It is well known that the surface which is formed during the mechanical fracture of crystals of silicon, diamond, silicon carbide, and several other materials manifests paramagnetic properties [ 1]. The ESR signal which is observed is usually ascribed to "broken bonds" which are localized in the surface layer. The scatter in the data for the surface spin density of the centers (2- 1012-2 �9 1013 cm -2 for ehippings [2, 3] and 3- 1014 cm -2 after crushing, polishing, grinding, etc., of silicon crystals [4, 5]) provides grounds for suggesting that there is a relationship between the formation of surface states and the conditions under which the crystals are fractured. The problem of fracture is closely associated with that of comminution, which is one of the most extensively used processes in powder technology, and also with the problem of the mechanical activation of disperse media. The lack of a single opinion concerning the nature of mechanical activation stimulated us to carry out a detailed investigation of the properties of powders as a function of the conditions under which they were prepared. In the present work, we have studied the properties of powders prepared by crushing silicon carbide in air in a mortar, with a ball mill, and with a disintegrator (UDA-2 with six in-line, fingerlike rotors at maximum impact rates of 100, 200, and 270 m/see) at room temperature. Crystalline powders of technical grade ~-SiC with an average particle size of N200 t~m served as the initial samples. The ESR spectra were measured on an RE-1301 radiospectromete r at room temperature. At 77~ an intense ESR signal was manifested by the samples which arose from impurity nitrogen atoms and made it difficult to observe the lines from the
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