關於海洋循環其中一段,請幫忙英翻中。

誰能幫忙翻譯一下…機器翻譯不要來。

because O2 enters seawater only at the ocean surface, the circulation of the ocean influences where organic carbon accumulates.

at present, the thermohaline circulation system "ventilates" most of the deep ocean.

cold O2-rich water sinks into the deep ocean from the surface waters of the North Atlantic and offshore Antarctica, spreads worldwide, and inhibits the accumulation of organic carbon in deep-ocean sediments.

organic-rich sediments can be found today where deep water is isolated from the global thermohaline circulation and has become anoxic,that is, starved of oxygen.

one example is the black sea, witch connects to the world ocean only through a shallow passage to the Mediterranean.

organic-rich sediments also accumulate within isolated depressions in the continental margin of southern California, where seafloor water stagnates beneath the coastal surface waters.

1 Answer

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  • EMED
    Lv 7
    1 decade ago
    Favorite Answer

    because O2 enters seawater only at the ocean surface, the circulation of the ocean influences where organic carbon accumulates.

    因為氧氣入海只在海洋表面上,海洋循環影響到有機碳累積的地方

    at present, the thermohaline circulation system "ventilates" most of the deep ocean.

    目前,溫鹽環流(輸送洋流)(深海環流)系統使多數深海逹到換氣的效果

    cold O2-rich water sinks into the deep ocean from the surface waters of the North Atlantic and offshore Antarctica, spreads worldwide, and inhibits the accumulation of organic carbon in deep-ocean sediments.

    冷的氧氣從北大西洋及南極近海的表面下沈到深海,延伸到世界各地,且抑制在深海有機碳的累積.

    organic-rich sediments can be found today where deep water is isolated from the global thermohaline circulation and has become anoxic,that is, starved of oxygen.

    今日在全球溫鹽環流(輸送洋流)(深海環流) 深海被分離的地方可發現富含有機的沈澱物且水質變得缺氧.

    one example is the black sea, witch connects to the world ocean only through a shallow passage to the Mediterranean.

    如黑海只透過淺水處流到地中海與世界海洋連結

    organic-rich sediments also accumulate within isolated depressions in the continental margin of southern California, where seafloor water stagnates beneath the coastal surface waters.

    富有的沈積物也累積在南加州大陸邊緣中隔離的溼地裡,那裡海底的水淤積在沿岸的海水表面之下.

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