文摘
To investigate transport and partitioning processes ofHgT in the Fox River, we coupled detailed time seriesdataof total mercury (HgT) at the river mouth withtransectsampling in the Lower Fox River. Unfiltered HgTconcentrationsin the Fox River during the study period (April 1994-October 1995) ranged from 1.8 to 182 ng L-1with a medianof 24.8 ng L-1, predominantly (93.6%) in theparticulatephase. These levels were significantly elevatedcomparedwith other large tributaries to Lake Michigan (Hurley, J.P.; Shafer, M. M.; Cowell, S. E.; Overdier, J. T.; Hughes,P.E.; Armstrong, D. E. Environ. Sci. Technol. 1996,30, 2093-2098). Transect sampling revealed progressivelyincreasingwater column HgT concentrations and HgTparticulateenrichment downstream, which were consistent with trendsin sediment HgT levels in the river. Resuspendedsedimentsare likely the predominant source of Hg from the Fox Riverinto Green Bay. Despite elevated HgTconcentrations,methyl mercury (MeHg) concentrations were relatively low,suggesting limited bioavailability of HgT associatedwithsediments.