The Aqueous Electrolyte Transport (aqt) interface (

), found under the
Electrochemistry branch (

), is used to solve for the mass transport of an arbitrary number of species in water-based systems subject to potential gradients. The species transported can be any combination of weak and strong acids and bases, ampholytes, and uncharged species. The transport of mass and charge is based on the Nernst–Planck equations for molecular transport, in combination with electroneutrality and dissociation equilibria for weak acids, bases, and ampholytes as well as the water autoionization reaction.
The Label is the default physics interface name.
The Name is used primarily as a scope prefix for variables defined by the physics interface. Refer to such physics interface variables in expressions using the pattern
<name>.<variable_name>. In order to distinguish between variables belonging to different physics interfaces, the
name string must be unique. Only letters, numbers, and underscores (_) are permitted in the
Name field. The first character must be a letter.
The default Name (for the first physics interface in the model) is
aqt.
The Include out-of-plane thickness in the time derivative in material balances (or
Include cross-sectional area in time derivative in material balances) checkbox (depending on component dimension) is by default selected. When selected, any time-dependent out-of-plane expansion or contraction will change the species concentration in the domain. Since the concentration is uniform in the out-of-plane direction, this setting can be useful to simulate thin films that grow or shrink; for instance, water evaporation or condensation.
Mass transport due to diffusion and migration is included by default. If the Solve for electrolyte phase potential checkbox is cleared, the potential can be set manually to a constant value (the default is 0 V) in the
Electrolyte node.
Use the checkbox available under Additional transport mechanisms to control convective transport. By default, the
Convection checkbox is cleared.
To display this section, click the Show More Options button (

) and select
Stabilization in the
Show More Options dialog. By default, the
Isotropic diffusion checkbox is not selected because this type of stabilization adds artificial diffusion and affects the accuracy of the original problem. However, this option can be used to get a good initial guess for under-resolved problems.
To display this section, click the Show More Options button (

) and select
Advanced Physics Options in the
Show More Options dialog. Normally these settings do not need to be changed. Select a
Material Balance Form —
Nonconservative (the default) or
Conservative. Use the conservative formulation for compressible flow. Note that the setting not only dictates the convective term but also the accumulation term in the material balance for porous media.
The Compute boundary fluxes checkbox is activated by default so that COMSOL Multiphysics computes predefined accurate boundary flux variables. When this option is checked, the solver computes variables storing accurate boundary fluxes from each boundary into the adjacent domain.
Also the Apply smoothing to boundary fluxes checkbox is available if the previous checkbox is checked. The smoothing can provide a more well-behaved flux value close to singularities.
The concentration-dependent variables are named as aqt.xxx, where
aqt is the name of the interface as set above, and the
xxx string is controlled by the
Species name setting on the individual species nodes.