Raman spectrum of the graphite edge plane is different from that of the cleaved basal plane because the 1355 cm-' and 1620 cm-' bands are clearly observed. These spectral features of the edge plane have been interpreted to be due to the structural imperfection caused by polishing. In the present wor
Raman spectra of ground natural graphite
โ Scribed by M. Nakamizo; H. Honda; M. Inagaki
- Publisher
- Elsevier Science
- Year
- 1978
- Tongue
- English
- Weight
- 430 KB
- Volume
- 16
- Category
- Article
- ISSN
- 0008-6223
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โฆ Synopsis
Structural changes in Ceylon natural graphite with grinding were studied by &man spectroscopy along with X-ray diffraction. The natural graphite shows a single Kaman band at 1580cm-', but the ground graphite samples exhibit two Raman bands at 1360 and 1620 cm-' in addition to the 1580 cm-' graphite band. The 1360 cm-' band increases in intensity with increasing grinding time, and becomes much stronger than the 1580 cm-' band after 200~hr grinding. Raman results are compared with structural parameters such as effective Debye parameter and CO spacing obtained from X-ray diffraction measurements, and discussed in terms of structural defects introduced into the crystal lattice of natural graphite. A linear rela~onship was obtained for the ground graphite when the relative intensity of the 1340 cm-' band is plotted as a function of effective Debye parameter. The slope of the linear plot is diKerent for the ground graphite from that for the graphitized cokes, indicating a difference in the type of structural defects involved.
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