Benthic biogeochemical cycling of mercury in two contaminated northern Adriatic coastal lagoons

被引:43
|
作者
Covelli, Stefano [1 ]
Emili, Andrea [1 ]
Acquavita, Alessandro [1 ,2 ]
Koron, Neza [3 ,4 ]
Faganeli, Jadran [3 ]
机构
[1] Univ Trieste, Dipartimento Geosci, I-34128 Trieste, Italy
[2] ARPA FVG, Osservatorio Alto Adriat, I-33057 Palmanova, Italy
[3] Natl Inst Biol, Marine Biol Stn, Piran 6330, Slovenia
[4] Jozef Stefan Inst, Dept Environm Sci, Ljubljana 1000, Slovenia
关键词
Mercury; Contamination; Sediment; Benthic fluxes; Biogeochemical cycling; Lagoon; GULF-OF-TRIESTE; ROOM-TEMPERATURE PRECOLLECTION; LEVEL ENVIRONMENTAL-SAMPLES; SOUTHERN VENICE LAGOON; MARINE-SEDIMENTS; ORGANIC-MATTER; HEAVY-METALS; PARTICULATE MATTER; MONOMETHYL MERCURY; FLUX MEASUREMENTS;
D O I
10.1016/j.csr.2011.08.005
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Previous research recognized most of the Northern Adriatic coastal lagoon environments as contaminated by mercury (Hg) from multiple anthropogenic sources. Among them, the Pialassa Baiona (P.B.) Lagoon, located near the city of Ravenna (Italy), received between 100 and 200 tons of Hg, generated by an acetaldehyde factory in the period 1957-1977. Further east, the Grado Lagoon has been mainly affected by a long-term Hg input from the Idrija mine (western Slovenia) through the Isonzo River since the 16th century. Hg cycling at the sediment-water interface (SW!) of the two lagoons was investigated and compared by means of an in situ benthic chamber, estimating diffusive Hg and Methyl-Hg fluxes in the summer season. Major chemical features in porewaters (Fe, Mn, H2S, dissolved inorganic (DIC) and organic carbon (DOC), nutrients) and in the solid phase (C-org, N and S) were also explored to understand the general biogeochemical conditions of the system in response to benthic respiration. The daily integrated flux for the methylated Hg form was extremely low in P.B. Lagoon, accounting for only 7% of the corresponding flux calculated for the Grado Lagoon. Despite a higher sedimentary Hg content in the P.B. Lagoon (14.4-79.0 mu g g(-1)) compared to the Grado Lagoon (10.7-12.5 mu g g(-1)), the in situ fluxes of Hg in the two experimental sites appeared similar. A selective sequential extraction procedure was applied to the solid phase, showing that the stable crystalline mineral phase cinnabar (HgS) is the predominant Hg fraction (about 50%) in the Grado Lagoon surface sediments. Conversely, Hg mobilization and sequestration in the P.B. Lagoon is related to the extremely anoxic redox conditions of the system where the intense sulfate reduction, by the release of sulfur and the formation of sulfides, limits the metal recycling at the SWI and its availability for methylation processes. Thus, the environmental conditions at the SWI in the P.B. Lagoon seem to represent a natural "barrier" for the potential risk of Hg transfer to the aquatic trophic chain. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1777 / 1789
页数:13
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