海洋界面

海洋界面层是水&大气之间气体交换的重要场所之一，因此海洋既可能是大气VHCs的源，也可能是汇。

Ocean interface layer is one of the important places of gases exchange between water and atmosphere , so the ocean may be the source of atmospheric VHCs , it also may become the sink of them .

模拟海洋沉积物界面邻近条件下，研究了吸附硅酸盐及Cu、Pb、Co、Ni的水合氧化铁颗粒和FeS沉淀对Mn（Ⅱ）氧化反应的影响。

Effects of hydrous Fe (ⅲ) oxide particulate that absorbs silicate and heavy matals like Cu , Pb , Co 、 Ni and the FeS Precipitate on the rate of Mn (ⅱ) oxidation have been studied under simulated conditions adjacent to seawater sediment interface .

在海洋水域，界面波对大尺度变化流的作用是一种典型的分层流动现象。

The interfacial waves on large-scale currents in the ocean is typical of stratified flow .

海洋沉积物&海水界面附近氮、磷、硅的生物地球化学

N , P and Si Biogeochemistry near Marine Sediment-Seawater Interface