Shock-induced drop size and distributions

Fuente: arXiv
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Autores principales: Park, J. E., Lee, T. -W.
Formato: Preprint
Publicado: 2024
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author Park, J. E.
Lee, T. -W.
author_facet Park, J. E.
Lee, T. -W.
contents We use an integral analysis of conservation equations of mass and energy, to determine the drop size and distributions during shock-induced drop break-up. The result is an updated form for the drop size as a function of its final velocity, from a series of work applied to various atomization geometries. Comparisons with experimental data demonstrate the validity and utility of this method. The shock-induced drop size and distributions can be predicted within reasonable accuracy as a function of the drop velocity ratio and fluid properties. The result also illustrates the dynamical process of kinetic energy deficit transferred to the surface tension energy, and the skewing of the drop size distribution due to the non-linear dependence on velocity ratio.
format Preprint
id arxiv_https___arxiv_org_abs_2407_05367
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Shock-induced drop size and distributions
Park, J. E.
Lee, T. -W.
Fluid Dynamics
We use an integral analysis of conservation equations of mass and energy, to determine the drop size and distributions during shock-induced drop break-up. The result is an updated form for the drop size as a function of its final velocity, from a series of work applied to various atomization geometries. Comparisons with experimental data demonstrate the validity and utility of this method. The shock-induced drop size and distributions can be predicted within reasonable accuracy as a function of the drop velocity ratio and fluid properties. The result also illustrates the dynamical process of kinetic energy deficit transferred to the surface tension energy, and the skewing of the drop size distribution due to the non-linear dependence on velocity ratio.
title Shock-induced drop size and distributions
topic Fluid Dynamics
url https://arxiv.org/abs/2407.05367