I. Balint et K. Aika, INTERACTION OF WATER WITH 1-PERCENT LI MGO - DC CONDUCTIVITY OF LI/MGO CATALYST FOR METHANE SELECTIVE ACTIVATION/, Journal of the Chemical Society. Faraday transactions, 91(12), 1995, pp. 1805-1811
Citations number
25
Categorie Soggetti
Chemistry Physical","Physics, Atomic, Molecular & Chemical
The dc conductivity of pure magnesium oxide and lithium-doped magnesiu
m oxide has been investigated using the four-electrodes method in He f
low between 673 and 1173 K. The influence of oxygen and water vapour o
n the surface conductivity was also studied. For the lithium-doped mag
nesium oxide, the activation energy of the conduction was 25 kcal mol(
-1) at low temperature (673-873 K) and 49 kcal mol(-1) at high tempera
ture (973-1173 K). The effect of replacing water with heavy water on t
he conduction activation energy of lithium-doped magnesium oxide was o
bserved. The activation energy when using D2O was 8 kcal mol(-1) highe
r than when using H2O in the high-temperature range, while the isotopi
c effect was not significant in the low-temperature region. Temperatur
e-programmed desorption (TPD) of water was performed on magnesium oxid
e and lithium-doped magnesium oxide. Remarkable hydrogen release was o
bserved at temperatures above 873 K on lithium-doped magnesium oxide.
A vehicle mechanism for proton conductivity by way of surface OH- was
suggested at low temperature, while holes (O-) generated from hydrogen
evolution in which O-H dissociation becomes the most important step w
ere proposed as charge carriers at high temperature. A mechanism where
multi O-H bonds rupture to produce a hole was proposed to explain the
extensive isotope effect. A probable mechanism for the formation of t
he active sites for methane activation at high temperatures is discuss
ed.