The theoretically predicted anisotropic nature of the indentation phase transformation in silicon (Si) is observed directly in experiments using hyperspectral, confocal Raman microscopy. The anisotropy is reflected in the two-dimensional distribution of the residual diamond cubic Si-I phase and high-pressure phases in indented Si(001), Si(110), and Si(111) surfaces, and is linked to the number and orientation of the {111}110 slip systems of the diamond cubic phase that are activated during indentation. Key to the observation of the anisotropic phase transformation is the local preservation of Si-I in the residual contact impression, which is controlled by the magnitude of the applied indentation strain, εI. The condition for islands of Si-I to be retained after indentation is 0.04 εI 0.01; strains outside of this range either do not result in a residual contact impression or completely transform the contacted material, rendering the underlying anisotropy of the phase transformation unobservable.
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Gerbig et al. (2011) studied this question.
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