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沿海河流降雨期间的动态氮素迁移与一氧化氮排放

Dynamic N transport and NO emission during rainfall events in the coastal river.

作者信息

Zhang Wen-Xi, Yue Fu-Jun, Wang Yong, Li Yun, Lang Yun-Chao, Li Si-Liang

机构信息

Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China.

Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China; Tianjin Bohai Rim Coastal Earth Critical Zone National Observation and Research Station, Tianjin University, Tianjin 300072, China.

出版信息

Sci Total Environ. 2023 Dec 10;903:166206. doi: 10.1016/j.scitotenv.2023.166206. Epub 2023 Aug 9.

Abstract

The coastal zone exhibited a high population density with highly impacted by anthropogenic activities, such as river impoundment to prevent saline intrusion, which resulted in weak hydrological conditions. Rainfall events can result in dramatic changes in hydrological and nutrient transportation conditions, especially in rivers with weak hydrological conditions. However, how the nitrogen transport and NO emissions or biogeochemistry responds to the different types of rainfall events in the weak hydrodynamics rivers is poorly understood. In this study, the hydrological, nitrogenous characteristic, as well as NO dynamics, were studied by high-frequency water sampling during two distinct rainfall events, high-intensity with short duration (E1) and low-intensity with long duration (E2). The results displayed that the hydrologic condition in E1 with a wider range of d-excess values (from -9.50 to 32.1 ‰), were more dynamic than those observed in E2. The NO concentrations (0.01-3.33 μmol/L) were higher during E1 compared to E2 (0.03-1.11 μmol/L), which indicated that high-intensity rainfall has a greater potential for NO emission. On the contrary, the concentrations of nitrogen (e.g., TN and NO-N) were lower during E1 compared to E2. Additionally, hysteresis was observed in both water and nitrogen components, resulting in a prolonged recovery time for pre-rainfall levels during the long-duration event. Moreover, the results showed that the higher average NO flux (78.3 μmol/m/h) in the rainfall event period was much larger than that in the non-rainfall period (1.63 μmol/m/h). The frequency dam regulation resulted in the water level fluctuation, which could enhance wet-dry alternation and simulated NO emissions. This study highlighted the characteristic of N dynamic and hydrological responses to diverse rainfall events occurrences in the coastal river. Rainfall could increase the NO emission, especially during high-intensity rainfall events, which cannot be ignored in the context of annual NO release.

摘要

沿海地区人口密度高,受人类活动影响大,如修建拦河坝以防止海水入侵,导致水文条件薄弱。降雨事件会导致水文和养分输送条件发生显著变化,尤其是在水文条件薄弱的河流中。然而,在水动力较弱的河流中,氮素迁移和一氧化氮排放或生物地球化学如何响应不同类型的降雨事件,目前尚不清楚。在本研究中,通过在两次不同降雨事件期间进行高频水样采集,研究了水文、含氮特性以及一氧化氮动态,这两次降雨事件分别为高强度短历时(E1)和低强度长历时(E2)。结果表明,E1的水文条件具有更宽的d-过剩值范围(从-9.50到32.1‰),比E2更具动态性。与E2(0.03 - 1.11 μmol/L)相比,E1期间的一氧化氮浓度(0.01 - 3.33 μmol/L)更高,这表明高强度降雨具有更大的一氧化氮排放潜力。相反,与E2相比,E1期间的氮浓度(如总氮和硝态氮)较低。此外,在水和氮成分中均观察到滞后现象,导致长历时降雨事件后恢复到降雨前水平的时间延长。此外,结果表明,降雨事件期间较高的平均一氧化氮通量(78.3 μmol/m/h)远大于非降雨期间(1.63 μmol/m/h)。频繁的大坝调节导致水位波动,这可能会增强干湿交替并模拟一氧化氮排放。本研究突出了沿海河流中氮动态和水文对不同降雨事件发生的响应特征。降雨会增加一氧化氮排放,尤其是在高强度降雨事件期间,在年度一氧化氮排放的背景下,这一点不容忽视。

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