锰铬尖晶石在H2-H2O-H2S气氛下转化为硫化物

P. Papaiacovou, H.J. Grabke, M. Danielewski, H.P. Schmidt
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引用次数: 2

摘要

研究了h22 - h2o - h2s混合物在1073 K、1173 K和1273 K条件下MnCr2O4向硫化物的转化。通过对块状尖晶石硫化过程的热重研究,确定了MnCr2O4的稳定极限。当超过一定的硫压时,对应于MnCr2O4 + 3/2S2 = MnS + 2CrS + 2O2的反应,尖晶石转变为混合硫化物(Mn,Cr)S和(Cr,Mn)S的多孔层。分压依赖性表明,反应速率受表面反应控制,即硫化物-尖晶石界面处硫化氢的转移,硫化氢易于通过硫化物层中的大孔隙进入。对Fe-Cr-Mn合金预氧化后得到的MnCr2O4层进行硫化处理,反应产物的动力学和形貌与此相似。结果提供了氧化硫化气氛下含锰高温合金氧化层稳定性的信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Conversion of manganese-chromium spinel to sulphides in H2-H2O-H2S atmospheres

The conversion of MnCr2O4 to sulphides was investigated at 1073 K, 1173 K and 1273 K in H2-H2O-H2S mixtures. From thermogravimetric studies on the sulphidation of the bulk spinel, the stability limit of MnCr2O4 was determined. When a certain sulphur pressure is exceeded corresponding to the reaction MnCr2O4 + 3/2S2 = MnS + 2CrS + 2O2, the spinel is converted to a porous layer of mixed sulphides (Mn,Cr)S and (Cr,Mn)S. The partial pressure dependences indicate that the reaction rate is controlled by a surface reaction, i.e. the sulphur transfer from H2S at the interface sulphide-spinel which is easily accessible through the large pores in the sulphide layer. Similar kinetics and morphology of the reaction products were observed when MnCr2O4 layers obtained by preoxidation of Fe-Cr-Mn alloys were sulphidized. The results provide information on the stability of oxide layers formed on Mn-containing high temperature alloys in oxidizing-sulphidizing atmospheres.

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