“…Several characteristic bands are observed; the bands in the range between 40,000 and 52,000 cm −1 were assigned to the transition due to Ag + ions, and the band in the range 25,000-40,000 cm −1 are ascribable to silver clusters with different sizes and oxidation states. A main band around 30,000-32,000 cm −1 is assignable to the species composed of Ag δ+ n clusters and the band at around 20,000 cm −1 is the species of Ag metal particles [14,15,20,21]. These data clearly indicate that the Ag + , Ag δ+ n , and Ag clusters coexist in the presence of a mixture of CH 4 and O 2 ; the catalytic reaction will be a continuous process in the present condition that causes the partial oxidation reaction of CH 4 .…”