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    Singularities at the Tip of a Crack Terminating Normally at an Interface Between Two Orthotropic Media

    Source: Journal of Applied Mechanics:;1996:;volume( 063 ):;issue: 002::page 264
    Author:
    J. C. Sung
    ,
    J. Y. Liou
    DOI: 10.1115/1.2788859
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: The order of stress singularities at the tip of a crack terminating normally at an interface between two orthotropic media is analyzed. Characteristic equation in complex form for the power of singularity s , where 0 < Re{s} < 1, is first set up for two general anisotropic materials. Attention is then focused on the problem that is composed by two orthotropic media where one of them (say, material #2 ) the material principal axes are aligned while the other one (say, material #1) the principal axes can have an angle γ relative to the interface. For such a problem, a real form of the characteristic equation is obtained. The roots are functions of γ in general. Two real roots exist for most values of γ; however, there are possible ranges of γ that the complex roots will occur. The roots s are found to be independent of γ when material #1 has the property that δ(1) = 1. When γ = 0, two roots are always real. Furthermore, each of these two roots is associated with symmetric or antisymmetric mode and they become equal when Δ = 1. Many other features of the effects of the material parameters on the behaviors of the roots s are further investigated in the present work, where the six generalized Dundurs’ constants, expressed in terms of Krenk’s parameters, play an important role in the analysis.
    keyword(s): Fracture (Materials) , Equations , Functions AND Stress singularity ,
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      Singularities at the Tip of a Crack Terminating Normally at an Interface Between Two Orthotropic Media

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    contributor authorJ. C. Sung
    contributor authorJ. Y. Liou
    date accessioned2017-05-08T23:49:10Z
    date available2017-05-08T23:49:10Z
    date copyrightJune, 1996
    date issued1996
    identifier issn0021-8936
    identifier otherJAMCAV-26392#264_1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/116433
    description abstractThe order of stress singularities at the tip of a crack terminating normally at an interface between two orthotropic media is analyzed. Characteristic equation in complex form for the power of singularity s , where 0 < Re{s} < 1, is first set up for two general anisotropic materials. Attention is then focused on the problem that is composed by two orthotropic media where one of them (say, material #2 ) the material principal axes are aligned while the other one (say, material #1) the principal axes can have an angle γ relative to the interface. For such a problem, a real form of the characteristic equation is obtained. The roots are functions of γ in general. Two real roots exist for most values of γ; however, there are possible ranges of γ that the complex roots will occur. The roots s are found to be independent of γ when material #1 has the property that δ(1) = 1. When γ = 0, two roots are always real. Furthermore, each of these two roots is associated with symmetric or antisymmetric mode and they become equal when Δ = 1. Many other features of the effects of the material parameters on the behaviors of the roots s are further investigated in the present work, where the six generalized Dundurs’ constants, expressed in terms of Krenk’s parameters, play an important role in the analysis.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleSingularities at the Tip of a Crack Terminating Normally at an Interface Between Two Orthotropic Media
    typeJournal Paper
    journal volume63
    journal issue2
    journal titleJournal of Applied Mechanics
    identifier doi10.1115/1.2788859
    journal fristpage264
    journal lastpage270
    identifier eissn1528-9036
    keywordsFracture (Materials)
    keywordsEquations
    keywordsFunctions AND Stress singularity
    treeJournal of Applied Mechanics:;1996:;volume( 063 ):;issue: 002
    contenttypeFulltext
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