{"title":"Trapping and extreme clustering of finitely-dense inertial particles near a rotating vortex pair","authors":"Saumav Kapoor, Divya Jaganathan, Rama Govindarajan","doi":"arxiv-2405.04949","DOIUrl":null,"url":null,"abstract":"Small heavy particles cannot get attracted into a region of closed\nstreamlines in a non-accelerating frame (Sapsis & Haller 2010). In a rotating\nsystem, however, particles can get trapped (Angilella 2010) near vortices. We\nperform numerical simulations examining trapping of inertial particles in a\nprototypical rotating flow: an identical pair of rotating Lamb-Oseen vortices,\nwithout gravity. Our parameter space includes the particle Stokes number $St$,\nmeasuring the particle's inertia, and a density parameter $R$, measuring the\nparticle-to-fluid relative density. We focus on inertial particles that are\nfinitely denser than the fluid. Particles can get indefinitely trapped near the\nvortices and display extreme clustering into smaller dimensional objects:\nattracting fixed-points, limit cycles and chaotic attractors. As $St$ increases\nfor a given $R$, we may have an incomplete or complete period-doubling route to\nchaos, as well as an unusual period-halving route back to a fixed-point\nattractor. The fraction of trapped particles can vary non-monotonically with\n$St$. We may even have windows in $St$ for which no particle trapping occurs.\nAt $St$ larger than a critical value, beyond no trapping occurs, significant\nfractions of particles can spend long but finite times in the vortex vicinity.\nThe inclusion of the Basset-Boussinesq history (BBH) force is imperative in our\nstudy due to particle's finite density. BBH force significantly increases the\nbasin of attraction as well as the range of $St$ where trapping can occur.\nExtreme clustering can be physically significant in planetesimal formation by\ndust aggregation in protoplanetary disks, phytoplankton aggregation in oceans,\netc.","PeriodicalId":501167,"journal":{"name":"arXiv - PHYS - Chaotic Dynamics","volume":"137 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-05-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Chaotic Dynamics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2405.04949","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Small heavy particles cannot get attracted into a region of closed
streamlines in a non-accelerating frame (Sapsis & Haller 2010). In a rotating
system, however, particles can get trapped (Angilella 2010) near vortices. We
perform numerical simulations examining trapping of inertial particles in a
prototypical rotating flow: an identical pair of rotating Lamb-Oseen vortices,
without gravity. Our parameter space includes the particle Stokes number $St$,
measuring the particle's inertia, and a density parameter $R$, measuring the
particle-to-fluid relative density. We focus on inertial particles that are
finitely denser than the fluid. Particles can get indefinitely trapped near the
vortices and display extreme clustering into smaller dimensional objects:
attracting fixed-points, limit cycles and chaotic attractors. As $St$ increases
for a given $R$, we may have an incomplete or complete period-doubling route to
chaos, as well as an unusual period-halving route back to a fixed-point
attractor. The fraction of trapped particles can vary non-monotonically with
$St$. We may even have windows in $St$ for which no particle trapping occurs.
At $St$ larger than a critical value, beyond no trapping occurs, significant
fractions of particles can spend long but finite times in the vortex vicinity.
The inclusion of the Basset-Boussinesq history (BBH) force is imperative in our
study due to particle's finite density. BBH force significantly increases the
basin of attraction as well as the range of $St$ where trapping can occur.
Extreme clustering can be physically significant in planetesimal formation by
dust aggregation in protoplanetary disks, phytoplankton aggregation in oceans,
etc.