The topological complexity inherent to all porous media imparts persistent chaotic advection under steady flow conditions, which, in concert with the no-slip boundary condition, generates anomalous transport. We explore the impact of this mechanism upon longitudinal dispersion via a model random porous network and develop a continuous-time random walk that predicts both preasymptotic and asymptotic transport. In the absence of diffusion, the ergodicity of chaotic fluid orbits acts to suppress longitudinal dispersion from ballistic to superdiffusive transport, with asymptotic variance scaling as σ2L(t)∼t2/(lnt)3. These results demonstrate that anomalous transport is inherent to homogeneous porous media and has significant implica...
International audienceFrom numerical simulations of pore-scale flow in porous media, we demonstrate ...
International audienceFrom numerical simulations of pore-scale flow in porous media, we demonstrate ...
International audienceWe study the intermittency of fluid velocities in porous media and its relatio...
The topological complexity inherent to all porous media can impart complicated transport dynamics un...
The macroscopic spreading and mixing of solute plumes in saturated porous media is ultimately contro...
We show that chaotic advection is inherent to flow through all types of porous media, from granular ...
We show that chaotic advection is inherent to flow through all types of porous media, from granular ...
International audienceUnder steady flow conditions, the topological complexity inherent to all rando...
Under steady flow conditions, the topological complexity inherent to all random three-dimensional (3...
International audienceUnder steady flow conditions, the topological complexity inherent to all rando...
Anomalous transport, understood as the nonlinear scaling with time of the mean square displacement o...
We study the origins of anomalous dispersion in heterogeneous porous media in terms of the medium a...
International audienceSolute transport in heterogeneous porous media is in generalnon-Fickian, this ...
International audienceSolute transport in heterogeneous porous media is in generalnon-Fickian, this ...
International audienceFrom numerical simulations of pore-scale flow in porous media, we demonstrate ...
International audienceFrom numerical simulations of pore-scale flow in porous media, we demonstrate ...
International audienceFrom numerical simulations of pore-scale flow in porous media, we demonstrate ...
International audienceWe study the intermittency of fluid velocities in porous media and its relatio...
The topological complexity inherent to all porous media can impart complicated transport dynamics un...
The macroscopic spreading and mixing of solute plumes in saturated porous media is ultimately contro...
We show that chaotic advection is inherent to flow through all types of porous media, from granular ...
We show that chaotic advection is inherent to flow through all types of porous media, from granular ...
International audienceUnder steady flow conditions, the topological complexity inherent to all rando...
Under steady flow conditions, the topological complexity inherent to all random three-dimensional (3...
International audienceUnder steady flow conditions, the topological complexity inherent to all rando...
Anomalous transport, understood as the nonlinear scaling with time of the mean square displacement o...
We study the origins of anomalous dispersion in heterogeneous porous media in terms of the medium a...
International audienceSolute transport in heterogeneous porous media is in generalnon-Fickian, this ...
International audienceSolute transport in heterogeneous porous media is in generalnon-Fickian, this ...
International audienceFrom numerical simulations of pore-scale flow in porous media, we demonstrate ...
International audienceFrom numerical simulations of pore-scale flow in porous media, we demonstrate ...
International audienceFrom numerical simulations of pore-scale flow in porous media, we demonstrate ...
International audienceWe study the intermittency of fluid velocities in porous media and its relatio...