水华引发总溶解气体过饱和增强CH4、N2O排放:以高坝洲水库为例
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1.三峡大学水利与环境学院;2.中国长江电力股份有限公司

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国家自然科学基金项目(52309095,52409097,U25A20361,52509102,32401364),中国长江电力股份有限公司科研项目(Z242602001)和三峡水库生态系统湖北省野外科学观测研究站开放基金(2024YWZ04)


Supersaturated total dissolved gases enhance CH4 and N2O emissions during algal bloom period: a Gaobazhou Reservoir case study
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Affiliation:

1.College of Hydraulic and Environmental Engineering, China Three Gorges University;2.China Yangtze Power Co.,Ltd.

Fund Project:

The National Natural Science Foundation of China (Nos. 52309095, 52409097, U25A20361, 52509102, 32401364),Scientific Research Project of China Yangtze Power Co., Ltd. (No. Z242602001) and Open Fund of Hubei Provincial Field Scientific Observation and Research Station of Three Gorges Reservoir Ecosystem (No. 2024YWZ04)

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    摘要:

    藻类水华对水库温室气体排放具有重要调控作用。为探究水华对温室气体的时空演变及释放机制影响,本研究在高坝洲水库水华暴发期开展了高分辨率水体表层和垂向 CO2、CH4、N2O浓度和释放通量监测。结果表明,水库CO2、CH4、N2O 浓度范围分别为 0.12~216.12 μmol/L(饱和度 1.8%~1332.9%)、0.01~0.41 μmol/L(饱和度 1198.2%~12789.5%) 和 17.83~48.78 nmol/L(饱和度 221.8%~538.5%),除水华区 CO2 ,其他区域温室气体均呈过饱和状态。浮箱法测量无水华区 CO2、CH4、N2O 释放通量分别为 204.39±170.93 mg/(m2·h)、0.36±0.42 mg/(m2·h) 和 0.01±0.01 mg/(m2·h),水华区分别为 -88.42±39.20 mg/(m2·h)、0.55±0.51 mg/(m2·h) 和 0.07±0.05 mg/(m2·h)。水库水华区表层水体因强烈光合作用由 CO2 的“源”转为“汇”,但 CH4 和 N2O 排放通量较无水华区分别激增 54% 和 342%。浮箱法和薄边界层法测量通量结果存在显著差异,浮箱法结果为薄边界层法的 3~10 倍,其中水华最严重地区达 10 倍左右。水华造成溶解气体组分差异且引发了表层水体总溶解气体过饱和(饱和度 111.6%~136.4%)产生微气泡,致使气体传输方式转变为扩散和微气泡排放,显著增强 CH4 和 N2O 向大气排放。本研究揭示了水华通过改变气体释放途径激发了强效温室气体排放,为精细化水库碳排放评估提供了关键机理支撑。

    Abstract:

    Algal blooms significantly alter biogeochemical cycling and greenhouse gas (GHG) fluxes in reservoir ecosystems. To investigate the impact of algal blooms on the spatial-temporal dynamics and interfacial transport mechanisms of GHGs, high-resolution monitoring of dissolved CO2, CH4 and N2O concentrations and fluxes were conducted in the Gaobazhou Reservoir during a bloom event. . Dissolved concentrations ranged from 0.12 to 215.82 μmol/L for CO2 (saturation: 1.8% to 1332.9%), 0.01 to 0.41 μmol/L for CH4 (saturation: 1198.2% to 12789.5%), and 17.83 to 48.78 nmol/L for N2O (saturation: 221.8% to 538.5%). Except CO2 in the bloom zone, all monitored GHGs were highly supersaturated. Floating chamber measured CO2, CH4 and N2O fluxes in non-algal bloom areas were 204.39±170.93 mg/(m2·h), 0.36±0.42 mg/(m2·h), and 0.01±0.01 mg/(m2·h), respectively, in the algal bloom areas were -88.42±39.20 mg/(m2·h) for CO2, 0.55±0.51 mg/(m2·h) for CH4, and 0.07±0.05 mg/(m2·h) for N2O. Driven by intense photosynthetic activity in the algal bloom areas, the surface water shifted from a CO2 source to a net sink;, compared to non-bloom areas However, CH4 and N2O emissions increased by 54% and 342%, respectively. Significant methodological discrepancies were found between the flux results of floating chamber and thin boundary layer methods: floating chamber estimations were 3-10 times higher than those derived from the thin boundary layer method, with the maximum divergence (~10×) occurring in the algal bloom regions. Algal blooms altered dissolved gas compositions and induced total dissolved gas (TDG) supersaturation (111.6% to 136.4%). The TDG supersaturation triggered microbubble formation, shifting the dominant gas transfer pathway to a coupled process of molecular diffusion and microbubble-mediated emission, which significantly enhanced CH4 and N2O emissions. This study demonstrates that algal blooms stimulate GHGs emissions by fundamentally altering interfacial gas transfer pathways, providing a new insight for accurate reservoir carbon budgeting and eco-hydraulic management.

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  • 收稿日期:2026-04-28
  • 最后修改日期:2026-07-01
  • 录用日期:2026-07-07
  • 在线发布日期: 2026-09-10
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