In-situ phase transformation in the field ion microscope.

Physics

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Scientific paper

Many materials undergo an athermal martensite transformation when cooled. This transformation has been observed in the Tishomingo meteorite during cooling to cryogenic temperatures. The meteorite is unstable when cooled to the cryogenic temperatures (40 - 85K) suitable for field ion imaging since the martensite start temperature of this material (Fe-32.5 wt%Ni) is approximately 235K.

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