creep introduction
TRANSCRIPT
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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