Oxygen was in-diffused into the float zone silicon either during oxidation or upon annealing in argon of previously oxidized Si wafers. The resultant in-depth profiles of the main isotope 16O were measured by secondary ion mass spectrometry (SIMS) with detection limit below 1016 cm−3. The oxygen solubility Cs, as determined from the 16O surface concentration, was found to be insensitive to the annealing ambient. This observation seems to contradict the effect of enhanced solubility under oxidizing conditions, reported for the in-diffused 18O isotope. Over a temperature range of 900–1250 °C, the solubility of oxygen can be expressed by a relationship Cs = 9.1 × 1022 cm−3 exp(−1.57 eV/kT). The surface concentration of oxygen out-diffused from supersaturated CZ Si appears to be significantly higher than that of in-diffused 16O. This is because the out-diffusion process is accompanied by precipitation of oxygen atoms into immobile SiO2 particles. As a consequence, SIMS measurements of the out-diffusion profile cannot provide reliable information on the solid solubility of oxygen.
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