The equilibrium constant for the reaction,
C(in liq. Fe)+
O(in liq. Fe)=CO(gas), has been studied by many workers, but their results do not agree with each other in the range of high carbon contents. In this range, the oxygen content is so small that accurate measurements of its values are difficult. The oxygen content is, however, to be proportional to the CO-pressure in the equilibrium state. For this reason, the experiments under high pressure were undertaken.
A pressure tight furnace was constructed. At the temperatures of 1200°∼1500°C, the oxygen content which was equilibrated with 0∼25 atm CO in carbon-saturated molten iron was measured by the vacuum fusion method. In the case of the furnace cooled samples, the analytical values of oxygen ranged from 20 to 40 ppm and were independent of the CO-pressure. It was considered that these samples absorbed a large quantity of oxygen after the sampling. In the case of the cast samples in the copper mould, on the other hand, the analytical values ranged from 2 to 10 ppm and the dependence on the CO-pressure was represented by
A×
PCO+
B at each temperature where
A was 0.23 and 0.16 (ppm/atm) at 1200° and 1500°C, respectively. It was concluded that the terms
A×
PCO and
B correspond to the dissolved and absorbed oxygen, respectively.
At the temperatures of 1200° and 1500°C, the equilibrium constant
K′(=
PCO⁄%
C×%
O=1⁄
A×%
C) is 10,000 and 12,000, and the activity coefficients of oxygen
f0 are calculated to be about 2 and 3 in the carbon-saturated melt. The values of interaction parameters,
e0(c)=∂log
f0⁄∂%
C and ε
0(c)=∂lnγ
0⁄∂Nc, are calculated to be about 0.1 and 5 at these experimental temperature. It should be noticed that these results are different in sign from the experimental results by other workers.
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