期刊
CARBON
卷 42, 期 8-9, 页码 1435-1445出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.carbon.2003.12.090
关键词
graphite; single crystals; scanning electronic microscopy; Raman spectroscopy; mechanical properties
Herein we report on the response of graphite single crystals-loaded parallel to their c-axis-to a 13.5 mum radius spherical diamond nanoindenter. Up to loads of 5 mN, corresponding to stresses of approximate to0.5 GPa, fully reversible hysteresis loops are observed. At stresses >0.5 GPa, the first loops are slightly open; subsequent loops, in the same location, are fully reversible and harder than the first. Simple compression experiments on polycrystalline cylinders yielded qualitatively similar results. Our results, together with much of the literature on the mechanical properties of graphite, can be explained by invoking the formation of incipient kink bands, IKB's, that give way to mobile dislocation walls that, in turn, coalesce into kink boundaries with increasing stress. The IKB's are fully reversible; the dislocation walls result in plastic deformation, and the kink boundaries explain the hardening. Since the dislocations are confined to the basal planes, they cannot entangle and can thus move reversibly over relatively large distances resulting in the dissipation of substantial amounts (up to 100 MJ/m(3)) of energy during each cycle. At stresses > 1. 5 GPa, massive pop-ins-of the order of 60 mum - are observed. Examination of the craters formed provided direct evidence for kink bands and the formation of a multitude of subgrains under the indenter. Based on this work, it is clear that graphite is a member of a larger class of solids-kinking nonlinear elastic solids-that includes the M(n+1)AX(n) phases, layered silicates, nonlinear mesoscopic elastic solids, among others. (C) 2004 Elsevier Ltd. All rights reserved.
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