By Isao Ishibe and Noboru Hirano.
The reducing velacities of the Johore hematite ore were tested by the various gas mixtures of CO, CO
2 and N
2. The reoucing gas, in which the sum of the partial preasures of CO and CO
2 was kept. at O.4 or O.6 atm. press., and the ratios of CO
2/CO were varied from zero to 2.5, Was passed through the sample in the rate of 100c per min. The temperature of the experiments were 700, 800, 90O and 1, 000°C The CO
2 in the exhausted gas passed through the sample was analysed every ten minutes, and thus the amount of oxygen from the iron ore was calculated from the diffbrehce between the volume of CO
2 cantained in the exhaused gas and the same in the reducing gas.
From the results of the above expedments we concluded as follows:
(1) The more the ratio of CO
2 to CO in the reducing gas increases, the more the reducing velocity of the ore deoreases, and at the lower temperature, a small variation. of that ratio effects more greately on the redncing velocity than at, the higher temperature. In general, when the value of C0
2/CO in the reducing gas approaches the value of CO
2/CO at the equilibrium condition of the reaction FeO+CO Fe+CO
2, the reducing velocities become very slow.
(2) Being referred our experimental results to the reports of W.A. Schlesinger, who had measured the temperatures and the ratios of CO
2 to CO in the furnace gases at the various heights in an iron blast furnace, the reducing velocities of an iron ore in the various heights of the stack of the aforesaid blast furnace were surveyed. Taking the tempetures, the partial pressures of CO+CO
2 and the ratics of CO
2 to CO equal to those measured by W.A. Schlesinger, we find from our experimental curves that the time taken for the reduction of the Johore are at 700°C is about 33 times of that at 1000°C in our experiment in which we passed 100cc. of the reducing gas per min, throngh 1g. of the sample of 1mm. size.
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