Pregled bibliografske jedinice broj: 1190400
A Simplified Approach to Modeling the Dispersion of Mercury from Precipitation to Surface Waters— The Bay of Kaštela Case Study
A Simplified Approach to Modeling the Dispersion of Mercury from Precipitation to Surface Waters— The Bay of Kaštela Case Study // Journal of Marine Science and Engineering, 10 (2022), 4; 539, 12 doi:10.3390/jmse10040539 (međunarodna recenzija, članak, znanstveni)
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Naslov
A Simplified Approach to Modeling the Dispersion
of Mercury from Precipitation to Surface Waters—
The Bay of Kaštela Case Study
Autori
Živković, Igor ; Gačnik, Jan ; Jozić, Slaven ; Kotnik, Jože ; Šolić, Mladen ; Horvat, Milena
Izvornik
Journal of Marine Science and Engineering (2077-1312) 10
(2022), 4;
539, 12
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
mercury ; wet deposition ; concentration gradient ; seawater mixing ; Adriatic Sea
Sažetak
Wet deposition is the main source of mercury (Hg) from the atmosphere to the Earth’s surface. However, the processes that govern the dispersion of deposited Hg in seawater are currently not well understood. To address this issue, total mercury (THg) concentrations in surface seawaters and precipitation were determined on a monthly basis in the Bay of Kaštela (Central Adriatic Sea). Following the assumption that deposited THg is diluted in the seawater bulk due to mixing processes, an exponential decay-like model was developed and the wet deposition of THg was normalized based on periods between precipitation events and seawater sampling. Normalized wet deposition of THg showed significant correlation with the THg gradient in surface seawater after removal of an outlier. To explain the observed outlier, further data normalization included wind data to account for enhanced seawater mixing due to strong winds. Wind-normalized THg deposition of all datapoints showed significant correlation with the THg gradient in surface seawater. The correlation showed that the THg gradient in surface seawater of 0.378 pg L−1 m−1 corresponds to THg wet deposition of 1 ng m−2 after including the influence of wind speed on seawater mixing.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Kemija
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus