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Empirical Modeling of Iron Oxide Dissolution in Sulphuric and Hydrochloric Acid
被引:0
|作者:
Jan C. Hemmelmann
Hao Xu
Wolfgang Krumm
机构:
[1] University of Siegen,
来源:
关键词:
Magnetite;
Hematite;
Wustite;
Scale Layer;
Oxide Dissolution;
D O I:
暂无
中图分类号:
学科分类号:
摘要:
A new approach is presented to an empirical modeling of chemical pickling processes, based on the activation energy of oxide dissolution in hydrochloric acid (HCl) and sulfuric acid (H2SO4). The model allows us to calculate pickling times as a function of definite parameters. The main oxide layers on hot-rolled materials are magnetite (Fe3O4), hematite (Fe2O3), and wustite (FeO). On the laboratory scale, the activation energy of each oxide has been determined. FeO is a metastable oxide and has been produced based on magnetite powder in a H2/H2O atmosphere. The oxide powders used for the experimental procedure have been analyzed by X-ray powder diffraction to insure the proper stoichiometry and composition. The model allows us to calculate the time of oxide dissolution based on the parameters temperature, acid concentration, and the composition of the oxide layer. Calculated values are verified by surface potential measurement on industrial oxide layers. The hot-rolled material used for verification is low carbon steel. A comparison between calculated pickling times and experimental data will be presented.
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页码:1232 / 1235
页数:3
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