Article ID Journal Published Year Pages File Type
10565755 Marine Chemistry 2015 9 Pages PDF
Abstract
T-Hg, DGM, RM, and MMHg in the seawater columns (n = 132) were in the range of 0.05-3.04 ng L− 1, 0.003-1.08 ng L− 1, 0.006-1.47 ng L− 1, 0.02-0.69 ng L− 1 for an entire sample. Although the average T-Hg values at the surface and middle layers (0-100 m) for each sample showed no significant seasonal variation throughout the year, those at the deeper layer (150-200 m) were high from summer to autumn and low in winter. The seasonal changes and vertical distributions of DGM, RM, and MMHg concentrations were similar to those of T-Hg. A thermocline was observed from spring to autumn and ceased in winter. Because the thermocline prohibits vertical circulation of seawater, the fumarole impact may increase during those months.
Related Topics
Physical Sciences and Engineering Chemistry Chemistry (General)
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