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海洋的氧化还原界面 现在已经知道,海水中溶有微量的重金属,而且由于海域不同其差别很大。但是,若把海水作为海底热液的重金属来源,其浓度又实在太低了。
The redox interface in the oceans now knows that trace amounts of heavy metals are dissolved in the seawater and vary greatly depending on the sea area. However, if seawater is used as a heavy metal source for seafloor hydrothermal fluids, the concentration is too low.