The sulfide contents in the surface sediment basically tended to be high in the north and to be low in the south, while the redox potential presented the opposite change tendency.

 
  • 硫化物的垂直分布基本表現為隨深度的增加而增加,氧化-還原電位的垂直分布基本表現為隨深度的增加而降低。
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