2.4.1. Temperature and the Change of States of Pure Water during a Cooling Process
In order to establish a vitrification protocol, it is essential to understand the following issues: (i) At which temperature (T°) do we obtain a vitrified state, (ii) at which temperature range does crystallization occur, (iii) under which (additional) conditions do we reach a vitrified state, (iv) the change of physical and chemical states during temperature changes according to the type of solutions or environment.
Water molecules are the major component of cells. Luyet has already postulated that an excess of free water is incompatible with survival after cryopreservation, due to ice crystal formation disrupting the cellular organelles and structures [
17]. In viable cells, water is the solvent for intracellular molecules, such as salts, acids, or bases, essential for cell function [
23]. In cryopreservation, water is also the solvent for permeable and non-permeable CPA. Water has to be considered as the major player to be mastered during the cryopreservation process [
24].
How can cells survive the cryopreservation process despite their high water content? Depending on the T° (and atmospheric pressure), water exists in three physical states: Solid, liquid, and gaseous. Generally, when the temperature drops (winter conditions, storage in the freezer), the solidification of water is thought to be associated with the formation of ice crystals. However, for the cryobiologist, water can solidify in two distinct forms. From the liquid state, water can either solidify as a liquid crystal of pure water or, under extremely rapid cooling conditions above 100,000 °C/min, a spray of water converts as a solid without crystal formation [
25,
26,
27]. It is then solidification of pure water, which is described as an amorphous or glassy state [
28,
29].
(A) The crystalline solid form of water
The formation of the crystalline solid form of water is shown on the left part of
Figure 1. The changes in the physical states of pure water in correlation to the decreasing temperature (T°) are presented. When the temperature falls below 0 °C, aqueous fluids do not freeze immediately but first “supercool”. The crystallization initiation temperature lies in a range between the equilibrium melting temperature (Tm) and the homogeneous nucleation temperature (Th). This zone is characterized by the phenomenon of supercooling and heterogeneous nucleation. Heterogeneous nucleation occurs when particles in water are present, promoting the formation of ice crystals. In the state of supercooling between Tm and Th, there is a competition between the formation of crystallization nuclei and the disappearance of these same nuclei in the liquid. The water molecules remain extremely mobile and free to reorient themselves almost independently of each other. Hydrogen bridges between water molecules are formed and break, due to the continuous movement of the molecules. As long as the crystal formation has not reached a critical mass, the tendency to dislocate prevails, explaining why water can remain supercooled down to temperatures as low as −40 °C [
30].
As the temperature drops, the state of supercooling cannot indefinitely continue. The movement of water molecules slows down, and the critical mass of the crystal nucleus formation is finally sufficient to induce solidification as Th approaches [
31,
32]. Once nucleation seeds are formed, the structure becomes rigid, and nucleation seeds can aggregate into larger crystals. When Th is reached, the system ends up crystallizing uniformly even in the absence of any crystallization seeds and transforms into a stable state as a crystalline solid [
33].
(B) The glassy solid-state of water
Solidification of pure water in a glassy solid form (vitrification) is achieved when the temperature decreases extremely rapidly below the glass transition temperature (Tg;
Figure 1). Is was found that Tg for pure water is −137 °C [
34] and only possible with cooling (C) rates exceeding 100,000 °C/min to avoid spontaneous crystal nucleation when crossing the zone between Tm and Tg [
22,
23,
24].
Below Tg, the movement of water molecules is too slow to organize the start of crystallization, and the solution solidifies with water molecules arranged in a completely disordered state. In other words, under these experimental conditions of very rapid cooling rates, water has the ability to remain in a supercooled state. Thereby, low temperatures in association with an extreme increase in viscosity are important. These two factors induce that water molecules are no longer be able to organize themselves into a crystalline structure, and an amorphous or vitreous solid-state is achieved. Almost intact intermolecular bonds are typical of the liquid state that characterizes the amorphous or vitreous solid-state [
28,
29].
Figure 1 shows that lethal ice crystal formation occurs during the transit through Tm and Tg. In the case of pure water, the probability of reaching the glassy state during the lowering the T° is dependent on the speed of cooling (C) and the volume (Vol) of the liquid. This can be expressed by the simple equation:
At slow cooling rates, the formation of crystals is directly observed (pure water becomes a milky color); in contrast, at extremely high cooling rates (which are not applicable in our IVF laboratories), a glassy solid-state is observed when pure water reaches Tg (with transparent appearance).
2.4.2. Shifting of the Glass Transition Temperature (Tg) in Cryoprotectant Solutions
During the development of the different cryopreservation techniques, it was soon recognized that biological material cannot survive at very low temperatures without the usage of water-soluble CPA. Due to their polarity, CPA have a great capacity to form hydrogen bonds with water molecules, due to their hydroxyl residues (glycerol, ethylene glycol, 1-2 propanediol, propylene glycol) or sulfoxide groups (e.g., DMSO). Membrane diffusible CPA are not only highly soluble in the aqueous environment, but also intracellularly and can enter into the cell mainly through specific aquaporin channels. During incubation of cells with solutions containing CPA, a part of the intracellular free water will be replaced by a CPA solution. CPAs increase the viscosity and thereby lead to a slowdown of the molecular movements of the water [
35]. An increase in viscosity results in (i) a delay of the nucleation phenomenon, (ii) a reduction of the growth rate of ice crystals, (iii) a limitation of the size of the crystals between Tm and Tg, and (iv) an impairment of crystal formation in the case of the huge increase in viscosity during drop in the T°.
It has to be considered that Tm, Th, Tg for pure water are defined and constant (
Figure 1). However, aqueous solutions (e.g., culture media containing salts, amino acids, and proteins, or cryopreservation solutions containing salts, amino acids, proteins, and CPA) show different Tm, Th, and Tg. The shift in these parameters depends on the respective concentration and composition of solved molecules and CPA [
23]. For each change in the concentration of salt or cryoprotectant Tm, Th and Tg have a specific value. The shift of Tm, and consequently, Th and Tg can be visualized on a phase diagram divided into three zones corresponding to the different phases: (i) Liquid, (ii) crystalline solid, and (iii) glassy or amorphous solid (
Figure 2) [
36].
Above Tg, the solutions are either supercooled or in a state of a crystalline solid. Below Tg, a supercooled solution can go directly transform from a liquid state into a state called a glassy solid, or amorphous ice. It should be mentioned, however, that crystalline solid water formed at a temperature above Tg will remain crystalline when cooling down below Tg. Therefore, to achieve a glassy solid-state Tm to Tg has to be passed without crystal formation.