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Freeze‐fracturing at defined temperatures provides information on temperature rise during fracture, and on membrane complementarity
Author(s) -
Gruijters W. T. M.,
Bullivant S.
Publication year - 1986
Publication title -
journal of microscopy
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.569
H-Index - 111
eISSN - 1365-2818
pISSN - 0022-2720
DOI - 10.1111/j.1365-2818.1986.tb02723.x
Subject(s) - fracture (geology) , liquid nitrogen , membrane , chemistry , composite material , mineralogy , materials science , geology , biochemistry , organic chemistry
SUMMARY An apparatus is described which allows freeze‐fracturing at defined temperatures, followed by immediate immersion of the specimen in liquid nitrogen. Replication is carried out in a Bullivant & Ames (1966) freeze‐fracture device. Using yeast as a test specimen, the following results were obtained with the apparatus: (a) It was confirmed that fracturing at temperatures between 243 K and 223 K gave undeformed volcanoes on the PF of the plasma membrane, as shown originally by Steere et al. (1980). (b) Considerable energy is released by the fracturing process, both as shown by thermocouple readings and by the fact that at relatively high fracture temperatures portions of the specimen surface were melted. A temperature rise of 50–70 K was indicated, (c) Under standard conditions, there is a lack of complementarity between the yeast plasma membrane fracture faces, trigonal point particles not being present opposite the corresponding depressions in the array. Fracturing yeast suspended in salt solutions at 203 K demonstrates these particles. Their absence in normal fractures can be explained by ‘secondary fracture’, a concept based on polymer fracture studies.