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II International Symposium on Carbon for Catalysis ABSTRACTS

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OP-I-28<br />

In 1970 Koenig et al have established a relati<strong>on</strong>ship between the ratio of intensities of G<br />

(1580 cm -1 ) and D (1350 cm -1 ) lines in the Raman spectra of various disordered sp 2 carb<strong>on</strong>s<br />

and the size of micro-crystallites in the basal plane L a [1]. The latter was measured by the<br />

WAXD method. Applicability of this relati<strong>on</strong>ship has been investigated by us, using the<br />

results of linear and planar Raman micro-mapping carried out <strong>for</strong> many samples of graphite of<br />

different origin and <strong>for</strong> other sp 2 -carb<strong>on</strong> modificati<strong>on</strong>s. The typical spectra of less-ordered sp 2<br />

carb<strong>on</strong> materials presented in Fig. 2 and 3 dem<strong>on</strong>strate their difference from the graphite<br />

spectrum.<br />

Fig.2 Raman spectrum of glassy carb<strong>on</strong><br />

Fig.3 Raman spectra of smoke-black<br />

1319<br />

1588<br />

1334<br />

1589<br />

1105<br />

900 1200 1500 1800<br />

Δν, cm -1<br />

800 1000 1200 1400 1600 1800<br />

Δν, cm -1<br />

The data obtained show that Koenig’s correlati<strong>on</strong> is not applicable to the crystallite<br />

size estimati<strong>on</strong>. Spectral criteria have been elaborated <strong>for</strong> identificati<strong>on</strong> of various sp 2<br />

carb<strong>on</strong> materials, based <strong>on</strong> the positi<strong>on</strong>, widths and c<strong>on</strong>tour of the D and G bands as well as<br />

I D /I G intensity ratio.<br />

Acknowledgements<br />

The authors acknowledge partial financial support from the Russian Foundati<strong>on</strong> <strong>for</strong> Basic<br />

Research (grant 04-03-32879) and from the program “Scientific School Support”<br />

(grant NSh-1765.2003.3).<br />

References<br />

[1] F. Tuinstra, J.L. Koenig, J. Chem. Phys. 1970, 53, 1126.<br />

92

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