Abstract
We report measurements of the heat capacity Cp of diamond with several isotopic compositions (12C1-x13C x) in the 20-280 K temperature range. The results, in particular the derivative of the specific heat with respect to the average isotopic mass, are compared with recent ab initio calculations. Agreement is good for T>150 K. At lower temperatures, the samples with isotopic compositions different from the natural one display an anomalous increase in Cp/T3 with decreasing temperature which is attributed to the presence of metallic inclusions stemming from the metal used as a solvent in the high-pressure high-temperature growth process.
Original language | English |
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Pages (from-to) | 465-468 |
Number of pages | 4 |
Journal | Solid State Communications |
Volume | 133 |
Issue number | 7 |
DOIs | |
State | Published - Feb 2005 |
Keywords
- A. Diamond
- D. Heat capacity
- D. Stable isotopes