大气颗粒态汞光还原机制研究
ID:1856
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Updated Time:2024-04-11 20:05:47 Hits:1759
Oral Presentation
Abstract
Particle bound mercury (PBM) deposition on the Earth's surface threatens biota and humans. The photoreduction of PBM competes with deposition and thereby modifies global mercury cycling, yet its pathway and mechanism remain poorly understood. Herein, we reveal the photoreduction process of PBM by comprehensively using field observation, mercury stable isotope analysis and controlled experiment. We found the Δ199Hg values in wet haze episodes (0.34‰±0.30‰) were significantly higher than those in clean periods (0.14‰±0.19‰), majorly attributed to the elevated aerosol water content (AWC) which shifts aerosol phase from solid state to liquid state, promoting soluble HgCl2 and HgBr2 photoreduction reactions. The carboxyl functional groups of water-soluble organic carbon (WSOC) was further identified as the crucial compound that induces PBM photoreduction, whose reaction rates were ~2 times higher than phenol and ketone ligands and 3–6 times higher than those observed in other atmospheric aqueous phases. Considering the ubiquitously distributed carboxyl ligands and significant positive Δ199Hg signals in the atmospheric aqueous phases, the PBM photoreduction mediated by carboxyl ligands is highlighted to significantly influence global mercury transformations, regional depositions and isotopic compositions of atmospheric mercury pools.
Submission Author
韩德明
国科大杭州高等研究院
史建波
中国科学院生态环境研究中心
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