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    Fouriers Law

    and theHeat Equation

    Chapter Two

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    Fouriers Law

    A rate equation that allows determination of the conduction heat fluxfrom knowledge of the temperature distribution in a medium

    Fouriers Law

    Its most general (vector) form for multidimensional conduction is:

    q k Tp p

    dd!

    Implications: Heat transfer is in the direction of decreasing temperature

    (basis for minus sign).

    Direction of heat transfer is perpendicular to lines of constant

    temperature (isotherms).

    Heat flux vector may be resolved into orthogonal components.

    Fouriers Law serves to define the thermal conductivity of the

    medium /k q Tp p

    dd|

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    Heat Flux Components

    (2.18)T T Tq k i k j k k r r zJ

    p p p px x xdd! x x x

    rqdd qJdd zqdd

    Cylindrical Coordinates: , ,T r zJ

    sin

    T T Tq k i k j k k

    r r rU U J

    p p p px x xdd! x x x

    (2.21)

    rqdd qUdd qJdd

    Spherical Coordinates: , ,T r J U

    Cartesian Coordinates: , ,T x y z

    T T Tq k i k j k k x y z

    p p p p

    x x xdd! x x x

    xqdd yqdd zqdd

    (2.3)

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    Heat Flux Components (cont.)

    In angular coordinates , the temperature gradient is still

    based on temperature change over a length scale and hence has

    units ofrC/m and not rC/deg.

    or ,J J U

    Heat rate forone-dimensional, radial conduction in a cylinder or sphere:

    Cylinder

    2r r r r q A q rLqTdd dd! !

    or,

    2r r r r q q rqTd ddd dd! !

    Sphere

    24r r r r q q r qTdd dd! !

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    Heat Equation

    The Heat Equation A differential equation whose solution provides the temperature distribution in a

    stationary medium. Based on applying conservation of energy to a differential control volume

    through which energy transfer is exclusively by conduction.

    Cartesian Coordinates:

    Net transferofthermal energy into the

    control volume (inflow-outflow)

    p

    T T T T k k k q c

    x x y y z z tV

    x x x x x x x ! x x x x x x x

    (2.13)

    Thermal energy

    generationChange in thermal

    energy storage

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    Heat Equation (Radial Systems)

    2

    1 1p

    T T T T kr k k q c

    r r r z z t r VJ J

    x x x x x x x ! x x x x x x x

    (2.20)

    Spherical Coordinates:

    Cylindri

    cal Coordinates:

    2

    2 2 2 2

    1 1 1sin

    sin sinp

    T T T T kr k k q c

    r r tr r rU V

    J J U UU U

    x x x x x x x ! x x x x x x x

    (2.33)

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    Heat Equation (Special Case)

    One-Dimensional Conduction in a Planar Medium with Constant Properties

    andNo Generation

    2

    2

    1T T

    tx E

    x x!

    xx

    thermal diffu osivit f the medy ium

    p

    k

    cE

    V| p

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    Boundary Conditions

    Boundary and Initial Conditions For transient conduction, heat equation is first order in time, requiring

    specification of an initial temperature distribution: 0, ,0tT x t T x! ! Since heat equation is second order in space, twoboundary conditions

    must be specified. Some common cases:

    Constant Surface Temperature:

    0,s

    T t T!

    Constant Heat Flux:

    0|x sT

    k qx !

    xdd !x

    Applied Flux Insulated Surface

    0 0x

    T

    x !

    x

    !x

    Convection

    0 0,xT

    k h T T tx

    ! gx

    ! x

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    Properties

    Thermophysical Properties

    Thermal Conductivity: A measure of a materials ability to transfer thermal

    energy by conduction.

    Thermal Diffusivity: A measure of a materials ability to respond to changes

    in its thermal environment.

    Property Tables:

    Solids: Tables A.1 A.3

    Gases: Table A.4

    Liquids: Tables A.5 A.7

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    Conduction Analysis

    Methodology of a Conduction Analysis

    Solve appropriate form of heat equation to obtain the temperaturedistribution.

    Knowing the temperature distribution, apply Fouriers Law to obtain the

    heat flux at any time, location and direction of interest.

    Applications:

    Chapter 3: One-Dimensional, Steady-State Conduction

    Chapter 4: Two-Dimensional, Steady-State Conduction

    Chapter 5: Transient Conduction

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    Problem : Thermal Response of Plane Wall

    Problem 2.46 Thermal response of a plane wall to convection heat transfer.

    KNOWN: Plane wall initiall at a niform temperat re is s enl e pose to convective

    heatin .

    FIND: a ifferential e ation an initial an bo n ar con itions which ma be se to fin

    the temperat re istrib tion T t ; b etch T t for the followin con itions: initial t

    0), steady-state (t pg), and two intermediate times; (c) Sketch heat fluxes as a function oftime at the two surfaces; (d) Expression for total energy transferred to wall per unit volume

    (J/m3).

    SCHEMATIC:

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    c) The heat flux, ddq x, txb g, asafunctionoftime, isshownonthesketchforthesurfacesx = 0 andx =L.

    in conv s0

    E q dtg

    dd!

    d) The total energy transferred to the wall may be expressed as

    in s 0E hA T T L,t dtg

    g!

    Dividing both sides by AsL, the energy transferred per unit volume is

    3in0

    E hT T L,t dt J/m

    V L

    gg

    !

    Problem: Thermal Response (Cont.)

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    Problem: Non-Uniform Generation due

    to Radiation Absorption

    Problem 2.28 Surface heat fluxes, heat generation and total rate of radiation

    absorption in an irradiated semi-transparent material with a

    prescribed temperature distribution.

    KNOWN: emperature distribution in a semi-transparent medium subjected to radiati e flux.

    FIND: (a) Expressions for the heat flux at the front and rear surfaces, (b) The heat generation rate

    ,q xbgand (c) Expression for absorbed radiation per unit surface area.

    SCHEMATIC:

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    Ona nitarea basis

    Alternativel ,eval ate ddEg b integration over the volume o the medium,

    .dd! !

    z zE q d Ae d -

    A

    ae

    A

    ae

    L -aL -aL

    -aL

    bg e j01

    .dd! dd dd ! dd dd ! E E E q q LA

    a

    eg i t x x-aLbg bg

    e

    Problem: Non-Uniform Generation (Cont.)