TY - JOUR
T1 - Mercury speciation in the water of Minamata Bay, Japan
AU - Matsuyama, Akito
AU - Eguchi, Tomomi
AU - Sonoda, Ikuko
AU - Tada, Akihide
AU - Yano, Shinichirou
AU - Tai, Akira
AU - Marumoto, Kohji
AU - Tomiyasu, Takashi
AU - Akagi, Hirokatsu
N1 - Funding Information:
Acknowledgments We acknowledge the financial support received in the form of a Grant-in-Aid for Scientific Research (C) (No.18560500) from the Japan Society for the Promotion of Science and a grant from the Kyushu University Foundation. We are also thankful to the kind support and help of Dr Steven J. Balogh with our investigation.
PY - 2011/6
Y1 - 2011/6
N2 - The speciation of mercury (Hg) in Minamata Bay (Japan) was studied over a 2-year period (2006-2008). Concentrations of dissolved total Hg, dissolved methylmercury (MeHg), particulate total Hg, and suspended solids were 0.43±0.14 ng/l (mean±standard deviation), 0.10±0.06 ng/l, 3.04±2.96 ng/l, and 5.94± 2.10 mg/l, respectively. Correlations between concentrations of particulate total Hg and suspended solids at four depths (surface: 0 m; mid-depth: -6 m,-10 m; and bottom +1 m layer) were only significant in the bottom +1 m layer. The mean dissolved MeHg concentration and the ratio of dissolved MeHg to dissolved total Hg were considerably higher in summer compared to other seasons. The data suggest that bottom sediment was not the sole source of MeHg, and that MeHg may be produced in the water column by the conversion of divalent Hg eluted from resuspended bottom sediment. The correlation between seawater characteristics such as salinity, temperature, dissolved oxygen (DO), and dissolved MeHg concentration indicates that Hg methylation could be influenced by the heterotrophic activity of microorganisms in the seawater. In particular, inverse correlations were observed between DO, salinity, and MeHg concentration. However, dissolved MeHg concentrations did not correlate with seawater characteristics such as pH or chlorophyll-a.
AB - The speciation of mercury (Hg) in Minamata Bay (Japan) was studied over a 2-year period (2006-2008). Concentrations of dissolved total Hg, dissolved methylmercury (MeHg), particulate total Hg, and suspended solids were 0.43±0.14 ng/l (mean±standard deviation), 0.10±0.06 ng/l, 3.04±2.96 ng/l, and 5.94± 2.10 mg/l, respectively. Correlations between concentrations of particulate total Hg and suspended solids at four depths (surface: 0 m; mid-depth: -6 m,-10 m; and bottom +1 m layer) were only significant in the bottom +1 m layer. The mean dissolved MeHg concentration and the ratio of dissolved MeHg to dissolved total Hg were considerably higher in summer compared to other seasons. The data suggest that bottom sediment was not the sole source of MeHg, and that MeHg may be produced in the water column by the conversion of divalent Hg eluted from resuspended bottom sediment. The correlation between seawater characteristics such as salinity, temperature, dissolved oxygen (DO), and dissolved MeHg concentration indicates that Hg methylation could be influenced by the heterotrophic activity of microorganisms in the seawater. In particular, inverse correlations were observed between DO, salinity, and MeHg concentration. However, dissolved MeHg concentrations did not correlate with seawater characteristics such as pH or chlorophyll-a.
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U2 - 10.1007/s11270-010-0654-z
DO - 10.1007/s11270-010-0654-z
M3 - Article
AN - SCOPUS:80053573522
SN - 0049-6979
VL - 218
SP - 399
EP - 412
JO - Water, Air, and Soil Pollution
JF - Water, Air, and Soil Pollution
IS - 1-4
ER -