State Key Laboratory of Environmental Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, PR China.
Shenzhen Key Laboratory of Soil and Groundwater Pollution Control, School of Environmental Science and Engineering, Southern University of Science and Technology, Shenzhen, Guangdong, 518055, PR China.
Environ Pollut. 2018 Dec;243(Pt B):1818-1824. doi: 10.1016/j.envpol.2018.09.113. Epub 2018 Sep 28.
Nitrous oxide (NO) is a major greenhouse gas, with elevated emission being reported from subtropical forests that receive high nitrogen (N) deposition. After 10 years of monthly addition of ammonium nitrate (NHNO) or sodium nitrate (NaNO) to a Mason pine forest at Tieshanping, near Chongqing city in Southwest China, the simulated N deposition was stopped in October 2014. The results of soil NO emissions monitoring in different seasons during the nitrogen application period showed that nitrogen addition significantly increased soil NO emission. In general, the NO emission fluxes were positively correlated to nitrate (NO) concentrations in soil solution, supporting the important role of denitrification in NO production, which was also modified by environmental factors such as soil temperature and moisture. After stopping the application of nitrogen, the soil NO emissions from the treatment plots were no longer significantly higher than those from the reference plots, implying that a decrease in nitrogen deposition in the future would cause a decrease in NO emission. Although the major forms of N deposition, NH and NO, had not shown significantly different effects on soil NO emission, the reduction in NH deposition may decrease the NO concentrations in soil solution faster than the reduction in NO deposition, and thus be more effective in reducing NO emission from N-saturated forest soil in the future.
一氧化二氮(NO)是一种主要的温室气体,有报道称,在亚热带森林中,由于氮(N)沉降量较高,NO 的排放量也有所增加。在中国西南部重庆市附近的铁山坪,对一片南方松人工林进行了 10 年每月添加硝酸铵(NHNO)或硝酸钠(NaNO)的模拟氮沉降实验,2014 年 10 月停止了模拟氮沉降。在施氮期间不同季节的土壤 NO 排放监测结果表明,氮添加显著增加了土壤 NO 排放。一般来说,NO 排放通量与土壤溶液中硝酸盐(NO)浓度呈正相关,这支持了反硝化作用在 NO 生成中的重要作用,而反硝化作用也受到土壤温度和湿度等环境因素的影响。停止施氮后,处理样地的土壤 NO 排放不再明显高于对照样地,这意味着未来氮沉降的减少将导致 NO 排放的减少。尽管主要的氮沉降形式,NH 和 NO,对土壤 NO 排放没有表现出明显不同的影响,但 NH 沉降的减少可能会比 NO 沉降的减少更快地降低土壤溶液中的 NO 浓度,从而在未来更有效地减少 N 饱和森林土壤的 NO 排放。