An ionic atmosphere. A negatively charged molecule attracts positive counterions and repels negative co-ions; signs reverse for a positive molecule. The resulting electric double layer partially screens the bare electric field. Far from an isolated molecule, the electrolyte recovers its neutral bulk composition. At thermodynamic equilibrium, spatial uniformity of each species' electrochemical potential requires
The logarithm implicitly uses a common reference density. This result for Boltzmann ion densities in a symmetric electrolyte neglects ion correlations, finite size and nonideal activities, but shows immediately why equal concentrations of the two signs do not persist close to a charged surface.
Self-consistent screening. Insert these densities into Poisson's equation, with solvent permittivity and fixed charge density :
This is the Poisson-Boltzmann equation. For a symmetric monovalent salt with bulk density of each sign, outside the fixed charge it becomes
For , linearizing and using bulk neutrality gives the Debye–Hückel approximation
Thus added salt shortens the Debye length: electrostatic screening becomes stronger over a shorter distance. The factor of two in a salt comes from two ionic species, not from double-counting the density of salt pairs.
For example, a charged sphere of radius and total charge has the exterior linearized solution
assuming fixed uniform surface charge and no ions inside. It follows from the decaying spherical solution and . At zero salt it reduces to the Coulomb potential; at finite salt it decays exponentially as well as geometrically. The excess mobile charge integrates to in an infinite neutralizing reservoir, although a finite sphere surrounding the molecule generally contains only part of that ionic atmosphere.
Biophysical scales and limitations. In water at room temperature, the monovalent formula is approximately , with the ionic strength. It gives about at and at . Consequently the same charged protein can exert very different long-range interactions mediated by electrostatics at different salt concentrations. Close to strongly charged DNA, the linear approximation fails; nonlinear screening, counterion condensation, ion-specific adsorption and changes of surface ionization through charge regulation may matter. Mean-field theory also misses strong multivalent-ion correlations and finite-size saturation: the exponential law cannot be extrapolated to arbitrarily large near-surface concentrations.
Write and take to be the reservoir density of each monovalent ion species. Equal electrochemical potentials in equilibrium give the Boltzmann ion densities in a symmetric electrolyte,
Combining this with the electrostatic Poisson equation gives the planar Poisson-Boltzmann equation,
The Debye length is . If the symbol instead denotes the combined density of both species, the factor two is absent; the per-species convention above makes the normalization explicit. At , the linearized planar screening solution obeys . With and ,
The positive ions are counterions and the negative ions are co-ions. At weak potential,
They approach from above and below respectively, with equal first-order excess and deficit. For stronger negative potential, interpret the source's strong-potential comparison as a statement about , since itself is negative. Counterions become strongly concentrated near the wall, while co-ions are exponentially depleted and remain nonnegative. Linearization misses this asymmetry and would eventually predict unphysical negative co-ion density. Point-ion mean-field theory itself eventually needs finite-size and correlation corrections; it provides no steric cap at arbitrarily large counterion concentration.
For steady tangential electro-osmosis, with no imposed pressure gradient and negligible inertia, the Stokes equation is . Since ,
The conditions and give
The printed constant speed is the bulk velocity outside the double layer, not the velocity at the no-slip wall. With negative the positive counterion excess drives fluid along the applied field. The far-field value is the Helmholtz-Smoluchowski electro-osmotic velocity.[ref]
For the finite channel, first model the added wall as an ideally uncharged insulating boundary with no normal field on its outer side: , while . The one-charged-wall electro-osmotic channel then has
Integrating the same force balance and enforcing gives
For , the maximum occurs at
In that limit : the velocity rises rapidly from zero at the charged wall, reaches a maximum a few screening lengths away, then falls approximately linearly to zero at the neutral wall. One charged wall does not give a symmetric plug across a channel with no-slip at the other wall.
An alternative electrode condition means a wall held at reservoir potential; it is not the same as zero surface charge. Under that convention,
with . Both boundary conventions have the same leading thin-double-layer profile above. An externally imposed pressure gradient would add a pressure-driven profile; none is specified here.
For dilute nonadsorbing uncharged polymers in equilibrium or sufficiently weak flow, the entropic polymer depletion near nonadsorbing walls suppresses chain configurations near each wall. A depletion layer of order the coil radius of gyration is expected at both walls, with a bulk-like central region when is much larger than the coil size. Strong confinement rounds this into a central enrichment. Neutrality removes a direct electrophoretic force, not excluded-volume entropy. Adsorption, concentration and strong-flow migration were not specified, so this is a conditional equilibrium sketch rather than a universal flowing-polymer profile.
Figure 1.
Weak screening gives symmetric first-order ion excess and deficit, while stronger potentials separate co-ion depletion from counterion accumulation
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Figure 2.
A channel driven at only one wall has an asymmetric velocity maximum; nonadsorbing polymer coils are depleted near either wall
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