Elevated atmospheric deposition and dynamics of mercury in a remote upland forest of southwestern China

被引:113
|
作者
Fu, Xuewu [1 ]
Feng, Xinbin [1 ]
Zhu, Wanze [2 ]
Rothenberg, S. [1 ]
Yao, Heng [1 ,3 ]
Zhang, Hui [1 ,3 ]
机构
[1] Chinese Acad Sci, State Key Lab Environm Geochem, Inst Geochem, Guiyang 550002, Peoples R China
[2] Chinese Acad Sci, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China
[3] Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
关键词
Hg; Atmospheric deposition; Flux; Upland forest; Hg budget; REACTIVE GASEOUS MERCURY; FLUX CHAMBER MEASUREMENT; METHYL MERCURY; BACKGROUND SOILS; EMISSION FLUXES; WET DEPOSITION; EASTERN SLOPE; NATIONAL-PARK; AMBIENT AIR; EXCHANGE;
D O I
10.1016/j.envpol.2010.01.032
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Mt. Gongga area in southwest China was impacted by Hg emissions from industrial activities and coal combustion, and annual means of atmospheric TGM and PHg concentrations at a regional background station were 3.98 ng m(-3) and 30.7 pg m(-3), respectively. This work presents a mass balance study of Hg in an upland forest in this area. Atmospheric deposition was highly elevated in the study area, with the annual mean THg deposition flux of 92.5 mu g m(-2) yr(-1). Total deposition was dominated by dry deposition (71.8%), and wet deposition accounted for the remaining 28.2%. Forest was a large pool of atmospheric Hg, and nearly 76% of the atmospheric input was stored in forest soil. Volatilization and stream outflow were identified as the two major pathways for THg losses from the forest, which yielded mean output fluxes of 14.0 and 8.6 mu g m(-2) yr(-1), respectively. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2324 / 2333
页数:10
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