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DOI | 10.1016/j.atmosenv.2021.118634 |
Mercury in precipitated and surface snow at Dome C and a first estimate of mercury depositional fluxes during the Austral summer on the high Antarctic plateau | |
Cairns W.R.; Turetta C.; Maffezzoli N.; Magand O.; Araujo B.F.; Angot H.; Segato D.; Cristofanelli P.; Sprovieri F.; Scarchilli C.; Grigioni P.; Ciardini V.; Barbante C.; Dommergue A.; Spolaor A. | |
发表日期 | 2021 |
ISSN | 1352-2310 |
卷号 | 262 |
英文摘要 | The role of deposition fluxes on the mercury cycle at Concordia station, on the high Antarctic plateau have been investigated over the Austral summer between December 2017 to January 2018. Wet/frozen deposition was collected daily from specially sited tables, simultaneously with the collection of surface (0–3 cm) and subsurface (3–6 cm) snow and the analysis of Hg0 in the ambient air. Over the course of the experiment the atmospheric Hg0 concentrations ranged from 0.58 ± 0.19 to 1.00 ± 0.33 ng m−3, surface snow Hg concentrations varied between (0–3 cm) 0.006 ± 0.003 to 0.001 ± 0.001 ng cm−3 and subsurface snow (3–6 cm) concentrations varied between 0.001 ± 0.001 to 0.003 ± 0.002 ng cm−3. The maximum daily wet deposition flux was found to be 23 ng m−2 d−1. Despite the low temporal resolution of our measurements combined with their potential errors, the linear regression of the Hg deposition fluxes against the snow accumulation rates allowed us to estimate the mean dry deposition rate from the intercept of the graph as −0.005 +- 0.008 ng m−2 d−1. From this analysis, we conclude that wet deposition accounts for the vast majority of the Hg deposition fluxes at Concordia Station. The number of snow events, together with the continuous GEM measurements have allowed us to make a first estimation of the mean snow scavenging factor at Dome C. Using the slope of the regression of mercury flux on snow accumulation we obtained a snow scavenging factor that ranges from 0.21 to 0.22 ± 0.02 (ngHg/g snow)/(ngHg/m3air). Our data indicate that the boundary layer height and local meteorological effects influence Hg0 reemission from the top of (0–3 cm) the snowpack into the atmosphere and into the deeper snowpack layer (3–6 cm). These data will help constrain numerical models on the behaviour of mercury in Antarctica. © 2021 Elsevier Ltd |
关键词 | Atmospheric conditionsHigh resolution samplingSnow scavenging factorSnow sublimation |
语种 | 英语 |
scopus关键词 | Boundary layers; Deposition rates; Domes; Mercury (metal); Antarctic plateau; Atmospheric conditions; Austral summers; Deposition fluxes; Depositional fluxes; High resolution sampling; Snow accumulation; Snow scavenging factor; Snow sublimation; Surface snow; Snow; ambient air; boundary layer; mercury (element); regression; scavenging (chemistry); snowpack; wet deposition; Antarctica; Dome Concordia; East Antarctica |
来源期刊 | ATMOSPHERIC ENVIRONMENT
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/248282 |
作者单位 | CNR-Institute of Polar Sciences (ISP-CNR), 155 Via Torino, Mestre, 30170, Italy; Institut des Géosciences de l'Environnement, Université Grenoble Alpes, CNRS, IRD, Grenoble INP, Grenoble, 38400, France; CNRS, IRD, CET, Université Paul Sabatier–Toulouse III, Toulouse, France; Institute of Arctic and Alpine Research (INSTAAR), University of Colorado Boulder, Boulder, United States; Department of Environmental Sciences, Informatics and Statistics, University Ca’ Foscari of Venice, 155 Via Torino, Mestre30170, Italy; Institute of Atmospheric Sciences and Climate (CNR-ISAC), Via P. Gobetti 101, Bologna, 40129, Italy; CNR-Institute of Atmospheric Pollution Research (IIA-CNR), Division of Rende, UNICAL-Polifunzionale, Rende87036, Italy; ENEA, C.R. Casaccia, Roma, 00123, Italy |
推荐引用方式 GB/T 7714 | Cairns W.R.,Turetta C.,Maffezzoli N.,et al. Mercury in precipitated and surface snow at Dome C and a first estimate of mercury depositional fluxes during the Austral summer on the high Antarctic plateau[J],2021,262. |
APA | Cairns W.R..,Turetta C..,Maffezzoli N..,Magand O..,Araujo B.F..,...&Spolaor A..(2021).Mercury in precipitated and surface snow at Dome C and a first estimate of mercury depositional fluxes during the Austral summer on the high Antarctic plateau.ATMOSPHERIC ENVIRONMENT,262. |
MLA | Cairns W.R.,et al."Mercury in precipitated and surface snow at Dome C and a first estimate of mercury depositional fluxes during the Austral summer on the high Antarctic plateau".ATMOSPHERIC ENVIRONMENT 262(2021). |
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