The catalytic properties of ferrisilicates (analogs of ZSM-5 zeolites)
in the reaction of N2O decomposition are studied. The catalytic behav
ior of ferrisilicates is shown to be determined by the presence of act
ive sites (so-called alpha-centers) involving iron atoms. Decompositio
n of N2O on alpha-centers proceeds with formation of an active form of
surface oxygen, which cannot be produced by O2 adsorption. The influe
nce of iron on the concentration of alpha-centers and the rate of N2O
decomposition is investigated in a wide range of iron contents (from 0
.003 to 4.8 wt % Fe2O3). Comparison of the dependences obtained with t
hose observed earlier for ZSM-5 type ferrialuminosilicates reveals the
identity of the specific catalytic activities of active sites in both
systems. Tle higher catalytic activity of the Fe-A-Si samples as comp
ared with the Fe-Si systems could be accounted for by the influence of
Al on the iron distribution in zeolite resulting in a higher concentr
ation of active sites at the same iron content.