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Title:Dissolved gaseous mercury production and sea-air gaseous exchange in impacted coastal environments of the northern Adriatic Sea
Authors:ID Floreani, Federico (Author)
ID Barago, Nicolò (Author)
ID Klun, Katja (Author)
ID Faganeli, Jadran (Author)
ID Covelli, Stefano (Author)
Files:URL URL - Source URL, visit https://doi.org/10.1016/j.envpol.2023.121926
 
.pdf PDF - Presentation file, download (6,86 MB)
MD5: 27D2D39379D530E53154A1E75EBC2F70
 
Language:English
Typology:1.01 - Original Scientific Article
Organization:Logo NIB - National Institute of Biology
Abstract:The northern Adriatic Sea is well known for mercury (Hg) contamination mainly due to historical Hg mining which took place in Idrija (Slovenia). The formation of dissolved gaseous mercury (DGM) and its subsequent volatilisation can reduce the amount of Hg available in the water column. In this work, the diurnal patterns of both DGM production and gaseous elemental Hg (Hg0) fluxes at the water-air interface were seasonally evaluated in two selected environments within this area, a highly Hg-impacted, confined fish farm (VN: Val Noghera, Italy) and an open coastal zone less impacted by Hg inputs (PR: Bay of Piran, Slovenia). A floating flux chamber coupled with a real-time Hg0 analyser was used for flux estimation in parallel with DGM concentrations determination through in-field incubations. Substantial DGM production was observed at VN (range = 126.0–711.3 pg L−1) driven by both strong photoreduction and possibly dark biotic reduction, resulting in higher values in spring and summer and comparable concentrations throughout both day and night. Significantly lower DGM was observed at PR (range = 21.8–183.4 pg L−1). Surprisingly, comparable Hg0 fluxes were found at the two sites (range VN = 7.43–41.17 ng m−2 h−1, PR = 0–81.49 ng m−2 h−1), likely due to enhanced gaseous exchanges at PR thanks to high water turbulence and to the strong limitation of evasion at VN by water stagnation and expected high DGM oxidation in saltwater. Slight differences between the temporal variation of DGM and fluxes indicate that Hg evasion is more controlled by factors such as water temperature and mixing conditions than DGM concentrations alone. The relative low Hg losses through volatilisation at VN (2.4–4.6% of total Hg) further confirm that static conditions in saltwater environments negatively affect the ability of this process in reducing the amount of Hg retained in the water column, therefore potentially leading to a greater availability for methylation and trophic transfer.
Keywords:Idrija mercury mine, mercury evasion, fish farm, flux chamber, water-air exchange, Adriatic Sea, Idrijski rudnik živega srebra, ribogojnica, pretočna komora, izmenjava voda-zrak, Jadransko morje
Publication status:Published
Publication version:Version of Record
Publication date:01.09.2023
Year of publishing:2023
Number of pages:[1]-16 str.
Numbering:Vol. 332, [art.] 121926
PID:20.500.12556/DiRROS-19263 New window
UDC:504.5
ISSN on article:0269-7491
DOI:10.1016/j.envpol.2023.121926 New window
COBISS.SI-ID:158532099 New window
Note:Soavtorji: Nicolò Barago, Katja Klun, Jadran Faganeli, Stefano Covelli;
Publication date in DiRROS:12.07.2024
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Downloads:2
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Record is a part of a journal

Title:Environmental pollution
Shortened title:Environ. pollut.
Publisher:Elsevier Applied Science Publishers
ISSN:0269-7491
COBISS.SI-ID:25405184 New window

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License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

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