Mercury budget of an upland-peatland watershed

Inputs, outputs, and pool sizes of total mercury (Hg) were measured in a fo rested 10 ha watershed consisting of a 7 ha hardwood-dominated upland surro unding a 3 ha conifer-dominated peatland. Hydrologic inputs via throughfall and stemflow, 13 +/- 0.4 mu g m(-2) yr(-1) over the entire watershed, were about double precipitation inputs in the open and were significantly highe r in the peatland than in the upland (19.6 vs. 9.8 mu g m(-2) yr(-1)). Inpu ts of Hg via litterfall were 12.3 +/- 0.7 mu g m(-2) yr(-1), not different in the peatland and upland (11.7 vs. 12.5 mu g m(-2) yr(-1)). Hydrologic ou tputs via streamflow were 2.8 +/- 0.3 mu g m(-2) yr(-1) and the contributio n from the peatland was higher despite its smaller area. The sum of Hg inpu ts were less than that in the overstory trees, 33 +/- 3 mu g m(-2) above-gr ound, and much less than either that in the upland soil, 5250 +/- 520 mu g m(-2), or in the peat, 3900 +/- 100 mu g m(-2) in the upper 50 cm. The annu al flux of Hg measured in streamflow and the calculated annual accumulation in the peatland are consistent with values reported by others. A sink for Hg of about 20 mu g m(-2) yr(-1) apparently exists in the upland, and could be due to either or both storage in the soil or volatilization.