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CONVECTIVE CONVECTIVE HEAT TRANSFER HEAT TRANSFER By: Prof K. M. Joshi, By: Prof K. M. Joshi, Assi Assi. Professor, MED, . Professor, MED, SSAS Institute of Technology, Surat. SSAS Institute of Technology, Surat.
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  • CONVECTIVE CONVECTIVE

    HEAT TRANSFER HEAT TRANSFER

    By: Prof K. M. Joshi,By: Prof K. M. Joshi,AssiAssi. Professor, MED,. Professor, MED,

    SSAS Institute of Technology, Surat.SSAS Institute of Technology, Surat.

  • MECHANISM BEHIND FREE /NATURAL CONVECTION

    The stagnate layer of fluid in

    immediate vicinity of hot body

    receives heat energy by

    conduction. The energy transfer by

    this, increases temperature and

    internal energy of fluid particles.

    Warmer air

    rising

    AIR.

    Q

    Because of temperature rise particles become less dance and hence lighter.

    The lighter particles move upward in low temperature region.

    These particles mix with the cool particles and transfer a part of energy.

    Simultaneously cool heavier particles moves downward to fill the space

    vacated by warm particles

    The circulation pattern, upward movement of hot particles and downward

    movement of cool particles causes convective currents. The se currents are

    set up naturally due to gravitational force only.

  • MECHANISM BEHIND FORCED CONVECTION

    AIR

    20°C

    5 m/s

    20°C.

    Q

    Fluid flow causing by the pump, fan or atmospheric wind…

    Therefore the rate of heat transfer is much higher by forced convection

    than it is by the natural convection or by conduction.

    In fact, the higher the fluid velocity, the higher the rate of heat transfer.

  • EXAMPLES OF NATURAL AND FORCED CONVECTION

    �Design of house heating, furnace, architectural

    projects, roads and concrete structures concerns with the

    free convection.

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    �Cooling in IC engines, air condition installations,

    temperature control in nuclear plant, condenser tubes or

    other heat exchangers are example of forced convection.

  • Convection heat transfer strongly depends on ….

    � fluid properties dynamic viscosity , thermal conductivity k, density

    and specific heat

    � fluid velocity V

    � Geometry and the roughness of the solid surface

    � Type of fluid flow (such as being laminar or turbulent).

    (((( ))))conv s sQ hA T T∞∞∞∞= −= −= −= −&&&&NEWTON’S LAW OF COOLING

    (((( ))))conv s s ∞∞∞∞h = Convection heat transfer coefficient

    As = Heat transfer surface area

    Ts = Temperature of the surface

    T∞∞∞∞= Temperature of the fluid sufficiently far from the surface

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    Heat flux, qconv =

  • The value of convective heat transfer coefficient (as well as

    temp difference may also) is not constant for entire surface it

    depends on location there for we can define

    Local and total convection transfer (a) Surface of arbitrary shape. (b) Flat plate.

    LOCAL HEAT FLUX convq′′

    (((( ))))conv l sq h T T∞∞∞∞′′′′′′′′ = −= −= −= −

    hl is the local convection coefficient

    Local and total convection transfer (a) Surface of arbitrary shape. (b) Flat plate.

    dAsq”

    As, Ts

    V ,T∞∞∞∞

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    q”

    x dxL

    As, Ts

    U ,T∞ ∞∞ ∞∞ ∞∞ ∞

  • TOTAL HEAT TRANSFER RATE

    s

    conv conv s

    A

    Q q dA′′= ∫&

    ( )s

    conv s l s

    A

    Q T T h dA∞= − ∫&

    convQ&

    (((( ))))conv l sq h T T∞∞∞∞′′′′′′′′ = −= −= −= −

    putting value of Q&

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    1

    s

    l ss A

    h h dAA

    = ∫

    putting value of convQ&

    ( )s

    conv s l s

    A

    Q T T h dA∞= − ∫&(((( ))))conv s sQ hA T T∞∞∞∞= −= −= −= −&&&&

  • An implication of the no-slip and the no-temperature jump

    conditions is that heat transfer from the solid surface to the

    fluid layer adjacent to the surface is by pure conduction, since

    the fluid layer is motionless,

    0conv cond fluid

    y

    Tq q k

    dy =

    ∂= = −& &

    T represents the temperature distribution in the fluid

    is the temperature gradient at the surface.

    ( ) 0yT y =∂ ∂is the temperature gradient at the surface.

    ( )conv l sq h T T∞′′ = −

    (((( ))))fluid ys

    k T yh

    T T====

    ∞∞∞∞

    − ∂ ∂− ∂ ∂− ∂ ∂− ∂ ∂====

    −−−−0

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  • A fluid flowing over a stationary surface comes to a complete stop

    at the surface because of the no-slip condition.

    Zero velocity

    at the surface

    Relative velocity

    of fluid layersUniform

    approach

    velocity, V

    Solid Block

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    A similar phenomenon occurs for the temperature. When two bodies at

    different temperatures are brought into contact, heat transfer occurs until

    both bodies assume the same temperature at the point of contact.

    Therefore, a fluid and a solid surface will have the same temperature at the

    point of contact. This is known as NO-TEMPERATURE-JUMP CONDITION.

  • A steam pipe is passed through a room in which air and walltemperature are al 30 oC while surface temperature of the pipe is400 oC If the diameter of the pipe is 40 mm and average heattransfer coefficient is 20 W/m2 oC, what is the rate of heat lossfrom the pipe for one meter length of pipe.

    Schematic:

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    Known: surface temperature and air temp

    Find: The rate of heat loss

    Assumptions: �Steady operating conditions exist. �Radiation effects are negligible. �Constant properties.

  • Analysis:

    Q = h X A X (Ts - Tα)

    = 20 X (πdL) X (400 - 30)

    = (20 W/m2 oC ) X ( π X 40 X 10 3 X 1 m2 ) X ( 370 oC )

    = 0.93 kW

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  • Laminar versus Turbulent FlowSome flows are smooth and orderly while others are rather chaotic. The

    highly ordered fluid motion characterized by smooth streamlines is called laminar.

    The flow of high-viscosity fluids such as oils at low velocities is typically laminar.

    The highly disordered fluid motion that typically occurs at high velocities

    characterized by velocities fluctuations is called turbulent. The flow of low-

    viscosity fluids such as air at high velocities is typically turbulent. This flow greatly

    influences the heat transfer rates and the required power for pumping

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    comDye Streak

    Smooth well rounded

    Entrance

    Q = VA

    Pipe

    Dye

    Transitional

    Turbulent

    Laminar

  • The Reynolds number can

    be viewed as the ratio of

    the inertia forces to viscous

    forces acting on a fluid

    volume element.

    Osborne Reynolds

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  • Dimensionless numbers and

    their Physical significance.

    Reynolds NumberReynolds NumberReynolds NumberReynolds Number

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    Leads to turbulent flowLeads to turbulent flowLeads to turbulent flowLeads to turbulent flow

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  • WILHEM NUSSELT

    (1882-1957)

    was a German engineer. Nusselt studied mechanical

    engineering at the Munich Technical University where

    he got his doctorate in 1907.

    �Doctoral thesis – CONDUCTIVITY OF INSULATING MATERIALS

    �Professor at Technical university of Karlsruhe - 1920 -1925

    �Professor at Technical university of Munchen - 1926 -1952

    �Worked till the age of 70 years. Lived for 75 years and died in Munchen on

    September 1, 1957.

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  • CHARACTERISTIC LENGTH OR EQUIVALENT DIAMETERIn the non-dimensional number expressions there has appeared a characteristic length L or diameter De. The equivalent diameter is usually defined as:

    For simple tube having internal diameter D,

  • Ludwig Prandtl

    1875-1953

    Professor of Applied

    Mechanics at Gottingen

    for forty-nine years (from

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    Mechanics at Gottingen

    for forty-nine years (from

    1904 until his death

    there on August 15,

    1953)

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  • 2

    32 )(

    µβρ Tgl

    Gr∆=

    Grashof NumberGrashof NumberGrashof NumberGrashof Number

    22

    2232

    )(

    )()(

    Vl

    lVTgl

    µρβρ ×∆= 2)(

    )()(

    forceviscous

    forceinertiaforcebuoyant ×=

    The Grashof number represents the product of bouyant force and inertia force to the square of viscous force.

    The natrual convection start with very small value of Gr and increase with significant increses in Gr.

    The role of Grashof number in natural convection is similar to the Reynold number in forced convection.

    Gr provides criteria whether the flow is laminar or turbulent.

    The critical Gr is 109 for a flow over a vertical plate for change over from laminar to turbulent. ww

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  • Stanton NumberStanton NumberStanton NumberStanton Number

    K

    KJ

    KKg

    KJ

    s

    m

    m

    Kg⇒

    ⋅××

    3

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  • PecletPecletPecletPeclet NumberNumberNumberNumber

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  • GraetzGraetzGraetzGraetz NumberNumberNumberNumber

    Heat capacity of Fluid Heat capacity of Fluid Heat capacity of Fluid Heat capacity of Fluid (in pipe) Per unit Length(in pipe) Per unit Length(in pipe) Per unit Length(in pipe) Per unit Length

    Thermal conductivity of Thermal conductivity of Thermal conductivity of Thermal conductivity of pipepipepipepipe

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