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Rayleigh-Taylor Instability

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This document explores the fundamental dynamics of the Rayleigh-Taylor (RT) instability and its critical role in applications such as Inertial Confinement Fusion (ICF), supernova explosions, and stockpile stewardship. It addresses the historical discrepancy in the turbulent growth constant alpha between experimental observations and high-resolution numerical simulations, resolving it through initial perturbation spectrum dynamics including mode-coupling and long-wavelength saturation.
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Page 1 - Overview and Experimental Dynamics

Rayleigh-Taylor Instability A heavy fluid (ρheavy) supported against gravity (g) by a lighter fluid (ρlight) constitutes an unstable situation (Rayleigh-Taylor instability – RT). A glass of water that is held inverted will cause the water to fall out the sides of the container, while a column of air rises along the center in its place. While the atmospheric pressure associated with the air column is sufficient to support the weight of the water, the instability is caused by tiny perturbations at the interface. More generally, the acceleration may be different from the earth’s gravity, or even impulsive where the resulting flow is called a Richtmyer-Meshkov instability. The interfacial perturbations may be of a single wavelength (λ), or comprise of a superposition of many waves (i.e. a spectrum). A single wavelength will grow exponentially in time, before saturating to a constant terminal velocity at late-time. Structures of the light fluid penetrating the heavy are called bubbles, while the corresponding fingers of the heavy fluid are termed spikes. When a spectrum of modes is present, the interactions between modes result in a turbulent flow, characterized by a high level of mixing between the fluids, and self-similarity. Figure 1 (a) An ICF pellet and (b) a schematic of laser-driven implosion. Such instabilities figure prominently during the implosion of fusion targets bombarded by high-energy lasers (Inertial Confinement Fusion). Small irregularities at the pusher-fuel interface are magnified by the unstable hydrodynamics, ultimately degrading the thermonuclear yield (Figure 1). Such fusion experiments are critical in modeling high-energy density processes that occur during the detonation of nuclear weapons. Consequently, reliable numerical simulations of RT are an essential component to the nation’s stockpile stewardship program, and play a key role in the certification of the nation’s stockpile. RT-driven mixing also occurs in diverse applications ranging from supernova explosions to temperature inversions in the atmosphere. A deeper understanding of the mechanism of such flows would shed light on the many processes that underpin fully developed turbulence. Hence, insights developed from studies of RT turbulence may be applied to other canonical flows. We use high-resolution numerical simulations to study the behavior of single bubbles, bubble interactions, and by extension RT turbulence. Figure 2 Laser induced fluorescence image from a Rayleigh-Taylor experiment. The difficulty inherent in sustaining an unstable density stratification has challenged experimentalists for over half a century. Several innovative approaches have been developed, and an example is shown in figure 2. Here, the unstable density stratification is set up by co-flowing streams¹ (heavy above light) of different densities that are initially kept separate by a splitter plate. As the two streams leave the edge of the splitter plate at the same velocity, buoyancy-driven mixing occurs. In the figure, the heavy fluid was seeded with a fluorescent dye sensitive to green laser light. Collectively, experiments have provided us with invaluable information on the nature of RT, and demonstrated that the turbulence is self-similar, with a growth constant α ~ 0.07. Center for Nonlinear Studies

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