Drivers, trends and impacts of nitrogen deposition in China

IF 74.1
Lei Liu, Xuejun Liu, Xuemei Wang, Wen Xu, Aohan Tang, Enzai Du, Lei Duan, Yuepeng Pan, Lin Zhang, Jianlin Shen, Ling Song, Kaihui Li, Xiaobing Zhou, Xiankai Lu, Yu Zhao, Qian Yu, Mengmeng Li, Xiuying Zhang, Zhang Wen, Tianxiang Hao, Liquan Yao, Keith Goulding, Jeffrey L. Collett Jr., Peter Vitousek, Fusuo Zhang
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Abstract

Since 1980, there have been substantial changes in reactive nitrogen (Nr) deposition in China, with implications for nutrient pollution, ecosystem health and the sustainability of food systems. This Review synthesizes evidence from national monitoring networks and modelling studies to elucidate the drivers and profound ecological consequences of these changes. Nr deposition increased to a maximum of 16.4 Tg N yr−1 in 2010–2012. Thereafter, stringent industrial nitrogen oxide (NOx) emission controls led to a 14% decline in total Nr deposition by 2020, to 13.3 Tg N yr−1, primarily through a 34% reduction in oxidized nitrogen. Reduced nitrogen from agriculture now dominates Nr deposition, constituting 60–70% of the total deposition. This dominance of reduced nitrogen has resulted in severe ecological impacts, including widespread soil acidification, freshwater eutrophication and biodiversity loss. As of 2020, ~15% of China’s land area is experiencing Nr deposition exceeding critical loads for eutrophication. Future climate change, particularly warming and intensified precipitation extremes, is projected to further reduce ecosystem resilience, thereby increasing the terrestrial area in which Nr deposition exceeds critical loads for eutrophication. China would need to achieve reductions in ammonia and NOx deposition of 56–76% and 53–60%, respectively, to match average Nr deposition levels in the USA and Western Europe. Thus, integrating agricultural ammonia management into wider climate and air quality policies is a priority to ensure ecosystem protection and long-term environmental sustainability in China. Reactive nitrogen deposition in China has changed markedly since 1980 owing to variations in emissions from industry and agriculture, with consequences for ecosystems, food systems and pollution control. This Review synthesizes deposition trends, emission and meteorological drivers, ecological impacts and management strategies for sustainable nitrogen mitigation in China.
中国氮沉降的驱动因素、趋势及影响
自1980年以来,中国活性氮(Nr)沉降发生了实质性变化,对养分污染、生态系统健康和粮食系统的可持续性具有重要意义。本综述综合了来自国家监测网络和建模研究的证据,以阐明这些变化的驱动因素和深远的生态后果。2010-2012年,Nr沉积量最大,达到16.4 Tg N yr−1。此后,严格的工业氮氧化物(NOx)排放控制导致到2020年总Nr沉积减少14%,至13.3 Tg N yr - 1,主要是通过氧化氮减少34%。农业减少的氮现在主导了Nr沉积,占总沉积的60-70%。这种减少氮的优势导致了严重的生态影响,包括广泛的土壤酸化、淡水富营养化和生物多样性丧失。截至2020年,中国约15%的陆地面积正经历超过富营养化临界负荷的Nr沉降。预计未来的气候变化,特别是变暖和极端降水加剧,将进一步降低生态系统的恢复能力,从而增加陆地上Nr沉降超过富营养化临界负荷的面积。中国需要实现氨氮和氮氧化物沉积分别减少56-76%和53-60%,以达到美国和西欧的平均Nr沉积水平。因此,将农业氨管理纳入更广泛的气候和空气质量政策是确保中国生态系统保护和长期环境可持续性的优先事项。自1980年以来,由于工业和农业排放的变化,中国的活性氮沉积发生了显著变化,对生态系统、粮食系统和污染控制产生了影响。本文综述了中国氮素可持续减排的沉积趋势、排放和气象驱动因素、生态影响和管理策略。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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