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HAL Id: jpa-00247629

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Submitted on 1 Jan 1992

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Calculations of drag coefficients via hydrodynamic cellular automata

G. Kohring

To cite this version:

G. Kohring. Calculations of drag coefficients via hydrodynamic cellular automata. Journal de Physique

II, EDP Sciences, 1992, 2 (3), pp.265-269. �10.1051/jp2:1992130�. �jpa-00247629�

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J. Pbys. II France 2 (1992) 265-269 MARDI 1992, PAGE 2G5

Classification Physics Abstracts

05.50 07.55M

Short Communication

Calculations of drag coefficients via hydrodynamic

cellular automata

GA- Kohring

Institut fir Theoretische Phj'sik, Uni,~ersitit zu I16111, Zfilpicherst.rafle 77, D-5000 I161n 41, Germany

(RecHved 17 December 1991, accepted 13 January 1992)

Abstract The drag coefficient, CD, of an arbitrary shaped object ca;; be calculated by two- dimensional hydrodynamic cellular automata. Results spanning nearly four orders of magnitude

in the Reynolds number (0.I < Re < 10~) are presented for a simple, hexagonal object, and

good quantitative agreement with previous experiments on cylinders is obtained.

Hydrodynamical cellular automata (IIDCA), also called "lattice gases", are believed to re-

produce the physics described by the Navier-Stokes equations [1-6]. Many different researchers

have shown during the past few years how conventional hydrodynamic phenomena can be sim- ulated using HDCA [2-4] and they have identified important applications not easily studied by

conventional methods, such as the simulation of low Reynolds number flows in porous media [3, 7, 8]. More recently, Duarte and Brosa have suggested that HDCA may also be fruitfully applied to the problem of calculating drag coefficients for an obstacle in a viscous fluid [4].

Their initial simulations covered Reynolds numbers in the range 8 < Re < 80 and demon- strated good agreement with the experimental results of Wieselsberger [5]. In this paper, their application of the HDCA is put to a more stringent test, by simulating flows for which the

Reynolds number ranges over nearly four orders of magnitude. Indeed, to our knowledge, this is the largest range of Reynolds numbers ever investigated by IIDCA for a single application.

Such a large range of Reynolds numbers is not easily obtained within a single IIDCA model,

because each model has an intrinsic number, ll~(p) [6], which sets the scale for the usable

Reynolds number. With the following definition for ll~:

lL(P) + ~((~

,

(l)

where cs is the speed of sound in the HDCA, p is the particle density per site, g(p) is the lat-

tice anisotropy factor and v(p) + q/p is the kinematic viscosity, the Reynolds number is defined

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2fif' JOURNAL DE PIIYSIQUE11 N03

by:

Re +

'~°~°~*~~~

(2)

cs

where uo is the characteristic speed of the flow, and Lo is the characteristic length scale of the system. At fixed lL, the Reynolds number can only be changed by changing uo or to,

this however presents several problems. First, the length scale, to, is bounded from below by

the mean free path of the HDCA particles ii, 8]. Experience has shown that to should be

no smaller than about seven mean-free paths in order to get reasonable agreement with the

asymptotic (I.e., I/£o

~

0) results [8]. Second, the characteristic speed, uo, cannot be too large

since the maximum flow velocity of uo

=

I (in units where the lattice spacing and the time step are equal to unity) corresponds to pure streaming without any particle interactions. On the other hand, if uo is too small, then the velocity fluctuations become too large [9]. Again, experience has shown that a value of uo in the range [0.1, 0.3] provides a good compromise to

thesi problems [8, 9].

The Reynolds number can also be adjusted by varying R+(p). In fact, ll~(p) can be made arbitrarily small by simply taking p

~

0 [6], however, such small densities require excessively large lattices in order to obtain meaningful space averages. Theoretically, it is also possible to

get R+

=

0 by taking p near 3 where g(p)

=

0 [6], however, our simulations here have shown that this method does not yield results compatible with previous experiments. This problem

is most likely due to a breakdown of the Boltzmann approximation for large densities [6]. We therefore use different variants of HDCA to efficiently vary R+(p).

The HDCA models used for these simulations have all been discussed before II, 10]. The

I-bit, FIIP-II model was used to achieve very large Reynolds number flows, while the FIIP-I model was used for intermediate Reynolds numbers near unity. Very small Reynolds numbers

were achieved using a recently introduced momentum non-conserving model [10]. The simula- tions were performed on a 2-D channel, with a hexagonal obstacle placed in the center of the

channel. (Circles would have rather rough surfaces on a lattice and are known from earlier simulations [4] to have approximately the same drag coefficients.) In most of the simulations, the span of the object, to, was fixed at 20 il of the channel height, H, and kept larger than the 71 limit indicated above. This value of H also seemed to be large enough to avoid problems

associated with the objects wake reflecting off the channel walls and small enough to avoid excessive computational effort. The channel length, L, was varied between one and four times the channel height, I-e-, H < L < 4 x L, but the data showed no systematic variation as a

function of L. The average channel velocity used in our simulations varied between 0.I and

0.2, and since the system was initialized with a Poiseuille flow profile, this means that the maximum channel velocity Was never greater than about 0.3.

The drag coefficient, CD is defined by:

CD + ~

,

(3)

~2 ~

2~ °

where, F is the force acting on the object and A is the object's cross-sectional area perpen- dicular to the direction of flow [5]. For 2-D flow, the cross-sectional area is replaced by the

cross-sectional length, £o. The force acting on the object can be easily calculated within the

cellular automata approach as the sum of the momentum change over all particles which hit

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N°3 CALCULATIONS OF DRAG COEFFICIENTS VIA HDCA 267

the object at some time t [4]. Since we use no slip boundary conditions, such particles undergo

a momentum change which is simply equal to twice the momentum with which they hit the object.

Both~ the definitions of the drag coefficient and the Reynolds numbers are ambiguous with respect to the characteristic length and characteristic velocity. Following Wieselsberger [5]~

we define £o as the total span of the hexagon~ although some authors prefer to use the radius [4]. Furthermore~ we take uo as the average channel velocity~ whereas other authors would use the maximum channel velocity [4]. In a real experiment~ one would try to use a homogeneous

flow profile, however, this is not efficient in our simulations because the channel walls cannot be made arbitrarily wide without excessive computational effort. Since the average channel

velocity is 2/3 of the maximum velocity for a Poiseuille flow, the different definitions here would give at most a multiplicative adjustment to the results, but the qualitative results would be

unchanged.

A statement about the simulation time is also needed. For simple flows, such as Couette

flow, it can be shown that the relaxation time from a random initial condition is on the order of (see for example Lim in [2]) :

~l/2

"

~~(~)"

(~)

In our simulations, we do not use a random initial condition, rather we initialize the channel to

a Poiseuille profile. For Reynolds numbers outside the turbulent regime, the final flow should

only be a perturbation upon the Poiseuille flow and therefore one could expect a faster relax- ation to equilibrium than that suggested by equation (4). Indeed, we find that the relaxation to equilibrium from our starting state occurs approximately 100 times faster than estimated by

equation (4). Hence, we allow for equilibration a number of iterations equal to approximately

HL/(100~~v). After the system has come into equilibrium, a number of iterations equal to four times the relaxation time was typically used for making measurements, with measure-

ments taken every 100 time steps. However, for the FHP-I model at small Reynolds number,

many more measurement iterations were needed in order to compensate for the inefficiency of the algorithm. At our smallest Reynolds number for the FHP-I model 10~ iterations were

performed.

Finally, it should be mentioned that the programs used here have been discussed before

[iii, and, for the FHP-I model, it is within 2 percent of the optimal speed according to the criteria of Bagnoli [12] for scalar and vector machines. The only reason for not using Bagnoli's algorithm is that it is not well suited to the Connection Machine, CM-2, where the previous algorithms are faster and consume less memory.

The data is presented in figure I. The solid line in the figure represents the experimental

work of Wieselsberger for a cylinder in three dimensions. As can be seen, the three different models taken together yield results which are in good agreement with the experimental data

over four orders of magnitude. Now, of course one could have used the FHP-II model over the entire range of Re, but as explained above, this would have been extremely inefficient

computationally. The problem of attaining larger Reynolds numbers would seem to be only a problem of using a computer with larger memory. Although, we would like to note that much

higher values for the Reynolds number can be obtained if the obstacle is omitted and one works with flow through a free channel, in which case £o equals the channel width H. For this

situation we obtained Reynolds numbers up to Re m 6000, however, no significant deviations

from laminar Poiseuille flow were found.

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268 JOURNAL DE PHYSIQUE II N°3

10~

~

e

Re

Fig. I. CD as a function of Re. The squares are for the FHP-II model, the circles are for the

FHP-I model and the triangles are for the momentum non-conserving model. The solid line represents experimental data for a cylinder taken by Wieselsberger. It should be mentioned that the last data

point required approximately 100 hours on the 16,384 processor CM-2, or twice as much as the time needed for all of the other data combined.

At this point one could speculate about potential industrial applications of this method. For

problems like the flow around automobiles one needs to reach Reynolds numbers about two orders ofmagnitude larger than those reached here. Since this would require about 100~ times

as much memory and speed, such "real-world" applications would be in reach of the teraflops coinputers which have recently been announced by several commercial companies.

Acknowledgements.

would like to thank A. Aharony, D. Stauffer and J-A-M-S- Duarte for many useful and

encouraging comments related to this work. I would also like to thank the University of

Cologne's Computer Department for a grant of time on the NEC-SX3/11 as well as the IILIIZ for time on their Cray-YMP /832 and their CM-2/16. Finally, I would like to thank the SFB-341 for financial support of this project.

References

[ii Frisch U., Hasslacher B. and Pomeau Y., Phvs. Rev. Lett. 56 (1986) 1505;

Renet J.-P., H4non M., Frisch U. and d'Humibres D., Evrophvs. Lent. 7 (1988) 231.

[2] H6non M., Complex Svst. 1 (1987) 763;

Lim H-A-, Phys. Rev. A40 (1989) 968;

Kadanolf P., McNamara G.R. and Zanetti G., Phvs. Rev. A40 (1989) 4527.

[3] Chen S., Diemer K., Doolen G-D-, Eggert K., Fu C., Gutman S. and Travis B., in the "Pro-

ceedings of the NATO Advanced Workshop on Lattice Gas Methods for PDE'S", G-D- Doolen Ed., Physica D 47 (1991);

Cancelliere A., Chang C., Foti E., Rothman D. and Succi S., Phvs. Fluids A2 (1990) 2085;

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N°3 CALCULATIONS OF DRAG COEFFICIENTS VIA HDCA 269

Kohring G.A., in proceedings of the "Seminar I Petroleumsfysikk" Stavanger, Norway (August 1991) to be published.

[4] Duarte J-A-M-S- and Brosa U., J. Stat. Phvs. 59 (1990) 501.

[5] see page is of Schlichting H., Grenzschicht-Theorie (Verlag G. Braun, Karlsruhe, 1951).

[6]Frisch U., d'Humibres D., Hasslacher B., Lallemand P., Pomeau Y. and Rivet J.-P., Complex Svst. 1 (1987) 649.

[7] Rothman D.H., Geophysics 53 (1988) 509.

[8] Kohring G-A-, J. Phvs. II France,1 (1991) 593.

[9] Brosa U., J. Phys. France 51(1990) lost;

Brosa U., C. Kfittner and Werner U., J. Stat. Phvs. 60 (1990) 875.

[10] Kohring, G.A. J. Stat. Phys. 66 (1992).

[iii Kohring G-A-, Int. J. Mod. Phvs. C 2 (1991) 755.

[12] Bagnoli F., Inn. J. Mod. Phvs. C (in press).

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