Physical review. E, Statistical physics, plasmas, fluids, and related interdisciplinary topics · 1996 · 262 citations · 51 references
Natural SciencesChemistryCondensed Matter PhysicsMolecular BiophysicsPhysical ChemistryCrystallization ProcessesPhase ChangePhase EquilibriaPhase TransitionsSolid-liquid InterfacesSolid-liquid SeparationAqueous Salt SolutionsCloud Point TemperatureLiquid - Liquid Phase SeparationLiquid-liquid Phase SeparationPhase Behavior Of BiomoleculesProtein Phase SeparationSalt Effects On Phase FormationSolid-liquid Phase Separation
The Derjaguin‑Landau‑Verwey‑Overbeek theory for charged spheres cannot explain our observations, indicating that hydration forces play an important role in protein interactions. We investigated liquid‑liquid and solid‑liquid phase separation of aqueous lysozyme solutions. We experimentally determined that the cloud‑point temperature is 15–45 °C below the crystallization temperature, indicating highly metastable liquid‑liquid phase separation, and that adding chloride, bromide, and sulfate salts shifts the cloud‑point by up to 60 °C depending on salt identity, with similar effects on crystallization temperature. © 1996 The American Physical Society.
We have investigated liquid-liquid and solid-liquid phase separation of aqueous solutions of lysozyme. We have determined experimentally how the phase transition temperatures depend on protein concentration and the ionic composition of the solution. For a wide range of solution conditions, we find that the cloud-point temperature ${\mathit{T}}_{\mathrm{cloud}}$---which signals the onset of liquid-liquid phase separation---is 15--45 \ifmmode^\circ\else\textdegree\fi{}C below the crystallization temperature ${\mathit{T}}_{\mathrm{xtal}}$. This indicates that liquid-liquid phase separation occurs in a highly metastable solution. When a series of chloride, bromide, and sulfate salts are added to lysozyme, we find that ${\mathit{T}}_{\mathrm{}\mathrm{cloud}}$ varies by as much as 60 \ifmmode^\circ\else\textdegree\fi{}C over the salt concentration range of 0.2M to 1.5M. The precise change in ${\mathit{T}}_{\mathrm{cloud}}$ depends sensitively on the identities of both the cation and the anion of the added salt. The effect of salts on ${\mathit{T}}_{\mathrm{xtal}}$ is very similar to their effect on ${\mathit{T}}_{\mathrm{cloud}}$. The Derjaguin-Landau-Verwey-Overbeek theory for the interaction energy between charged spheres cannot account for our observations and indicates that hydration forces play an important role in protein interactions. \textcopyright{} 1996 The American Physical Society.
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