State Key Laboratory of Organic Geochemistry, Guangdong Province Key Laboratory of Environmental Protection and Resources Utilization, and Guangdong-Hong Kong-Macao Joint Laboratory for Environmental Pollution and Control, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, P. R. China.
University of Chinese Academy of Sciences, Beijing 100049, P. R. China.
Environ Sci Technol. 2024 Apr 16;58(15):6682-6692. doi: 10.1021/acs.est.3c09173. Epub 2024 Mar 28.
The atmospheric deposition of anthropogenic active nitrogen significantly influences marine primary productivity and contributes to eutrophication. The form of nitrogen deposition has been evolving annually, alongside changes in human activities. A disparity arises between observation results and simulation conclusions due to the limited field observation and research in the ocean. To address this gap, our study undertook three field cruises in the South China Sea in 2021, the largest marginal sea of China. The objective was to investigate the latest atmospheric particulate inorganic nitrogen deposition pattern and changes in nitrogen sources, employing nitrogen-stable isotopes of nitrate (δN-NO) and ammonia (δN-NH) linked to a mixing model. The findings reveal that the N-NH deposition generally surpasses N-NO deposition, attributed to a decline in the level of NO emission from coal combustion and an upswing in the level of NH emission from agricultural sources. The disparity in deposition between N-NH and N-NO intensifies from the coast to the offshore, establishing N-NH as the primary contributor to oceanic nitrogen deposition, particularly in ocean background regions. Fertilizer (33 ± 21%) and livestock (20 ± 6%) emerge as the primary sources of N-NH. While coal combustion continues to be a significant contributor to marine atmospheric N-NO, its proportion has diminished to 22 (Northern Coast)-35% (background area) due to effective NO emission controls by the countries surrounding the South China Sea, especially the Chinese Government. As coal combustion's contribution dwindles, the significance of vessel and marine biogenic emissions grows. The daytime higher atmospheric N-NO concentration and lower δN-NO compared with nighttime further underscore the substantial role of marine biogenic emissions.
人为活性氮的大气沉降显著影响海洋初级生产力,并导致富营养化。随着人类活动的变化,氮沉降的形式也在逐年演变。由于海洋领域的实地观测和研究有限,观测结果与模拟结论之间存在差异。为了解决这一差距,我们在 2021 年在中国最大的边缘海——南海进行了三次实地考察。目的是研究大气颗粒态无机氮沉降最新模式和氮源变化,采用硝酸盐(δN-NO)和氨(δN-NH)的氮稳定同位素与混合模型相结合。研究结果表明,N-NH 沉降一般超过 N-NO 沉降,这归因于煤炭燃烧过程中 NO 排放水平的下降和农业源 NH 排放水平的上升。从沿海到近海,N-NH 和 N-NO 之间的沉降差异加剧,表明 N-NH 是海洋氮沉降的主要贡献者,特别是在海洋背景区域。化肥(33 ± 21%)和牲畜(20 ± 6%)是 N-NH 的主要来源。虽然煤炭燃烧仍然是海洋大气 N-NO 的重要贡献者,但由于南海周边国家,特别是中国政府,对其进行了有效的 NO 排放控制,其比例已降至 22%(北部沿海地区)-35%(背景地区)。随着煤炭燃烧的贡献减少,船舶和海洋生物源排放的重要性增加。与夜间相比,白天大气 N-NO 浓度较高,δN-NO 较低,进一步强调了海洋生物源排放的重要作用。