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Updated: May 6, 2026

Generation and Control of Electrohydrodynamic Flows in Aqueous Electrolyte Solutions
Published on: September 7, 2018
Ionic flows through a single homogeneous membrane : A thermodynamic analysis
1Institute of Physiology, Aarhus University, Aarhus, Denmark.
The Kedem-Katchalsky equation, a model for salt flow through membranes, is expanded from Kirkwood-Bearman-Spiegler equations. This provides a more general ionic flow equation applicable even with impermeable salts.
Area of Science:
- Physical Chemistry
- Membrane Science
- Transport Phenomena
Background:
- The Kedem-Katchalsky (KK) equation models mono-monovalent salt flow across permselective membranes.
- It's derived as an expansion of the Kirkwood-Bearman-Spiegler (KBS) equations.
- Assumptions include concentration-independent frictional coefficients.
Purpose of the Study:
- To present a first-order expansion of the KBS equations for salt flow.
- To explore the validity conditions for this expansion.
- To derive a more general ionic flow equation applicable when impermeable salts are present.
Main Methods:
- Integration of the Kirkwood-Bearman-Spiegler equations under specific assumptions.
- Derivation of a generalized ionic flow equation.
- Comparison with the existing Kedem-Katchalsky and Goldman equations.
Main Results:
- A first-order expansion of the KBS equations, closely related to the Goldman equation, is presented.
- Conditions for the validity of this expansion are established.
- A new, more general ionic flow equation is derived, encompassing situations with impermeable salts where KK parameters may be ill-defined.
Conclusions:
- The derived general equation offers a broader framework for understanding ionic flow across membranes.
- The Kedem-Katchalsky equation for salt flow is shown to be a special case of this more general formulation.
- This work refines the understanding of transport phenomena in charged membranes, especially under complex solution conditions.
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