F. Becker et al., DECOMPOSITION OF METHANE ON POLYCRYSTALLINE THICK-FILMS OF GA2O3 INVESTIGATED BY THERMAL-DESORPTION SPECTROSCOPY WITH A MASS-SPECTROMETER, Fresenius' journal of analytical chemistry, 358(1-2), 1997, pp. 187-189
Methane in air can be detected by the conductivity increase of Ga2O3 f
ilms. Films (200 mu m) of beta-Ga2O3 were prepared by depositing a sus
pension of beta-Ga2O3 powder (Johnson Matthey; 32102; 99,99%) on alumi
na substrates. The films were exposed to 20 kPa O-2 for 15 min at 934
K. In thermal desorption spectroscopy (TDS, beta = 4,6 K/s, UHV condit
ions) only O-2 occured at temperatures above 934 K. On reduction in 10
0 Pa H-2 for 5 min at 800 K, only a suboxide, Ga2O (above 880 K), indi
cating a destabilisation of the lattice [1], a broad hydrogen peak (44
0-930 K) and the formation of water (700-900 K) were observed. No Ga2O
3 and O-2 were found in desorption. At temperatures between 260 K and
934 K the film was exposed to methane (100 Pa, 5 min). For exposure te
mperatures between 630 K and 934 K, CO, CO2, H-2, and small amounts of
CH4 and the suboxide Ga2O appeared in desorption. A reaction scheme f
or the decomposition of methane is proposed. It includes the adsorptio
n of CH4, the dissociation of CH4, the desorption of H2O and the forma
tion of oxygen vacancies. These vacancies and the adsorbed hydrogen bo
th acting as donors may explain the conductance increase on exposure t
o methane observed by other authors.