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用XPS,UPS和AES研究铁早期氧化过程,认为在温度不太高和氧分压不太大的条件下,多晶铁片与氧作用生成的化合物是Fe3O4而不是FeO和α-Fe2O3,也不是三种化合物的分层分布。在600℃以上高温下,氧分压近于1×10-6Torr下,出现了铁表面上氧的热脱附过程而不是氧化过程。The early oxidation process of pure Fe was studied by XPS, UPS and AES. When the temperature and partial pressure of oxygen is not too high, the product of the reaction between polycrystalline Fe and oxygen is pure Fe3O4, but not FeO or a-Fe2O3 or a structure of layers of the three compounds. If the temperature is higher than 600℃ and the partial pressure of oxygen approach 1 × 10-6 Torr, the thermo-desorption process occurs instead of oxidation process on polystalline Fe surface.







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