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Thermodynamic calculations in the Fe–O–C–H system and decomposition–reduction of iron oxalate in a complex gas medium

✍ Scribed by T. E. Babutina; D. P. Zyatkevich; I. V. Uvarova


Publisher
Springer
Year
2009
Tongue
English
Weight
248 KB
Volume
48
Category
Article
ISSN
1573-9066

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Morphological changes in an iron catalys
✍ A. Sacco Jr.; R.C. Reid 📂 Article 📅 1979 🏛 Elsevier Science 🌐 English ⚖ 990 KB

When H2 and CO? are exposed to iron at 800-900 K and I bar pressure, they react to form H20, CH,,, CO and carbon. The equilibrium water yield, however, is never achieved even after long residence time. Magnetite (Fe,Ol) and wustite (Fe,O), which form during reaction, inhibit carbon deposition. Thus,