as a significant emission source to the atmosphere and, thus, considerably affects atmospheric oxidizing capacity and formation of secondary air pollutants. Soil HONO emissions are controlled by soil water content, soil temperature, and nitrogen content, which are affected by climatic conditions and fertilizer application rates. However, long-term global soil HONO emissions driven by climate change and increasing fertilizer use have not yet been quantified, hindering the assessment and prediction of the global impact of soil emissions on air quality and vegetation. Here, we derive the first global soil HONO emissions from natural and fertilized lands over the past four decades and evaluate the variation of their impacts on global ozone (O3) and vegetation exposure. Our results show that climate change and the enhanced fertilizer use have increased global soil HONO emissions from 11.0 Tg N in 1980 to 13.4 Tg N in 2016. The rise in fertilizer consumption has substantially intensified soil emissions in the three major grain-producing regions, India, China, and North America with growth rates of 14.9, 9.5, and 0.9 kt N yr-1 , respectively; climate change has predominantly increased soil emissions in Africa and South America with growth rates of 22.3 and 10.9 kt N yr-1 , respectively. Incorporating soil HONO emissions in a global chemistry-climate model improves the model performance in simulating global Page 2 of 22 atmospheric HONO. Simulations with the updated model showed that soil HONO emissions increased global surface O3 concentrations by 2.9% (up to 29%) and the subsequent risk of vegetation exposure to O3, especially in crop-production regions. The enhancement effect of soil HONO emissions on O3 is increased from 1980s to 2016 in regions with low anthropogenic emissions. Therefore, we speculate that with future decreases in anthropogenic emissions, the relative impact of soil HONO emissions on air quality and vegetation is expected to increase. Thus, we recommend the consideration of soil HONO emissions in strategies for mitigating global air pollution.
08 Jul 2024Submitted to ESS Open Archive
08 Jul 2024Published in ESS Open Archive