Abstract
The intensity of the infrared absorption band at 1107 cm −1, related to interstitial oxygen (O i ) concentration, decreased as the Ge concentration increased in Ga and Ge codoped CZ–Si crystals. In contrast, the number of precipitates observed on the etched surfaces of CZ–Si wafers increased as the Ge concentration increased. From an energy dispersive X-ray (EDX) analysis, O was observed to be one of the major components of the precipitates. Moreover, Ge was found as one of the components in the precipitate observed on the heavily Ge (>1×10 18 cm −3) codoped CZ–Si wafers. These results suggest that the grown-in O precipitates increase as the O i concentration decreases when the Ge concentration increases in the Si crystal. The Ge-vacancy ( V) complex in the Si lattice probably acted as a heterogeneous nucleation center and may enhanced the grown-in O precipitates thereby reducing the dissolved O i concentration in the Si lattice.
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