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SHADOWGRAPH STUDY OF GRADIENT DRIVEN FLUCTUATIONS Gennady Nikolaenko and David S. Cannell Department of Physics UC Santa Barbara Santa Barbara, CA 93106 ABSTRACT A fluid or fluid mixture, subjected to a vertical temperature and/or concentration gradient in a gravitational field, exhibits greatly enhanced light scattering at small angles [1-3]. This effect is caused by coupling between the vertical velocity fluctuations due to thermal energy and the vertically varying refractive index. Physically, small upward or downward moving regions will be displaced into fluid having a refractive index different from that of the moving region, thus giving rise to the enhanced scattering [4]. The scattered intensity is predicted [5-7] to vary with scattering wave vector q, as q-4, for sufficiently large q, but the divergence is quenched by gravity [8] at small q. In the absence of gravity, the long wavelength fluctuations responsible for the enhanced scattering are predicted to grow until limited by the sample dimensions [9, 10]. It is thus of interest to measure the mean-squared amplitude of such fluctuations in the microgravity environment for comparison with existing theory and ground based measurements. The relevant wave vectors are extremely small, making traditional low-angle light scattering difficult or impossible because of stray elastically scattered light generated by optical surfaces. An alternative technique is offered by the shadowgraph method, which is normally used to visualize fluid flows, but which can also serve as a quantitative tool to measure fluctuations [11, 12]. A somewhat novel shadowgraph apparatus and the necessary data analysis methods will be described. The apparatus uses a spatially coherent, but temporally incoherent, light source consisting of a super-luminescent diode coupled to a single-mode optical fiber in order to achieve extremely high spatial resolution, while avoiding effects caused by interference of light reflected from the various optical surfaces that are present when using laser sources. Results obtained for a critical mixture of aniline and cyclohexane subjected to a vertical temperature gradient will be presented. The sample was confined between two horizontal parallel sapphire plates with a vertical spacing of 1 mm. The temperatures of the sapphire plates were controlled by independent circulating water loops that used Peltier devices to add or remove heat from the room air as required. For a mixture with a temperature gradient, two effects are involved in generating the vertical refractive index gradient, namely thermal expansion and the Soret effect, which generates a concentration gradient in response to the applied temperature gradient. For the aniline/cyclohexane system, the denser component (aniline) migrates toward the colder surface. Consequently, when heating from above, both effects result in the sample density decreasing with altitude and are stabilizing in the sense that no convective motion occurs regardless of the magnitude of the applied temperature gradient. The Soret effect is strong near a binary liquid critical point, and thus the dominant effect is due to the induced concentration gradient. The results clearly show the divergence at low q and the predicted gravitational quenching. Results obtained for different applied temperature gradients at varying temperature differences from the critical temperature, clearly demonstrate the predicted divergence of the thermal diffusion ratio. NASA/CP--2002-211212/VOL 1 325
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Shadowgraph Study of Gradient Driven Fluctuations

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Page 1: Shadowgraph Study of Gradient Driven Fluctuations

SHADOWGRAPH STUDY OF GRADIENT DRIVEN FLUCTUATIONS

Gennady Nikolaenko and David S. Cannell

Department of Physics

UC Santa Barbara

Santa Barbara, CA 93106

ABSTRACT

A fluid or fluid mixture, subjected to a vertical temperature and/or concentration gradient

in a gravitational field, exhibits greatly enhanced light scattering at small angles [1-3]. This effect

is caused by coupling between the vertical velocity fluctuations due to thermal energy and the

vertically varying refractive index. Physically, small upward or downward moving regions will

be displaced into fluid having a refractive index different from that of the moving region, thus

giving rise to the enhanced scattering [4]. The scattered intensity is predicted [5-7] to vary with

scattering wave vector q, as q-4, for sufficiently large q, but the divergence is quenched by

gravity [8] at small q. In the absence of gravity, the long wavelength fluctuations responsible for

the enhanced scattering are predicted to grow until limited by the sample dimensions [9, 10]. It

is thus of interest to measure the mean-squared amplitude of such fluctuations in the

microgravity environment for comparison with existing theory and ground based measurements.The relevant wave vectors are extremely small, making traditional low-angle light

scattering difficult or impossible because of stray elastically scattered light generated by optical

surfaces. An alternative technique is offered by the shadowgraph method, which is normally

used to visualize fluid flows, but which can also serve as a quantitative tool to measure

fluctuations [11, 12]. A somewhat novel shadowgraph apparatus and the necessary data analysis

methods will be described. The apparatus uses a spatially coherent, but temporally incoherent,

light source consisting of a super-luminescent diode coupled to a single-mode optical fiber in

order to achieve extremely high spatial resolution, while avoiding effects caused by interference

of light reflected from the various optical surfaces that are present when using laser sources.Results obtained for a critical mixture of aniline and cyclohexane subjected to a vertical

temperature gradient will be presented. The sample was confined between two horizontal

parallel sapphire plates with a vertical spacing of 1 mm. The temperatures of the sapphire plates

were controlled by independent circulating water loops that used Peltier devices to add or remove

heat from the room air as required.

For a mixture with a temperature gradient, two effects are involved in generating the

vertical refractive index gradient, namely thermal expansion and the Soret effect, which

generates a concentration gradient in response to the applied temperature gradient. For the

aniline/cyclohexane system, the denser component (aniline) migrates toward the colder surface.

Consequently, when heating from above, both effects result in the sample density decreasing with

altitude and are stabilizing in the sense that no convective motion occurs regardless of the

magnitude of the applied temperature gradient. The Soret effect is strong near a binary liquid

critical point, and thus the dominant effect is due to the induced concentration gradient. The

results clearly show the divergence at low q and the predicted gravitational quenching. Results

obtained for different applied temperature gradients at varying temperature differences from the

critical temperature, clearly demonstrate the predicted divergence of the thermal diffusion ratio.

NASA/CP--2002-211212/VOL 1 325

Page 2: Shadowgraph Study of Gradient Driven Fluctuations

Thus, the more closely the critical point is approached, the smaller becomes the temperature

gradient required to generate the same signal.

Two different methods have been used to generate pure concentration gradients. In the

first, a sample cell was filled with a single fluid, ethylene glycol, and a denser miscible fluid,

water, was added from below thus establishing a sharp interface to begin the experiment. As

time went on the two fluids diffused into each other, and large amplitude fluctuations were

clearly observed at low q. The effects of gravitational quenching were also evident. In the

second method, the aniline/cyclohexane sample was used, and after applying a vertical

temperature gradient for several hours, the top and bottom temperatures were set equal and the

thermal gradient died on a time scale of seconds, leaving the Soret induced concentration

gradient in place. Again, large-scale fluctuations were observed and died away slowly in

amplitude as diffusion destroyed the initial concentration gradient.

I. B. M. Law, R. W. Gammon, and J. V. Sengers, Light-scattering observations of long-

range correlations in a nonequilibrium liquid, Phys. Rev. Lett. 60, 1554 (1988).

2. P.N. Segr6, R. W. Gammon, J. V. Sengers, and B. M. Law, Rayleigh scattering in a liquid

far from thermal equilibrium, Phys. Rev. A 45, 714 (1992).

3. A. Vailati and M. Giglio, Giant fluctuations in a free diffusion process, Nature (London)

390, 262 (1997).

4. D.A. Weitz, Diffusion in a Different Direction, Nature, 390, 233 (1997).

5. T. R. Kirkpatrick, E. G. D. Cohen, and J. R. Dorfman, Light scattering by a fluid in a

nonequilibrium steady state. II. Large gradients, Phys. Rev. A 26, 995 (1982).6. R. Schmitz and E. G. D. Cohen, Fluctuations in a fluid under a stationary heat flux. II

Slow part of the correlation matrix, J. Stat. Phys. 40, 431 (1985).

7. P.N. Segr6 and J. V. Sengers, Nonequilibrium fluctuations in liquid mixtures under the

influence of gravity, Physica A 198, 46 (1993).

8. A. Vailati and M. Giglio, q divergence of nonequilibrium fluctuations and its gravity-

induced frustration in a temperature stressed liquid mixture, Phys. Rev. Lett. 77, 1484

(1996).

9. J. M. Ortiz de Zarate, R. Perez Cordon, and J. V. Sengers, Finite-size effects on

fluctuations in a fluid out of thermal equilibrium, Physica A 291, 113 (2001).

10. J. M. Ortiz de Z_ate and J. V. Sengers, Boundary effects on the nonequilibrium structure

factor of fluids below the Rayleigh-BEnard instability, Preprint November, 2001.

11. M. Wu, G. Ahlers, and D. S. Cannell, Thermally induced fluctuations below the onset of

Rayleigh-B_nard convection, Phys. Rev. Lett. 75, 1743 (1995).

12. S. P. Trainoff and D. S. Cannell, Physical Optics Treatment of the Shadowgraph, Physics

of Fluids, 14, 1340 (2002).

NASA/CP--2002-211212/VOL I 326

Page 3: Shadowgraph Study of Gradient Driven Fluctuations

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Page 4: Shadowgraph Study of Gradient Driven Fluctuations

Basic Physics:

G(R, r) - < dp(R, r)dp(O,O) >

S(q, co)- FT[G(R,r)]

Normally short ranged and decays

quickly, except near Critical Points

sed b "tT I " eft t " uppres ', "'_' "

NASAJCP--2002-2112 i 2/VOL ! 328

Page 5: Shadowgraph Study of Gradient Driven Fluctuations

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Page 6: Shadowgraph Study of Gradient Driven Fluctuations

i̧ i: i

<,

Short wavelength fluctuations are

suppressed by viscosity and

therlnal diffusion.

r = 1/(D v q2), 1/(v q2)

q = 2a/A

¢,

Quel_ched by gravity°

NASA/CP--2002-211212/VOL 1 330

Page 7: Shadowgraph Study of Gradient Driven Fluctuations

1

0.1

0.01

0.001

0.0001

g-O

\k\

J .... iI I i | I i i i i I I i i

0.1 0.2 0.5 1 2 5 10

q/qx

" rThe structure tacto S(q), predicted

for a bulk fluid subjected to a

the_ ma _rad_ent.

NAS A/CP--2002-211212/VOL 1 331

Page 8: Shadowgraph Study of Gradient Driven Fluctuations

Fused Silica

Cross section of the sample

cell used to impose controlled

thermal gradients on fluid.s.

__mall angle scattering ?

[n te vl:ero m etrv ?

NASA/CP--2002-211212/VOL i 332

Page 9: Shadowgraph Study of Gradient Driven Fluctuations

Z

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Page 10: Shadowgraph Study of Gradient Driven Fluctuations

Physical Optics Treatment

g_

Wave fi'onts emerging from the

sample are phase modulated.

NAS A/CP--2002-211212/VOL 1 334

Page 11: Shadowgraph Study of Gradient Driven Fluctuations

z>

Tl,a

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I,.a

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,,a_a

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,,j

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ii

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Page 12: Shadowgraph Study of Gradient Driven Fluctuations

Ratio of two images taken 1 second

Apart for aniline/cyclohexane at

40 ° C with a gradient of 160 K/cm.

NAS A/CP--2002-211212/VOL I 336

Page 13: Shadowgraph Study of Gradient Driven Fluctuations

I2(q) for a 1 mm thick sample of 47

Wt.% aniline in cyclohexane at

40 ° C with a gradient of 160 K/cm.

Measured at z- 18 cm.

NASAJCP--2002-211212/VOL 1 337

Page 14: Shadowgraph Study of Gradient Driven Fluctuations

•aldtues auexaqolaz(a/aU!l!Ue 0q!

aoj suo!l_nlan U aql jo tUrUlaads

_oAxod ie!leds oq1 jo lold _oIi-_o7

(L_wo) b0001, 001,

I ' ' ' ' ' ' ' ' I ' ' ' ' ' ' '

01,I i u ! !

wo/>l 09 I, '0 o01;'auexeqolo_O/eU!l!UV

I I I 1 I I I i i I I

//

/• /

//

.O•

"qJo"'I .... , , I , | l l

60L

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Page 15: Shadowgraph Study of Gradient Driven Fluctuations

./.@Optical windows

//

//

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, i_ _ ,_ , ,, ,_

,/_ i/iiil ¸ ii _ii iil!i/i! ii

A large concentration gradient is

present for many hours, during the

process of free diffusion.

NASA/CP--2002-211212/VOL 1 339

Page 16: Shadowgraph Study of Gradient Driven Fluctuations

I2(q) for water diffusing into

ethylene glycol.

NAS A/CP--2002-211212/VOL 1 340

Page 17: Shadowgraph Study of Gradient Driven Fluctuations

4xl 01° .... , , , i , , , , |

>,.,0103xl

L

K..

2x101°

13"

lx10 _°

0

7_

//

//

0________0_0 _'_0

10 100

q (cm -1)

Log-Linear plot of the spatial

power spectrum of the fluctuations

for water diffusing into ethylene

glycol.

NASAJCP--2002-211212/VOL 1 34 i

Page 18: Shadowgraph Study of Gradient Driven Fluctuations

1.2X10 9

5,--

8.0xl 08<v

v

"-- 4.0xl 08

i i ! i I i i i i i i i i I

//

/i

kt.

V '-w',_0 I I I I i I I I I I I t I I I I I

10 -1 100q (era)

Log-Linear plot of the spatial power

spectrum of the fluctuations for a

1 mm thick toluene sample with a

gradient of 200 K/cm.

NASAJCP--2002-211212/VOL 1 342

Page 19: Shadowgraph Study of Gradient Driven Fluctuations

.A.

_3×10 -9

2xlO -9

_ 0-9,..,1 xl¢q

0

//

.,.,':

I I i

• /..,.,

/"i

/ IiI

//

//

10 20 50 100 200 500

q(cm -1)

Log-Linear plot of the shadowgraph

signal expected for a lmm thick toluene

sample subjected to a gradient of

200 K/cm, and with an imaging distance

of 50 cm.

NASA/CP--2002-211212/VOL 1 343

Page 20: Shadowgraph Study of Gradient Driven Fluctuations

1.4xlO 9

_' 1.2 x 10 9k_

09_- lxlml=l

._ 088xl

<_.. 6x108

4xlO 8eq

-- 2xlO 8

_S

0

0

0

%_O

0

t_S®

100 200 300 400

q(cm -1)

Results of fitting existing theory to the

data for toluene. The theory.* includes

both gravity and finite-size effects.

_!_ _12_ii_iii iiZ _ii!_(i!_ i̧i__i_i!ii!(_ _i ili i_̧_ !i

NASA/CP--2002-211212/VOL 1 344