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Spatial distribution, photo-production and flux of Hydrogen in the East China Sea in autumn |
JIANG Yu-cheng1,2, XU Gao-bin2, ZHOU Li-min2, ZHANG Hong-hai1,2 |
1. Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Frontiers Science Center for Deep Ocean Multispheres and Earth System, Ocean University of China, Qingdao 266100, China; 2. College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China |
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Abstract The spatial distribution, photo-production rate and sea-to-air flux of hydrogen (H2) were investigated in the East China Sea in October, 2021. The concentration of H2 in the surface seawater ranged from 2.94 to 7.67nmol/L, with a mean of value (4.82 ±1.12) nmol/L. As the vertical distribution of H2, the higher concentrations appeared at the bottom (11.86nmol/L) which attributed to the release from sediment, as an important source of H2 in the bottom seawater, according to the sediment incubation experiment. The photo-productionrates varied between 0.42 and 1.14nmol/(L·h), with an average of (0.72 ±0.25) nmol/L. The ratio of the quotient of H2 photo-production rates and cumulative photon flux under UV and PAR was 33:1. In addition, the saturation factors of H2 ranged from 7.14 to 24.37, suggesting the concentrations of H2 were oversaturated in seawater. The sea-to-air fluxes of H2 were estimated to be from 0.53 to 9.19 μmol/(m2·d), with a meanof (3.50 ±1.86) μmol/(m2·d), which indicated that the East China Sea is the net source of atmospheric H2.
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Received: 13 January 2023
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