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- W3104993417 abstract "The sedimentation of a heavy Stokes particle in a laminar plane or axisymmetric flow is investigated by means of asymptotic methods. We focus on the occurrence of Stommel's retention zones, and on the splitting of their separatrices. The goal of this paper is to analyze under which conditions these retention zones can form, and under which conditions they can break and induce chaotic particle settling. The terminal velocity of the particle in still fluid is of the order of the typical velocity of the flow, and the particle response time is much smaller than the typical flow time-scale. It is observed that if the flow is steady and has an upward streamline where the vertical velocity has a strict local maximum, then inertialess particle trajectories can take locally the form of elliptic Stommel cells, provided the particle terminal velocity is close enough to the local peak flow velocity. These structures only depend on the local flow topology and do not require the flow to have closed streamlines or stagnation points. If, in addition, the flow is submitted to a weak time-periodic perturbation, classical expansions enable one to write the particle dynamics as a hamiltonian system with one degree of freedom, plus a perturbation containing both the dissipative terms of the particle motion equation and the flow unsteadiness. Melnikov's method therefore provides accurate criteria to predict the splitting of the separatrices of the elliptic cell mentioned above, leading to chaotic particle trapping and chaotic settling. The effect of particle inertia and flow unsteadiness on the occurrence of simple zeros in Melnikov's function is discussed. Particle motion in a plane cellular flow and in a vertical pipe is then investigated to illustrate these results." @default.
- W3104993417 created "2020-11-23" @default.
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- W3104993417 date "2007-07-01" @default.
- W3104993417 modified "2023-09-25" @default.
- W3104993417 title "Asymptotic analysis of chaotic particle sedimentation and trapping in the vicinity of a vertical upward streamline" @default.
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- W3104993417 doi "https://doi.org/10.1063/1.2751387" @default.
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