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Ice nucleation and freezing in undercooled cells.
Cryobiology
|June 1, 1983
Summary
Differential scanning calorimetry (DSC) reveals that cells freeze above the homogeneous nucleation temperature for water. This suggests heterogeneous ice nucleation occurs within or on the cell surface, impacting cryobiology research.
Area of Science:
- Cryobiology
- Biophysics
- Materials Science
Background:
- Understanding cellular freezing is crucial for cryopreservation.
- Extracellular ice formation and chemical cryoprotectants are common considerations in cell cooling.
- Previous studies have not fully elucidated the intracellular freezing mechanisms.
Purpose of the Study:
- To investigate cellular freezing behavior using differential scanning calorimetry (DSC).
- To determine if cells freeze at temperatures above homogeneous nucleation of ice.
- To explore potential mechanisms of heterogeneous ice nucleation in various cell types.
Main Methods:
- Differential scanning calorimetry (DSC) was used to monitor cellular freezing.
- Experiments were conducted excluding extracellular ice and chemical cryoprotectants.
- Kinetic analysis of ice nucleation temperature dependence was performed.
- Freeze-fracture electron microscopy validated assumptions about ice growth rates.
Main Results:
- All studied cells, including human erythrocytes, yeast, and plant cells, froze above the homogeneous nucleation temperature of water.
- Plant cells and yeast showed a significant difference (approx. 9°C) compared to homogeneous nucleation, while human erythrocytes showed a smaller difference (0.5°C).
- Ice nucleation kinetics suggest heterogeneous mechanisms initiated within or on the cell, with plant cells/organelles as potential nucleators.
Conclusions:
- Cellular freezing is initiated by heterogeneous nucleation, either intracellularly or at the cell membrane.
- The kinetics of ice nucleation in human erythrocytes are highly temperature-sensitive and distinct from the suspension medium.
- Cell dimensions and internal structures likely play a role in heterogeneous ice nucleation during cooling.