Mae 493n 593t Lec5

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    TribologyinMechanicalEngineering

    MAE493N/593T

    Dr.Konstantinos

    A.

    Sierros

    WestVirginiaUniversity

    Mechanical&AerospaceEngineering

    ESBAnnex

    263

    [email protected]

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    Project

    listEachteammustchooseoneproject

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    Contactbetweensurfaces

    Nonconformingcontacts

    Conformal

    contacts

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    Contactbetweensurfaces

    Surface

    contact

    can

    be

    viewed

    at

    two

    different

    scales

    macroscopic

    scale

    microscopic

    scale

    Expressingdistortionsofsurfaces

    w.r.t.to

    deflections

    as

    aproportion

    ofradii

    Singleasperityelastoplastic

    deformationW

    http://www.tribologyabc.com/

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    Predictingdamagetocomponents

    Predictionofcomponentdamageandlifetime

    Arealisticestimateofthetruestressesexperiencedbythematerialsincontactis

    crucial

    Analysisofsurfacecontact forbothmacroscaleandmicroscale

    geometries

    Macroscalelevel:

    Contactbetweenrollers/ballsandtheracesinrollingelement

    bearings

    Microscopiclevel:Modelingofindividualsurfaceasperities

    Understandhowthestressesatsurfaces(andjustbelowthem)dependon;

    Appliedload

    Shapeofsurfaceprofiles

    Materialproperties

    Case1:

    Normal

    load

    only

    Case2:Normalloadand

    frictionload

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    Hertziancontacts

    Deformationintheelasticregime

    Smallstrains

    Macroscale:Radiiofcurvatureofbodiesincontact>>Contactarea

    Nonconformingsurfaces

    Continuoussurfaces

    Deformationiscalculatedusingthehalfspace

    approximation

    Wedonottakeintoaccountfrictionaleffects

    Ahalf

    space

    is

    either

    of

    the

    twopartsintowhicha

    hyperplanedividesanaffine

    space

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    Geometryofnonconformingsurfacesincontact Longdeformablecylinder

    incontactwithaflatrigidsurface

    Analysiscanbeextendedtocaseswherebothsurfacesarecurvedanddeformablebutstilllonginthe3rd

    dimension

    3Dcaseoftwospheresincontactwillbedescribed

    Unloadedlongdeformable

    cylinderonrigidflatsurface

    Rxz2

    2

    i.e.wemodelthesurface

    profileasparabolicoverthe

    smallregionatandnearthe

    contact

    Gapbetween

    flatrigid

    and

    cylinderprofile

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    Geometryofnonconformingsurfacesincontact NowsupposethataloadperunitlengthW/Lisapplied

    Cylinderdeforms

    (its

    centre

    moves

    avertical

    distance

    towardstherigidsurface)

    Weneedtorelatethesizeofthecontactpatch(2)withthenormalload(W/L)and

    thegeometryandmaterialpropertiesofthecylinder

    Dottedlineisoriginalcylinderprofile

    wz isverticaldisplacementofcylinder

    surface

    hgapbetweenthetwosurfaces

    += zwRxh2

    2

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    Geometryofnonconformingsurfacesincontact

    Nowsupposethatthe2nd

    surfaceisalsoacylinder(withitsaxisparalleltothefirst)

    Itis

    also

    deformable

    R

    xww zz

    2

    2

    21 =+

    Rxww zz2

    2

    21 >+

    Withincontactregion

    |x|

    Outsidecontactregion

    |x|>

    Verticaldisplacement

    ofcylindersurface1

    Vertical

    displacement

    ofcylindersurface2

    1+2Totalrelativedistance

    ofapproachofthe

    centersofthetwo

    cylinders

    21

    111RRR +=

    Widthofinterest

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    Geometryofnonconformingsurfacesincontact

    3

    D

    case:

    Contact

    between

    two

    deformable

    spheres Contactpatchwillnowbecircularinshapeofradius

    Rrww zz2

    2

    21=+

    R

    rww zz

    2

    2

    21 >+

    Withincontact

    |r|

    where

    x2+y2

    r2=x2+y2

    f d b f

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    Surfaceandsubsurfacestresses Lineloadingofanelastic

    halfspace

    Equilibriumequations

    0=+

    zx

    xzx 0=+

    xz

    xzz

    Correspondingstrainsmustsatisfy

    thecompatibility

    condition

    z

    xzzx

    xxz

    =

    +

    2

    2

    2

    2

    2

    Planestrain

    y =0

    HookesLawrelatingstressandstrain

    Smalldisplacements

    ))1()1((1 2

    zxx

    E

    +=

    ))1()1((1 2

    xzzE

    +=

    xzxzxz E

    v

    G

    )1(21 +

    ==

    K.L.Johnson,ContactMechanics,p.12

    Solution

    Findstressesandstrainstosatisfyequations

    Boundaryconditions

    Arriveat

    analytical

    solutions;

    FEA

    S f d b f

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    Surfaceandsubsurfacestresses

    cos2rL

    Wr =

    Polarcoordinates

    0== r

    Cartesiancoordinates

    ( )

    222

    2

    2 2sin

    zx

    zx

    L

    Wrx

    +

    ==

    ( )2223

    2 2cos

    zx

    z

    L

    Wrz

    +==

    222

    2

    )(

    2cossin

    zx

    xz

    L

    Wrxz +

    ==

    S f d f ti

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    SurfacedeformationsUniformnormalpressure

    +

    ++

    =222

    ln)(ln)()1(

    axax

    xaxp

    E

    vwz

    Constantofintegration

    (dependondatumselection

    fromwhich

    vertical

    displacementsaremeasured)

    wz

    =0

    Forx=

    Pleasenote

    discontinuity

    in

    slope!

    S f d f ti

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    SurfacedeformationsInversesemiellipticalpressure

    22/1

    )(x

    pxp o

    =

    L

    Wpo =

    Infinitestressatedgeofcontact

    Rigidpunchcontact

    Photoelastic measurements of contact

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    Photoelasticmeasurementsofcontact

    Surface deformations under traction loading

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    Surfacedeformationsundertractionloading

    o

    Stresses below surface

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    Stressesbelowsurface

    Maximum

    Tangentialstressundersurfaceis

    equal

    to

    normal

    direct

    pressure

    p

    Maxshearstressof0.3po

    ata

    distance0.79

    belowthesurface

    wherepo

    ismaxHertzianpressure

    and

    is

    contact

    width

    x

    z

    Hertzian line contact with sliding

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    Hertzianlinecontactwithsliding

    Bothtractionandnormalloading

    Frictionaltractionisequalto1/3

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    Loading beyond the elastic limit

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    LoadingbeyondtheelasticlimitElastoplasticcontact

    Whole regime From elastic to fully plastic

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    Wholeregime Fromelastictofullyplastic

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    Summary

    Conformalandnonconformalcontacts

    Hertzian

    contacts

    Surfaceandsubsurfacestresses

    Lineandpointcontact

    Elastic

    Elastoplastic

    Fullyplasticdeformation