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Field evaporation of silicon as positive and negative ions in the field ion microscope and scanning tunneling microscope configurations is investigated with the charge-exchange model using atomic potentials from an empirical potential due to Tersoff [Phys. Rev. B 37, 6991 (1988)] and an environment dependent potential developed by Bolding and Andersen [Phys. Rev. B 41, 10 568 (1990)]. For the geometry of the field ion microscope, Si⁺ should be the observable ion species. In the close-spaced electrode geometry of the scanning tunneling microscope, Si^2- should be the favored ion species since it requires the lowest evaporation field.
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Miskovsky et al. (1992) studied this question.
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