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Spatial and temporal variations of methane diffusive fluxes across the sediment-water interface in Lake Taihu
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Li-fei DING1, 2, Tong LI2, Wen-xin WEI1, 2, En-qin YAO3, Ji-cheng ZHONG2, He-zhong YUAN1, Lei ZHANG2, *
China Environmental Science | 2025, 45(3) : 1474 - 1482
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China Environmental Science | 2025, 45(3): 1474-1482
Environmental Ecology
Spatial and temporal variations of methane diffusive fluxes across the sediment-water interface in Lake Taihu
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Li-fei DING1, 2, Tong LI2, Wen-xin WEI1, 2, En-qin YAO3, Ji-cheng ZHONG2, He-zhong YUAN1, Lei ZHANG2, *
Affiliations
  • 1.School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China
  • 2.State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
  • 3.Huzhou Municipal Bureau of Ecology and Environment, Zhejiang Province, Huzhou 313000, China
Published: 2025-03-20
Outline
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A year-long study was conducted in Taihu Lake with the objective of investigate the diffusive fluxes of methane(CH4)across the sediment-water interface in different ecological zones, namely the algal bloom zone, the macrophyte zone, and the open water zone. The CH4 concentrations in the sediment porewaters and the relevant fluxes at the sediment-water interface from different ecological zones of the lake were analyzed and evaluated. Results showed that CH4 concentrations in porewaters increased with the sediment depth. The CH4 concentrations in the open water zone were found significantly lower than that in the other zones. The organic carbon was identified as the key factor driving the spatial and temporal variations of CH4. The mean diffusive fluxes of CH4 across the sediment-water interface were 122.56±32.2, 108.75±23.8, and 3.36±0.6 µmol/(m2·d)in the algal bloom zone, the macrophyte zone, and the open water zone, respectively, with the open water zone showing the significantly lower fluxes. Seasonal variations of CH4 fluxes were observed in the lake while the fluxes were significantly higher in the spring and the summer than the other two seasons. The regression result showed that the CH4 flux was strongly influenced by the CH4 concentration in the porewater and the sediment porosity. Our study also demonstrated that algal blooms and macrophyte reproductions enhanced CH4 concentrations in porewaters and significantly increased the diffusive CH4 fluxes across the sediment-water interface in Lake Taihu.

Lake Taihu  /  methane  /  diffusive flux  /  sediment-water interface  /  greenhouse gas
Li-fei DING, Tong LI, Wen-xin WEI, En-qin YAO, Ji-cheng ZHONG, He-zhong YUAN, Lei ZHANG. Spatial and temporal variations of methane diffusive fluxes across the sediment-water interface in Lake Taihu[J]. China Environmental Science, 2025 , 45 (3) : 1474 -1482 .
Year 2025 volume 45 Issue 3
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  • Receive Date:2024-08-26
  • Online Date:2026-03-18
  • Published:2025-03-20
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  • Received:2024-08-26
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Affiliations
    1.School of Environmental Science and Engineering, Nanjing University of Information Science & Technology, Nanjing 210044, China
    2.State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China
    3.Huzhou Municipal Bureau of Ecology and Environment, Zhejiang Province, Huzhou 313000, China
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表12种不同金属材料的力学参数

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Number of
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Number of
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鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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