Preferential interactions of proteins with water and osmolytes play a major role in controlling the thermodynamics of protein solutions. While changes in protein stability and shifts in phase behavior are often reported with the addition of osmolytes, the underlying protein interactions with water and/or osmolytes are typically inferred rather than measured directly. In this work, Kirkwood−Buff integrals for protein−water interactions (G 12 ) and protein−osmolyte interactions (G 23 ) were determined as a function of osmolyte concentration from density measurements of antistreptavidin immunoglobulin gamma-1 (AS-IgG1) in ternary aqueous solutions for a set of common neutral osmolytes: sucrose, trehalose, sorbitol, and poly(ethylene glycol) (PEG). For sucrose and PEG solutions, both protein−water and protein−osmolyte interactions depend strongly on osmolyte concentrations (c 3 ). Strikingly, both osmolytes change from being preferentially excluded to preferentially accumulated with increasing c 3 . In contrast, sorbitol and trehalose solutions do not show large enough preferential interactions to be detected by densimetry. G 12 and G 23 values are used to estimate the transfer free energy for native AS-IgG1 (Δμ 2 N ) and compared with existing models. AS-IgG1 unfolding via calorimetry shows a linear increase in midpoint temperatures as a function of trehalose, sucrose, and sorbitol concentrations, but the opposite behavior for PEG. Together, the results highlight limitations of existing models and common assumptions regarding the mechanisms of protein stabilization by osmolytes. Finally, PEG preferential interactions destabilize the Fab regions of AS-IgG1 more so than the C H 2 or C H 3 domains, illustrating preferential interactions can be specific to different protein domains.