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Coarse-Grained Strategy for Modeling Protein Stability in Concentrated Solutions. II: Phase Behavior

Vincent K. Shen ^*, Jason K. Cheung , Jeffrey R. Errington  and Thomas M. Truskett 

^* Physical and Chemical Properties Division, National Institute of Standards and Technology, Gaithersburg, Maryland; Department of Chemical Engineering, and Department of Chemical Engineering and Institute for Theoretical Chemistry, The University of Texas at Austin, Austin, Texas; and Department of Chemical and Biological Engineering, The State University of New York at Buffalo, Buffalo, New York

Correspondence: Address reprint requests to T. M. Truskett, Tel.: 512-471-6308; E-mail: truskett{at}che.utexas.edu.

We use highly efficient transition-matrix Monte Carlo simulations to determine equilibrium unfolding curves and fluid phase boundaries for solutions of coarse-grained globular proteins. The model we analyze derives the intrinsic stability of the native state and protein-protein interactions from basic information about protein sequence using heteropolymer collapse theory. It predicts that solutions of low hydrophobicity proteins generally exhibit a single liquid phase near their midpoint temperatures for unfolding, while solutions of proteins with high sequence hydrophobicity display the type of temperature-inverted, liquid-liquid transition associated with aggregation processes of proteins and other amphiphilic molecules. The phase transition occurring in solutions of the most hydrophobic protein we study extends below the unfolding curve, creating an immiscibility gap between a dilute, mostly native phase and a concentrated, mostly denatured phase. The results are qualitatively consistent with the solution behavior of hemoglobin (HbA) and its sickle variant (HbS), and they suggest that a liquid-liquid transition resulting in significant protein denaturation should generally be expected on the phase diagram of high-hydrophobicity protein solutions. The concentration fluctuations associated with this transition could be a driving force for the nonnative aggregation that can occur below the midpoint temperature.

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