Abstract
Diffusion in purified natural graphite crystals was studied by two techniques. Crystals with C14 atoms on the surface were prepared by heating at 1575°C for thirty minutes in a mixture of radioactive carbon monoxide and helium. These crystals were heated at diffusion temperatures in vacuo, and the C14 distribution within the crystals was determined by burning them slowly and measuring the radioactivity in the carbon dioxide produced. Diffusion measurements were carried out for times up to twenty-five hours in the temperature range 1995°-2195°C. The results indicated that simultaneous diffusion into single-crystal regions and into disordered regions occurred.

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