Effect of Scale Formation on Copper Enrichment Behavior in Continuously Cast Slab

来源 :Journal of Iron and Steel Research(International) | 被引量 : 0次 | 上传用户:iamup
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Copper enrichment behavior in continuously cast slab induced by scale formation during continuous cooling was experimentally investigated,and the effects of initial slab surface temperature and oxygen potential in atmosphere were discussed.The results showed that a loose scale adhered to the substrate was formed in H_2O-N_2 atmosphere at higher slab surface temperature compared to a gap formed between the scale and the steel substrate after continuous cooling in H_2O-O_2-N_2 atmosphere.Under the condition of continuous cooling in H_2O-N_2 atmosphere,the copper enrichment occurred both within the loose scale and at the scale/steel interface with simultaneous Ni enrichment near the interface at higher slab surface temperature.The combined effects of the loose scale and nickel enrichment were thought to promote the back-migration of Cu-rich phase from the interface and occlusion within the scale layer.While in H_2O-O_2-N_2 atmosphere,the Cu enrichment was found on the steel side and the formed gap prevented the migration of Cu to the scale. Copper enrichment behavior in continuously cast slab induced by scale formation during continuous cooling was experimentally investigated, and the effects of initial slab surface temperature and oxygen potential in atmosphere were discussed. The results showed that a loose scale adhered to the substrate was formed in H_2O- N 2 atmosphere at higher slab surface temperature compared to a gap formed between the scale and the steel substrate after continuous cooling in H 2 O-O 2 -N 2 atmosphere. Undertaking the condition of continuous cooling in H 2 O-N 2 atmosphere, the copper enrichment occurred both within the loose scale and at the scale / steel interface with simultaneous Ni enrichment near the interface at higher slab surface temperature. combined effects of the loose scale and nickel enrichment were thought to promote the back-migration of Cu-rich phase from the interface and occlusion within the scale layer. Window in H 2 O-O 2 -N 2 atmosphere, the Cu enrichment was found on the steel side and the f ormed gap prevented the migration of Cu to the scale.
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