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Science 6 December 1991:
Vol. 254. no. 5037, pp. 1489 - 1491
DOI: 10.1126/science.254.5037.1489

Articles

Phase Transformations in Carbon Fullerenes at High Shock Pressures

C. S. YOO 1 and W. J. NELLIS 1

1 Physics Department, H Division and Institute of Geophysics and Planetary Physics, Lawrence Livermore National Laboratory, University of California, Livermore, CA 94550

C60 powders were shock-compressed quasi-isentropically and quenched from pressures in the range 10 to 110 GPa (0.1 to 1.1 Mbar). Recovered specimens were analyzed by Raman spectroscopy and optical microscopy. C60 fullerenes are stable into the 13- to 17-GPa pressure range. The onset of a fast (sim0.5 µs) reconstructive transformation to graphite occurs near 17 GPa. The graphite recovered from 27 GPa and about 600°C is relatively well ordered with crystal planar domain size of about 100 Å. Above 50 GPa a continuous transformation to an amorphous state is observed in recovered specimens. The fast transformation to graphite is proposed to occur by pgr-electron rehybridization which initiates breakup of the ball structure and formation of the graphite structure at high density.

Submitted on September 17, 1991
Accepted on October 28, 1991


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
"Debye-Scherrer Ellipses" from 3D Fullerene Polymers: An Anisotropic Pressure Memory Signature.
L. Marques, M. Mezouar, J. Hodeau, M. Núñez-Regueiro, N. R. Serebryanaya, V. A. Ivdenko, V. D. Blank, and G. A. Dubitsky (1999)
Science 283, 1720-1723
   Abstract »    Full Text »
Fullerenes from the Geological Environment.
P. R. Buseck, P. R. Buseck, S. J. Tsipursky, and R. Hettich (1992)
Science 257, 215-217
   Abstract »    PDF »



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Science. ISSN 0036-8075 (print), 1095-9203 (online)