首页> 外文会议>International Conference on Microalloying for New Steel Processes and Applications; 20050907-09; Basque Country(ES) >The Microstructure Evolution of Nb,Ti Complex Microalloyed Steel During the CSP Process
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The Microstructure Evolution of Nb,Ti Complex Microalloyed Steel During the CSP Process

机译:CSP过程中Nb,Ti复合微合金钢的组织演变

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The development of microstructure of Nb,Ti-bearing microalloyed steel during the CSP process was studied. Three samples were taken from the as-cast slab prior to tunnel furnace, intermediate bar after stand F2 and the hot band, respectively. In the as-cast slab, the average austenite grain size is 654 μm with a large size range from 150 to 2000 μm. In the intermediate bar after stand F2, the austenite grains are remarkably refined, but are heterogenous due to the incomplete recrystallization, which are in the size range of 23 to 116 μm. In the hot band is mainly non-polygonal ferrite. Microstructural heterogeneity exists in the hot band. It is attributed to the heterogeneous austenite grain size in the intermediate bar and the less rolling reduction after stand F2. With regards to precipitation, cubic TiN and fine precipitates less than 20nm are commonly observed in the as-cast slab and the intermediate bar. Some complex (Ti,Nb)(C,N) precipitates with a slightly larger size also exist. In the hot band, most particles are complex (Ti,Nb)(C,N) precipitates, in a shape of irregular or cruciform. The fine precipitates which can strengthen the ferrite matrix are seldom seen. These results are in good agreement with the size distribution of the precipitates determined using small angle X-ray scattering method. The chemical phase analysis reveals that 45%Nb of the total and 43%Ti of the total are still in solution in ferrite of the hot band.
机译:研究了CSP过程中含Nb,Ti的微合金钢的组织发展。从隧道炉前的铸坯,F2机架后的中间棒和热轧带分别采集了三个样品。在铸坯中,平均奥氏体晶粒尺寸为654μm,尺寸范围在150至2000μm之间。在机架F2之后的中间棒中,奥氏体晶粒显着细化,但是由于不完全重结晶而异质,其尺寸范围为23至116μm。在热带中主要是非多边形铁氧体。热带中存在微观结构异质性。这归因于中间棒材中奥氏体的不均匀晶粒尺寸以及机架F2之后轧制减少的程度较小。关于沉淀,通常在铸态板坯和中间棒中观察到立方氮化钛和小于20nm的细小沉淀。还存在一些尺寸稍大的复合(Ti,Nb)(C,N)沉淀物。在热带中,大多数颗粒是不规则或十字形的复杂(Ti,Nb)(C,N)沉淀。可以增强铁素体基体的细小析出物很少见。这些结果与使用小角度X射线散射法测定的沉淀物的尺寸分布非常吻合。化学相分析表明,总含量的45%Nb和总含量的43%Ti仍存在于热带的铁氧体中。

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