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    Studies on flow through and around a porous permeable sphere: II.

    Heat Transfer

    A. K. Jain and S. Basu1

    Department of Chemical EngineeringIndian Institute of Technology Delhi

    New Delhi 110016, India

    ABSTRACT

    Heat transfer from a porous-permeable sphere due to flowing of fluid through and around

    it is studied for a wide range of Reynolds number (0.02 to 2000) and Pradtl number (0.7

    to 7) using standard CFD software. CFD simulated results for impermeable sphere

    predicts the Whitaker correlation quite well. The Simulation is then extended for heattransfer from an isothermal porous-permeable sphere. The results are presented in terms

    of four dimensionless parameters - particle Reynolds number (Re) based on the free

    stream velocity and diameter of the porous sphere, permeability ratio, Pradtl number (Pr)

    and Nusselt number (Nu). The results show that the heat transfer rate from porous

    permeable sphere increases with the increase in permeability. At low Re, the Nu for a

    permeable sphere is higher than that for solid sphere when the Pr is low, whereas, for

    high Pr, permeability has only a weak effect on the Nu. At high Re, the Nu for permeable

    sphere is much higher than that for solid sphere irrespective Pr values. The correlation

    obtained from the CFD simulation data for heat transfer from porous permeable sphere is

    useful in predicting Nu for porous permeable sphere for a wide range of Re from 0.02 to

    2000 and Pr from 0.7 to 7 at different permeability ratios.

    Keywords:Porous permeable sphere, Heat transfer, Permeability Ratio

    INTRODUCTION

    Heat transfer from an object due to flowing of surrounding fluid is a topic of industrial

    importance. The object concerned may be relatively simple, such as a cylinder or sphere,

    or it may be more complex, such as a tube bundle made up of a set of cylindrical tubes

    with a stream of gas or liquid flowing between them. In the present investigation,

    spherical aggregates forming porous permeable sphere is considered because of

    1Corresponding author; e-mail: [email protected]; Fax +011 91 26581120

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    simplicity in analyzing symmetric flow condition, availability of data and for the purpose

    of comparing results for solid sphere. The results may be applicable to many processes

    that involve spray of bubbles or droplets (Bird et al., 2002). Also, it may be useful in

    understanding the geothermal energy transportation under varied geological structures

    (Vasudeviah and Balamurugan, 1998).

    Acrivos and Taylor (1962) studied the problem of forced convection from an isothermal

    sphere for small and large Peclet number (Pe). Their analysis is valid when Reynolds

    number (Re) and Pe ( = Re. Pr) is less than one, with no restriction on the Prandtl number

    (Pr). Different empirical heat transfer correlations were given by different investigators

    for single impermeable sphere along with experimental data e.g., Ranz and Marshall

    (1952), Whitaker (1972), Achenbach (1978) and Romkes et al. (2003). The different

    empirical correlations are given below.

    Ranz and Marshall (1952)

    31

    21

    PrRe66.00.2 +=Nu for 3.5 < Re < 7.6 x 104 (1)

    Whitaker (1972)

    32

    32

    21

    PrRe06.0Re4.00.2

    ++=Nu (2)

    for 3.5 < Re < 7.6 x 104

    and 0.7 < Pr < 380Achenbach (1978)

    ++= 6.14 Re10*34

    10.2Nu for 10

    2< Re < 2 x 10

    5 (3)

    It is well known fact that the Nusselt number (Nu) is equal to 2 for a sphere immersed in

    an infinite medium as the steady state conduction solution prevails (Whitaker, 1972).

    Johnson and Smet (1984) examined the heat transfer from a permeable sphere in uniform

    flow and at low Re. They considered the case when conduction is dominant heat transfer

    mechanism in the exterior fluid, i.e. small Pe, and the case when convection was

    dominant, i.e. large Pe. They found from their study that at small Peclet numbers the heat

    transfer rate from a permeable sphere differ at leading-order from that found for an

    impermeable sphere, whereas, for large Peclet numbers permeability has only a weak or

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    second-order effect on the heat transfer rate. But their theoretical work was only limited

    to Stokes flow. They did not study the system for high Reynolds number.

    In the present work heat transfer study on flow through and around a porous permeable

    sphere for a wide range of Re (0.02 to 2000) and Pr (0.7 to 7) is studied using standard

    CFD software. The main objective is to study the effect of permeability and to examine

    how the heat transfer process is influenced by fluid flow not only around but also through

    the porous permeable sphere. A generalized correlation is suggested based on all

    simulation results obtained for a wide range of Reynolds number, Prandtl number and

    permeability ratio.

    COMPUTATIONAL FLUID DYNAMICS SIMULATION

    Porous permeable sphere is assumed to consist of small spherical particles (grains) with

    some specific void fraction. Mass and energy conservation expressions and the Navier-

    Stokes equations are used for the outer region of porous permeable sphere. Whereas, in

    the inner region, mass and energy conservation and Darcys law of Brinkmans extension

    are applied in order to solve the temperature, pressure and velocity fields. Thus, the flow

    regions through and around a porous permeable sphere are divided into two parts,

    namely, internal flow and external flow. The flow regions and the coordinate systems for

    flow through and around a porous permeable sphere are shown in figure 1 of Jain et al.

    (submitted).

    External flow:

    Equation of continuity, Reynolds-average Navier-Stokes (RANS) given in Jain et al.

    (submitted) were used along with the energy equation. The energy equation is given

    below.

    Equation of energy

    ( ) ( )( ) ( ) heffjjj

    eff SvJHTPEvEt

    +

    +=++

    (1)

    Where E is total energy, is the density, P is the pressure, T is the temperature, H is the

    enthalpy, effis the effective shear stress, Jj is the diffusion flux of speciesjand effis the

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    effective thermal conductivity. eff = + Cp t / Prt, where Prt is the turbulent Prandtl

    number, Cpis the specific heat of fluid and is the thermal conductivity of the flowing

    fluid. The first three terms on the right-hand side of eq. (9), represent energy transfer due

    to conduction, species diffusion, and viscous dissipation, respectively. Sh includes the

    heat of chemical reaction, and any other volumetric heat sources have been defined. In

    the present study Shis zero.

    Internal flow:

    (i) Momentum equations for porous media:

    Porous media are modeled by the addition of a momentum source term to the Reynolds-

    average Navier-Stokes equation. The source term is composed of two parts, a viscous

    loss term and an inertial loss term. For simple homogeneous porous media, the source

    term, the Kozeny equation for relating relating permeability and porosity, the inertial

    resistance factor, Darcys equation and intertial loss term given in Jain et al. (submitted)

    were used for the modeling of internal flow region. It should be noted that isothermal

    condition is assumed inside of the porous permeable sphere.

    Meshing of the system and setting of tolerance limit was done following same procedure

    as described in Jain et al (submitted). Laminar model was used for low Reynolds number

    and k- model is used at high Reynolds number. Inside the porous permeable sphere

    laminar model is used.

    Calculation of heat transfer coefficient (h) and Nusselt number (Nu):

    The temperature of the surface of the particle, constitutes the porous permeable sphere,

    was set to a surface temperature, Ts, whereas the fluid at the boundary of the domain

    (inlet condition) was set to a lower bulk temperature, T. As a result of the temperature

    difference between the particle surface and the fluid, heat is transferred from the particle

    to the fluid. The particle-to-fluid heat transfer rate, q, for flow around sphere of diameter

    d, and heat transfer coefficient, h, is expressed as, q = h d2 (Ts-T) and Nusselt number

    is expressed as, Nu = h d / .

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    RESULT AND DISCUSSION

    Solid sphere:

    At first, simulations are carried out for solid sphere for different Reynolds number

    ranging from 0.02 to 2000 and different Prandtl number varying from 0.7 to 7. The

    simulation results are plotted in the form of Whitaker correlation (Whitaker, 1972) and

    compared with the experimental data. In figure 1, the symbols show experimental data

    whereas dashed line indicates the Whitaker correlation (eq. 1). It is well known fact that

    the correlations available in the literature (Holman, 1986) slightly under predict the

    experimental value for Nu at low Re. It is seen in figure 1 that the experimental data are

    well predicted by the CFD simulations, as shown by solid line at low Re. The simulated

    Nu values for high Reynolds number are also in good agreement with the experimental

    data available in literature.

    Porous permeable sphere:

    In figure 2, Nu, is plotted against Re Pr2/3

    at different permeability ratio, K/d2for flowing

    of air through and around the porous permeable sphere. The solid line indicates the Nu

    for impermeable sphere whereas different dashed lines indicate Nu for permeable sphere

    of different K/d2values. Nu for solid sphere approaches to the asymptotic value of 2 with

    the decrease in Re. Nu increases with the increase in Re for all K/d2values. The increase

    in heat transfer coefficient with the increase in Re is due to the increase in velocity field

    inside the porous permeable sphere, which in turn increased the heat transfer rate. The

    increase in Nu with K/d2

    values for porous permeable sphere is significant for high

    Reynolds number. The heat transfer coefficient increases with the increase in K/d2value

    because of the lower resistance to flow offered by highly permeable sphere. At low

    Reynolds number, value of Nu for permeable sphere approaches to that for solid sphere.

    Present simulation result on Nu for porous permeable sphere is verified with the

    analytical solution given by Johnson and Smet (1984) at low Re (Table 1). They

    concluded that the Nu for porous permeable sphere is higher than that for solid sphere at

    low Pe ( = Re. Pr) of 0.015. On the other hand, Nu has weak dependence on permeability

    at a slightly higher Pe (say, 0.14) and hence heat transfer rate from permeable and solid

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    sphere is almost the same. It is seen in table 1 that the Nu for porous permeable sphere

    differs by 15 % from that for impermeable sphere at low Re and Pr. However, Nu for

    porous permeable sphere differs only by 0.09 % from that for impermeable sphere at low

    Re and high Pr. Further, at high Re, permeability has strong effect on Nu irrespective of

    the Prandtl number. Thus, Nu for porous permeable sphere is higher than that for solid

    sphere at high Reynolds number. The Nu increases with the increase in Pr for both

    permeable and impermeable sphere at high Re, whereas no significant increase in Nu is

    with the increase in Pr at low Re.

    Based on simulated results a correlation for heat transfer from porous permeable sphere is

    generated using non-linear regression analyses. The regression coefficient of 0.91 was

    obtained. The correlation for heat transfer from porous permeable sphere is given by,

    ( ) ( )1.13

    21

    23

    22

    1

    1PrRe7.32

    +=

    dKNu (15)

    valid for, 0.02 < Re < 2000, 0.7 < Pr < 7 and 10-5

    < K/d2< 10

    -2

    When predicting the Whitaker correlation (for solid sphere) using above equation (eq.

    15), an average error of 15 % was obtained at low Re with zero permeability value (K/d2

    = 0). This correlation can be extended for mass transfer from porous permeable sphere

    since the phenomena of mass transfer is analogous to heat transfer. In eq. (15), Nu and Prhave to be replaced by Sherwood number and Schimdt number. This would work fine for

    no change in size of porous permeable sphere due to mass transfer.

    CONCLUSION

    Heat transfer study on flow through and around a porous permeable sphere is investigated

    with the help of standard CFD software for wide ranges of Reynolds number and Prandtl

    number. Experimental data and Whitaker correlation (1972) for heat transfer from solid

    sphere are excellently predicted by present CFD simulation. The CFD simulation then

    extended for heat transfer from isothermal porous permeable sphere by considering mass,

    momentum and energy equations outside of the porous permeable sphere and Darcys

    law with Brinkmans extension inside the porous permeable sphere. Present simulated

    results show that the heat transfer rate increases with the increase in permeability. At low

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    Re, the Nu for a permeable sphere is higher than that for solid sphere when the Pr is low,

    whereas, for high Pr, permeability has only a weak effect on the Nu. At high Re, the Nu

    for permeable sphere is much higher than that for solid sphere irrespective Pr values. The

    correlation obtained from the CFD simulation data for heat transfer from porous

    permeable sphere is useful in predicting Nu for porous permeable sphere for a wide range

    of Re from 0.02 to 2000 and Pr from 0.7 to 7 at different permeability ratios.

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    Notation

    Cp specific heat of fluid, J kg-1

    K-1

    d diameter of sphere, m

    E total energy, N m

    h heat transfer coefficient, Wm-2

    K-1

    H enthalpy, N m

    Jj diffusion flux of species j, mole m-2

    s-1

    K permeability, m2

    K/d

    2

    permeability ratio, dimensionless

    Nu Nusselt number (= h D / ), dimensionless

    P pressure, N/m2

    Pe Peclet number (= Re. Pr), dimensionless

    Pr Prandtl number (= Cp/ ), dimensionless

    Prt turbulent Prandtl number, dimensionless

    q heat transfer rate, Watt

    Re Reynolds number (= d v / ), dimensionless

    Sh heat source term in eq. 1

    t time, s

    T temperature, K

    Ts sphere temperature, K

    T bulk temperature, K

    vi velocity component in xidirection

    vj velocity component in xjdirection

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    vl velocity component in xldirection

    v approaching velocity, m/s

    Greek letters

    thermal conductivity, W m-1K

    eff effective thermal conductivity, W m-1

    K

    viscosity of fluid, Pa s

    t turbulent viscosity of fluid, Pa s

    density of fluid, kg/m3

    eff Effective shear stress, N m-2

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    References

    Achenbach, E., in: Proceeding of the 6th

    international heat transfer conference on heat

    transfer from sphere up to Re = 6 x 106, Vol. 5, Hemisphere 1978 Washington DC.

    Acrivos, A., and T. D. Taylor, Heat and mass transfer from single sphere in stokes flow,

    J. Phys. Fluids, (1962) 5(4), 387-394.

    Bird R. B., Stewart E. W., Lightfoot N. E., Transport Phenomena, John Wiley and

    Sons 2002, India.

    FLUENT Users Guide, Fluent Inc., 1998.

    Hinze, J. O., Turbulence, McGraw-Hill, 1975 New york.

    Holman, J. P., Heat transfer, McGraw-Hill, 1986 New York.

    Jain, A. K., C. Sirker, and S. Basu, Studies on flow through and around a porous

    permeable sphere: I. Hydrodynamics (Submitted)

    Johnson, R. E., and R. P. Smet, On the heat transfer from a permeable sphere in stokes

    flow, Chem. Eng. Sci., (1984) 22(7) 947-958.

    McCabe L. W., and C. J. Smith, Unit operation of chemical engineering, 3rd

    edition,

    10

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    McGraw-Hill Kogakusha, Ltd, 1980, Japan.

    Ranz, W. E., and W. R. Marshall, Evaporation from drops, Chem. Eng. Prog., (1952) 48,

    141-146.

    Romkes, S. J. P., F. M. Dautzenberg, and C. M. van den Bleek, and H. P. A. Calis, CFD

    modeling and experimental validation of particle-to-fluid mass and heat transfer in a

    packed bed at very low channel to particle diameter ratio, Chem. Eng. J., (2003) 96, 3-13.

    Vasudeviah, M., and K. Balamurugan, Heat transfer from a porous sphere in a slow

    viscous flow, Int. J. Non-linear Mechanics, (1998) 33(1), 111-124.

    Whitaker S., Forced convection heat transfer correlations for flow in pipes, past flat

    plates, single cylinders, single spheres, and for flow in packed beds and tube bundles,

    AIChE J. (1972) 18 (2), 361-370.

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    Figure captions

    Fig. 1. Comparison of simulated results with Whitaker (1972) correlation and

    experimental results for heat transfer from impermeable sphere

    Fig. 2. Forced-convection heat transfer from a porous permeable sphere

    Table caption

    Table 1: Nusselt number values for flow through and around sphere at different Reynolds

    number

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    Fig. 1. Comparison of simulated results with Whitaker (1972) correlation

    and experimental results for heat transfer from a impermeale sphere

    Re

    0.01 0.1 1 10 100 1000 10000

    (Nu-2)/Pr

    0.4

    0.01

    0.1

    1

    10

    100

    Whitaker correlation

    (Nu-2)/Pr0.4

    =0.4Re0.5

    +0.06Re2/3

    Experimental

    Present simulation

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    Fig. 2. Forced-convection heat transfer from a porous permeable sphere

    Re Pr2/3

    0.001 0.01 0.1 1 10 100 1000 10000

    Nu

    1

    10

    100

    1000

    k/d2= 1e-2

    k/d2= 1e-3

    k/d2= 1e-4

    k/d2= 1.82e-5

    solid sphere

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    Table 1: Nusselt number values for flow through and around sphere at different Reynolds

    number

    PecletNumber(Pe=Re. Pr)

    Reynoldsnumber(Re)

    Prandtlnumber(Pr)

    Nu for permeablesphere(K/d

    2= 1e-2)

    Nu forimpermeablesphere

    (K/d2= 0)

    Variationbetween Nu forpermeable and

    impermeable

    sphere

    0.0149 0.02 0.7442 2.5371 2.2062 14.99 %

    0.1398 0.02 6.9909 2.2428 2.2408 0.09 %

    1488 2000 0.7442 265.7559 26.4973 902.95 %

    13980 2000 6.9909 2410.7440 69.6281 3361.32 %

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