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Spatial and seasonal variability of nitrous oxide in a large freshwater lake in the lower reaches of the Yangtze River, China

机译:中国长江下游大型淡水湖中一氧化氮的空间和季节变异性

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摘要

Aquatic ecosystems are recognized as a source of N_2O in accordance with the flux estimations of rivers and estuaries; however, limited research has been conducted on large lakes. In this study, we report the annual N_2O dynamics of a large eutrophic freshwater lake located in the subtropical zone of East China. The dissolved N_2O concentrations in Lake Chaohu were observed to be between 8.5 and 92.3 nmol L~(-1) with emission rates between 0.3 and 53.6 μmol m~(-2) d~(-1) exhibiting considerable spatiotemporal variability. The average seasonal N_2O concentrations were obtained, with the highest value of 23.4 nmol L~(-1) found in winter and the lowest value of 12.7 nmol L~(-1) found in summer. In contrast to the N_2O concentrations observed, the highest N_2O emission rates occurred during summer, while the lowest emission rates occurred in autumn. The emissions of N_2O were substantially high in the western part of the lake, which suffers from serious eutrophication. In addition, the hotspots of N_2O emissions have been found around the inflowing mouth of the Nanfei River, which transports large amounts of nutrients into the lake. The results suggest that anthropogenically enhanced nutrient inputs may have a significant role in the production and emission of N_2O. However, the negative relationship between the surface water temperature and the N_2O concentration suggests that, N_2O fluxes might be influenced by other inconspicuous mechanisms. In the future the nitrogen dynamics of water and sediment in the lake should be collated to reveal mechanisms controlling N_2O emissions. In summary, Lake Chaohu acts as a source of N_2O with its most eutrophic part contributing 54.9% of the total N_2O emissions of the whole lake.
机译:水生生态系统根据河流和河口的助焊剂估算被认为是N_2O的来源;然而,有限的研究已经在大湖泊上进行。在这项研究中,我们报告了位于华东亚热带地区的大型Eutrophic淡水湖的年度N_2O动态。观察到巢湖湖中的溶解N_2O浓度为8.5至92.3nmol L〜(-1),排放率在0.3和53.6μmolm〜(-2)d〜(-1)之间,其表现出相当的时空变异性。获得平均季节性N_2O浓度,在冬季发现的最高值为23.4 nmol L〜(-1),在夏季发现的12.7 nmol L〜(-1)的最低值。与观察到的N_2O浓度相反,夏季发生最高的N_2O排放率,而最低排放率在秋季发生。 N_2O的排放在湖的西部大大高,这遭受严重的富营养化。此外,N_2O排放的热点已经发现了南飞河流入的嘴巴,其将大量的营养物质运送到湖中。结果表明,人为增强的营养素输入可能在N_2O的生产和排放中具有重要作用。然而,表面水温与N_2O浓度之间的负关系表明,N_2O助熔剂可能受到其他不起眼的机制的影响。将来,应整理湖泊水和沉积物的氮动力学,以揭示控制N_2O排放的机制。总之,巢湖湖作为N_2O的来源,其最富营养的部分有助于整个湖泊总N_2O排放的54.9%。

著录项

  • 来源
    《The Science of the Total Environment》 |2020年第15期|137716.1-137716.12|共12页
  • 作者单位

    State Key Laboratory of Lake Science and Environment Nanjing Institute of Geography and Limnology Chinese Academy of Sciences Nanjing 210008 PR China School of Geography and Tourism Anhui Normal University Wuhu 241002 PR China Anhui Province Key Laboratory of Earth Surface Processes and Regional Response in the Yangtze-Huaihe River Basin Wuhu 241002 PR China;

    State Key Laboratory of Water Environment Simulation School of Environment Beijing Normal University 19 Xinjiekouwai Street Haidian District Beijing 100875 PR China;

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

    Institute of Geographical Sciences Hebei Academy of Sciences Shijiazhuang 050011 PR China;

    School of Geography and Tourism Anhui Normal University Wuhu 241002 PR China;

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

    State Key Laboratory of Lake Science and Environment Nanjing Institute of Geography and Limnology Chinese Academy of Sciences Nanjing 210008 PR China Sino-Danish Centre for Education and Research University of Chinese Academy of Sciences Beijing PR China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Lake Chaohu; N_2O flux; N_2O concentration; Spatiotemporal variability;

    机译:巢湖湖;n_2o助焊剂;n_2o浓度;时空变异性;

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