Rayleigh-Taylor is a hydrodynamic instability that occurs when there is a sharp interface between two fluids of different densities. The instability arises due to the effects of buoyancy, which can cause the lighter fluid to accelerate faster than the surrounding heavier fluid. This creates a complex and dynamic flow pattern, which can lead to mixing between the two fluids.
The Rayleigh-Taylor instability was first discovered by Lord Rayleigh in 1883, who noted a similar phenomenon in the context of surface waves in fluids of different densities. It has since been studied extensively in many different contexts, including in astrophysical systems, inertial confinement fusion, and in laboratory experiments.
The instability can be characterized by a dimensionless parameter known as the Atwood number, which represents the difference in density between the two fluids. When the Atwood number is small, the Rayleigh-Taylor instability is weak, and the mixing between the two fluids is less pronounced. However, when the Atwood number is large, the instability can become highly nonlinear, resulting in the formation of complex structures and turbulence.
Understanding the Rayleigh-Taylor instability is important in a wide range of fields, including in the development of more efficient combustion engines, the design of more effective shock absorbers, and in the study of astrophysical phenomena such as supernovae and accretion disks.
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