Beginning with motivating examples of chaotic fluid advection applied to control mixing and scalar transport in devices, in biophysical flows, and in environmental and geophysical flows, I discuss basic features and organizing ideas of chaotic advection and transport in planar flows. Due to the combination of kinematics and continuity, steady planar flows must mix poorly; the flow designer must add some time-dependence that causes streamlines to cross at successive times (a simple though effective heuristic). Unstable manifolds of hyperbolic points in flows are the "highways" along which transport takes place. These structures emerge from the way the fluid is stirred and change as stirring parameters vary, leading to fractal distributions o...
Goal is explicit demarcation of the region of validity of a linear canonical representation for chao...
Goal is explicit demarcation of the region of validity of a linear canonical representation for chao...
The macroscopic spreading and mixing of solute plumes in saturated porous media is ultimately contro...
Enhancement of heat and/or mass transfer via turbulence is often not feasible for highly viscous, no...
While mixing and particle transport in 2D incompressible flows are well-understood, much less is kno...
This work focuses on the role of chaotic advection in promoting mixing, transition, and aggregation....
The minimum-energy method to generate chaotic advection should be to use an irrotational flow. Howev...
Fluid mixing is a complex process consisting of a variety of physical mechanisms. This work focuses ...
Many remediation activities in the terrestrial subsurface involve the need to recover/emplace distri...
We show that chaotic advection is inherent to flow through all types of porous media, from granular ...
This volume collects a number of theoretical and experimental lectures on various aspects of transpo...
The aim of these notes is to provide an overview of the different approaches used to address the adv...
We show that chaotic advection is inherent to flow through all types of porous media, from granular ...
Goal is explicit demarcation of the region of validity of a linear canonical representation for chao...
Passive scalar transport involves complex interactions between advection and diffusion, where the gl...
Goal is explicit demarcation of the region of validity of a linear canonical representation for chao...
Goal is explicit demarcation of the region of validity of a linear canonical representation for chao...
The macroscopic spreading and mixing of solute plumes in saturated porous media is ultimately contro...
Enhancement of heat and/or mass transfer via turbulence is often not feasible for highly viscous, no...
While mixing and particle transport in 2D incompressible flows are well-understood, much less is kno...
This work focuses on the role of chaotic advection in promoting mixing, transition, and aggregation....
The minimum-energy method to generate chaotic advection should be to use an irrotational flow. Howev...
Fluid mixing is a complex process consisting of a variety of physical mechanisms. This work focuses ...
Many remediation activities in the terrestrial subsurface involve the need to recover/emplace distri...
We show that chaotic advection is inherent to flow through all types of porous media, from granular ...
This volume collects a number of theoretical and experimental lectures on various aspects of transpo...
The aim of these notes is to provide an overview of the different approaches used to address the adv...
We show that chaotic advection is inherent to flow through all types of porous media, from granular ...
Goal is explicit demarcation of the region of validity of a linear canonical representation for chao...
Passive scalar transport involves complex interactions between advection and diffusion, where the gl...
Goal is explicit demarcation of the region of validity of a linear canonical representation for chao...
Goal is explicit demarcation of the region of validity of a linear canonical representation for chao...
The macroscopic spreading and mixing of solute plumes in saturated porous media is ultimately contro...