日本鉱業会誌
Online ISSN : 2185-6729
Print ISSN : 0369-4194
銅の熔錬に関する研究 (第4報)
珪酸飽和のFeO-SiO2緩と平衡する皮へのFeOの溶解
矢沢 彬亀田 満雄
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ジャーナル フリー

1955 年 71 巻 802 号 p. 187-190

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In order to determine the solubility of FeO in Cu2S-FeS mattes coexisting with the Si02-saturated FeO-Si02 slag, briquetts of powdered mixture of Cu2S, FeS and somewhat excess FeO were melted in silica crucibles at temperatures of 1, 200, 1, 250 and 1, 300°C. The components of matte were calculated from the analytical values obtained, and the solubility of FeO was determined as is shown in Fig. 1. Although the FeS-matte containing no Cu2S dissolves 27.5 pct FeO, the content of dissolved FeO decreases as the matte grade increases, and reaches substantially down to zero for the Cu2S-matte. The solubility of FeO is practically unaffected by the change in temperature, or by the addition of lime or alumina. The contents of S in the mattes in this case are found between 26.5 and 20 pct as are shown in Fig. 3, and in general these are considerably smaller than those in the matte composed merely of Cu2S and FeS, especially in the mattes of the lower grade. The decrease in S content with increasing Cu2S content is comparatively slight as far as the grade of matte is low. Such general trend of the change in S content is analogous to that encountered in practice, and hence considerable contents of FeO are expected to be soluble in actual mattes. In fact, the microscopic examination revealed the dissolution of FeO in actual mattes. Moreover, the presumed FeO content was calculated from the data in practice, and the same general trend with the results obtained in the present investigation could be recognized.

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