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    Shear Constraint and Macroscopic Fracture Criteria for Ductile Metals

    Source: Journal of Applied Mechanics:;1975:;volume( 042 ):;issue: 001::page 15
    Author:
    M. A. Kaplan
    ,
    G. A. Rowell
    DOI: 10.1115/1.3423509
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: The role of material constraint in the shear fracture of ductile metals is investigated by means of a series of torsion and internal pressure tests on aluminum alloy tubing combined with analytical descriptions of the stress states at fracture. These descriptions include work hardening and, in the case of a tube under internal pressure, account for the nonaxisymmetric deformations that always precede fracture. The results, which indicate that shear fracture initiation depends on conditions at points far removed from the initiation site when the maximum shear stress vector there is directed through the interior of the body, are supported by the results of tensile tests on plates with shallow notches. These latter experiments are also used to show that tensile and shear fracture are governed by independent fracture criteria. A continuum fracture theory for ductile metals, based on the concepts of material constraint and independent fracture criteria, is proposed. The theory predicts fracture in terms of the stress state. A critical analysis of the theory is provided along with examples of fracture phenomena which the theory predicts, but which are not explained by existing theories.
    keyword(s): Metals , Shear (Mechanics) , Fracture (Process) , Stress , Pressure , Deformation , Aluminum alloys , Tubing , Torsion , Plates (structures) AND Work hardening ,
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      Shear Constraint and Macroscopic Fracture Criteria for Ductile Metals

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/87156
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    contributor authorM. A. Kaplan
    contributor authorG. A. Rowell
    date accessioned2017-05-08T22:58:00Z
    date available2017-05-08T22:58:00Z
    date copyrightMarch, 1975
    date issued1975
    identifier issn0021-8936
    identifier otherJAMCAV-26030#15_1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/87156
    description abstractThe role of material constraint in the shear fracture of ductile metals is investigated by means of a series of torsion and internal pressure tests on aluminum alloy tubing combined with analytical descriptions of the stress states at fracture. These descriptions include work hardening and, in the case of a tube under internal pressure, account for the nonaxisymmetric deformations that always precede fracture. The results, which indicate that shear fracture initiation depends on conditions at points far removed from the initiation site when the maximum shear stress vector there is directed through the interior of the body, are supported by the results of tensile tests on plates with shallow notches. These latter experiments are also used to show that tensile and shear fracture are governed by independent fracture criteria. A continuum fracture theory for ductile metals, based on the concepts of material constraint and independent fracture criteria, is proposed. The theory predicts fracture in terms of the stress state. A critical analysis of the theory is provided along with examples of fracture phenomena which the theory predicts, but which are not explained by existing theories.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleShear Constraint and Macroscopic Fracture Criteria for Ductile Metals
    typeJournal Paper
    journal volume42
    journal issue1
    journal titleJournal of Applied Mechanics
    identifier doi10.1115/1.3423509
    journal fristpage15
    journal lastpage24
    identifier eissn1528-9036
    keywordsMetals
    keywordsShear (Mechanics)
    keywordsFracture (Process)
    keywordsStress
    keywordsPressure
    keywordsDeformation
    keywordsAluminum alloys
    keywordsTubing
    keywordsTorsion
    keywordsPlates (structures) AND Work hardening
    treeJournal of Applied Mechanics:;1975:;volume( 042 ):;issue: 001
    contenttypeFulltext
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