Advection and diffusion in a chemically induced compressible flow
Florence Raynal, Mickael Bourgoin, C\'ecile Cottin-Bizonne, Christophe, Ybert, Romain Volk

TL;DR
This paper provides an analytical study of how salt gradients influence colloid dispersion in linear flows, revealing the effects of diffusiophoresis on mixing times, scales, and concentration limits, with predictions validated against experimental observations.
Contribution
It introduces an analytical framework for understanding diffusiophoretic effects on dispersion in constant-gradient flows, including predictions of mixing scales and maximum concentrations.
Findings
Diffusiophoresis modifies mixing times and Batchelor scales.
Global concentration evolution matches experimental chaotic advection.
Maximum colloid concentration depends on salt and colloid properties, not flow topology.
Abstract
We study analytically the joint dispersion of Gaussian patches of salt and colloids in linear flows, and how salt gradients accelerate or delay colloid spreading by diffusiophoretic effects. Because these flows have constant gradients in space, the problem can be solved almost entirely for any set of parameters, leading to predictions of how the mixing time and the Batchelor scale are modified by diffusiophoresis. We observe that the evolution of global concentrations, defined as the inverse of the patches areas, are very similar to those obtained experimentally in chaotic advection. They are quantitatively explained by examining the area dilatation factor, in which diffusive and diffusiophoretic effects are shown to be additive and appear as the divergence of a diffusive contribution or of a drift velocity. An analysis based on compressibility is developed in the salt-attracting case,…
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