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Unit 2 HT by Conduction

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    HEAT TRANSFERby

    CONDUCTION

    Prepared by,

    Kumargaurao D PunaseAssistant Professor

    Dept of Chemical Engg.COES, UPES

    Dehradun

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    First mechanism - molecularinteraction (e.g. gas)

    Greater motion of molecule

    at higher energy level(temperature) imparts energyto adjacent molecules atlower energy levels

    Second mechanism by free

    electrons (e.g. solid)The mechanism of heat conduction

    in different phases of substance

    Fouriers law of Heat Conduction

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    Steady state heat conduction

    One directional heat flow

    Isotropic and homogeneous material i.e. thermal conductivityhas a constant value in all the directions

    Constant temperature gradient and a linear temperature profile

    No internal heat generation

    Assumptions of Fouriers law: Contd .

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    Summary: Fouriers Law

    It is phenomenological, i.e. based on experimental evidence

    Is a vector expression indicating that the heat flux is normal toan isotherm, in the direction of decreasing temperature

    Applies to all states of matter

    Defines the thermal conductivity, ie.

    )/( xT

    qk x

    Contd .

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    Chapter 2 6

    Thermal Properties of Matter

    Fouriers law for heat conduction:

    The proportionality constant is a transport property , known asthermal conductivity k (units W/m.K)

    the thermal conductivity of a material can be defined as therate of heat transfer through a unit thickness of the material

    per unit area per unit temperature difference. The thermal

    conductivity of a material is a measure of the ability of thematerial to conduct heat.

    Usually assumed to be isotropic (independent of the direction

    of transfer): k x=ky=kz=k

    dxdT

    k q x

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    7

    Thermal Conductivity: Solids

    Solid comprised of free electrons and atoms bound in lattice

    Thermal energy transported through Migration of free electrons, k e Lattice vibrational waves, k l

    l e k k k )(y,resistivitelectrical1

    eek where

    Contd .

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    Thermal Conductivity: Gases

    Intermolecular spacing is much larger Molecular motion is random Thermal energy transport less effective than in solids; thermal

    conductivity is lower

    Kinetic theory of gases:

    cnk Where, n the number of particles per unit volume,the mean molecular speed and

    the mean free path (average distance travelled before a collision) c

    Contd .

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    Thermal Conductivity: Liquids

    Physical mechanisms controlling thermal conductivity not well

    understood in the liquid state

    Generally k decreases with increasing temperature (exceptions

    glycerine and water)

    k decreases with increasing molecular weight.

    3/1

    3/4

    M Ac

    k p

    The parameter A depends on the temperature of the liquid;

    The quantity (Ac p) is constant for all liquids

    Contd .

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    Thermal Conductivity: Insulators Low temperature insulation (cork, rock wool, glass wool and thermocole)

    are used when the enclosures is at a temperature lower than the ambienttemperature and it is desired to prevent the enclosure from gaining heat.

    High temperature insulation (asbestos, diatomaceous earth, magnesia

    etc.) are used when the enclosures is at a temperature higher than theambient temperature and it is desired to prevent the enclosure fromloosing heat.

    Super insulators include powders, fibres or multi-layer materials that

    have been evacuated of all air

    The low conductivity of insulating materials is due primarily to air that iscontained in the pores rather than the low conductivity of the solidsubstance.

    Contd .

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    Variation of Thermal Conductivity with temperatureand pressure

    For most materials, the dependence of thermal conductivityon temperature is almost linear

    T k k 10Where, k 0 is the thermal conductivity at 0 0C and

    Is a constant value depending upon the material; may be positive ornegative depending on whether k increases or decreases withtemperature.

    Thermal conductivity is very weakly dependent on pressurefor solids and liquids and essentially independent of pressurefor gases at standard atmospheric pressure

    Contd .

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    The variation of the thermal conductivity of the various solids,

    liquids and gases with the temperature

    Contd .

    Adapted from Heat and MassTransfer A Practical Approach,Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    The range of thermal conductivity of various materials at room

    temperature

    Contd .

    Adapted from Heat and MassTransfer A Practical Approach,Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    Thermal Diffusivity

    The product C p , which is frequently encountered in heattransfer analysis, is called the heat capacity of a material.

    Both the specific heat C p and the heat capacity C p representthe heat storage capability of a material.

    But C p expresses it per unit mass whereas C p expresses it perunit volume, as can be noticed from their units J/kgC andJ/m 3C, respectively.

    Thermal diffusivity is the ratio of the thermal conductivity to

    the heat capacity:

    pck

    storedHeatconductedHeat

    (m 2/s)

    Contd .

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    Note that the thermal conductivity k represents how well amaterial conducts heat, and the heat capacity C p represents

    how much energy a material stores per unit volume.

    Therefore, the thermal diffusivity of a material can be viewed asthe ratio of the heat conducted through the material to the heatstored per unit volume.

    A material that has a high thermal conductivity or a low heatcapacity will obviously have a large thermal diffusivity. Thelarger the thermal diffusivity, the faster the propagation of heat

    into the medium.

    A small value of thermal diffusivity means that heat is mostlyabsorbed by the material and a small amount of heat will beconducted further.

    Contd .

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    Introduction to development of 3D equation

    d

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    Contd .

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

    C d

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    Contd .

    C d

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    Contd .

    C td

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    Contd .

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    The Conduction Rate Equation

    In reality we must account for heat transfer in three dimensions Temperature is a scalar field T(x,y,z) Heat flux is a vector quantity. In Cartesian coordinates:

    z y x qqq k jiq

    for isotropic medium z T k q

    yT k q

    xT k q z y x ,,

    T k z

    T

    y

    T

    x

    T

    k

    k jiqWhere three dimensional del operator in Cartesian coordinates:

    z y x k ji

    C td

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    Energy Conservation Equation st

    st g out in E dt

    dE E E E

    dz z dy ydx xout qqq E z y xin qqq E

    Contd .

    Contd

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    E=mcpT=( V)cpT= (dxdydz)c pT

    dy

    dx

    qx qx+dx

    x

    y

    q KA T

    x K dydz

    T

    x

    q q dq q q

    xdx

    x x x

    x dx x x x x

    ( )

    dx

    dy

    dz

    Contd .

    Contd

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    where from Fouriers law

    z

    T dxdyk

    z

    T kAq

    yT

    dxdz k yT

    kAq

    x

    T dydz k

    x

    T kAq

    z z

    y y

    x x

    )(

    )(

    )(

    dz z

    qqq

    dy y

    qqq

    dx

    x

    qqq

    z

    z dz z

    y ydy y

    x xdx x

    Energy in

    Energy out

    Contd .

    Contd

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    Thermal energy generation due to an energy source : Manifestation of energy conversion process (between thermal

    energy and chemical/electrical/nuclear energy)

    Positive (source) if thermal energy is generatedNegative (sink) if thermal energy is consumed

    )(dV dz dydxqq E g

    Energy storage term Represents the rate of change of thermal energy stored in the

    matter in the absence of phase change.

    )( dz dydxt T

    c E p st

    t T c p /is the time rate of change of the sensible (thermal) energy ofthe medium per unit volume (W/m 3)

    q is the rate at which energy is generated per unit volume of themedium (W/m 3)

    Contd .

    Contd

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    dxdydz t T

    C dxdydz qqqqqqq pdz z dy ydx x z y x

    dxdydz t

    T C dxdydz qdz

    z

    qdy

    y

    qdx

    x

    q p

    z y x

    z

    T kdxdyq

    yT kdxdz q

    xT

    kdydz q

    z

    y

    x

    st st

    g out in E dt dE

    E E E Contd .

    Contd

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    dxdydz t

    T C dxdydz qdxdydz

    z

    T k

    z dxdydz

    y

    T k

    ydxdydz

    x

    T k

    x P

    t T C q

    z T k

    z yT k

    y xT k

    x P

    Heat (Diffusion) Equation: at any point in the medium the rate of

    energy transfer by conduction in a unit volume plus thevolumetric rate of thermal energy must equal to the rate ofchange of thermal energy stored within the volume.

    Contd .

    Contd

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    dx x x qqdx

    x

    T k

    x

    t T

    k q

    z T

    yT

    xT

    1

    2

    2

    2

    2

    2

    2

    Net conduction heat flux into the controlled volume

    If the thermal conductivity is constant.

    Where = k /( Cp) is the thermal diffusivity

    t T

    C q z T

    k z y

    T k

    y xT

    k x P

    Contd .

    Contd

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    0

    q z T

    k z y

    T k

    y xT

    k x

    0)( dxdT

    k dxd

    Under steady-state condition, there can be no change in theamount of energy storage.

    If the heat transfer is one-dimensional and there is noenergy generation, the above equation reduces to

    Under steady-state, one-dimensional conditions with noenergy generation, the heat flux is a constant in the

    direction of transfer.

    Contd .

    Contd

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    Boundary and Initial Conditions Heat equation is a differential equation:

    Second order in spatial coordinates: Need 2 boundary conditions First order in time: Need 1 initial condition

    Boundary Conditions

    1) B.C. of first kind (Dirichlet condition):

    x

    T(x,t)

    Ts

    Constant Surface Temperature At x=0, T(x,t)=T(0,t)=T s

    x=0

    Contd .

    Contd

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    Boundary and Initial Conditions2) B.C. of second kind (Neumann condition): Constant heat flux at the

    surface

    1. Finite heat flux

    xT

    xT

    k q x

    s slopeconst0

    "

    0slope00

    "

    xT

    xT

    k q x

    s

    xT(x,t)

    x

    T(x,t)

    qx = q s

    2. Adiabatic surface qx=0

    Contd .

    Contd .

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    Boundary and Initial Conditions3) B.C. of third kind: When convective heat transfer occurs

    at the surface

    )],0([0

    t T T h x

    T k

    x

    T(x,t)

    T(0,t)

    x

    hT ,

    = q conduction q convection

    Contd .

    Contd .

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    Contd .

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    Cylindrical coordinates

    Contd .

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    Cylindrical coordinates

    z T

    k z qT

    r k

    qr T

    k r q ";";"

    )1

    (" Z T

    k T

    r j

    r T

    ik T k q

    When the del operator is expressed in cylindrical coordinates,the general form of the heat flux vector , and hence the FouriersLaw, is

    Contd .

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    Heat Conduction Equation

    In cylindrical coordinates:

    t T

    cq z T

    k z

    T k

    r r T

    kr r r p

    211

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    Spherical coordinates

    Contd .

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    Spherical coordinates

    T

    r k

    qT

    r k

    qr T

    k r q ";sin";"

    )sin11

    ("

    T r

    k T

    r j

    r T

    ik T k q

    When the del operator is expressed in spherical coordinates,the general form of the heat flux vector , and hence the FouriersLaw, is

    Contd .

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    Heat Conduction Equation

    In spherical coordinates:

    t T

    cqT

    k r

    T k

    r r T

    kr r r

    p

    sinsin

    1

    sin

    11222

    22

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    Energy balance for the wall

    rate ofheat transferinto the wall

    rate ofheat transferout of the wall

    rate of changeof the energyof the wall

    - =

    dt dE

    QQ wall out in

    0dt

    dE wall

    consQ wall cond ,

    steady operation; since there is no change in the

    temperature of the wall with time at any point

    The rate of heat transfer through the wall is constant

    If there is no heat generation

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    FOURIERS LAW OF HEAT CONDUCTION

    wall cond Q , dx

    dT kAQ wall cond , (W)

    and A constant, then

    dxdT constant also

    Temperature through the wall varies linearly withx. Temperature distribution in the wall understeady conditions is a straight line.

    2

    1,0

    T

    T T wall cond

    L

    x kAdT dxQ

    LT T

    kAQ wall cond 21

    ,

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    THERMAL RESISTANCE

    wall wall cond R

    T T Q 21,

    kA L

    Rwall

    (W)

    (0C / W)

    Depends on the geometry andthe thermal properties of themedium

    e RV V I 21 A L R ee

    e R21 V V e

    Electrical resistance

    Voltage differenceacross the resistance

    Electricalconductivity

    Contd .

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    NEWTONS LAW OF COOLING FORCONVECTION HEAT TRANSFER RATE

    )( T T hAQ S S conv

    conv

    S conv R

    T T Q

    S

    conv

    hA

    R1

    conv R

    h

    Convection resistance of surface

    (W)

    (0C / W)

    Convection heat transfercoefficient

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

    Contd .

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    RADIATION

    rad

    surr S surr S S rad rad R

    T T T T AhQ

    )(

    S rad rad Ah

    R1

    surr s surr s surr S S

    rad rad T T T T T T A

    Qh 22)(

    rad convcombined hhh

    )( 44 surr S S rad T T AQ

    Contd .

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    The thermal resistance network for heat transfer through a plane wallsubjected to convection on both sides and the electrical analogy

    THERMAL RESISTANCE NETWORK

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    ONE DIMENSIONAL STEADY HEATFLOW

    Rate of

    heat convection

    from the wall

    Rate of

    heat convection

    into the wall

    Rate of

    heat conduction

    through the wall

    = =

    )()( 22221

    111 T T Ah LT T

    kAT T AhQ

    Ah

    T T

    kA L

    T T

    Ah

    T T Q

    2

    2221

    1

    11

    /1//1

    2,

    2221

    1,

    11

    convwall conv RT T

    RT T

    RT T

    Q

    adding the numerators and denominators

    total RT T

    Q 21

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    Total Thermal Resistance

    total RT T

    Q 21

    Ah Ak L

    Ak L

    Ah R

    R R R R R

    total

    convwall wall convtotal

    22

    2

    1

    1

    1

    2,2,1,1,

    11

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    Thermal Contact Resistance

    gapcontact QQQ

    erfacec T AhQ int

    erfacec T

    AQh

    int

    /(W/m 2 0C)

    (m 2 0C/ W) AQ

    T

    h R erface

    cc

    /

    1 int

    hC: thermal contact conductance

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

    Contd .

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    Thermal contact resistance is inverse of thermalcontact conduction,

    Depends on

    Surface roughness, Material properties,

    Temperature and pressure at interface, Type of fluid trapped at interface

    Contd .

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    Effect of metalliccoatings on thermalcontact conductance

    For soft metals withsmoot surfaces at highpressures

    Thermal contactconductance

    Thermal contactresistance

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    Overall heat transfer coefficient

    q1 = convection

    q2 = conduction

    q3 = convection

    q = q 1 = q2 = q3

    The overall heat transfer bycombined conduction andconvection is frequently expressed interms of an overall heat transfercoefficient U

    overall T UAq

    ?U

    Contd

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    )( T T hAq wconv

    hAT T

    q wconv /1

    hA Rconv /1

    Convection Boundary condition

    Conduction

    )( 12 T T xkA

    qcond

    Ak x

    Rn

    ncond

    kA xT T

    qcond /21

    Contd

    Contd

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    )()()( 222111 B A T T AhT T xkA

    T T Ahq

    AhkA x Ah

    T T q B A

    21 /1//1

    R Ahk xhU

    11/1//1

    1

    21

    Overall heat transfer coefficient

    Contd

    21

    111hk

    xhU

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    Thermal resistance networkthrough a two-layer plane

    T UAQ

    total RUA

    1

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    THERMAL RESISTANCE NETWORKS

    )11

    )((21

    212

    21

    1

    2121 R R

    T T R

    T T R

    T T QQQ

    total RT T

    Q 21

    21

    111 R R Rtotal

    21

    21

    R R R R Rtotal

    Resistances are parallel

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    COMBINED SERIES-PARALLEL ARRANGEMENT

    total RT T Q 1

    convconvtotal R R R R R R

    R R R R 321

    21312

    11

    11 Ak

    L R

    22

    22 Ak

    L R

    33

    33 Ak

    L R 3

    1hA Rconv

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

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    Problem:

    Two slabs, each 100mm thick and made of materials with thermalconductivities of 16 and 200 W/m 0C, are placed in contact whichis not perfect. Due to roughness of surfaces, only 40% of area is incontact and air fills 0.02 mm thick gap in the remaining area.If the extreme surfaces of the arrangement are at temperaturesof 250 0C and 30 0C, determine the heat flow through thecomposite system, the contact resistance and temperature dropin contact.

    Take thermal conductivity of air as 0.032 W/m 0C and assume thathalf of the contact is due to either metal.

    1 D Steady Heat Transfer in the Plane Wall

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    For an infinite flat plate (y, z

    infinite),find the steady statetemperature profile with thetemperature at x=0 remainsat T 1 and the temperature atx=L remains at T 2

    X=0 X=L

    T1

    T2

    1-D, Steady Heat Transfer in the Plane Wall

    The Governing Differential Equation

    t T

    C q z T

    k z y

    T k

    y xT

    k x P

    =0 =0 =0 =0

    T is not function of y and z

    H t E tiContd .

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    022

    xT ---

    Heat Equation :

    0

    d dT

    k dx dx

    022

    dxT d k

    Contd .

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    Integrate eq.

    Integrate again,

    T=C1.x+C2

    Apply the boundary conditions:

    T1=C2 --- T2=C1.L+C2 ---

    1C dxdT

    B. C. T=T1 at x=0B. C. T=T2 at x=L

    Contd .

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    Putting, into

    L x

    T T T T

    L x

    T T T T

    T x L

    T T T

    LT T C T LC T

    12

    1

    121

    112

    121112

    ).(

    .

    .

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    HEAT CONDUCTION IN CYLINDERS AND SPHERES

    Steady-state heat conduction

    Heat is lost from a hot-water

    pipe to the air outside in theradial direction.

    Heat transfer from a longpipe is one dimensional

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,McGraw Hill 2007.

    A LONG CYLINDERICAL PIPE

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    STEADY STATE OPERATION

    dr dT

    kAQ cy l cond ,

    Fouriers law of conduction

    cyl cond Q , constant

    2

    1

    2

    1

    , T

    T T

    r

    r r

    cyl cond

    kdT dr A

    Q

    rL A 2

    )/ln(2 1221, r r

    T T Lk Q cyl cond

    cyl cyl cond

    R

    T T Q 21,

    Lk

    r r Rcy l

    2

    )/ln( 12

    There are flow of gases on bothComposite cylindrical wall

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    sides of the wall, which remainat temp T i & To. Looking for(1) temperature profile(2) heat flux requited to

    maintain steady state

    r1 r2

    r3

    Ti

    T1 T2

    T3 To

    p y

    ))(2(

    )()/ln(

    2

    )()/ln(

    2))(2(

    33

    3223

    2

    2112

    1

    11

    oo

    ii

    T T Lr h

    T T r r Lk

    T T r r

    Lk T T Lr hQ

    Contd .

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    65

    oi

    oi

    Lhr Lk r r

    Lk r r

    Lhr

    T T Q

    32

    23

    1

    12

    1 21

    2)/ln(

    2)/ln(

    21

    ResistanceTotalDifferenceeTemperatur OverallQ

    I fi it C li dFor steady radial flow of heat through the

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    Infinite Cylindery g

    wall of a hollow cylinder. The inner surfaceis maintained at temperature T 1, whileouter surface is kept at temperature T 2.

    Find the temperature profile across thewall and the heat flux required to maintainsteady state.T1

    T2

    r1

    r2

    T is not function of and z

    t T

    cq z T

    k z

    T k

    r r T

    kr r r p

    2

    11

    Governing equation in cylindrical coordinate=0 =0 =0 =0

    The GDE isContd .

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    The GDE is

    0)(1

    r

    T r

    r r k

    21

    1

    1

    ln

    0)(

    cr cT

    r

    c

    r

    T

    cr

    T r

    r

    T r

    r

    ---

    Contd .

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    68

    Apply boundary conditions

    2212

    2111

    ln

    ln

    cr cT

    cr cT

    B.C. r=r 1, T=T1 r=r 2, T=T2

    Contd .

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    )/ln(

    )/ln()ln(ln

    21

    211

    21121121

    r r T T c

    r r cr r cT T

    222122122

    2221212

    2221

    212

    lnlnlnlnln)()ln(ln

    ln.)/ln(

    r T r T r T r T ccr T T r r T

    cr r r

    T T T

    Contd .

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    70

    )ln)(ln()ln)(ln(

    )ln)(ln()ln(ln)ln(ln

    lnlnlnlnlnlnln

    221212

    22121221

    2221221221

    21

    r r T T r r T T

    r r T T r r T r r T

    r T r T r T r T r r r

    T T T

    )/ln()/ln(

    21

    2

    21

    2

    r r r r

    T T T T

    The variation of temperature within the cylinder is determined to be

    STEADY STATE HEAT

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    Ti

    To ri

    ro

    dr dT

    kAQ

    24 r A

    dr

    dT r k Q 24

    oi

    o

    i

    T

    T

    r

    r dT

    r

    dr

    k

    Q24

    io

    o

    i

    i

    o

    o

    i

    T T

    r

    r

    T

    T

    r

    r T

    r k Q

    dT r dr

    k Q 1

    44 2

    STEADY STATE HEATCONDUCTION FOR

    SPHERES

    TContd .

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    RT

    Q

    oi

    oi

    r r

    T T k Q

    11)(4

    k r r R oi

    4

    11

    k r r

    r r R

    oi

    io

    sph 4OR

    Contd .

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    k r r r r

    R sph21

    12

    4

    sph sphcond R

    T T Q 21,

    including convection

    22

    221

    12

    41

    4 hr k r r r r

    Rtotal

    total RT T

    Q 1

    Temperature distribution inside the spherical shell

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    p p

    t T cqT k

    r T k

    r r T kr

    r r p

    sinsin1

    sin11 222

    22

    =0 =0 =0 =0

    01 2

    2

    r

    T kr

    r r

    02

    r T

    r r

    21

    r C

    dr dT

    21)( C

    r

    C r T

    1)(C

    Contd .

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    22

    1222

    21

    1111

    )(

    )(

    C r C

    T T r T

    C r

    T T r T

    12

    11222

    21

    12

    211

    r r T r T r

    C

    T T

    r r

    r r C

    12

    112221

    12

    21)(r r

    T r T r T T

    r r r r r

    r T

    Applying BoundaryConditions

    The constantsobtained are as:

    The variation of temperature within the spherical shell isdetermined to be

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    CRITICAL RADIUS OFINSULATION

    )2(1

    2)/ln(

    2

    12

    11

    Lr h Lk r r

    T T R RT T

    Qconvins

    CYLINDER

    However, as r 2 A 0 convection heat transfer resistance of surface

    =>Q

    As r2 thickness of wall heat resistance in the wall => Q

    The heat transfer from the pipe may increase or decrease,Contd .

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    0/ 2 dr Qd

    The heat transfer from the pipe may increase or decrease,depending on which effect dominates.

    T 1 ,T

    2 , k, L, h, r

    i are constant terms, therefore:

    The variation of Q with the outerradius of the insulation r 2 is plotted:

    The value of r 2 at which Q reachesa maximum is determined from therequirement that

    Adapted from Heat and Mass Transfer A PracticalApproach, Y.A. Cengel, Third Edition, McGraw Hill2007.

    Contd .

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    222

    2

    21

    2

    2

    21

    2

    2

    11.

    1ln

    1

    )(2

    1ln

    1)(2

    0

    r hkr

    r hr r

    k

    T T L

    dr hr r

    r k

    T T Ld

    dr dQ

    o

    o

    oi

    oi

    o

    c

    o

    o

    h

    k r

    r hkr

    r hkr

    ,2

    222

    222

    11

    011

    Critical radius of insulation for cylinderContd .

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    hk

    r cylinder cr ,Thermal conductivity

    External convection heattransfer coefficient

    y

    Critical radius of insulation for shpere

    hk

    r spherecr 2

    ,

    CHOSING INSULATION THICKNESSContd .

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    cr

    cr

    cr

    r r

    r r

    r r

    2

    2

    2

    Q max

    Before insulation check for critical radius

    CHOSING INSULATION THICKNESS

    Contd .

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    Contd .

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    Optimum thickness of insulation

    Conduction with Generation

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    Conduction with GenerationThermal energy may be generated or consumed due to

    conversion from some other energy form.If thermal energy is generated in the material at the expense ofsome other energy form, we have a source: is +ve Deceleration and absorption of neutrons in a nuclear reactor

    Exothermic reactions Conversion of electrical to thermal energy:

    V R I

    V

    E q

    e g 2 where I is the current, R e the electrical

    resistance, V the volume of the medium

    If thermal energy is consumed we have a sink : is -ve

    Endothermic reactions

    q

    q

    The Plane Wall

    0 L

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    Consider one-dimensional,steady-state conduction in aplane wall of constant k, withuniform generation, andasymmetric surface conditions:

    Heat conduction equation

    02

    2

    k

    q

    dx

    T d

    The Governing Differential Equation

    t

    T C q

    z

    T k

    z y

    T k

    y x

    T k

    x P

    =0 =0 =0

    2 qTd Contd .

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    02 k q

    dxT d

    222

    2

    dxk qT d

    k q

    dxT d

    1c xdxk

    qdT

    Boundary Conditions:

    2,1, )(,)0( s s T LT T T

    General Solution:

    212

    2C xC x

    k

    qT

    Temperature ProfileContd .

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    p

    1,1,2,2 )(2)( s s s T L x

    T T x Lxk

    q xT

    Profile is parabolic.Heat flux not independent of x

    0 L

    1,2 sT C Lk

    q

    L

    T T C s s

    2

    )( 1,2,1

    1,1,2, )(2)( s s s T x

    L

    T T x L

    k q

    xT

    OR

    Symmetrical DistributionContd .

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    When both surfaces are maintained at a commontemperature, T s,1= Ts,2 = Ts 0 L

    1,1,2, )(2)( s s s T x

    L

    T T x L

    k q

    xT

    sT x x Lk q

    xT 2

    )(

    Maximum temperature within a symmetric systemContd .

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    0 L

    sT x x L

    k

    q xT

    2)(

    0dxdT

    The maximum temperature at anyposition x can be obtained as:

    02

    2 x L

    k

    q

    dx

    dT

    02k q or02 x L

    2

    L x

    At x=L/2, T = Tmax

    Contd .

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    , max

    sT x x Lk q xT 2)(

    sT L L

    Lk

    qT

    222(max)

    Putting x=L/2,

    sT Lk q

    T 28

    (max)

    Heat transfer then occurs towards both surfaces and for

    Contd .

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    Heat transfer then occurs towards both surfaces, and foreach surface it is given by:

    L x xdxdT kAQ

    or0

    q

    ALQ

    x Lk q

    kAQ L x x

    2

    22 or0

    Heat transfer for both surfaces,

    q ALQ

    =(volume of conducting medium)(heat generating capacity)

    Heat conducted to the wall surface is finally dissipated to the

    Contd .

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    a s T T hAq AL2

    Heat conducted to the wall surface is finally dissipated to thesurrounding atmosphere at temperature T a

    Lh

    qT T a s 2

    OR

    Substituting this value of wall temperature, the temperature

    distribution in term of surrounding atmospheric temperature T a

    x x Lk

    q L

    hq

    T xT a 22)(

    Contd

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    Note that at the plane of symmetry:

    0q" 00

    0

    x xdx

    dT

    Equivalent to adiabatic surface

    Cylinder with uniform heat generation

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    Solid Cylinder Temperature distribution within a solid cylinder

    224)( r Rk qT r T s

    R

    Ts

    h,Ta

    Temperature distribution is parabolic andthe maximum temperature T max occurring at the centre (r=0) of the rod isgiven by

    2max 4

    Rk

    qT T s

    The temperature distribution in term of surrounding atmospherictemperature T a

    2242

    r Rk

    q R

    hq

    T T a

    Hollow Cylinder with temperatures specified at the inside andt id f

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    outside surfaces

    Temperature distribution within a thickness of hollow cylinder

    2

    1

    121

    2221

    2211

    ln

    ln

    44)(

    r r

    r r

    r r k

    qT T r r

    k q

    T r T

    Sphere with uniform heat generation

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    Temperature distribution within a solid cylinder

    226)( r Rk qT r T s R

    Ts

    h,Ta

    Temperature distribution is parabolic and themaximum temperature T max occurring at thecentre (r=0) of the rod is given by

    2max 6

    Rk

    qT T s

    The temperature distribution in term of surrounding atmospherictemperature T a

    2263

    r Rk

    q R

    hq

    T T a

    Heat Transfer from Extended Surfaces

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    An extended surface (also know as a combined conduction-convectionsystem or a fin) is a solid within which heat transfer by conduction isassumed to be one dimensional , while heat is also transferred by convection (and/or radiation ) from the surface in a direction transverse to that ofconduction.

    Anatomy of A STRIP FIN

    io n

    Contd .

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    thickness

    x

    x

    Direction of Heat Conduction

    D i r e c t i o n o

    f H e a t C o n v e c t i o

    Basic Geometric Features of Fins

    Contd .

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    profilePROFILE AREA

    cross-section

    CROSS-SECTION AREA

    Basic Geometric Features of Fins

    GARDNER-MURRAY ANALYSIS : ASSUMPTIONSContd .

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    Steady state one dimensional conduction Model.No Heat sources or sinks within the fin .Thermal conductivity is constant and uniform in all directions.Heat transfer coefficient is constant and uniform over fin faces.Surrounding temperature is constant and uniform.Base temperature is constant and uniform over fin base.Fin width much smaller than fin height or length.No bond resistance between fin base and prime surface.

    Heat flow off fin proportional to temperature excess.

    Why Fins are needed?

    Contd .

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    Temperature gradient dT/dx ,

    Surface temperature, T, Are expressed such that T is a function of x only.

    Newtons law of cooling

    Two ways to increase the rate of heat transfer: increasing the heat transfer coefficient , increase the surface area fins

    conv s sQ hA T T

    Extended surfaces may exist in many situations but are commonly used as

    Contd .

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    fins to enhance heat transfer by increasing the surface area available forconvection (and/or radiation).

    Some typical fin configurations:

    Straight fins of (a) uniform and (b) non-uniform cross sections; (c) annularfin, and (d) pin fin of non-uniform cross section.

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    Innovative Fin Designs

    Steady One-dimensional Conduction through Fins

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    Steady One dimensional Conduction through Fins

    Adapted from Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition,

    McGraw Hill 2007.

    Contd .

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    Energy Balance on Volume Element (fin)Contd .

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    Energy Balance on Volume Element (fin)

    rate of heatconduction intothe element at x

    rate of heatconduction fromthe element at

    x+x

    rate of heatconvection fromthe element

    +=

    ))(( T T x P hQ S conv

    conv x xcond xcond QQQ ,,

    0)(,, T T xhP QQ xcond x xcond

    Expressing the surface area, A s, in terms of width, x, times the perimeter P

    QQ

    Contd .

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    0 x

    0)( T T hP dxdQ cond

    0)(,, T T hP x

    QQ xcond x xcond

    Taking limit x tends to zero and using the definition of derivative:

    dxdT

    kAQ ccond

    0)(

    TThPdT

    kAd

    Contd .

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    0)(

    T T hP dx

    kAdx c

    At constant A C and kSolution is;

    C kAhp

    m 2 T T

    0)(22

    T T kAhP

    dxT d

    c

    Putting following constants as:

    2d

    Contd .

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    022

    mdxd

    mxmx eC eC x 21)(

    Equation (A) is a linear, homogeneous, second-order differentialequation with constant coefficients.

    The general solution of Eq. (A) is

    (A)

    Boundary Conditions

    Contd .

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    Several boundary conditions are typically employed: At the fin base

    Specified temperature boundary condition, expressedas: (0)= b= T b-T

    At the fin tip1. Specified temperature

    2. Infinitely Long Fin3. Adiabatic tip

    4. Convection (andcombined convection).

    Contd .

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    Base ( x = 0) condition 0 b bT T

    Tip ( x = L) conditions A. :Conve ti |c on / x Lkd dx h L

    B. :A / |diabati 0c x Ld dx

    Fixed temper C. :ature L L D. (I >2.65): 0nfinite fin mL L Fin Heat Rate:

    0| f f c x A sd

    q kA h x dAdx

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    Solutions of Differential EquationContd .

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    )( T T hPkAq bc f

    Fin Efficiency

    To maximize the heat transfer from a fin the temperature

    Fin Performance

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    To maximize the heat transfer from a fin the temperatureof the fin should be uniform (maximized) at the base value

    of T b In reality, the temperature drops along the fin , and thus

    the heat transfer from the fin is less To account for the effect we define

    a fin efficiency

    or,max

    fin fin

    fin

    Q

    Q Actual heat transfer rate from the fin

    Ideal heat transfer rate from the finif the entire fin were at base temperature

    ,max ( ) fin fin fin fin fin bQ Q hA T T

    For constant cross section of very long fins:

    Contd .

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    For constant cross section of very long fins:

    For constant cross section with adiabatic tip:

    , ,max

    1 1 fin c b clong fin

    fin fin b

    Q hpkA T T kAQ hA T T L hp mL

    , ,max

    tanh

    tanh

    fin c badiabatic fin

    fin fin b

    Q hpkA T T mL

    Q hA T T

    mLmL

    Afin = P*L

    Fin Effectiveness

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    The performance of the fins is judged on the basis of the

    enhancement in heat transfer relative to the no-fin case. The performance of fins is expressed

    in terms of the fin effectiveness fin

    defined as

    fin fin

    finno fin b b

    Q Q

    Q hA T T

    Heat transfer ratefrom the surface

    of area A b

    Heat transfer ratefrom the fin of base

    area A b

    with , and / f ch k A P

    Fin Arrays

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    Representative arrays of(a) rectangular and(b) annular fins.

    Total surface area:t f b A NA A

    Number of fins Area of exposed base ( prime surface)

    Define terms: A b: base area exposed to coolantAf : surface area of a single finAt: total area including base area and total finned surface,

    N: total number of fins

    ( ) ( )t b f b b f f bq q Nq hA T T N hA T T

    Overall fin efficiency for an array of fins: Contd .

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    Overall surface efficiency and resistance :

    ,1b

    t o

    t o t

    Rq hA

    1 1 f o f t

    NA

    A

    bt

    t t o hA

    qq

    q

    max

    OR

    [( ) ]( ) [ (1 )]( )

    [1 (1 )]( ) ( )

    Define overall fin efficiency: 1 (1 )

    t f f f b t f f b

    f t f b O t bt

    f O f

    t

    h A NA N A T T h A NA T T

    NAhA T T hA T T A

    NA

    A

    Total heat rate:

    ,

    bt f f b b b o t b

    t o

    q N hA hA hA R

    Contd .

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    ,,

    ,

    ,

    1( ) where

    Compare to heat transfer without fins

    1( ) ( )( )

    where is the base area (unexposed) for the finTo enhance heat transfer

    Th

    bt t O b t O

    t O t O

    b b b f b

    b f

    t O

    T T q hA T T R

    R hA

    q hA T T h A NA T T hA

    A A A

    Oat is, to increase the effective area . t A

    =Ab+NAb,f

    Thermal Resistance ConceptContd .

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    T1 T

    Tb T2

    T1 T Tb T2

    L1 t

    R1=L1/(k 1A)

    Rb=t/(k bA)

    )/(1, Ot Ot hA R

    1 1

    1 ,b t O

    T T T T q R R R R

    A=Ab+NAb,f

    Topics to be referred by the students from Textbooks

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    Topics to be referred by the students from Textbooks

    Shape factor

    Effect of variable conductivity

    Logarithmic mean radius

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    References:

    Heat Transfer A Practical Approach, Y.A. Cengel, Second Edition, Tata McGraw Hill2003.

    Heat and Mass Transfer A Practical Approach, Y.A. Cengel, Third Edition, TataMcGraw Hill 2007.

    Heat Transfer , P. K. Nag, First Edition, Tata McGraw Hill 2002.

    Heat and Mass Transfer , D.S. Kumar, Sixth Edition, S.K. Kataria & Sons 2004.


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