Abstract
In plane-stress ductile fracture, the irreversible work dissipated inside the fracture process zone (FPZ) is a material constant for a given sheet thickness and is called the specific essential fracture work (we). However, work dissipated elsewhere in the outer plastic zone is nonessential and is dependent on specimen geometry and size. In this paper, a theoretical basis for the essential fracture work is given and a simple but elegant experimental method is presented to separate the essential work from the total fracture work. In-plane mode I (opening) and mixed mode I/II (opening/sliding) as well as out-of-plane tearing mode III fractures are analysed. Experiments are conducted on a range of ductile engineering materials including metals, polymers and papers to illustrate the working principles of the theory.
Original language | English |
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Pages (from-to) | 995-1005 |
Number of pages | 11 |
Journal | International Journal of Mechanical Sciences |
Volume | 35 |
Issue number | 12 |
DOIs | |
Publication status | Published - Dec 1993 |
Externally published | Yes |
ASJC Scopus subject areas
- Civil and Structural Engineering
- General Materials Science
- Condensed Matter Physics
- Aerospace Engineering
- Ocean Engineering
- Mechanics of Materials
- Mechanical Engineering
- Applied Mathematics