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    University of Illinois

    University of Illinois

    Modeling Heat Transfer and Pressure

    Drop for Liquid-Vapor Flows in theElongated-Bubble Flow Regime

    Anthony M. JacobiRichard W. Kritzer Distinguished Professor of Mechanical Engineering

    Co-Director ACRCUniversity of Illinois at Urbana-Champaign

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    Motivation A vapor-compression system

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    Motivation Heat exchangers

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    Motivation Integrated as the IMCC

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    Motivation Personal cooling systems

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    Outline

    Statement of goals

    Summary of a heat transfer model

    Background for modeling

    Focus on the physical model

    Review some validation

    Pressure drop modeling

    How is two-phase pressure-drop modeling approached?

    A directly mechanistic model is superior

    There are problems with our mechanistic models.

    Some ideas for modelingrather loose ideas that you might shoot down.

    Field and Hrnjak 2007, ACRC TR-271

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    Statement of goals

    Shamelessly promote the heat transfer model?

    The apparent success of the model might say something about physics.

    Present a loose overview of pressure-drop models.

    Their apparent success might not say something about physicsIdentify problems in our mechanistic descriptions

    There appear to be obvious weakness in our descriptions of the flows

    Propose some ideas that might improve our models.

    Backward boundary layers and surface tensionRelate back to application

    To show that everything I presented might be meaningless

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    Flow regime observations

    Observations of flow regimes in microchannel f lows (modified from Qu et al . (2005) elongated bubble flow and annular flowdominate.

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    University of Illinois

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    A two-zone model of heat transfer to elongated-bubble flow (Jacobi and Thome 2002)

    LPLV

    LL

    D

    q

    U

    Initial bubble growth per Plessets theory gives the time required to generate apair, with Teff prescribed. With this period known, initial conditions on thepair geometry are determined for a known mass flux. An energy balance isapplied to the pair, and heat transfer is modeled as thin-film evaporation througho;

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    A two-zone model of heat transfer to elongated-bubble flow (Jacobi and Thome 2002)

    2

    )(

    ))()((

    +=R

    t Lt LqD

    dt

    dL

    V

    LV V

    Conservation of energy yields coupled ODEs for pair geometry

    With pair geometry known at all times (locations), a thin-filmevaporation model is used to calculate heat transfer coefficient.

    1

    )(4

    )();(

    =

    t U

    t qLk t sh

    L

    poL

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    A two-zone model of heat transfer to elongated-bubble flow (Jacobi and Thome 2002)

    0

    5000

    10000

    15000

    20000

    40000 80000 120000 160000 200000

    q (W/m 2)

    Teff

    =30 oC Teff

    =38 oC

    Teff

    =45 oC

    h (W/ m2K)

    q (W/m2)

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    A two-zone model of heat transfer to elongated-bubble flow (Jacobi and Thome 2002)

    0

    5000

    10000

    15000

    20000

    150 200 250 300 350 400 450

    m (kg/m 2s)

    T=30 oC

    T=38 oC

    T=45 oC

    h (W/m 2K )

    G (kg/m2s)

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    A two-zone model of heat transfer to elongated-bubble flow (Jacobi and Thome 2002)

    0

    5000

    10000

    15000

    20000

    0 50000 100000 150000 200000

    Current ModelData of Bao et al. (2000)

    q (W/m 2)

    A simple thin-film heattransfer model predictsthe observed trends. It isunnecessary--probably

    wrong--to extrapolateconventional-scale datainterpretations to themesoscale. The successof this model suggestsnucleate boiling might

    not dominate.h (W/ m2K )

    q (W/m2)

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    A three-zone model of heat transfer to elongated-bubble flow (Thome et al. 2004)

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    A three-zone model of heat transfer to elongated-bubble flow (Thome et al. 2004)

    Initial conditions

    Pair length and velocity evolve

    Down the tube

    1p

    v l

    G x xL

    f = +

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    1717

    A three-zone model of heat transfer to elongated-bubble flow (Thome et al. 2004)

    Two or three zones?

    Motivated by Moriyama and Inoue (1996):

    The constant C o is left as a free parameter

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    A three-zone model of heat transfer to elongated-bubble flow (Thome et al. 2004)

    Two or three zones?

    Minimum film thickness, min, left as adjustable parameter

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    A three-zone model of heat transfer to elongated-bubble flow (Thome et al. 2004)

    Two or three zones?

    ,dry film vt t >If

    ,dry film vt t > , )

    0, CS=V0(cos cos )

    ( ) ( )

    c f b shear

    pl l v v c p l l v v c

    pA P F

    dU d L L A U L L A

    dt dt

    +

    + = +

    , ,( )sx bx rf x X X X X CS C C CS

    F F a d V d V V V dAt

    + = +

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    Pressure Drop

    A proposal. 3 31

    0

    pv

    v

    LLv v p l l p

    shear L

    U U F C P dx dx

    x x

    = +

    3 / 248( )

    2

    pv v l l v l l l

    p p p

    p l vp l v

    p p

    U pL L

    L DL DL

    dU L LU

    dz L L

    + + +

    +

    :

    Then

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    4646

    Pressure Drop

    Surface tension:

    Shear:

    Growth and acceleration of the triplet:

    8

    p pDL DL

    3 / 24( )p pv v l l v l l l

    p

    U LL L

    DL D +

    2 p l vp l vp p

    dU L LU yuk

    dz L L

    +

    (cos )

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    Pressure Drop

    Will it work?

    1/ 2

    ( )4 8

    16

    0 1

    p

    l v v l l v l l l l p p l p

    p l vl v

    l p p

    U L L

    L U L

    dU L LDdz L L

    C C

    = + + +

    +

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    4848

    Outline

    Statement of goals

    Summary of a heat transfer model

    Background for modeling

    Focus on the physical model

    Review some validation

    Pressure drop modeling

    How is two-phase pressure-drop modeling approached?

    A directly mechanistic model is superior

    There are problems with our mechanistic models.Some ideas for modelingrather loose ideas that you might shoot down.

    Field and Hrnjak, 2007 ACRC TR-261.

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

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    Field and Hrnjak, 2007, ACRC TR-261

    Mechanistic Adjusted S.F.