扫描电镜观察了AerMet100钢中稀土夹杂物的形貌、尺寸;原位观察了单轴拉伸条件下稀土夹杂物的微观力学行为.结果表明:稀土夹杂物呈球状或椭球状,拉伸过程中稀土夹杂物内部最先萌生裂纹.建立了裂纹萌生的应力判据.裂纹在夹杂物内部扩展,不易向基体延伸.数值模拟单轴拉伸试验和理论计算结果与原位观察基本一致.
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