a Use of a fictitious Marangoni number for natural simulation

Francisco J. Arias∗ and Geoffrey T. Parks Department of Engineering, University of Cambridge Trumpington Street, Cambridge, CB2 1PZ, United Kingdom

In this paper, a method based on the use of a fictitious Marangoni number is proposed for the simulation of natural thermocapillary convection as an alternative to the traditional effective diffusivity approach. The fundamental difference between these two methods is that the new method adopts convective mass flows in simulating natural convection. Heat transfer in the natural convection simulation is calculated through the mass transport. Therefore, empirical Nusselt num- bers correlations required in the effective diffusivity method are eliminated. This represents a clear advantage in the context of design studies where flexibility in varying the geometry unconstrained by the availability of appropriate correlations is highly desirable. The new method is demonstrated using a simple geometrical model. An analytical expression of the fictitious Marangoni number associated with convection between vertical plates is derived and a computational fluid dynamics (CFD) simulation is performed to study the efficacy of the proposed method. The results show that the new method can approximate real natural convection quite accurately and can be used to simulate the convective flow in complex, obstructed or finned structures where the specific Nusselt correlation is not known.

aKeywords. Natural convection, Effective thermal conductivity, Marangoni convection, Compu- tational (CFD)

I. INTRODUCTION ship for the specific geometry, such as finned structures; however, these correlations are often not available. This Natural convection in enclosed cavities is of great im- then motivates us to find an alternative approach that portance in many engineering and scientific applications does not require knowledge of correla- such as energy transfer, boilers, nuclear reactor systems, tions. energy storage devices, etc. In the design of such systems In this paper, an alternative approach is proposed for numerical simulation using computational fluid dynamics natural convection simulations in which the momentum (CFD) and experimental testing of prototypes are exten- equation is modified and then the mass flow represented sively used. However, these methods are not well suited by using a fictitious Marangoni term in the stress ten- to activities such as parametric analysis due to their time- sor inducing thermocapillary currents. The heat trans- consuming nature and high cost [1]. fer is then the result of this mass flow. In the next Natural convection analysis often involves complex section the theoretical background behind the proposed simulations. Such simulations entail a set of relaxation approach will be presented. Although prior knowledge factors to converge and no easy way to find the relax- of Marangoni convection is not essential to understand ation factors except through continuous trials demanding the material presented in the next section, the interested significant computational resources. This frequently dis- reader is referred to the text by Kuhlmann and Rath suades thermal analysts and designers from attempting [4] for further information about fundamental Marangoni 3D simulations. In order to overcome this problem, the theory and to recent research outputs [5–14] and the book traditional approach is to use an effective diffusivity term by Lappa [15] to obtain an overview of thermal convec- (effective thermal conductivity) to convert effects of con- tion and the state of the art. vection into pure conduction [2, 3]. The fluid within an enclosure behaves like a fluid the thermal conductivity κ of which is modified by an effective thermal conductivity II. THEORETICAL BACKGROUND κeff as κeff = κ · Nu, with the Nusselt number Nu being determined by an appropriate correlation. This provides A. The fictitious Marangoni approach (FMA) a challenge to engineers when they are designing a com- plex or novel system. The engineers must have knowledge of the appropriate Nusselt number correlation relation- Let us start by considering the Navier-Stokes equation, which has, in presence of a gravitational field, the follow- ing tensorial form   ∗Corresponding author: Tel.: +32 14 33 21 94; Electronic address: ∂vi ∂vi 1 ∂p ∂ 0 + vk = − + {σik} + gi (1) [email protected] ∂t ∂xk ρ ∂xi ∂xk 2

0 where v is the velocity, p is the static pressure, σik is the or, considering the velocity profile between the parallel viscous stress tension (described below), and gi is the plates [17], gravitational body force per unit volume. The viscous stress tensor is given by dp ηw = −12 3 (8) dxi loss ρs  ∂v ∂v 2 ∂v  σ0 = η i + k − δ l (2) ik ∂x ∂x 3 ik ∂x where w is the mass flow rate per unit of width. k i l For natural convection flow, this flow resistance is bal- where η is the dynamic viscosity and δik is the Kronecker anced by the buoyant potential [17] given by delta. dp Now let us derive the equation describing the natural = −ρβdT gi (9) convection. For the sake of simplicity, we will assume the dxi buoy fluid is incompressible. This assumption implies that the Equating the dp/dx terms in Eq. (8) and Eq. (9) we variation of density due to variation in pressure may be i obtain the well-known solution given by Bar-Cohen and neglected. We can express the variations in temperature, Rohsenow [18] for the mass flow rate per unit width in density and pressure as functions of small variations dT , the channel: dρ and dp, respectively. This is the well-known Boussi- nesq approximation (for buoyancy). Introducing this into ρ2g βs3dT w = i (10) the Navier-Stokes equation (Eq. (1)), results in the fol- 12η lowing expression [16]: As mentioned, we want to find an appropriate ficti-   ∂vi ∂vi 1 ∂dp ∂ 0 tious surface-tension gradient ∂γ/∂xi. In this case, using + vk = − + {σik} − βdT gi (3) ∂t ∂xk ρ ∂xi ∂xk Eqs. (5) and (7), we can write the stress tensor as  ∂v  ∂γ∗ where, with our assumption that the fluid is incompress- σ0 = η i = (11) ik ∂x ∂x ible, i.e. div · u = 0, the stress tensor is simplified as k xk=0 i   0 ∂vi ∂vk where ∂γ∗/∂xi is the fictitious surface-tension gradient σik = η + (4) ∂xk ∂xi associated with the wall. Taking into account Eqs. (6), (9) and (11) we find that Let us now consider the situation of a boundary con- the fictitious surface-tension gradient must be given by dition that must be satisfied at the boundary between ∂γ∗ ρβg sdT the fluid and the walls, when surface-tension forces are = i (12) taken into account. If we assume that the surface-tension ∂xi 2 coefficient γ is not constant over the surface (in our case Given that because of temperature variation), then a force tangen- tial to the surface is developed ∂γ , and the stress tensor ∂γ∗ ∂γ∗ ∂xi = ∂sT (13) then becomes ∂xi ∂Ts

 ∂v ∂v  ∂γ where ∂sT = ∂Ts/∂xi and the subscript s means that σ0 = η i + k + (5) ik ∂x ∂x ∂x the temperature is evaluated at the wall, Eqs. (12) and k i i (13) can be combined to give Now, our objective in this paper is to define a ficti-   ∂γ∗ ρβgis dT tious surface-tension gradient, ∂γ/∂xi, which emulates = (14) ∂T 2 ∂ T the buoyancy potential, βdT gi. Although there are sev- s s eral ways in which to do this, perhaps the following anal- Using the definitions of the Ras and ogy is easiest in applying this approach to cases involving the Marangoni number Ma: plates and finned structures. In laminar, fully developed, two-dimensional (2D) flow ρβg s3 Ra = i dT (15) between parallel plates (see Fig. 1), the pressure drop is s ηα given by [16]

dp σ0 ∂γ∗ hdT = −2 ik (6) Ma = − (16) ∂Ts ηα dxi loss s where α is the thermal diffusivity and h is a characteristic where s is the distance between the plates and the stress length, here the length of the channel, Eq. (14) can then tensor is given by be rewritten as   ∂vi C ∂ T  σ0 = η (7) Ma = 1 f Ra (17) ik ∂x s k xk=0 2 ∂sT 3

Combining Eq. (19) with Eq. (14) then yields 2 ∂γ∗ ρβgis ≈ C1 (20) ∂Ts 2 All parameters in this equation are known once the geom- etry is specified. This then enables natural convection to be simulated without knowledge of the appropriate Nus- selt number correlation.

B. The effective diffusivity approach (EDA)

In the previous section we propose a new approach for natural convection simulation based on the introduction of a “fictitious” Marangoni term in the stress tensor in the momentum equations. In this proposed approach heat transfer will be obtained as a result of the induced mass flow. In contrast, the problem of computational natural con- FIG. 1: Simulated cavity model with a bottom wall temper- vection simulation is often these days tackled from a to- ature of Th, a top wall temperature of Tc and adiabatic side tally different point of view using more traditional ap- walls. proaches. Instead of modifying the momentum equations (and then considering mass transport) it is the energy equation that is modified. There are several approaches where ∂f T = dT/h is the linear average fluid temperature to representing the effects of convection by modifying gradient and C1 is a geometry-dependent constant. the energy equation: for example, by introducing em- Eq. (17) presents a relationship between the fictitious pirical velocities into the convection terms in the energy Marangoni number and the Rayleigh number. The dif- equation [19]. However, undoubtedly the most commonly ference between these two dimensionless numbers relates used approach of this kind is the so-called effective diffu- to mechanism by which natural convection is initiated. sive approach, so it is worth providing a brief outline of The Marangoni number is associated with natural con- that model here. vection caused by a surface temperature gradient ∇sT Let us consider the energy equation, and for the sake via mass transfer while the Rayleigh number is associated of illustration, let us assume, as before, laminar flow in with natural convection caused by buoyancy-driven flow. the liquid where no external sources are present. The This equation provides an important result. The Nusselt energy equation is given by number correlation, which is required in the traditional ∂T ∂T 1 ∂  ∂T  effective diffusive approach, is no longer required. It can cp + vi = κ (21) ∂t ∂xi ρ ∂xi ∂xi be replaced by a ratio ∇f T/∇sT that is determined by the specific geometry. where cp is the specific heat capacity of the fluid. The ∂T convective term in the above equation (vi ) makes it For the sake of generality, the relationship between the ∂xi fictitious Marangoni number and the Rayleigh number difficult to solve computationally, so it is modeled as an can be expressed through a simple polytropic equation: effective diffusive term as [20]   n ∂T 1 ∂ ∂T Ma = C1Ra (18) vi = − D (22) ∂xi ρ ∂xi ∂xi where C1 and n are constants. Based on Eq. (17), n where would be expected to be close to 1. The value of C 1 D = κCRaa (23) depends on the specified geometry. If the surface temperature gradient ∇sT is assumed to or be proportional to the thermal gradient of the fluid then: D = κNu (24) dT In this way, it is possible to eliminate the non-linear con- ∂ T ≈ C (19) s 1 s vective term in the energy equation (Eq. (21)), represent- ing the energy equation for a simple purely conductive In the Appendix a simple application for a finned geom- system [21] etry is presented, for which the existence of a simple lin- ∂T 1 ∂  ∂T  ear relationship between the surface temperature gradi- c = κ (25) p ∂t ρ ∂x eff ∂x ent ∇sT and the thermal gradient can be demonstrated. i i 4

5

10 8.0x10

Natural convection simulation ) 2

Using a Fictitious Marangoni number (FMA)

9 Effective Thermal Diffusivity Approach (EDA)

8 5

6.0x10

7 Nu

6

5

4.0x10

5

4

Natural convection simulation

5

2.0x10

Fictitious Marangoni Approach. (FMA)

3

Effective Therm al Diffusivity Approach (EDA) Nusseltnumber,

2

0.0

1 Total surface heat flux at hot plate,hot(W/m surfaceTotal heat at flux

0

5 6 6 6 6 6 5 6 6 6 6 6

0.0 0.0 5.0x10 1.0x10 1.5x10 2.0x10 2.5x10 3.0x10 5.0x10 1.0x10 1.5x10 2.0x10 2.5x10 3.0x10

Rayleigh number, Ra Rayleigh number, Ra

s s

FIG. 2: Comparison of the Nusselt number predictions. FIG. 3: Comparison of the total surface heat flux predictions.

III. RESULTS AND DISCUSSION C. FMA versus EDA In order to demonstrate the efficacy of the proposed FMA method, a computational fluid dynamics (CFD) In the previous section, two different alternative ap- analysis using FLUENT-6.3r was performed on a sim- proaches for natural convection simulation were de- ple cavity model (see Fig. 1) consisting of a square box scribed. The first, proposed in this paper, is through with a hot bottom wall, a cold top wall and adiabatic side the modification of the momentum equations by the in- walls. Gravity acted downwards. The values of physi- troduction of a fictitious Marangoni stress (Eq. (20)), an cal properties and operating conditions (e.g. the gravi- approach that we have called the fictitious Marangoni tational acceleration) were adjusted according to the de- approach or FMA. The second is the traditional effective sired Rayleigh number [22]. In this study, the values 3 diffusivity approach or EDA, in which the energy equa- were chosen as: ρ = 1000 kg/m , cp = 11.030 kJ/kgK, −3 −5 tion is modified by replacing the convective term by an κ = 15.309 W/mK, η = 10 kg/ms, β = 10 , −5 2 effective diffusive term (Eq. (22)). gi = 6.96 × 10 m/s , h = l = s = 1 m. The case was set with a pressure-based, segregated, As will be apparent to the reader, the FMA approach steady solver with Green-Gauss cell-based gradient treat- offers a powerful tool for systems where, because the ment. The Semi-Implicit Method for Pressure Linked Nusselt number is not known, it is not possible to de- Equations (SIMPLE) algorithm was selected for the fine an effective thermal diffusivity (thermal conductiv- pressure-velocity coupling with relaxation factors of 0.3 ity), i.e. to apply the EDA directly. Such a situation fre- for pressure, 0.7 for momentum and 1 for energy as quently arises in the simulation of complex designs with the defaults. The pressure was discretized with a dramatic variations in geometry (e.g. in the microelec- standard Rhie-Chow discretisation scheme [23] and and tronics field) where there is no available Nusselt number Quadratic Upstream Interpolation for Convective Kine- correlation for the specific system available in handbooks matics (QUICK) was chosen as the advection scheme for or the literature, thus forcing thermal engineers adopting momentum and energy discretization. The convergence the EDA to use the Nusselt number correlation for the criteria were set for absolute residuals below 1 × 10−7 for most similar geometry available. If this is not a good all the variables in all cases and the overall imbalance in approximation, poor results are inevitable. the domain was less than 1% for all variables, then con- vergence of the solution was checked at each time step Thus the FMA can be used either as a method for the by using the scaled residuals. The mesh resolution inde- simulation of natural convection, or at least as a tool for pendence was checked running an initial mesh and en- pre-screening and obtaining an estimate of the Nusselt suring that the convergency criteria of RMS of 10−7, and number, which can then be used in applying the EDA. In an imbalance in the domain was less than 1%, then, a the next section, we will examine a numerical comparison second simulation was performed using a second mesh between these models. with finer cells throughout the domain, then the sim- 5 ulation was run until the convergency criteria and im- balance in the domain were satisfied. The criteria for selection of the mesh was that the temperature values for two consecutive stimulations were less than a 1%, then the mesh at the previous step was considered ac- curate enough to capture the result. Finally, time step independence was achieved using time-steps of 0.5 s. The temperature difference between the top and bottom walls was set based on Rayleigh numbers of Ra = 3.28 × 104, 6.55 × 105, 1.31 × 106, 1.97 × 106 and 2.62 × 106. Simula- tions were performed at each Rayleigh number for three cases: 1) a real natural convection simulation; 2) using the proposed FMA; and 3) using the traditional EDA. For the FMA cases, the gravitational acceleration was set to zero and Eq. (20) was used for the effective surface tension gradient with the best fit using C1 = 0.06 and −8 ∂γ∗/∂Ts = 1.2 × 10 N/mK. For the EDA cases, the effective thermal diffusivity was calculated using

κeff = κNu (26) FIG. 4: Temperature distribution calculated using the pro- where the Nusselt number was calculated from [21] posed FMA-based method.

1 4 Nu = 0.27Ras (27)

Figs. 2 and 3 show comparisons between the Nusselt numbers and the total heat fluxes at various channel Rayleigh numbers for the three cases. It is found that the proposed FMA-based method can track the real nat- ural convection simulation far better than the traditional EDA-based method. Figs. 4–6 further demonstrate the advantage of the pro- posed FMA-based method via comparison of the tem- perature distributions obtained for the convection simu- lations. It is obvious that the temperature distribution obtained using the FMA agrees much better with the real natural convection CFD simulation than that given by the EDA-based method. The advantage of the proposed FMA method is due its use of mass transfer. The FMA method emulates the con- vective flow via mass transport which is associated with the momentum balance. This method can easily take into consideration the effect on mass transfer of the real ge- ometry of the system. It provides a powerful tool for the FIG. 5: Temperature distribution of the real natural convec- simulation of 2D natural convection in complex geome- tion CFD simulation. tries such as finned structures, obstruction-type struc- tures and generally dramatically varying geometries for which the Nusselt number correlation is unknown. In precisely what we are trying to calculate. So, if we in- contrast, the EDA method relies on knowledge of the troduce a geometrical variation and re-launch the same Nusselt number correlation which can vary significantly calculations, the weakness of the EDA is exposed and with subtle changes in geometry. In particular, when the the difference between it and the proposed FMA is made real geometry has unusual shapes or variations from stan- manifestly clear. dard shapes, it is hard to find an accurate Nusselt number To illustrate, let us consider the case of the cavity correlation in the literature for the specific geometry. model shown in Fig. 1 where now the flow is obstructed As mentioned before, there is a certain trick behind by a sphere of radius 0.5 m located at the center of the the apparently good results given through the use of the cavity. The calculated results for the total surface heat EDA depicted in Fig. 3, a trick that is also a weakness. flux in this new scenario are shown in Fig. 7. It is clear The good results are basically due to the introduction that the effect on the natural convection of the modi- of the Nusselt number correlation, but in a way that is fication to the system geometry can be easily and well 6

5

8.0x10 ) 2

Natural convection simulation

Using a Fictitious Marangoni number (FMA)

Effective Thermal Diffusivity Approach (EDA)

5

6.0x10

5

4.0x10

5

2.0x10

0.0 Total surface heat flux at hot plate,hot(W/m surfaceTotal heat at flux

5 6 6 6 6 6

0.0 5.0x10 1.0x10 1.5x10 2.0x10 2.5x10 3.0x10

Rayleigh number, Ra

s

FIG. 6: Temperature distribution calculated using the tradi- FIG. 7: Comparison of the total surface heat flux predictions tional EDA-based method. for the case of a cavity with a sphere of radius 0.5 m at its center. captured by the FMA method. However, the results ob- tained from the EDA method are unchanged (and there- approach which requires knowledge of the Nusselt fore now very inaccurate) if the same Nusselt number number correlations associated with different ge- correlation as before is used (as has been done here). ometries. The new method is especially suitable If a more appropriate Nusselt number correlation is for application to complex geometries. known then, of course, it can be used with the EDA method instead and improved results will follow, but • A further advantage of the proposed fictitious such an adjustment is only possible if the new correla- Marangoni number method is the possibility that it tion is known. Restricting the thermal engineer/designer can be applied not just to steady-state convection to the consideration of geometries for which correlations simulation but also to transient cases where the sur- are already known will severely limit the range of system face temperature profile follows the bulk tempera- designs can that be analysed and may well exclude the ture profile of the fluid and thus the relationship optimal geometry for the application in question. between these used in the definition of the ficti- tious Marangoni number is maintained during the transient. Such a relationship may hold (to a good IV. CONCLUSIONS approximation) in many transient cases where no abrupt changes take place. Additional research is A fictitious Marangoni number method has been pro- required to investigate the applications and limita- posed and demonstrated for 2D natural convection sim- tions of this novel approach in simulating natural ulation. It was shown that the proposed method is much convection transients. superior to the traditional effective thermal diffusivity approach often used in 1D or 2D modeling of natural convection. The key conclusions are: V. APPENDIX

• The proposed fictitious Marangoni number method A. Finned geometries can realistically simulate convective flow via mass transport and does not rely on prior knowledge of any empirical Nusselt number correlations. It can In the main body of the paper, for the sake of illustra- model the real natural convection flow field accu- tion, it was assumed that there was a simple linear rela- rately. tionship between the surface temperature gradient ∂sT and the thermal gradient in the fluid ∂f T (see Eq. (19)). • The proposed fictitious Marangoni number method Although the specific relationship between ∂sT and ∂f T can easily incorporate the effects of the system ge- will depend on the specified geometry, we demonstrate ometry (and changes to that geometry) on natural here in a more rigorous way that for finned geometries convection simulation. It eliminates the disadvan- a linear approximation is good enough for preliminary tage of the traditional effective thermal diffusivity calculations. 7

Differentiating Eq. (30), the surface temperature gra- dient along the fin is sinh(m(l − z)) ∂ T = −[T − T ]m · (32) s 0 a cosh(ml)

The fin efficiency ηfin is defined as the ratio of the heat transferred to that transferred for an infinitely long fin of the same cross-section. For this kind of fin ηfin is given by [21]

ηfin = tanh(ml) (33) Thus, in practice, a fin length that corresponds to ml ≈ 1 will transfer 76.2% of the heat that can be transferred by an infinitely long fin, and offers a good compromise between heat transfer performance and fin size [21]. So, assuming ml = 1, Eq. (32) becomes ∆T  z  ∂sT = −0.648 sinh 1 − (34) FIG. 8: Detail of the straight rectangular fin studied. l l z where ∆T = T0 − Ta. The function f(z) = sinh(1 − l ) is integrable on [0, l]. This an average value f(z) for z in Let us consider, as an example, the straight rectangu- the interval [0, l] may be defined by: lar fin depicted in Fig. 8. Assuming that the Marangoni stress will act on all the available walls, then from mo- 1 Z l  z  mentum balance considerations f(z) = sinh 1 − dz = 0.543 (35) l 0 l (2hl + sh)σ0 = −ρβg ∆T (hsl) (28) ik i Incorporating this value into Eq. (34) yields where ∆T = Th − Tc. The fictitious surface tension gra- ∆T dient then gives ∂ T ≈ −0.352 (36) s l ∂γ∗  ls  ρβg dT = i (29) Inserting Eq. (36) into Eq. (29), we have for our ficti- ∂Ts 2l + s ∂Ts tious surface gradient

The only unknown parameter in Eq. (29) is the surface ∂γ∗  l2s  temperature gradient ∂T which can be calculated from = 2.85C1 ρβgi (37) s ∂Ts 2l + s the following considerations. The temperature distribu- tion profile along the length of a fin of finite length l with where a constant C1 has been introduced to take into an insulated end can be expressed as [24] account the error introduced by the use of an average value from Eq. (34). cosh(m(l − z)) T (z) − T = [T − T ] (30) a 0 a cosh(ml) NOMENCLATURE where T0 is the temperature at the base of the fin and Ta Ac = fin base-area is the ambient temperature, and C1 = constant cp = specific heat capacity rh P D = diffusion coefficient m = f (31) gi = gravitational acceleration κAc h = channel or plate length where hf is the heat transfer coefficient along the fin, P is hf = heat transfer coefficient the perimeter of the fin and Ac is its base-area. Although l = plate width or fin length Eq. (30) is valid for a fin of finite length with an insulated m = fin temperature profile parameter end and in general the end of a fin is not insulated, this Ma = Marangoni number is a good approximation if the heat transfer from the end n = exponent of the fin is negligible in comparison to the heat transfer Nu = Nusselt number from the surface of the fin, a common situation since P = fin perimeter the area of the end of a fin is frequently negligible in Ra = Rayleigh number comparison to the total exposed surface area [24]. s = plate spacing 8

T = temperature v = velocity Subscripts w = mass flow per unit width a = ambient value z = length coordinate c = cold eff = effective value Greek symbols f = fluid α = thermal diffusivity h = hot β = thermal expansion coefficient i, j, k = coordinate directions γ∗ = fictitious surface tension s = surface κ = thermal conductivity ρ = density σ = surface tension η = dynamic viscosity REFERENCES ηfin = fin efficiency

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