Reduction Behavior of Cold-bonded Briquettes under Simulated Blast Furnace Conditions

Recycling of fine sized iron-rich by-products back to blast furnace (BF) process in the form of cement-bonded briquettes has become a common procedure in steel plants. Replacing part of the cement by Ground Granulated Blast Furnace Slag (GGBFS) is also a common method to reduce cement consumption. W...

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Veröffentlicht in:ISIJ International 2014/07/15, Vol.54(7), pp.1539-1545
Hauptverfasser: Kemppainen, Antti, Iljana, Mikko, Heikkinen, Eetu-Pekka, Paananen, Timo, Mattila, Olli, Fabritius, Timo
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Sprache:eng
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Zusammenfassung:Recycling of fine sized iron-rich by-products back to blast furnace (BF) process in the form of cement-bonded briquettes has become a common procedure in steel plants. Replacing part of the cement by Ground Granulated Blast Furnace Slag (GGBFS) is also a common method to reduce cement consumption. When the briquettes are subjected to high temperature and reducing atmosphere in the BF, the cement phases decompose and the iron oxides undergo a series of phase transformations. To avoid early disintegration and to improve the performance of the briquettes, it is necessary to study these reactions during the reduction. In the present study the reduction behavior of the BF briquette samples was studied by experimental methods in a laboratory scale furnace, which simulates the conditions of the BF shaft in a CO–CO2–N2 atmosphere. With interrupted experiments the composition of the briquette was studied in different reduction stages of the BF shaft. The effect of GGBFS as a binder material on the reduction was studied with GGBFS containing briquette samples. The reduction of briquettes was compared to an olivine pellet which was used as a reference sample. Considerably higher reduction rate was detected with the briquettes compared to the pellet at 1100°C when reduced to metallic iron. 25–50 vol-% swelling in the briquette samples was detected during the wüstite-iron reduction step at 900–1000°C. X-ray diffraction (XRD) was used to observe the phase transformations in the Fe–Fe2O3–CaO system of the briquette and the results are in agreement with the theory.
ISSN:0915-1559
1347-5460
DOI:10.2355/isijinternational.54.1539