Abstract
Kaiser and Bond1 showed, by mass-spectrographic analysis, that many type I diamonds contain up to 0.2 per cent of nitrogen-14 as impurity, and quantitatively correlated this fact with certain features of the type I infra-red and ultra-violet spectra. Smith et al.2 also found by electro-spin resonance measurements that there is a C—N bond in about one half of the diamonds examined. A correlation has now been established between spike intensity and ultra-violet transparency in natural diamonds3, and dislocation loops and segregated platelets, presumed to be nitrogen, have been observed in etched diamonds by transmission electron microscopy4. Kaiser and Bond deduced that the nitrogen is substitutional and not interstitial, on the basis of density measurements on eight diamonds of gem quality.
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References
Kaiser, W., and Bond, W. L., Phys. Rev., 115, 857 (1959).
Smith, W. V., Sorokin, P. P., Geller, I. L., and Lasher, G. J., Phys. Rev., 115, 1546 (1959).
Takagi, M., and Lang, A. R. (to be published).
Evans, T., First Intern. Congr. Diamonds in Indust. (Paris, 1962).
Lonsdale, K., Phil. Trans. Roy. Soc., A, 240, 219 (1947).
Grenville-Wells, H. J., Min. Mag., 29, 803 (1952).
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MILLEDGE, H., MEYER, H. Nitrogen-14 in Natural Diamonds. Nature 195, 171–172 (1962). https://doi.org/10.1038/195171a0
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DOI: https://doi.org/10.1038/195171a0
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