Electro-osmosis is fluid motion driven by an applied electric field acting on mobile electric charge near a surface. A charged interface attracts a diffuse population of counterions in an electric double layer. A field component tangent to the interface exerts a force density on that mobile charge; momentum transfer to the surrounding solvent drives flow opposed by viscous stress. In a capillary electrophoresis measurement, this flow advects the sample as well as its electrical drift relative to the fluid. Locally, the measured axial velocity is , where is the electroosmotic fluid velocity and is the electrophoretic mobility. [ref]
A homogeneous charged channel can add a constant electro-osmotic drift to the ideal electrophoretic velocity at fixed field. It changes the coefficient of a linear length-versus-entry-time law without generating a new length exponent. Charge-dependent adsorption, heterogeneous trapping or cancellation of drift followed by diffusion lies outside that simple claim; wall charge cannot be excluded as an indirect cause in every real experiment.
With , and no slip at either wall, linear screening gives . The velocity is . This electrically neutral-wall boundary assumes no external normal field; it differs from a grounded wall.
Zero wall charge constrains the jump in normal electric displacement, while fixing a wall potential is a separate electrical condition. Taking the external normal field to vanish gives a zero normal derivative at an ideal uncharged wall. A grounded wall may carry induced charge even though its imposed potential is zero.
Differentiating the screened-channel velocity gives . For , . The outer flow declines almost linearly to the passive no-slip wall rather than forming a symmetric plug.
In a half-space with no pressure gradient, Stokes balance and Poisson electrostatics give . No slip at the wall and zero bulk shear imply . The bulk velocity is ; it is not the fluid speed at the no-slip wall.

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Electro-osmosis is a phenomenon that occurs when an electric field is applied to a fluid that contains charged particles or ions, causing the fluid to move through a porous medium or a gel. This movement is driven by the interaction between the electric field and the charged species in the fluid, leading to the bulk flow of the liquid.