Carbothermic reduction roasting for processing of ferruginous chromite ore using conventional and microwave heating

Author(s):  
Sunil Kumar Tripathy ◽  
Y. Rama Murthy ◽  
Nikkam Suresh ◽  
Lev O. Filippov
2021 ◽  
Vol 24 (6) ◽  
Author(s):  
Giulio Antunes de Medeiros ◽  
Leonardo Martins da Silva ◽  
Márcio Teodoro Fernandes ◽  
Daniel Gomes de Souza dos Santos ◽  
José Adilson de Castro

2016 ◽  
Vol 870 ◽  
pp. 578-583
Author(s):  
A.V. Senin

The gasphase-solidphase model is used to explain the results of solid chromite ore carbothermic reduction. The reducing agent is carbon atoms. Carbon is brought to the surface of chromite grains by gaseous carbon-containing molecules and radicals, such as C3O2, CH4, CH3, CH2, CH, C2H2 and other carbon containing particles. Gas particles penetrate a piece of ore through the pores and cracks. Active carbon atoms C are formed by the dissociation of gaseous particles. Reduction by carbon is carried out on the chromite grain surface due to the cations and anions diffusion in the oxide lattice towards the grain surface. Porosity of chromite ores is experimentally defined under reducing conditions; it is estimated at up to 20 – 25 vol.%. Up to 1/4 of porosity is accounted for macropores and macrocracks that have the radius of over 50 microns, the remaining porosity share is accounted for the pore dimensions that are estimated at 0.5 – 50 microns in radius. The carbon presence in the pores of partially reduced ores is deduced based on experiment. There is also carbon in the reduced metal that is situated deep in the lump ore. The experimental results agree with the gasphase-solidphase reduction model.


2015 ◽  
Vol 87 (5) ◽  
pp. 562-570 ◽  
Author(s):  
Xianfeng Hu ◽  
Qixing Yang ◽  
Lena Sundqvist Ökvist ◽  
Bo Björkman

2011 ◽  
pp. 941-951 ◽  
Author(s):  
Yi Ling-yun ◽  
Huang Zhu-cheng ◽  
Hu Bing ◽  
Wang Xia ◽  
Jiang Tao

2009 ◽  
Vol 41 (1) ◽  
pp. 10-18 ◽  
Author(s):  
Dolly Chakraborty ◽  
S. Ranganathan ◽  
S.N. Sinha

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