Mercury biogeochemistry in the Idrija River, Slovenia, from above the mine into the Gulf of Trieste

被引:178
|
作者
Hines, ME
Horvat, M
Faganeli, J
Bonzongo, JCJ
Barkay, T
Major, EB
Scott, KJ
Bailey, EA
Warwick, JJ
Lyons, WB
机构
[1] Univ Alaska, Dept Biol Sci, Anchorage, AK 99508 USA
[2] Jozef Stefan Inst, Dept Environm Sci, Ljubljana, Slovenia
[3] Marine Biol Stn, Piran, Slovenia
[4] Austin Coll, Dept Environm Sci, Sherman, TX 75090 USA
[5] Rutgers State Univ, Dept Microbiol & Biochem, New Brunswick, NJ 08903 USA
[6] Univ Alaska, Environm & Nat Resources Inst, Anchorage, AK 99508 USA
[7] Univ Manitoba, Dept Microbiol, Winnipeg, MB R3T 2N2, Canada
[8] US Geol Survey, Anchorage, AK USA
[9] Univ Florida, Dept Environm Engn Sci, Gainesville, FL 32601 USA
[10] Univ Alabama, Dept Geol, Tuscaloosa, AL 35486 USA
关键词
mercury; biogeochemistry; mer operon; methylation; demethylation;
D O I
10.1006/enrs.2000.4052
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Idrija Mine is the second largest Hg mine in the world which operated for 500 years. Mercury (Hg)-laden tailings still line the banks, and the system is a threat to the Idrija River and water bodies downstream including the Soca/Isonzo River and the Gulf of Trieste in the northern Adriatic Sea. A multidisciplinary study was conducted in June 1998 on water samples collected throughout the Idrija and Soca River systems and waters and sediments in the Gulf Total Hg in the Idrija River increased >20-fold downstream of the mine from <3 to > 60 ng liter(-1) with methyl mercury (MeHg) accounting for similar to 0.5%, Concentrations increased again downstream and into the estuary with MeHg accounting for nearly 1.5% of the total. While bacteria upstream of the mine did not contain mercury detoxification genes (mer), such genes were detected in bacteria collected downstream. Benthic macroinvertebrate diversity decreased downstream of the mine. Gulf waters near the river mouth contained up to 65 ng liter(-1) total Hg with similar to 0.05 ng liter(-1) MeHg. Gulf sediments near the river mouth contained 40 mu g g(-1) total Hg with MeHg concentrations of about 3 ng g(-1), Hg in sediment pore waters varied between 1 and 8 ng liter(-1), with MeHg accounting for up to 85%, Hg methylation and MeHg demethylation were active in Gulf sediments with highest activities near the surface. MeHg was degraded by an oxidative pathway with >97% C released from MeHg as CO2. Hg methylation depth profiles resembled profiles of dissolved MeHg. Hg-laden waters still strongly impact the riverine, estuarine, and marine systems, Macroinvertebrates and bacteria in the Idrija River responded to Hg stress, and high Hg levels persist into the Gulf. Increases in total Hg and MeHg in the estuary demonstrate the remobilization of Hg, presumably as HgS dissolution and recycling, Gulf sediments actively produce MeHg, which enters bottom waters and presumably the marine food chain. (C) 2000 Academic Press.
引用
收藏
页码:129 / 139
页数:11
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