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AMAP评估报告解读:北极环境的汞

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北极监测与评估计划(AMAP)工作组于2021年发布了《北极环境的汞》科学评估报告,基于近年来北极环境介质中汞的观测和模拟研究,评估了北极环境介质的汞含量和储量水平,并预测了未来北极环境中汞含量的潜在变化。报告指出,全球大气汞排放主要源于北极以外地区(>98%),部分大气汞可随大气环流远距离传输并沉降至北极生态系统,进而参与北极地区汞的生物地球化学循环。其中2/3的北极大气汞沉降至陆地环境,1/3沉降至海洋环境。陆地环境的汞主要储存于土壤、冰川和积雪中,这部分汞可在河流输运和海岸侵蚀作用下输入北冰洋。汞也可经洋流作用输入北冰洋。储存于北冰洋的汞又可经逃逸至大气、埋藏于大陆架和深海盆地及洋流流出而去除。北极环境的汞主要以无机形式赋存,部分可在厌氧环境中经微生物甲基化过程转化为甲基汞。相比气候变化,初级排放减少对未来北极环境汞含量变化的影响更大。因此,需实施严格且可行的全球人为汞减排政策,以期在未来20年降低北极环境汞含量。报告也指出,未来需更好地量化北极局地汞排放、加强汞的关键环境过程的研究和模型开发、研究携带汞甲基化和去甲基化基因的微生物群落、进行一致的初级排放和气候变化预测及编制全球人为汞排放清单等,以准确评估北极环境汞循环、预测北极环境汞含量变化。
Interpretation of AMAP Assessment Reports:mercury in the Arctic environment
The Arctic Monitoring and Assessment Programme(AMAP)Workgroup released a scientific assess-ment of"Mercury(Hg)in the Arctic"in 2021,which evaluated the contents and storages of Hg over Arctic en-vironmental media and predicted the potential future changes of Hg contents in Arctic environment based on the observational and modelling studies of Hg in Arctic environmental media from recent years.The report stated that global atmospheric Hg emissions originated mainly outside the Arctic(>98%),and some of which could be transported over long distances in the atmospheric circulation and deposited in Arctic ecosystems,where them participated in the biogeochemical cycling of Hg in the Arctic.The 2/3 of the Arctic atmospheric Hg was deposit-ed to terrestrial environments and 1/3 to marine environments.Hg in terrestrial environments was mainly stored in soils,glaciers,and snow,and could be transported to the Arctic Ocean by riverine transport and coastal ero-sion.Hg could also be transported into the Arctic Ocean by ocean currents.Hg stored in the Arctic Ocean could be removed by escaping into the atmosphere,burying on the continental shelf and in deep-sea basins,and out-flowing by ocean currents.The Arctic environmental Hg was predominantly in inorganic form and could be par-tially converted to methylmercury(MeHg)by microbial methylation processes in anaerobic environments.Re-ductions in primary emissions will have a greater impact on future changes of Hg contents in Arctic environment than climate change.And thus stringent and feasible global anthropogenic Hg reduction policies are needed to re-duce the ambient Hg levels in the Arctic over the next 20 years.The report also noted that in the future,better quantification of local Hg releases from the Arctic,enhanced research and modelling of key environmental pro-cesses for Hg,studies of microbial communities carrying Hg methylation and demethylation genes,consistent projections of primary emissions and climate change,and global inventories of anthropogenic Hg emissions are needed to accurately assess Hg cycling in the Arctic environment and predict changes in Arctic environmental Hg levels.

Arcticmercuryemissions reductionclimate changeAMAP

杨争争、孙世威、苗希文、张玉兰、王兆清、郭军明、康世昌

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兰州大学 资源环境学院 西部环境教育部重点实验室,甘肃 兰州 730000

中国科学院 西北生态环境资源研究院冰冻圈科学与冻土工程重点实验室,甘肃 兰州 730000

中国科学院大学 资源与环境学院,北京 100049

北极 减排 气候变化 AMAP

国家自然科学基金项目国家重点研发计划项目甘肃省博士后研究资助项目中国博士后科学基金项目中国科学院西北生态环境资源研究院自主部署项目

422011612020YFA06085032021M6933752021000198

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(5)