Freeze-fracture

Freeze-fracture is a natural occurrence leading to processes like erosion of the earths crust or simply deterioration of food via freeze-thaw cycles.

Ambient gases, often water vapor, will condense on the cold surfaces, reacting with them, obscuring detail and further warming the object allowing it to reshape.

Freezing something from liquid or gas phase to a solid allows fracture but has different effects depending on the material involved and how quickly it is frozen.

In the example of water, ice forming slowly results in larger crystals leading to a clear glass like substance.

If frozen quickly as with snow, the crystals are smaller and less organized, scattering light and appearing white.

Changes in the eutectic around the forming crystals is also significant which can be disadvantageous, or used in the case of cooling solder advantageous.

The requirement for freeze-fracture studies may increase with extra-planetary objects having surface temperatures cold enough for elements that are gases on earth to be naturally solid.

Excessive stress results in multiple almost simultaneous fractures, as when shattering a sheet of glass with a hammer.

Better know examples relate to preventing freeze-fracture damage to water supply pipes or engine cooling systems in colder climates.

The sudden release of the energy fractures the entire pane into small less damaging pieces, as with a car windscreen.

[20] Materials and colloid sciences use freeze-fracture techniques to investigate the nature of more complex substances.

Due to the conditions required for the transmission electron microscope at the time the rapidly frozen and fractured virus itself could not be viewed directly.

Instead Steere made a carbon re-enforced chromium replica of the fractured surface based on a procedure devised by others.

[23] Steere overcame the problem of ice crystals forming on the fractured viruses by etching them away as done by others in 1955 prior to making the copy for viewing.

[25] Much cheaper, non-commercial alternatives which did not rely on a microtome or etching to clean the fracture face were later established.

[26] For the Bullivant & Ames method cheaply modified standard coating machines already routinely used in electron microscope laboratories, initially using a Meccano set.

For smaller electron microsopy labs these could be more easily used than a large, specialized, commercial piece of freeze-fracture etch replication equipment.

During the 1960s-1980's it became apparent that the cell's lipid bilayer was shown to split into two halves revealing the interior when fractured under suitable conditions.

Natural freeze-fracture. An iceberg fractured off a glacier. Erosion reveals the layering hidden within the original glacier
Snowflake macro photography
Two forms of amorphous ice. High density (HDA) top and low density amorphous (LDA) ice bottom
Iceplanet
Freeze-fracture and replicated yeast cell at -50°C with two prominent circular bud scars. The ice surrounding the cell melted due to the heat of the fracture, flowed a few microns, and quickly refroze again.
Ice blocks are cut and loaded onto a horse drawn sled circa 1935
Ais kacang
Fracture failure of a steel pipe due to cold temperatures
Concrete fracture
Platinum coated surface of fracture face of glass reinforced plastic SEM Stereo 500x
Freeze fracture under liquid nitrogen followed by production of a platinum/carbon replica.
Freeze-fracture Replication shielding block built in 1984 after Bullivant and Ames 1966
Commercial Freeze Etching Replication device circa 2000
The interior of a sheep lens cell plasma membrane. The smooth areas mainly at the top of the picture are mainly lipid membrane. The rough areas correlate to areas of protein in the membrane. When viewed closely the Freeze-fracture replica immunolabling (FRIL) reveals the gold beads averaging 5nm in size coated in anti-Cxn46 antibodies. They pepper the visible portion of the gap junction containing the protein [ 17 ]