4.3 Article Proceedings Paper

Oxygen isotopic exchange occurring during dry thermal oxidation of 6H SiC

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ELSEVIER SCIENCE BV
DOI: 10.1016/S0168-583X(01)01303-9

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silicon carbide; oxidation mechanisms; isotopic tracing

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SiC is a large band gap semiconductor, promising for high power and high frequency devices. The thermal oxide is SiO2 however the growth rates of thermal oxide on SiC are substantially slower than on Si. and different along the polar directions (<000 (1) over bar > and <0001> in the hexagonal polytypes). Thorough understanding of the oxide growth mechanisms may give us new insights into the nature of the SiO2/SiC interface, crucial for device applications. We have determined growth kinetics for ultra-dry thermal oxidation of 6H SiC at 1100 degreesC for pressures from 3 to 200 mbar. At 3 mbar, the lowest pressure studied. the oxide growth rates along the two polar directions are virtually the same. At higher pressures growth is faster on the carbon-terminated (000 (1) over bar) face. After consecutive oxidations at 1100 degreesC and 100 mbar in O-18(2) and O-16(2) gases, O-18 depth profiles show significant isotopic exchange and oxygen movement within the oxide during oxidation. (C) 2002 Elsevier Science B.V. All rights reserved.

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