Droplet breakup by multimodal nonlinear Rayleigh Taylor instability

A droplet impacted by a shock wave will undergo a process of fragmentation due to the development of interfacial hydrodynamic instabilities. The interface experiences variable acceleration and shear that result in the development of both inertial (Rayleigh–Taylor) and shear (Kelvin–Helmholtz) instabilities. These perturbations grow in time and drive the fragmentation and breakup of the deformed droplet. Experiments are performed on nominally 0.86 mm water droplet subjected to a Mach 7 . 6 detonation wave, resulting in a high Weber number ( ∼ 36 , 000 ) breakup event. Perturbation growth is measured from a series of high-speed ( > 1 MHz ) shadowgraph images. It is proposed that, given the size of the large-scale perturbations observed in experiments, these instabilities are growing in the non-linear regime and can be described by bubble-merger models for nonlinear mixing. Calculations are performed for the growth rates and size of these instabilities using deformation and external flow models to establish the time-dependent boundary conditions. The concurrence of the measured perturbation widths and the predictions of the simple model lend credence to the theory. This novel approach serves to open a new avenue in the characterization of droplet breakup via hydrodynamic instabilities. • Droplet breakup begins through a combination of Kelvin–Helmholtz and Rayleigh–Taylor instabilities. • The dominant instability varies in time and location. • The instability length scales are predicted by non-linear multimode hydrodynamic instability theory.

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Publication Details

Journal
International Journal of Multiphase Flow
Published
2025-10-21
DOI
https://doi.org/10.1016/j.ijmultiphaseflow.2025.105490
Primary Topic
Fluid Dynamics and Heat Transfer
Type
article
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article

Droplet breakup by multimodal nonlinear Rayleigh Taylor instability

Jacob McFarland, Andrew W. Cook, Calvin J. Young
International Journal of Multiphase Flow
Fluid Dynamics and Heat Transfer
article

Droplet breakup by multimodal nonlinear Rayleigh Taylor instability

Jacob McFarland, Andrew W. Cook, Calvin J. Young
article en

Abstract

A droplet impacted by a shock wave will undergo a process of fragmentation due to the development of interfacial hydrodynamic instabilities. The interface experiences variable acceleration and shear that result in the development of both inertial (Rayleigh–Taylor) and shear (Kelvin–Helmholtz) instabilities. These perturbations grow in time and drive the fragmentation and breakup of the deformed droplet. Experiments are performed on nominally 0.86 mm water droplet subjected to a Mach 7 . 6 detonation wave, resulting in a high Weber number ( ∼ 36 , 000 ) breakup event. Perturbation growth is measured from a series of high-speed ( > 1 MHz ) shadowgraph images. It is proposed that, given the size of the large-scale perturbations observed in experiments, these instabilities are growing in the non-linear regime and can be described by bubble-merger models for nonlinear mixing. Calculations are performed for the growth rates and size of these instabilities using deformation and external flow models to establish the time-dependent boundary conditions. The concurrence of the measured perturbation widths and the predictions of the simple model lend credence to the theory. This novel approach serves to open a new avenue in the characterization of droplet breakup via hydrodynamic instabilities. • Droplet breakup begins through a combination of Kelvin–Helmholtz and Rayleigh–Taylor instabilities. • The dominant instability varies in time and location. • The instability length scales are predicted by non-linear multimode hydrodynamic instability theory.

International Journal of Multiphase FlowVol. 194
Lawrence Livermore National Laboratory (US), Texas College (US), Texas A&M University (US)
Openalex Percentile: Top 68%
Fluid Dynamics and Heat Transfer
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Droplet breakup by multimodal nonlinear Rayleigh Taylor instability — Jacob McFarland, Andrew W. Cook, et al. · International Journal of Multiphase Flow (2025) | TGRS Research Map | TGRS