中国东部及渤、黄、东海大气全氟辛酸沉降通量研究OA
Study on Atmospheric Deposition Fluxes of Perfluorooctanoic Acid over Eastern China and the Bohai,Yellow,and East China Seas
针对全氟辛酸(Perfluorooctanoic acid,PFOA)通过大气传输影响海洋环境的现状,本研究基于改进的社区多尺度空气质量模型-全氟和多氟烷基化合物(Community multiscale air quality model-per/polyfluoroalkyl substances,CMAQ-PFAS)模块,结合新建的2019年1、4、7、10月中国工业源大气PFOA排放清单,系统研究了中国东部大气PFOA干/湿沉降通量的时空特征及渤、黄、东海大气PFOA输入的贡献.结果表明:2019年中国东部大陆地区总PFOA年均干沉降通量(1.20 ng·m-2·d-1)显著高于渤、黄、东海海域(0.31 ng·m-2·d-1),其中颗粒态约占92.5%(1.11 ng·m-2·d-1).海陆干沉降通量均呈现冬季高、夏季低的季节性差异,陆地区域冬季(2.38 ng·m-2·d-1)为夏季(0.53 ng·m-2·d-1)的4.5倍,渤、黄、东海海域冬季为夏季的6.9倍.2019年中国东部大陆地区总PFOA年均湿沉降通量约为0.40 ng·m-2·d-1,颗粒态与气态组分贡献占比分别为20.0%(0.08 ng·m-2·d-1)和80.0%(0.32 ng·m-2·d-1).中国东部大陆地区PFOA湿沉降通量呈现夏季(0.76 ng·m-2·d-1)>冬季(0.67 ng·m-2·d-1)>春季(0.20 ng·m-2·d-1)>秋季(0.12 ng·m-2·d-1)的梯度特征.大气沉降对表层海水(<30 cm)PFOA浓度的贡献具有空间梯度特征:冬季渤海、黄海和东海贡献率分别为2.3%、1.5%和9.3%,而夏季则分别降至0.8%、0.3%和1.3%.东海由于海水PFOA环境暴露浓度最低,其大气沉降的平均贡献率最高(5.3%).相比之下,黄海海水PFOA环境暴露浓度较高,其大气沉降的平均贡献率最低(1.4%).本研究揭示了大气沉降作为PFOA进入渤、黄、东海的途径,其贡献率呈现显著时空差异,为评估PFOA在海洋环境中的迁移与风险提供了科学依据.
In view of the current situation where Perfluorooctanoic acid(PFOA)affects the marine en-vironment through atmospheric transport.In this study,based on the improved three-dimensional at-mospheric chemical transport model—the community multiscale air quality model-per/polyfluoroalkyl substances(CMAQ-PFAS)module.Based on the newly established inventories of industrial source at-mospheric PFOA emissions in China for January,April,July and October,2019,the spatial and tempo-ral characteristics of the dry/wet deposition fluxes of atmospheric PFOA in eastern China and the contri-bution of atmospheric PFOA input from the Bohai,Yellow,and East China Seas were systematically investigated.The results show that the annual mean dry deposition flux of total PFOA in the eastern Chinese mainland in 2019(1.20 ng·m-2·d-1)is significantly higher than that in the Bohai,Yellow,and East China Seas(0.31 ng·m-2·d-1),with the share of the particulate state reaching 92.5%(1.11 ng·m-2·d-1).Dry deposition fluxes showed seasonal differences of high winter and low summer,with winter(2.38 ng·m-2·d-1)being 4.5 times higher than summer(0.53 ng·m-2·d-1)in the land region,and winter being 6.9 times higher than summer in the Bohai,Yellow,and East China Seas.The annual mean wet deposition flux of total PFOA in eastern mainland China in 2019 was about 0.40 ng·m-2·d-1,with the particulate and gaseous components contributing 20.0%(0.08 ng·m-2·d-1)and 80.0%(0.32 ng·m-2·d-1).The PFOA wet deposition fluxes in the eastern mainland of China showed summer(0.76 ng·m-2·d-1)>winter(0.67 ng·m-2·d-1)>spring(0.20 ng·m-2·d-1)>significant gradient in fall(0.12 ng·m-2·d-1).The contribution of atmospheric deposition to the PFOA concentration in surface seawater(<30 cm)was characterized by a spatial gradient:in winter,the contributions of the Bohai Sea,Yellow Sea,and East China Sea were 2.3%,1.5%,and 9.3%,respectively,while in summer they decreased to 0.8%,0.3%,and 1.3%.Due to the lowest back-ground concentration of PFOA in seawater,the East China Sea has the highest average contribution rate of atmospheric deposition(5.3%).In contrast,the background concentration of PFOA in the Yellow Sea seawater is relatively high,thus the average contribution rate of atmospheric deposition is the lowest(1.4%).This study reveals that atmospheric deposition,as a pathway for PFOA to enter the Bohai Sea,the Yellow Sea,and the East China Seas,has significant spatial and temporal differences in its con-tribution rate,which provides a scientific basis for assessing the risk of PFOA to the marine environ-ment.
李芬香;刘晓环;刘震泽;张月;刘兰莹
中国海洋大学环境科学与工程学院,山东 青岛 266100中国海洋大学环境科学与工程学院,山东 青岛 266100||中国海洋大学海洋环境与生态教育部重点实验室,山东 青岛 266100中国海洋大学环境科学与工程学院,山东 青岛 266100中国海洋大学环境科学与工程学院,山东 青岛 266100中国海洋大学环境科学与工程学院,山东 青岛 266100
资源环境
全氟辛酸大气排放清单社区多尺度空气质量模型-全氟和多氟烷基化合物模块渤海黄海东海沉降通量空间分布
perfluorooctanoic acidatmospheric emission inventorycommunity multiscale air quality model-per/polyfluoroalkyl substances moduleBohai Seathe Yellow SeaEast China Seadeposition fluxspatial distribution
《中国海洋大学学报(自然科学版)》 2026 (6)
78-92,15
国家自然科学基金面上项目(42175129)资助Supported by the General Program of the National Natural Science Foundation of China(42175129)
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