Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
10565755 | Marine Chemistry | 2015 | 9 Pages |
Abstract
T-Hg, DGM, RM, and MMHg in the seawater columns (n = 132) were in the range of 0.05-3.04 ng Lâ 1, 0.003-1.08 ng Lâ 1, 0.006-1.47 ng Lâ 1, 0.02-0.69 ng Lâ 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.
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Authors
Takashi Tomiyasu, Takuya Minato, Wilder Leonardo Gamboa Ruiz, Hitoshi Kodamatani, Yuriko Kono, Masayasu Hidaka, Kimihiko Oki, Ryo Kanzaki, Yoko Taniguchi, Akito Matsuyama,