Measurement for Transport of Trace Mercury by Highly- Frequent Water Sampling in Minamata Bay

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  • 水俣湾における高頻度な水銀採水調査による微量水銀輸送量の測定
  • ミナマタワン ニ オケル コウヒンド ナ スイギン サイスイ チョウサ ニ ヨル ビリョウ スイギン ユソウリョウ ノ ソクテイ

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Abstract

We conducted highly-frequent water sampling for mercury speciation in sea water and suspended solid (SS) in Minamata Bay with continuous current and SS measurements. As a result, the followings were clarified: i) Particulate total mercury (T-Hg) in bottom layer was higher than that in surface and middle layer; ii) Dissolved T-Hg and methylmerculy (MeHg) were almost uniform vertically. Negative correlation between T-Hg and MeHg was shown; iii) Annual particulate T-Hg transport from Minamata Bay to the Yatsushiro Sea was estimated as 5-13kg. These results suggest that highly-frequent mercury measurement plays an important role in an accurate estimation of mercury mass balance.

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