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Scientific and Technical Aerospace Reports Volume 39 April 6, 2001

Scientific and Technical Aerospace Reports Volume 39 April 6, 2001

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Newtonian fluids in the laboratory, a useful configuration involves a cylinder of liquid placed between two solid plates, which<br />

are then stretched at an exponential rate. The quantitative results of these calculations will be presented in detail elsewhere, but<br />

for example we will exhibit snapshots of the stretched bridges, <strong>and</strong> such quantities as the minimum radius, normalized force on<br />

the plates, <strong>and</strong> Trout on ratio as a function of Hencky strain. These results resemble those found in experiment <strong>and</strong> simulation,<br />

respectively.<br />

Author (revised)<br />

Molecular Dynamics; Fluid Flow; Field Theory (Physics); Newtonian Fluids; Equations of Motion<br />

<strong>2001</strong>0024923 California Univ., Physics Dept., Los Angeles, CA USA<br />

Diffusing Light Photography of Containerless Ripple Turbulence<br />

Wright, William, California Univ., USA; Putterman, Seth, California Univ., USA; Proceedings of the Fifth Microgravity Fluid<br />

Physics <strong>and</strong> Transport Phenomena Conference; December 2000, pp. 800-819; In English; See also <strong>2001</strong>0024890; No Copyright;<br />

Avail: CASI; A03, Hardcopy; A10, Microfiche<br />

The high amplitude motion of the surface of a fluid displays a number of extraordinary phenomena ranging from localized<br />

structures to turbulence. Among localized structures there can appear breather <strong>and</strong> kink solitons [sometimes called darkons] <strong>and</strong><br />

aspects of turbulence can be studied via the mutual scattering of ripples running along the surface of a fluid. As the height of the<br />

surface of a fluid Zeta(r,t) as a function of position <strong>and</strong> time is the key parameter measurement of the above phenomena requires<br />

a technique that can resolve large variations in Zeta(r,t). In our experiments the surface motion is made visible by suspending into<br />

the water a .04% solution of polyballs. This concentration is sufficiently dense that light travelling through the water is so strongly<br />

scattered that it diffuses. In this way the technique overcomes the problems presented by the appearance of caustics in attempts<br />

to apply shadowgraphs to high amplitude fluid motion. The key criterion for the application of diffusing light principles to resolve<br />

surface height is that the overall depth of the fluid must be greater than the transport mean free path which in turn must be comparable<br />

to the maximum surface heights resolved. The concentration is sufficiently dilute that it does not affect the viscosity. Light<br />

is then incident on the fluid from below <strong>and</strong> a charge coupled device (CCD) records the light to exit the fluid. Typically the image<br />

of the surface is broken up into one million pixels [1024x1024] where each pixel is capable of recording a dynamic range of 65,000<br />

gray scales [or 16 bits]. This image is converted into the surface height with the help of a calibration plot.This plot shows the<br />

amount of light to exit the surface as a function of fluid depth. The deeper the fluid the smaller is the amount of light to make it<br />

to the surface at that location. The dependence on surface slope is weak as demonstrated from photos of jello molds in the shape<br />

of sine waves that are formed from these water polyball solutions. The maximum slopes of these molds corresponds to capillary<br />

wave mach numbers of about 1/2, This imaging technique is useful for obtaining an instantaneous realization of the surface height<br />

when the illumination is in the form of a short [microsecond] flash of light. The surface height as a function of time at a single<br />

point in the fluid can be obtained by reading out the calibrated signal from a single pixel as a function of time. This technique has<br />

been able to resolve, the hyperbolic secant profile of a breather soliton, the hyperbolic tangent profile of a darkon, the unusual<br />

shear thinned states of non-Newtonian fluids, <strong>and</strong> the Kolmogorov spectrum of ripple turbulence. This last case constitutes the<br />

core of a proposed experiment in microgravity <strong>and</strong> will be described further. The law for the spectrum in the inertial region can<br />

be derived in parallel with Kolmogorov’s law of vortex turbulence. If E(sub k) denotes the ripple energy per unit area between<br />

k <strong>and</strong> 2k then E(sub k) must be sufficiently large that nonlinear reversible processes dominate damping of mechanical energy due<br />

to viscosity.. Furthermore the density of modes excited must be sufficiently large that their spacing in frequency space is less than<br />

their broadening due to nonlinear interactions. In this limit one finds for the power spectrum of surface motion: Measurements<br />

reveal reasonable agreement with both of theses formulas. The fact the the temporal spectrum agrees with the spatial spectrum<br />

is another test of the imaging technique. A number of key assumptions underly the ’derivation’ of Kolmogorov’s law from the<br />

theory of interacting propagating waves. They are 1) the r<strong>and</strong>om phase approximation <strong>and</strong> 2) a closure hypothesis. In its simplest<br />

form the closure hypothesis says that the average of the product of action of two modes is the product of the averages [this can<br />

be called a stosszahl ansatz]. The abiding question of turbulence is the extent to which these assumptions are violated. These issues<br />

will be addressed in a microgravity environment where ripples will be studied on the surface of a positioned fluid sphere that is<br />

about 12cm in diameter. The sphere will be held in place <strong>and</strong> excited by acoustic forces. Light will be brought in with an optical<br />

fiber to the center of the sphere. From that point light will diffuse out to the surface where it will be imaged. On the surface of<br />

a sphere the wavenumber k is replaced with l/R where l is an integer <strong>and</strong> R is the radius of the sphere. For a cascade starting at<br />

1Hz [l about 8], the turbulent regime in k should extend over more than 1.5 decades. The advantages of microgravity are that the<br />

forces of capillarity dominate the motion over a wider ranger of wave numbers than on the ground. This is desirable as the nonlinear<br />

properties of capillary waves are much stronger than those of gravity waves. At these longer wavelengths capillary waves also<br />

suffer less dissipation <strong>and</strong> so the effects of turbulent motion are more accessible. In low g it is possible to levitate a large drop of<br />

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