The reason why oxygen contents in grey iron scatter greatly seems to be caused by adsorption of gases in atmosphere, therefore, the mechanism of adsorption was investigated in CO and H
2O+Ar atmospheres. The results obtained were summarized as follows: 1) If grey iron was treated thoroughly by degassing hold in vacuum of 10
-5 mmHg at 900°C, oxygen contents turned to the values corresponding to those of white iron. 2) Increase of oxygen content in grey iron with increase of holding time was deduced by adsorption of gas to graphite presented in matrix and diffusion of adsorbed gas into the graphite. 3) Moisture in the air was adsorbed selectively in the early stage of adsorption. 4) The reason that even in the same sample oxygen contents in the part of grey iron are higher than those of white iron part participates in the precipitation mechanism of graphite, the difference of directional growth of graphite crystal and thermal expansion, and micro gap between matrix and graphite.
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