IMECH-IR  > 力学所知识产出(1956-2008)
韧性断裂裂纹尖端的物理特征和力学行为
叶裕恭; 洪友士
Source Publication力学进展
1989
Volume19Issue:3Pages:320-335
ISSN1000-0992
Abstract本文综述了金属材料发生韧性断裂的裂尖钝化,孔洞成核和长大,孔洞-孔洞或孔洞-裂尖汇合导致裂纹扩展的物理特征,和描述这些特征的本构理论及物理模型。
Keyword韧性断裂 断裂机制 本构理论 裂尖行为 断裂模型 第二相粒子
Language中文
Document Type期刊论文
Identifierhttp://dspace.imech.ac.cn/handle/311007/36540
Collection力学所知识产出(1956-2008)
Corresponding Author叶裕恭
Recommended Citation
GB/T 7714
叶裕恭,洪友士. 韧性断裂裂纹尖端的物理特征和力学行为[J]. 力学进展,1989,19,3,:320-335.
APA 叶裕恭,&洪友士.(1989).韧性断裂裂纹尖端的物理特征和力学行为.力学进展,19(3),320-335.
MLA 叶裕恭,et al."韧性断裂裂纹尖端的物理特征和力学行为".力学进展 19.3(1989):320-335.
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