creep introduction

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    CREEP

    FAILURE

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    Definition:

    When materials under severe

    service conditions are

    required to sustain steadyloadsfor long periodsof time,

    they undergoa time dependent deformation.

    This is known as creep

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    CREEP

    can also be defined as

    the slow and progressive

    deformation of a material

    with time at constant stress.

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    Creep is found to occur at higher

    temperature than at lower temp.

    Therefore the study of creep is veryimportant for those materials which

    are used at high temp like

    components of gas turbines,furnaces, rockets, missiles etc.

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    Creep curve:

    The creep curve is obtained

    by applying a constanttensile loadbelow the yieldpointto a specimen

    maintained at constanttemp.

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    CREEP CURVE

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    As soon as the specimen

    is loaded, there will be aninstantaneous strain

    which is denoted by o

    on the creep curve.

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    Further deformation of the

    metal only after theinstantaneous strain is

    considered as creep deformation.

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    Creep deformation of

    materials up to failure aredivided into 3 stages

    i) primary creep ii) secondary creep

    iii) tertiary creep.

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    CREEP CURVE

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    Primary creep: OR TRANSIENT CREEP

    This is the first stage of thecreep which represents a

    region of decreasing creep

    rate.

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    In this region the rate at

    which the material deformsdecreases with time until it

    reaches a constant value.

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    The creep rate goes on

    reducing because as the

    metal deforms it undergoes

    strain hardeningand offers

    more and more resistance tofurther elongation.

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    Transient creep:

    The princ iple character ist ic of

    trans ien t creep is the decreasingrate in deformat ion .

    Deformat ion is rapid at f i rs t but

    gradual ly becomes slower andslower as the rate approaches

    some fixed value.

    Transient c reep in metals isobserved at al l temp, even near

    abso lute zero . Hence it is some

    times referred to as cold creep

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    Secondary creep: [steady statecreep]

    Nearly constantcreep rate,

    because strain-hardening and

    recovery effectsbalanceeach other.

    Creep in this region takesplace by the viscous flowin the materials.

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    Viscous creep: SECONDARY CREEP] It is characterized by the

    viscous flow of the material

    means that there is a constant

    or a steady increase in

    deformation at constant stress.

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    Although strain hardening is

    present, its effect is just

    balanced by the recoveryprocess which has the

    opposite effect i.e softening the metal.

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    viscous creep is stopped when

    there is considerable reduction

    in cross sectional area andenters the tertiary stage .

    The rate of deformation

    increases rapidly in this 3rd

    stage and fracture occurs atthe end of this stage.

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    Viscous creep also knownas hot creep', since it is

    observed only at higher

    temperature.

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    Tertiary creep :

    This stage is period ofincreasing strain rate.

    Tertiary creep occurs when

    there is an effectivereduction in cross-sectional area due tonecking or internal voidformation.

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    If the stress is kept constantof the load or if true strain is

    taken into considerationthen the resulting fracture

    due to creep would be at B.

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    Effect of low temperature :

    Temperature below Tm/4

    are called as LOWER TEMP.

    lower temp have an effect of

    decreasing the creep rate.

    This is because strain

    hardening effects will bemore and recovery process

    is negligible.

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    STRAIN

    STRESS

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    Creep occurring at lower temp

    is known as logarithmic creep

    = ln twhere - strain ,

    a constantttime .

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    lowtemp. logarithmic creep

    obeys a mechanical

    equation of state i.e the rate

    of strainat a given time

    dependsonly on theinstantaneous values of

    stress and strain and notonthe previous strain history.

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    Effect of hightemperature:

    At Higher temp. the creep rate

    increases.

    structural changes takes

    place.

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    Mobility of atomsincreases with temp and

    occupy lower energypositions.

    Mobility of dislocation alsoincreases and theyovercome the obstacles bythe mechanism of climb.

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    The concentration of vacancies

    increases with temp and the rate of diffusion

    increases.

    Recrystallization takes place as

    a result of increased rate ofdiffusion.

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    Mechanism of creep:The chief

    mechanism responsible for creep

    deformation are , Dislocation glide

    Dislocation creep ordislocation climb

    Diffusion creep

    Grain boundary sliding.

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    1) Dislocation glide :

    The creep rate is established

    by the ease with which the

    dislocation move across

    obstacles such as

    precipitates etc.

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    Dislocation glide

    Dislocation

    Grasin Boundary

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    This may include cross-slip

    of dislocations with the aid

    of thermal energy.

    Dislocation glide results in

    increase in plastic strain

    during creep deformation

    Di l ti

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    2) Dislocation creep or

    dislocation climb:

    This is caused due to mutualmovement of dislocations &

    vacancies.

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    At high temp the diffusion rate of

    vacancies is more which make the

    dislocations to glide & climb, edge dislocation can move end of

    a slip plane

    OR to a plane above or below the

    slip Plane.

    This is called dislocation climb.

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    .

    Vacancy

    Dislocation

    Mutual movement of

    dislocations & vacancies.

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    This occurs at high temperature

    (T>0.4Tm) &

    When dislocation cause across

    obstacles, they use vacancies/or interstitial

    atoms to climb and go around them

    for slip & hence plastic deformation continues.

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    3) Diffusion creep: -

    It occurs when temp. is high &

    at relatively low stresses.

    diffusion of vacancies controlsthe creep rate.

    But edge dislocation is notinvolved in them.

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    vacancies move from the surface of

    the specimen towards the stress

    axis

    Stress axis

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    i.e when load is applied &

    kept constant ,the vertical

    boundaries are subjected tocompression& the horizontal

    grain boundaries aresubjected to tensilestress.

    so vacancies migrate from

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    so vacancies migrate from

    tensile region to compression

    region &atoms migrate in opposite

    direction to vacancies.

    i.e causing the creep strain

    along tensile axis,

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    the mechanism is called

    Nabarro-herring creepbecause the flux of atoms is

    through the bulk of atoms.

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    4) Grain boundary sliding:-

    At low tempthe Grain

    boundaries will notflow

    viscously & provide obstacles

    to dislocation motion.

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    At elevated temp, the grains inpolycrystalline materials areable to move relative to each

    other, this is called grainboundary slidingand is anshear process which occurs in

    the direction of grain boundary[GB] .

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    a large no. of grains sliding with

    each other results in plastic

    deformation due to creep .

    GB sliding is promoted by

    increases the temp. T & or

    decreasingthe strain rate.

    C

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    Creep properties :-

    1) creep strength/ or creep

    limit:

    It is defined as the higheststress that material can

    withstand without excessivedeformation for a specified

    length of time.

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    Ex :- creep strength for a steam

    turbine blade may be that

    stress which will produce just

    0.2% creep for 10,000 hours of

    working at 800o

    C.

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    Creep strength can also be

    defined as the stress at given

    temperature which produces

    steady state creep rate of fixed

    amount say 10-11

    to 10-8

    /sec.OR

    It is the stress to cause a creep

    strain of 1% in fixed time say

    105 hours.

    C t t th it i

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    2) Creep rupture strength:- it is

    defined as the highest stress that

    a material can withstand withoutrupture for a specified length of

    time.

    Ex : For the same turbine blade . the

    rupture strength is that stress whichproduces a fracture in 1000HR OR

    10000HR OR 100 000 hrs at 800oC.

    Thus creep rupture strength is

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    Thus creep rupture strength is

    also defined as the limiting

    stress below which creep is soslow that will not result in

    fracture within any finite length

    of time.

    It is also called as stress ruptures

    strength.

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    3) Creep life:

    it is defined as the

    TIME to fracture under a given

    static load.

    0

    C

    0

    ff C

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    Factors affecting Creep:

    Load :

    Temperature: Composition:

    Grain size Heat treatment

    L d C t i

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    Load : Creep rate increases as

    load increases.

    Temperature: Creep rate

    increases as T increases.

    Composition: Pure metals aresofter than alloys , the

    different phases present stops

    the dislocation glide .

    Hence creep is more in pure

    metals.

    G i i S ll th i

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    Grain size: Smaller the grain,

    stronger the material.

    But above Equicohessive temp.

    this effect will be reversed one.

    Equicohessive temp. (Kelvin) Te >Tm/2

    Heat Treatment: This changes the

    structure,Obviously the materials

    property changes, creep resistance

    also changes.

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    .

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    Creep curve equations:

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    Strain Rate = increment of strain / increment in time