State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200241, China; Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China.
Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China.
Water Res. 2022 Apr 1;212:118110. doi: 10.1016/j.watres.2022.118110. Epub 2022 Jan 20.
Estuaries are expected to contribute large nitrous oxide (NO) emissions, however the environmental controls and implications of NO emissions have not been well understood. Here we investigated water NO concentrations, fluxes and sources in wet and dry seasons for 2019-2020 in five subtropical estuaries spanning hydrologic characteristics and nitrogen concentrations gradient. Water dissolved NO concentrations and fluxes were in a range of 15.8-84.9 nmol L and 0.66-22.2 µg m h, respectively. These studied estuaries were oversaturated in NO, with the saturations of 118-615%. Water dissolved NO concentrations, saturations and fluxes increased significantly as nitrogen concentrations increase, whereas they did not differ significantly between the wet and dry seasons. Water NO emissions, however, were also lower in the estuaries characterized by large discharge and water flow. NO saturations and fluxes were determined directly by water nitrogen and oxygen concentrations and more indirectly by water temperature and velocity. The δN-NO and site preference-NO varied respectively from 2.86 to 11.31‰ and from 1.58 to 11.72‰, which overlapped the values between nitrification and denitrification. Nitrification and denitrification were responsible for 18.7-38.1% and 61.9-81.3% of NO emissions, respectively. Indirect NO emission factors were 0.08-0.14% and decreased with increasing total nitrogen concentrations. It is estimated that water NO emissions in CO equiv could offset approximately 4.9% of average CO sink of China estuaries. Therefore, these results suggest that nitrogen concentrations and hydrologic characteristics together modify NO emissions and that estuaries may be the important contributors to NO emissions.
预计河口将贡献大量的一氧化二氮(NO)排放,但对 NO 排放的环境控制和影响尚未得到很好的理解。在这里,我们调查了 2019-2020 年五个亚热带河口在干湿两季的水 NO 浓度、通量和来源,这些河口具有不同的水文特征和氮浓度梯度。水溶解 NO 浓度和通量的范围分别为 15.8-84.9 nmol L 和 0.66-22.2 µg m h。这些研究中的河口的 NO 均处于过饱和状态,饱和度为 118-615%。水溶解 NO 浓度、饱和度和通量随着氮浓度的增加而显著增加,而在干湿两季之间没有显著差异。然而,在具有大流量和水流的河口,NO 排放量也较低。NO 饱和度和通量直接由水中氮和氧的浓度决定,更间接由水温、流速决定。δN-NO 和位偏好-NO 分别从 2.86 到 11.31‰和从 1.58 到 11.72‰变化,与硝化和反硝化之间的数值重叠。硝化和反硝化分别负责 18.7-38.1%和 61.9-81.3%的 NO 排放。间接 NO 排放因子为 0.08-0.14%,并随总氮浓度的增加而降低。据估计,水中的 NO 排放相当于中国河口平均 CO 汇的 4.9%左右。因此,这些结果表明,氮浓度和水文特征共同调节 NO 排放,河口可能是 NO 排放的重要贡献者。