“…Less certain, however, is the temperature at which its formation becomes significant. Calculations carried out by McAfee et al [13,14], Yan et al [18] and Wood et al [5] showed that GeO becomes a significant product in GeCl 4 oxidation at temperatures above 1700, 1800 and 1900 K, respectively. Unfortunately, even though limited data are available for the GeO M GeO 2 equilibrium reaction [5,19], no forward or backward reaction rate data could be found in the literature, as also noted recently by Tandon and Murtagh [20].…”