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Evaluation of Intergranular Embrittlement of a Low Carbon Steel in Austenite Temperature Range

机译:奥氏体温度范围内低碳钢晶间脆化的评估

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The hot ductility of a low carbon steel was investigated at various strain rates in austenite temperature range. The embrittlement with intergranular fracture occurs in the specimen deformed in lower temperature range of austenite following solution-treatment at higher temperature range of austenite, especially at 1680 K just under the melting point. Sulphides are dissolved and sulphur is segregated to grain boundary by volume diffusion during the solution-treatment. Fine particles of FeS precipitate on grain boundaries during colling to deformation temperatures. Voids are initiated at such fine precipitates because of incoherence with the matrix. The precipitation of FeS is caused by decrease in sulphur solubility with lowering temperature. The embrittlement occurs when a difference in the solubility of sulphur between at solution-treatment temperature and at deformation temperature reaches higher than 65 ppm. The critical reduction in area, at which brittle fracture was distinguished from ductile fracture, was 60. The intergranular fracture feature depends on strain rate. At high strain rates, the specimen was fractured after plastic deformation and the dimple pattern is found in the intergranular fracture. At low strain rates, the specimen was fractured with extremely small plastic deformation after a crack is initiated and intergranular decohesion fracture is found. The energy required for crack propagation is calculated to be 3.45 J/m~2 at low strain rates.
机译:研究了低碳钢在奥氏体温度范围内各种应变速率下的热延展性。在较高的奥氏体温度范围内,特别是在熔点以下的1680 K下进行固溶处理后,在较低的奥氏体温度范围内变形的试样中发生晶间断裂脆化。在固溶处理期间,硫化物溶解,硫通过体积扩散而扩散到晶界。 FeS细颗粒在冷却至变形温度期间会沉淀在晶界上。由于与基质的不连贯性,空位以这种细小的沉淀物引发。 FeS的沉淀是由于温度降低导致硫溶解度降低而引起的。当在固溶处理温度和变形温度下硫的溶解度差超过65ppm时,发生脆化。将脆性断裂与延性断裂区分开的临界减小面积为60。晶间断裂特征取决于应变率。在高应变率下,试样在塑性变形后断裂,并且在晶间断裂中发现了凹痕图案。在低应变率下,试样在产生裂纹后以很小的塑性变形断裂,并发现晶间脱粘断裂。在低应变速率下,裂纹扩展所需的能量经计算为3.45 J / m〜2。

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