Models for calculating activity coefficients in electrolyte solutions are essential tools for predicting the effective concentration of ions. They vary based on ionic strength:
Debye–Hückel (limiting law): For very dilute solutions (I ≤ 0.01 M).
Davies equation: A simple, general-purpose model for moderate concentrations (I ≤ 0.5 M).
Extended Debye–Hückel: Offers improved accuracy for multivalent ions by including an ion size parameter.
Pitzer / SIT models: For high ionic strength solutions (I > 0.5 M), accounting for complex ion interactions.
These models are primarily for 25°C aqueous solutions, and parameter adjustments are needed for other conditions.
Reference: Ronteltap M, Maurer M, Gujer W. Struvite precipitation thermodynamics in source-separated urine. Water Res. 2007 Mar;41(5):977-84. doi: 10.1016/j.watres.2006.11.046. Epub 2007 Jan 25. PMID: 17258264.