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Crystallographic orientation analysis of cleavage facets adjacent to a fracture trigger in low carbon steel

机译:低碳钢中与断裂触发点相邻的裂解面的晶体学取向分析

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摘要

The microstructure and crystallographic orientation under a cleavage crack trigger point, which was detected on a fracture toughness specimen of low carbon steel, were investigated. SEM fractographs of an etched cleavage facet reveal that a flat cleavage facet between facet ridges spreading from the trigger point is divided by a grain boundary between ferrite and pearlite. Even a different phase boundary does not occasionally create any steps and ridges on the cleavage facet: it suggests this phase boundary is not an obstacle to cleavage cracking. Electron diffraction analysis for the thin foil sample milled out from this phase boundary demonstrates that the crystallographic orientation of the ferrite grain is consistent with that of the ferrite in the adjacent pearlite block. It is strictly examined that the ferrite/pearlite boundary does not act as a local resistance to cleavage crack growth when the crystallographic orientation of the ferrite in the pearlite block is aligned with an adjacent ferrite grain.
机译:研究了在低碳钢的断裂韧性试样上检测到的在解理裂纹触发点下的显微组织和晶体学取向。蚀刻的解理小平面的SEM断裂图显示,从触发点扩展的小面脊之间的平坦解理小平面被铁素体和珠光体之间的晶界所分割。即使是不同的相界,也不会偶尔在解理面上产生任何台阶和隆起:这表明该相界并不是解理裂纹的障碍。从该相边界铣削出的薄箔样品的电子衍射分析表明,铁素体晶粒的晶体取向与相邻珠光体块中的铁素体的晶体取向一致。严格检查的是,当珠光体块中的铁素体的晶体学取向与相邻的铁素体晶粒对齐时,铁素体/珠光体边界不会起到抵抗裂开裂纹的作用。

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