2020
DOI: 10.1115/1.4048345
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Experiments and Simulations on the Turbulent, Rarefaction Wave Driven Rayleigh–Taylor Instability

Abstract: Experiments were performed to observe the growth of the turbulent Rayleigh-Taylor unstable mixing layer generated between air and SF6, with an Atwood number of A=(?2-?1)/(?2+?1)=0.64, where ?1 and ?2 are the densities of air and SF6 respectively. A non-constant acceleration with an average value of 2300g0, where g0 is the acceleration due to gravity, was generated by interaction of the interface between the two gases with a rarefaction wave. Three-dimensional multi-mode perturbations were generated on the diff… Show more

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Cited by 8 publications
(4 citation statements)
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“…Experimentally, Morgan et al (2018); Morgan, Likhachev & Jacobs (2016) generated two-(2-D) and three-dimensional (3-D) single-mode interfaces using the membraneless technique (Jones & Jacobs 1997), and studied the linear and nonlinear instability evolution in a vertical rarefaction tube. Later, 3-D multi-mode perturbations were generated by Morgan & Jacobs (2020), and turbulent mixing induced by rarefaction-driven RT instability was focused on.…”
Section: Introductionmentioning
confidence: 99%
“…Experimentally, Morgan et al (2018); Morgan, Likhachev & Jacobs (2016) generated two-(2-D) and three-dimensional (3-D) single-mode interfaces using the membraneless technique (Jones & Jacobs 1997), and studied the linear and nonlinear instability evolution in a vertical rarefaction tube. Later, 3-D multi-mode perturbations were generated by Morgan & Jacobs (2020), and turbulent mixing induced by rarefaction-driven RT instability was focused on.…”
Section: Introductionmentioning
confidence: 99%
“…The early evolution of the density and vertical velocity variance spectra suggest that velocity fluctuations are the dominant mechanism driving the development of instability. Morgan et al [18] performed experiments to observe the growth of the turbulent Rayleigh-Taylor unstable mixing layer generated between air and SF 6 . They used the membraneless vertical oscillation technique to make the three-dimensional multi-mode perturbations on the diffuse interface, and the 20 experiments were performed to establish a statistical ensemble.…”
Section: Introductionmentioning
confidence: 99%
“…The early evolution of the density and vertical velocity variance spectra suggest that velocity fluctuations are the dominant mechanism driving the development of instability. Morgan, et al [18] performed experiments to observe the growth of the turbulent Rayleigh-Taylor unstable mixing layer generated between air and SF 6 . They used the membraneless vertical oscillation technique to make the three-dimensional multi-mode perturbations on the diffuse interface, and 20 experiments were performed to establish a statistical ensemble.…”
Section: Introductionmentioning
confidence: 99%