Abstract

Isochoric (constant volume) preservation is an alternative to traditional cryopreservation methods because it requires less cryoprotectant and is simple to operate. In order to validate that this method automatically minimizes the pressure for a given temperature, pressure and temperature data were collected from a specially designed pressure vessel. This vessel was then used to examine the effect of an isochoric environment on freezing point nucleation in an aqueous antifreeze protein solution, and to generate pressure–temperature phase diagrams for various cryoprotectant solutions. Our results show that the isochoric pressure vessel follows the pressure–temperature phase diagram of water, thereby minimizing the pressure for the given temperature. We also show that the nucleation temperature of the antifreeze protein in an isochoric vessel is lower than that of the isobaric method. Furthermore, the nucleation temperature decreased with increasing concentration in the isochoric vessel while the isobaric nucleation temperature showed no change. These results indicate that the isochoric environment imposes additional constraints on ice formation and warrants further study as these results may change when a different type of cryoprotectant is used. Finally, all of the cryoprotectant phase diagrams exhibited a similar pressure–temperature slope indicating that, regardless of the cryoprotectant used or the mechanism by which it suppresses freezing, isochoric freezing affects the molecules in the same manner. Together, all of these results indicate that the isochoric method of preservation is a valuable tool for characterizing the thermodynamic properties of cryoprotectants and has great potential as a cryopreservation method in the field of cryobiology.

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