The selective catalytic reduction (SCR) of NOx by ammonia SCR: 4 NO + 4 NH3 + O2 In diesel vehicles: 4 N2 + 6 H2O NOx N2 (NH2)2CO + H2O → CO2 + 2 NH3 H2O SCR mechanism over Fe-ZSM-5: 2 NO + O2 2 NO2ads (metal ions) 2 NO + 2 NO2ads + 4 NH3 rate limiting step 4 N2 + 6 H2O S. Brandenberger, October 2008 Structure of iron sites in Fe-ZSM-5 ZSM-5 zeolite with channel structure: S i z e Exchange of H+ with Fe: a large variety of Fe species are formed in Fe-ZSM-5: Fe2O3 particles FexOy clusters HO Fe O OH Fe OH Which one is the active species? 3+ Fe S. Brandenberger, October 2008 Problem: Identification of the SCR active sites in Fe-ZSM-5 Reason: No method (e.g. UV/VIS, IR, EPR, EXAFS, XPS, XRD) can definitively distinguish between isolated iron species and iron oxide clusters of different nuclearity in the same sample Solution: A statistical approach Idea: At least two iron ions, located on Al -sites, must be present within a sphere with r = 6.5 Å to form an oxygen bridged Fe-O-Fe species 6.5 A° Procedure: Calculating of the averaged number of Al sites bearing an iron ion = NFe ; NFe = f(Si/Al,Fe/Al) Assumption: Al Atoms are statistical distributed and the variation of the local Si/Al ratio can x N Fe ⋅ e − N be described by a Poisson distribution: P ( x; N Fe ) = Fe x! Rice, M.J., Chakraborty, A.K., and Bell, A.T., J. Catal. 186 (1999) 222. Goodman, B.R., Hass, K.C., Schneider, W.F., and Adams, J.B., Catal. Lett. 68 (2000) 85. S. Brandenberger, October 2008 Si/Al: 14 1 ies pec s ed ster u l c 0.6 N ⋅ e − N Fe 1 − P( x = 0; N Fe ) = 1 − Fe = 1 − e − N Fe 0! 0 0.4 0.2 dimeric spec ies 0 0 0.2 0.4 0.6 N Fe ⋅ e − N Fe − N Fe ⋅e 1! 1 P= 0.8 1 Fe/Al 100 Fe/Al 90 0.74 0.45 0.41 0.3 0.15 0.09 0.04 0.02 H-ZSM-5 80 70 Correlation of the measured SCR activity with the calculated concentration of different species DeNOx [%] Probability 0.8 60 50 40 30 20 10 0 200 300 400 500 600 700 Temperature [°C] S. Brandenberger, October 2008 SCR activity of the different iron species Temperature Isolated species OH HO 3+ Fe 200-300 °C FexOy Fe2O3 - - - Active - - Active - Active Active Fe O s-1 s-1 Fe OH (250 °C) (350 °C) Active TOF ≈ 100 ≥ 450 °C s-1 Active TOF ≈ 46 ≈ 400 °C Particles Active TOF ≈ 14 ≈ 350 °C Oligomeric species Dimeric species (400 °C) Active TOF ≈ 120 s-1 (350 °C) Active TOF ≈ 170 s-1 (400 °C) Active TOF ≈ 27 s-1 (500 °C) S. Brandenberger, October 2008
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