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Distribution, flux, microbial consumption and dark production of carbon monoxide in the East China Sea in autumn
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Jiao-jiao PANG1, Li-xuan CHU1, Wen-yu HOU1, Jing ZHANG1, 2, Zhen HE1, 2, Gui-peng YANG1, 2, *
China Environmental Science | 2025, 45(8) : 4656 - 4666
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China Environmental Science | 2025, 45(8): 4656-4666
• Carbon Emission Control •
Distribution, flux, microbial consumption and dark production of carbon monoxide in the East China Sea in autumn
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Jiao-jiao PANG1, Li-xuan CHU1, Wen-yu HOU1, Jing ZHANG1, 2, Zhen HE1, 2, Gui-peng YANG1, 2, *
Affiliations
  • 1.College of Chemistry Engineering, Ocean University of China, Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, Qingdao 266100, China
  • 2.Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
Published: 2025-08-20
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A field survey was conducted in the East China Sea in autumn 2023 to study the distributions of carbon monoxide (CO) concentration, estimate the sea-to-air fluxes, and measure the microbial consumption and dark production rates of CO in the surface seawater. The results showed that atmospheric CO mixing ratios of the East China Sea ranged from 61.15 to 234.26 ppbv, with an average of (98.47 ± 49.64) ppbv. A headspace analysis system was used to determine CO. The concentrations of CO in the surface seawater ranged from 0.20 to 1.63 nmol/L, with an average of (0.63 ± 0.71) nmol/L. The CO concentrations exhibited noticeable daily variations across different water layers, with a maximum at noon and a minimum around dawn. The results of vertical distributions showed that the CO concentrations decreased gradually with the increase of depth. The sea-to-air fluxes of CO ranged from 0.45 to 5.66μmol/(m2·d), with an average of (2.11 ± 2.89) μmol/(m2·d). The results of sea-to-air fluxes estimation showed that the East China Sea was a source of atmospheric CO. The microbial consumption rate constants of CO in the surface seawater ranged from 0.16 to 0.33/h, with an average of (0.22 ± 0.07)/h. The consumption process showed the characteristics of first-order reaction. Dark production rates varied from 0.023 to 0.20nmol/(L·h), with an average of (0.12 ± 0.14) nmol/(L·h). The concentrations of CO increased linearly with the increase of time. This survey complements the source-sink processes of CO in the East China Sea, and contributes to a further understanding of the CO biogeochemical processes and its climatic effect in the continental shelf sea area.

carbon monoxide  /  distribution  /  sea-to-air flux  /  microbial consumption  /  dark production  /  East China Sea
庞娇娇, 褚礼轩, 侯雯彧, 张婧, 何真, 杨桂朋. 秋季东海一氧化碳的分布、通量、微生物消耗和暗反应生成研究. 中国环境科学, 2025 , 45 (8) : 4656 -4666 .
Jiao-jiao PANG, Li-xuan CHU, Wen-yu HOU, Jing ZHANG, Zhen HE, Gui-peng YANG. Distribution, flux, microbial consumption and dark production of carbon monoxide in the East China Sea in autumn[J]. China Environmental Science, 2025 , 45 (8) : 4656 -4666 .
Year 2025 volume 45 Issue 8
60
13
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  • Receive Date:2025-01-20
  • Online Date:2026-10-08
  • Published:2025-08-20
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  • Received:2025-01-20
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Affiliations
    1.College of Chemistry Engineering, Ocean University of China, Key Laboratory of Ministry of Education for Marine Chemistry Theory and Technology, Qingdao 266100, China
    2.Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
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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