The activation energy of GeO2 was studied by determining the oxide thickness versus temperature from lower to higher oxidation temperature in the range between 450˚C and 600. It was found that a linear relationship can be obtained between oxidation time and oxide thickness for the oxidation temperature between 450 and 575 while for the 600 , a linear relationship can be obtained for the shorter oxidation time. The rate of oxidation increased until 0.55 and abruptly decreased after increasing oxidation temperature to 600 which implies that the oxygen intermixing occurs during higher oxidation (600) rather that diffusion mechanism that leads to the lower activation energy.

No abstract

No abstract