Evaluating atmospheric mercury (Hg) uptake by vegetation in a chemistry-transport model

被引:0
作者
Feinberg, Aryeh [1 ]
Dlamini, Thandolwethu [1 ]
Jiskra, Martin [2 ]
Shah, Viral [3 ]
Selin, Noelle E. [1 ,4 ]
机构
[1] MIT, Inst Data Syst & Soc, Cambridge, MA 02139 USA
[2] Univ Basel, Environm Geosci, Basel, Switzerland
[3] Harvard Univ, Harvard John A Paulson Sch Engn & Appl Sci, Cambridge, MA 02138 USA
[4] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
基金
美国国家科学基金会; 瑞士国家科学基金会;
关键词
PARTICLE DRY DEPOSITION; LAND-USE; MONITORING SITES; REDOX CHEMISTRY; WET DEPOSITION; CLIMATE; AMAZON; FOREST; SIMULATION; EMISSIONS;
D O I
10.1039/d2em00032f
中图分类号
O65 [分析化学];
学科分类号
070302 ; 081704 ;
摘要
Mercury (Hg), a neurotoxic heavy metal, is transferred to marine and terrestrial ecosystems through atmospheric transport. Recent studies have highlighted the role of vegetation uptake as a sink for atmospheric elemental mercury (Hg-0) and a source of Hg to soils. However, the global magnitude of the Hg-0 vegetation uptake flux is highly uncertain, with estimates ranging 1000-4000 Mg per year. To constrain this sink, we compare simulations in the chemical transport model GEOS-Chem with a compiled database of litterfall, throughfall, and flux tower measurements from 93 forested sites. The prior version of GEOS-Chem predicts median Hg-0 dry deposition velocities similar to litterfall measurements from Northern hemisphere temperate and boreal forests (similar to 0.03 cm s(-1)), yet it underestimates measurements from a flux tower study (0.04 cm s(-1)vs. 0.07 cm s(-1)) and Amazon litterfall (0.05 cm s(-1)vs. 0.17 cm s(-1)). After revising the Hg-0 reactivity within the dry deposition parametrization to match flux tower and Amazon measurements, GEOS-Chem displays improved agreement with the seasonality of atmospheric Hg-0 observations in the Northern midlatitudes. Additionally, the modelled bias in Hg-0 concentrations in South America decreases from +0.21 ng m(-3) to +0.05 ng m(-3). We calculate a global flux of Hg-0 dry deposition to land of 2276 Mg per year, approximately double previous model estimates. The Amazon rainforest contributes 29% of the total Hg-0 land sink, yet continued deforestation and climate change threatens the rainforest's stability and thus its role as an important Hg sink. In an illustrative worst-case scenario where the Amazon is completely converted to savannah, GEOS-Chem predicts that an additional 283 Mg Hg per year would deposit to the ocean, where it can bioaccumulate in the marine food chain. Biosphere-atmosphere interactions thus play a crucial role in global Hg cycling and should be considered in assessments of future Hg pollution.
引用
收藏
页码:1303 / 1318
页数:16
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