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  • Title: Optimum conditions for cryoquenching of small tissue blocks in liquid coolants.
    Author: Elder HY, Gray CC, Jardine AG, Chapman JN, Biddlecombe WH.
    Journal: J Microsc; 1982 Apr; 126(Pt 1):45-61. PubMed ID: 7069794.
    Abstract:
    Three approaches were taken with the aim of defining the optimum conditions of rapid cryopreservation in liquid quenchants. In a theoretical approach, two mathematical models were used. The first is of value in defining the absolute maximum rates of cooling which could be achieved at various depths in the tissues. The second highlights the poor thermal properties of liquid coolants and therefore emphasizes the essential requirement for vigorous quenchant mixing and rapid specimen entry. Experimental work with thermocouples showed that fastest cooling rates occur at the leading edge of the object entering coolant. Of five quenchants investigated, cooling rates were in the order, propane greater than Freon 22 greater than Freon 12 greater than liquid nitrogen slush greater than liquid nitrogen. Other considerations, however, may affect the choice of quenchant. For a given quenchant, cooling rate is maximal near the equilibrium freezing point. The consequences of quenching in the presence of thermal gradients either within the coolant or in the gas layer above it are shown. Cooling rate was found to be approximately proportional to entry velocity at least up to approximately 2 m s-1 in our system. Stereological analysis of rapidly quenched, freeze-substituted tissue samples, of geometry which imposed an approximately unidirectional heat flow, revealed four zones: (i) a narrow surface layer (approximately 10 micrometers) of low image contrast and apparent of ice crystals; (ii) a zone of enhanced contrast with ice crystals whose size increased rapidly with depth from the surface (the 'slope'); (iii) a sharply defined zone (the 'ridge') of maximum ice crystal size beyond which there is (iv) an extensive 'plateau' with smaller ice crystals and no marked increase in size with depth. The 'ridge' of maximal ice-crystal damage was consistently found but varied considerably in depth from the surface (approximately 25-120 micrometers) between samples. The existence of the deeper plateau region of relatively uniform ice-crystal-size may be of significance in X-ray microanalytical studies of physiological processes at some depth from the sample surface. In terms of our present understanding of the quenching process, the conditions for optimal cryofixation of small tissue samples are listed.
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