Abstract
A three-dimensional transient round liquid jet within a low-speed coaxial outer gas flow is numerically simulated and analysed via vortex dynamics ($\unicode[STIX]{x1D706}_{2}$ analysis). Two types of surface deformations are distinguished, which are separated by a large indentation on the jet stem. First, there are those inside the recirculation zone behind the leading cap – directly affecting the cap dynamics and well explained by the local vortices. Second, deformations upstream of the cap are mainly driven by the Kelvin–Helmholtz (KH) instability, unaffected by the vortices in the behind-the-cap region (BCR), and are important in the eventual atomization process. Different atomization mechanisms are identified and are delineated on a gas Weber number ($We_{g}$) versus liquid Reynolds number ($Re_{l}$) map based on the relative gas–liquid velocity. In a frame moving with the liquid velocity, this result is consistent with prior temporal studies. A simpler and clearer portrait of similarity of the atomization domains is shown by using the relative gas–liquid axial velocity, i.e. $We_{r}$ and $Re_{r}$, and avoiding the widely used velocity ratio as a third key parameter. A detailed comparison of vorticity along the axis in an Eulerian frame versus a frame fixed to a surface wave reveals that the vortex development and surface deformations are periodic in the upstream region, but this periodicity is lost closer to the BCR. In the practical range of the density ratio and for early times in the process, axial vorticity is mainly generated by baroclinicity while streamwise vortex stretching becomes more important at later times and only at lower relative velocities when pressure gradients are reduced. The inertia, vortex, pressure, viscous and surface tension forces are analysed to delineate the dominant causes of the three-dimensional instability of the axisymmetric KH structure due to surface acceleration in the axial, radial and azimuthal directions. The inertia force related to the axial gradient of kinetic energy is the main cause of the axial acceleration of the waves, while the azimuthal acceleration is mainly caused by the pressure and viscous forces. The viscous forces are negligible in the radial direction and away from the nozzle exit in the axial direction. It is interesting to note that azimuthal viscous forces are important even at high $Re_{l}$, indicating that inertia is not totally dominant in this instability occurring early in the atomization cascade.
Highlights
When a liquid jet discharges into a gaseous medium, it becomes unstable and breaks into droplets due to instabilities
The vortices in the behind-the-cap region (BCR) are inside the recirculation zone behind the cap – the region inside the box in figure 4 – and the surface deformations are directly related to the dynamics of the growing cap and can be explained by the vortex interactions in that region
Shinjo & Umemura (2010) briefly discussed this region in their 3-D simulation of a round liquid-jet with no coaxial flow, and while describing that the vortex dynamics in this region are very complex, they showed that the vortex orientation determines the orientation of the ligaments that are broken from the cap
Summary
When a liquid jet discharges into a gaseous medium, it becomes unstable and breaks into droplets due to instabilities. The main objective here is to examine the interaction of the vortices near the gas–liquid interface, and to see how those interactions vary with gas-to-liquid velocity ratio, and their consequent effects on the surface deformation and instabilities. In this respect, the causes of the axial vorticity generation are analysed to find the main source of the three-dimensional (3-D) instabilities of the initially axisymmetric jets. The causes of the axial vorticity generation are analysed to find the main source of the three-dimensional (3-D) instabilities of the initially axisymmetric jets To understand these causes and their variation with velocity ratio, the acting forces on the liquid surface are analysed separately in the three coordinate directions
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