Salinity gradients induce cross-streamline colloid migration that alters transit time and dispersion in porous media by an order of magnitude.
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Hydrostatic pressure modifies nonlinear concentration and surface potential profiles in diffusioosmosis through charged slits, enabling tuning of flow rate and direct inference of surface potentials from measurements.
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Diffusiophoretic transport of colloids in porous media
Salinity gradients induce cross-streamline colloid migration that alters transit time and dispersion in porous media by an order of magnitude.
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Tuning diffusioosmosis of electrolyte solutions by hydrostatic pressure
Hydrostatic pressure modifies nonlinear concentration and surface potential profiles in diffusioosmosis through charged slits, enabling tuning of flow rate and direct inference of surface potentials from measurements.