九龙江口水体中N2O的产生、释放和输出

production,emission and export of nitrous oxide from the Jiulong river estuary

  • 摘要: 本研究分别于2020年7月和2020年12月采集九龙江口表层水体,测定了溶解氧化亚氮(N2O)浓度及其相关的理化参数,同时进行培养实验,测定硝化速率和N2O产生速率,分析九龙江口N2O的空间分布特征和季节变化规律,探讨了影响N2O分布的主要过程及关键因素,并利用LOICZ箱式模型计算了九龙江口N2O的河流输入、水—气交换、生物生产和河口输出通量。结果表明,九龙江口N2O浓度和饱和度存在显著的空间差异,其浓度范围为15.3~50.2 nmol/L,饱和度范围为214.6%~699.1%。冬季航次N2O的水—气通量为5.02×103 mol/d,夏季航次为4.09×103 mol/d,说明九龙江口是大气N2O的重要排放源。硝化作用是九龙江口水体N2O产生的主要途径,是调控水体N2O分布的主要过程,溶解无机氮是影响硝化作用的关键因素。夏季航次硝化作用产生的N2O通量占九龙江口水体N2O总输出通量的53.8%,冬季航次占50.3%。

     

    Abstract: In order to investigate the spatio-temporal variations of dissolved nitrous oxide (N2O), and to explore the main processes and key factors affecting the distribution of N2O in the Jiulong river estuary. N2O concentration and the related physical and chemical parameters were measured along the estuary with salinity gradient in July 2020 and December 2020. Nitrification rate and N2O production rate were also determined via incubation experiments. A Land-Ocean Interaction Coastal Zone (LOICZ) box model was used to evaluate the N2O budget in the Jiulong river estuary, including river input, water-gas exchange, biological production, and estuarine output fluxes. The results showed that the concentration and saturation of N2O in the Jiulong river estuary have significant spatial variations, ranging from 15.3~50.2 nmol/L and 214.6%~699.1%, respectively. The water-air flux of N2O was 5.02×103 mol/d in December 2020 and 4.09×103 mol/d in July 2020, indicating that the Jiulong river estuary was an important source of atmospheric N2O. Nitrification was the main process of N2O production, which was thus the main process of regulating the distribution of N2O in the estuary. The amount of N2O produced by nitrification to total N2O output in the Jiulong river estuary was 53.8% in July 2020 and 50.3% in December 2020.

     

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