Gradient measurements of gaseous elemental mercury (Hg0) in the marine boundary layer of the northwest Sea of Japan (East Sea)
Autor: | V. V. Kalinchuk, Evgeny Lopatnikov, Anatoly Astakhov |
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Rok vydání: | 2018 |
Předmět: |
Pollution
Daytime Marine boundary layer 010504 meteorology & atmospheric sciences Health Toxicology and Mutagenesis media_common.quotation_subject chemistry.chemical_element Environmental pollution Elemental mercury General Medicine 010501 environmental sciences Toxicology Atmospheric sciences 01 natural sciences Research vessel Mercury (element) chemistry Environmental science Underwater 0105 earth and related environmental sciences media_common |
Zdroj: | Environmental Pollution. 237:1124-1136 |
ISSN: | 0269-7491 |
DOI: | 10.1016/j.envpol.2017.11.055 |
Popis: | Gaseous elemental mercury (Hg0) is a prolific and persistent contaminant in the atmosphere. Atmospheric concentrations of Hg0 were determined from 17 September to 7 October 2015 in the northwest Sea of Japan aboard the Russian research vessel Professor Gagarinsky. Simultaneous measurements of Hg0 concentrations were performed 2 m and 20 m above the sea surface using automatic Hg0 analysers RA-915M and RA-915+, respectively. Concentrations ranged from 0.3 to 25.9 ng/m3 (n = 5207) and from 0.3 to 27.8 ng/m3 (n = 4415), with medians of 1.7 and 1.6 ng/m3, respectively. Elevated Hg0 was observed during three episodes from 19 to 22 September, likely caused by one or more of the following factors: 1) atmospheric transport of Hg0 from the west and south-west (from N. Korea, China, and the Yellow Sea region); 2) Hg0 emission from the sea due to pollution by water from the Tumannaya River; or 3) underwater geological activities. Increased Hg0 concentration was observed during periods when air masses flowed from the south, and low concentrations were observed when air masses came from the north. A daytime increase of Hg0 concentrations at a height of 2 m occurred simultaneously with decreasing Hg0 at a height of 20 m. These diurnal variations suggest that two contrasting processes occur during the daytime in the marine boundary layer (MBL): Hg0 emission from the sea surface and Hg0 oxidation in the MBL by active halogens formed by photolysis. |
Databáze: | OpenAIRE |
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