Transport of a passive scalar in wide channels with surface topography
arXiv:2210.02354 · doi:10.1088/1361-648X/acc8ad
Abstract
We generalize classical dispersion theory for a passive scalar to derive an asymptotic long-time convection-diffusion equation for a solute suspended in a wide, structured channel and subject to a steady low-Reynolds-number shear flow. Our theory, valid for small roughness amplitudes of the channel, holds for general surface shapes expandable as a Fourier series. We determine an anisotropic dispersion tensor, which depends on the characteristic wavelengths and amplitude of the surface structure. For surfaces whose corrugations are tilted with respect to the applied flow direction, we find that dispersion along the principal direction (i.e., the principal eigenvector of the dispersion tensor) is at an angle to the main flow direction and becomes enhanced relative to classical Taylor dispersion. In contrast, dispersion perpendicular to it can decrease compared to the short-time diffusivity of the particles. Furthermore, for an arbitrary surface shape represented in terms of a Fourier decomposition, we find that each Fourier mode contributes at leading order a linearly-independent correction to the classical Taylor dispersion tensor.
arXiv commentunder consideration for publication in the Journal of Physics: Condensed Matter (JPCM)
References in corpus (8)
- Active Particles in Complex and Crowded Environments
- Anomalous transport in the crowded world of biological cells
- Effective slip boundary conditions for arbitrary periodic surfaces: The surface mobility tensor
- Transport and dispersion of active particles in periodic porous media
- Controlling effective dispersion within a channel with flow and active walls
- Geometry controlled dispersion in periodic corrugated channels
- Time dependence of advection-diffusion coupling for nanoparticle ensembles
- Particle motion nearby rough surfaces