State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, PR China; School of Geographical Sciences, Key Laboratory of Geographic Information Science (Ministry of Education), East China Normal University, Shanghai, 200241, PR China.
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 210008, PR China.
Environ Res. 2024 Nov 15;261:119691. doi: 10.1016/j.envres.2024.119691. Epub 2024 Jul 27.
Algae and macrophytes in lake ecosystems regulate nitrous oxide (NO) emissions from eutrophic lakes. However, knowledge of diurnal NO emission patterns from different habitats remains limited. To understand the diurnal patterns and driving mechanisms of NO emissions from contrasting habitats, continuous in situ observations (72 h) of NO fluxes from an algae-dominated zone (ADZ) and reed-dominated zone (RDZ) in Lake Taihu were conducted using the Floating Chamber method. The results showed average NO emission fluxes of 0.15 ± 0.06 and 0.02 ± 0.04 μmol m h in the ADZ and RDZ in autumn, respectively. The significantly higher (p < 0.05) NO fluxes in the ADZ were mainly attributed to differences in nitrogen (N) levels. The results also showed significant diurnal differences (p < 0.05) in the NO emission fluxes within the ADZ and RDZ, and daytime fluxes were significantly higher (p < 0.05) than nighttime fluxes. The statistical results indicated that NO emissions from the ADZ were mainly driven by diurnal variations in N loading and the dissolved oxygen (DO) concentration, and those from the RDZ were more influenced by DO, redox potential, and pH. Finally, we determined the proper time for routine monitoring of NO flux in the two habitats. Our results highlight the importance of considering diverse habitats and diurnal variations when estimating NO budgets at a whole-lake scale.
湖泊生态系统中的藻类和大型植物调节富营养化湖泊中氧化亚氮(NO)的排放。然而,不同生境中昼夜 NO 排放模式的知识仍然有限。为了了解不同生境中 NO 排放的昼夜模式和驱动机制,本研究采用浮室法对太湖藻型区(ADZ)和芦苇型区(RDZ)进行了 72 小时的原位连续观测(72 h)。结果表明,秋季 ADZ 和 RDZ 的平均 NO 排放通量分别为 0.15 ± 0.06 和 0.02 ± 0.04 μmol·m h。ADZ 中明显更高(p < 0.05)的 NO 通量主要归因于氮(N)水平的差异。结果还表明,ADZ 和 RDZ 内的 NO 排放通量存在显著的昼夜差异(p < 0.05),白天通量明显高于夜间通量。统计结果表明,ADZ 中的 NO 排放主要受 N 负荷和溶解氧(DO)浓度的昼夜变化驱动,而 RDZ 中的 NO 排放则更多地受到 DO、氧化还原电位和 pH 的影响。最后,我们确定了在这两种生境中进行常规监测 NO 通量的适当时间。我们的研究结果强调了在整个湖泊尺度上估算 NO 收支时考虑多种生境和昼夜变化的重要性。