Abstract

MgO-containing flux may have a series of effects on the quality of sinter and performances of the blast furnace. Thus, the fundamental mechanism of the effects of MgO on the sinter strength was investigated. Both the chemical reagent and industrial flux were used for preparing the specimens. The experimental results show that the sinter strength decreases with MgO addition. There are three reasons for it. The first reason is diffusion rate. Almost all of the CaO may react with Fe2O3 and generate CaO·Fe2O3, but most of MgO cannot react with Fe2O3, and it still remains in the state of original minerals. The diffusion rate of MgO in iron oxide is only 17.51 μm/min in 30 min. The second reason is the fluidity and ability to generate liquid phase. In the case of Fe2O3 mixed with CaO, there is some liquid phase formed above 1200 °C, while in the case of Fe2O3 mixed with MgO, even at 1200 and 1220 °C, there is still no liquid phase. The third reason is self-strength. In the case of industrial flux, the compression strength of the specimens made of Fe2O3 and limestone is 0.52 and 0.71 kN at 1150 and 1180 °C, respectively, while that of the specimens made of Fe2O3 and magnesite is 0.48 and 0.56 kN, respectively. Therefore, the fundamental mechanism of the effects of MgO additive on sinter strength can be better understood based on the diffusion rate of MgO in iron oxides, the fluidity of liquid phase, and the self-strength of bonding phase.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.