Abstract
Migration of vacancies in crystalline, n-type silicon at room temperature from Ge+-implanted (150 keV, 5×109-1×1011 cm-2) surface layers was studied by tracing the presence of P-V pairs (E centers) in the underlying layer using deep level transient spectroscopy (DLTS). Under the conditions we have examined, the vacancies migrate to a maximum depth of about 1 μm and at least one vacancy per implanted Ge ion migrates into the silicon crystal. The annealing of the E centers is accompanied, in an almost one-to-one fashion, by the appearance of a new DLTS line corresponding to a level at EC-Et≈0.15eV that has donor character. It is argued that the center associated with this line is most probably the P2-V complex; it anneals at about 550 K. A lower limit of the RT-diffusion coefficient of the doubly charged, negative vacancy is estimated to be 4 × 10-11 cm2/s. © 1999 American Institute of Physics.
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CITATION STYLE
Nylandsted Larsen, A., Christensen, C., & Wulff Petersen, J. (1999). Room-temperature vacancy migration in crystalline Si from an ion-implanted surface layer. Journal of Applied Physics, 86(9), 4861–4864. https://doi.org/10.1063/1.371453
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