Abstract The advantages of the original form of the predictive expression for the gas/particle partition constant Kp (m3 μg−1) are considered. The expression Kp,i for compound i contains p L , i o , ζ i and MW ¯ . These are the pure-compound liquid vapor pressure, the mole-fraction-scale activity coefficient in the absorbing particulate matter (PM) phase, and the mean molecular weight (g mol−1) of the absorbing phase. Algorithms are available for predicting ζ i values in mixtures of organic compounds and water as they are affected by energetic and entropic effects; Flory–Huggins Theory provides a convenient way to examine the entropic effects of the presence of high MW compounds on the ζ i values of lower MW compounds. In the exposition of their volatility basis set (VBS) approach for modeling organic aerosol condensation, Donahue et al. (2006, Environ. Sci. Technol., 40, 2635–2643, Supplementary Material) argued that the need to consider MW ¯ values can be avoided by switching from the mole fraction scale to a mass fraction scale and accompanying C i ∗ values that incorporate mass-fraction-scale activity coefficient values ζ i ′ . In practice however, the VBS approach usually ignores both activity and MW ¯ corrections by setting ζ i ′ = 1 . (An equation for ζ i ′ is developed here in the event that modeling with ζ i ′ ≠ 1 becomes of interest.) Regardless of the advantages of the prediction equation for Kp,i, there will undoubtedly be circumstances when MW ¯ and ζ i values become inaccessible, as for aged organic particulate matter in which a large mass fraction of the absorbing PM of is of indeterminable molecular nature. In such cases, “prediction” of Kp,i values may only be possible by means of empirical correlation of log Kp,i vs. log p L , i o for the PM type of interest.