Battery knowledge · Transport and modelling

Bruggeman relation

The common estimate of effective transport in a porous layer: multiply the bulk conductivity or diffusivity by porosity to the power 1.5. Real electrodes often deviate, so measured tortuosity is preferred when available. [1]

Relationship
D_eff = D · ε^1.5

Example

Estimate an effective diffusivity

Using the illustrative relation D_eff = D ε^1.5 with porosity ε = 0.4 gives D_eff ≈ 0.253D. This empirical geometry approximation does not replace a measured tortuosity.

Explore the graph

A Bruggeman relation approximates transport through a porous medium.

Effective diffusivity fraction
Effective diffusivity fractionPorosity ε (fraction) versus D_eff / D (fraction). εᵇ; Straight-pore scaling ε. Interpretation follows the graphs.000.250.250.50.50.750.7511Porosity ε (fraction)D_eff / D (fraction)
εᵇStraight-pore scaling ε (dashed)

At 40% porosity, D_eff is 25.298% of bulk diffusivity.

D_eff = D εᵇ

Illustrative model. An empirical pore-structure assumption; actual tortuosity must be characterized.

Use in Lemonergy

Specify phase, direction and boundaries.

This is a reference concept. No executable Lemonergy block has been verified for this term.

References & further reading

Technical references

  1. Modeling of Galvanostatic Charge and Discharge of the Lithium/Polymer/Insertion Cell

    Marc Doyle, Thomas F. Fuller, John Newman · Journal of The Electrochemical Society · 1993

    Technical reference · Porous-electrode transport and insertion-cell modeling; foundational work rather than a specification for a particular commercial cell.

Further reading on this topic

These sources provide broader context; they are not presented as citations for every statement in this entry.

  1. Quantities, Units and Symbols in Physical Chemistry, 3rd edition, 2nd printing

    IUPAC · 2011

    Topic background · Physical-chemistry notation, thermodynamics, electrochemistry and transport quantities.