Selective catalytic reduction of nitric oxide by ammonia over Cu-FAU catalysts in oxygen-rich atmosphere

Citation
S. Kieger et al., Selective catalytic reduction of nitric oxide by ammonia over Cu-FAU catalysts in oxygen-rich atmosphere, J CATALYSIS, 183(2), 1999, pp. 267-280
Citations number
46
Categorie Soggetti
Physical Chemistry/Chemical Physics","Chemical Engineering
Journal title
JOURNAL OF CATALYSIS
ISSN journal
00219517 → ACNP
Volume
183
Issue
2
Year of publication
1999
Pages
267 - 280
Database
ISI
SICI code
0021-9517(19990425)183:2<267:SCRONO>2.0.ZU;2-6
Abstract
The selective catalytic reduction (SCR) of NO (2000 ppm) by NH3 (2000 ppm) in the presence of oxygen (3%) was carried out on Cu(x)-FAU (x = theoretica l exchange degree) catalysts prepared by ion exchange or impregnation and c alcined at 773 K. The samples were characterized by UV-visible and IR spect roscopy, temperature-programmed reduction (TPR), temperature-programmed oxi dation (TPO), and temperature-programmed desorption (TPD) of NH3. Ion-excha nged Cu(x)-FAU contains mainly Cu ions located in both supercages and sodal ite cavities. In contrast, the impregnated sample contains mainly CuO. Ioni c Cu is more active and selective to N-2 than CuO in the temperature range 450-750 K. In contrast, CuO aggregates lead to significant formation of N2O , with a bell-shaped dependency centered at ca. 540 K. IR spectroscopy and TPD of NH3 show that the last NH3 ligand was removed from Cu ions above 550 K. The SCR on Cu ions obeys a Cu2+ <-> Cu+ redox mechanism in which Cu2+ i s reduced to Cu+ by NO + NH3 and Cu+ is oxidized to Cu2+ by NO + O-2, with evolution of N-2 and H2O. Both reduction and oxidation steps of Cu in the c atalytic cycle encompass the reduction of NO in agreement with the SCR of ( NO)-N-14 with (NH3)-N-15. A new overall SCR reaction below 550 K was propos ed: 10NH(3) + 13NO + O-2 --> 15H(2)O --> (23/2)N-2. The active sites below 550 K are formed by several Cu neighbor ions, maybe [CuOCu](2+), probably l ocated in the supercages. All Cu ions become active above 600 K. The partia l reduction of NO to N2O occurs at high temperature (>650 K) on exchanged s amples. This formation, up to 17% at full NO conversion, is likely to take place on Cu ions located within the sodalite cavities. (C) 1999 Academic Pr ess.