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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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the inorganic synthesis using pressure as an additional process variable, existing synthesis strategies may benefit from enhanced<br />

control of the reaction process, <strong>and</strong> entirely new strategies may be contemplated.<br />

Author (revised)<br />

Drops (Liquids); Emulsions; Diffusion Coefficient; Pressure Effects; Microstructure<br />

<strong>2001</strong>0024950 Oklahoma State Univ., Dept. of Physics, Stillwater, OK USA<br />

Non-Equilibrium Particle Configuration in Sedimentation<br />

Lei, X.-Y., Oklahoma State Univ., USA; Ackerson, B. J., Oklahoma State Univ., USA; Tong, P., Oklahoma State Univ., USA;<br />

Proceedings of the Fifth Microgravity Fluid Physics <strong>and</strong> Transport Phenomena Conference; December 2000, pp. 1168-1170; In<br />

English; See also <strong>2001</strong>0024890; No Copyright; Abstract Only; Available from CASI only as part of the entire parent document<br />

In the study of the settling of large non-Brownian particles, one is interested in underst<strong>and</strong>ing the effect of the long-range<br />

hydrodynamic interactions on the microstructures formed in the settling suspension <strong>and</strong> finding the direct link between the microscopic<br />

particle configuration <strong>and</strong> the macroscopic properties of the suspension, such as the mean sedimentation velocity <strong>and</strong> the<br />

velocity fluctuations (the rms velocity) as a function of the particle concentration. We have recently proposed that statistical or<br />

spontaneous number fluctuations of the particles can produce regions having more (or less) particles than the average. These<br />

heavier (or lighter) regions are convectively unstable, when the size becomes larger than the diffusive dissipation length delta(sub<br />

d). Using the Rayleigh criterion, the value of delta(sub d) is calculated <strong>and</strong> the result agrees with experiment. Above the length<br />

delta(sub d), a set of coarse-grained equations of motion is used to describe the concentration <strong>and</strong> velocity fluctuations in sedimentation.<br />

The model provides a physical interpretation for the emergence of a velocity cut-off length, which prevents hydrodynamic<br />

dispersion coefficients from being divergent. to test these theoretical ideas, we conduct measurements of the particle configuration<br />

in a settling suspension of large non-Brownian particles. The particles used in the experiment are 40 microns diameter polymer<br />

latex spheres suspended in polyalkylene glycol at the volume fraction 0.4%. A sheet of laser light is used to illuminate a vertical<br />

section of the settling suspension <strong>and</strong> images of the particles are obtained using a CCD camera situated normal to the illuminating<br />

light sheet. A figure shows a typical particle configuration in sedimentation. Superimposing a series of such pictures taken at<br />

15-second intervals shows a turbulent looking velocity field with rather large velocity fluctuations. The particle configurations<br />

in sedimentation look r<strong>and</strong>om but the number fluctuations of the particles are found to be suppressed when compared with Poisson<br />

statistics for pure r<strong>and</strong>om configurations. A figure compares typical number fluctuations (number of particles in a circle of fixed<br />

area) measured in sedimentation (upper curve) with those in pure r<strong>and</strong>om configurations (lower curve). Systematic statistical analysis<br />

shows that the number fluctuations of the settling particles become more <strong>and</strong> more suppressed with time. At the later stage<br />

of the settling process, the suppression is most striking at large length scales. These findings are consistent with the notion that<br />

the convective response of the suspension to ordinary number fluctuations reduces <strong>and</strong> eliminates them, bringing the suspension<br />

to a marginally stable state, in which the statistics are such that unstable convection is minimized.<br />

Author (revised)<br />

Sediments; Settling; Microparticles; Dispersions; Suspending (Mixing)<br />

<strong>2001</strong>0024951 Pittsburgh Univ., Dept. of Physics <strong>and</strong> Astronomy, Pittsburgh, PA USA<br />

Dynamics of Grain Boundaries in 2D Colloids<br />

Wei, Q.-H., Pittsburgh Univ., USA; Wu, X.-L., Pittsburgh Univ., USA; Proceedings of the Fifth Microgravity Fluid Physics <strong>and</strong><br />

Transport Phenomena Conference; December 2000, pp. 1171-1182; In English; See also <strong>2001</strong>0024890; No Copyright; Avail:<br />

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

Grain boundaries are the longest known crystal defects <strong>and</strong> the development of grain structures plays a critical role in the<br />

properties of many kinds of materials such as ceramics, metals, <strong>and</strong> semiconductors. While the equilibrium structures of grain<br />

boundaries have been known very well to atomic resolution through electron microscopy <strong>and</strong> soap bubble model studies, the<br />

dynamics process of grain boundary migration driven by external forces or thermal fluctuation is not well established. In this presentation,<br />

we report the non-equilibrium behavior of grain boundaries in a model system, consisting of a monolayer of colloidal<br />

particles confined in a soap film. A great advantage of this model system is that structure <strong>and</strong> dynamics of grain boundaries can<br />

be studied instantaneously. The 2D film is formed by drawing a thin plastic frame with a hole in the center from a bulk monodispersed<br />

colloidal suspension. Due to the gravity <strong>and</strong> water evaporation, the thickness of the soap film becomes comparable to the<br />

particle diameter, leading to the curving of the water-air interface. This curved meniscus between particles poses an attractive<br />

interaction between colloidal particles, which are otherwise hard-sphere like. This attractive capillary force causes the colloidal<br />

particles to self-assemble forming crystals which are usually polycrystalline with an average grain size up to hundreds of lattice<br />

constants, as shown. Using a larger magnification, one can easily distinguish large- <strong>and</strong> small-angle grain boundaries, which, as<br />

indicated respectively by L <strong>and</strong> S as seen in an accompanying figure, are different from those commonly seen in textbooks. An<br />

interesting observation is that when an external periodic vertical vibration is applied to the particle suspension, the grain bound-<br />

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