International audienceThe deformation of elementary fluid volumes by velocity gradients is a key process for scalar mixing, chemical reactions and biological processes in flows. Whilst fluid deformation in unsteady, turbulent flow has gained much attention over the past half century, deformation in steady random flows with complex structure-such as flow through heterogeneous porous mediahas received significantly less attention. In contrast to turbulent flow, the steady nature of these flows constrains fluid deformation to be anisotropic with respect to the fluid velocity, with significant implications for e.g. longitudinal and transverse mixing and dispersion. In this study we derive an ab initio coupled continuous time random walk (CTRW) ...
International audienceThe deformation of fluid elements governs many processes in porous media, incl...
International audienceUnder steady flow conditions, the topological complexity inherent to all rando...
The macroscopic spreading and mixing of solute plumes in saturated porous media is ultimately contro...
International audienceThe deformation of elementary fluid volumes by velocity gradients is a key pro...
The deformation of elementary fluid volumes by velocity gradients is a key process for scalar mixing...
The deformation of elementary fluid volumes by velocity gradients is a key process for scalar mixing...
International audienceFluid stretching and deformation as quantified by the fluid deformation gradie...
International audienceFluid stretching and deformation as quantified by the fluid deformation gradie...
International audienceStretching and compression of material fluid elements is key for the understan...
International audienceStretching and compression of material fluid elements is key for the understan...
International audienceStretching and compression of material fluid elements is key for the understan...
The topological complexity inherent to all porous media can impart complicated transport dynamics un...
International audienceThe deformation of fluid elements governs many processes in porous media, incl...
International audienceThe deformation of fluid elements governs many processes in porous media, incl...
International audienceThe deformation of fluid elements governs many processes in porous media, incl...
International audienceThe deformation of fluid elements governs many processes in porous media, incl...
International audienceUnder steady flow conditions, the topological complexity inherent to all rando...
The macroscopic spreading and mixing of solute plumes in saturated porous media is ultimately contro...
International audienceThe deformation of elementary fluid volumes by velocity gradients is a key pro...
The deformation of elementary fluid volumes by velocity gradients is a key process for scalar mixing...
The deformation of elementary fluid volumes by velocity gradients is a key process for scalar mixing...
International audienceFluid stretching and deformation as quantified by the fluid deformation gradie...
International audienceFluid stretching and deformation as quantified by the fluid deformation gradie...
International audienceStretching and compression of material fluid elements is key for the understan...
International audienceStretching and compression of material fluid elements is key for the understan...
International audienceStretching and compression of material fluid elements is key for the understan...
The topological complexity inherent to all porous media can impart complicated transport dynamics un...
International audienceThe deformation of fluid elements governs many processes in porous media, incl...
International audienceThe deformation of fluid elements governs many processes in porous media, incl...
International audienceThe deformation of fluid elements governs many processes in porous media, incl...
International audienceThe deformation of fluid elements governs many processes in porous media, incl...
International audienceUnder steady flow conditions, the topological complexity inherent to all rando...
The macroscopic spreading and mixing of solute plumes in saturated porous media is ultimately contro...