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[天津市滨海河流NO的扩散通量与控制]

[Diffusive Fluxes and Controls of NO from Coastal Rivers in Tianjin City].

作者信息

Tang Meng-Yao, Hu Xiao-Kang, Wang Hong-Wei, Wang Yun-Cang, Chang Su-Yun, Wang Song-Qing, Zhong Ji-Cheng

机构信息

State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China.

College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China.

出版信息

Huan Jing Ke Xue. 2022 Mar 8;43(3):1481-1491. doi: 10.13227/j.hjkx.202106144.

Abstract

Rivers are an important emission source of greenhouse gases. To explore the spatial characteristics and influencing factors of NO emission from the coastal rivers in Tianjin City, six rivers into the Bohai Sea from different land-use types were selected, and the NO concentrations, saturation, and diffusive fluxes were measured using the headspace-gas chromatography method. The NO concentration was in supersaturation, and the rivers were the source of atmospheric NO. The average concentration, saturation, and diffusive fluxes of NO were (23.85±15.20) nmol·L, (309.71±197.38)%, and (27.04±16.46) μmol·(m·d), with the ranges of 12.70-115.69 nmol·L, 164%-1502%, and 9.17-244.79 μmol·(m·d), respectively. The NO concentrations and diffusive fluxes of the rivers presented great spatial heterogeneity, with the sewage river (Huangdipai River)>urban river (Haihe River main stream, Jiyun River)>suburban river (Duliujian River, Yongding Xinhe River)>agricultural river (Chaobai Xinhe River). The NO concentration and diffusion fluxes were significantly correlated with salinity, nutrients, and carbon sources. NO-N and TP contributed greatly to the diffusive flux differences. NO production and emission greatly related to the nitrogen cycle process in the Tianjin River, and different forms of nitrogen variously contributed to NO diffusive fluxes. The salinity gradient had the opposite effect on the NO emission in urban rivers and drainage rivers. The NO diffusive fluxes of the sewage river in Tianjin were significantly higher than that of other river types. In the future, due to the development of urbanization and the expansion of urban land, more management measures should focus on the hotspots such as the downstream of wastewater treatment plants of sewage rivers, the estuaries of urban rivers, and the residential gathering areas of suburban rivers to reduce NO emission.

摘要

河流是温室气体的重要排放源。为探究天津市沿海河流一氧化氮(NO)排放的空间特征及影响因素,选取了6条从不同土地利用类型流入渤海的河流,采用顶空-气相色谱法测定了NO浓度、饱和度及扩散通量。NO浓度呈过饱和状态,河流是大气NO的排放源。NO的平均浓度、饱和度及扩散通量分别为(23.85±15.20)nmol·L、(309.71±197.38)%和(27.04±16.46)μmol·(m²·d),范围分别为12.70 - 115.69 nmol·L、164% - 1502%和9.17 - 244.79 μmol·(m²·d)。河流的NO浓度和扩散通量呈现出较大的空间异质性,顺序为污水河(黄排水河)>城市河流(海河干流、蓟运河)>城郊河流(独流减河、永定新河)>农业河流(潮白新河)。NO浓度和扩散通量与盐度、营养物质及碳源显著相关。NO-N和TP对扩散通量差异贡献较大。NO的产生和排放与天津河流中的氮循环过程密切相关,不同形态的氮对NO扩散通量的贡献各异。盐度梯度对城市河流和排水河流中的NO排放有相反影响。天津市污水河的NO扩散通量显著高于其他河流类型。未来,由于城市化发展和城市土地扩张,更多管理措施应聚焦于污水河污水处理厂下游、城市河河口及城郊河居民聚集区等热点区域,以减少NO排放。

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