Shifts in the pH of buffer solutions
upon freezing have received
much attention particularly in the life sciences, as such pH variations
during freezing may damage biological samples, biomolecules, and pharmaceuticals.
The understanding and prediction of the said pH changes upon freezing
are essential to utilize buffer solutions in a wide temperature range,
including subzero temperatures. Phosphate is of particular importance
for aqueous buffer preparation as it covers a wide pH range and displays
high biocompatibility. However, the phase behavior and pH changes
in phosphate buffers at subzero temperatures are very complex due
to the variety of species involved in the phase and acid–base
equilibria. This paper focuses on the interpretation of the pH changes
in phosphate buffers under freezing conditions using an extended universal
quasichemical (EUQ) model. This model has been previously applied
to understand the phase behavior (solid precipitation) in phosphate
buffers at subzero temperatures but not to the calculation of the
pH of the liquid phase (freeze-concentrated solution, FCS) that coexists
with ice and salt precipitate. Since the EUQ model provides activity
coefficients for all of the components in the system, not only the
phase behavior but also the pH value can be estimated. The calculated
pH values are compared to experimental values and are interpreted
from the viewpoints of salt deposition, salt enrichment in the FCS,
and supercooling effects.