Abstract

Potassium (K) ion-exchanged ZSM-5 zeolites were investigated for catalytic soot combustion. X-ray absorption fine-structure (XAFS), Raman, in situ IR and NH3-temperature programmed desorption (NH3-TPD) confirmed the location of K+ at the ion-exchanged sites. Temperature-programmed oxidation (TPO) reactions showed that K-ZSM-5 decreased ignition tempeatures of soot combustion and increased selectivity to CO2. The improved activity for soot combustion by increasing K+-exchanged amounts via decreasing the Si/Al ratio reinforced the K+ ions participating in soot combustion. 18O2 isotopic isothermal reactions suggested the activation of gaseous oxygen by the K+ ions. This demonstrated a new appliction of alkali metal exchanged zeolites and the strategy for enhancement of catalytic soot combustion activity.

Highlights

  • Soot particulates are one of the main pollutants emitted from diesel engines, which represents a significant threat to environment and human health

  • Na-ZSM-5 zeolites were hydrothermally synthesized with Si/Al ratios of 100 (Na-ZSM-5-100) and 25 (Na-ZSM-5-25)[16], followed by ion-exchanges of H+ and K+, which results in H-ZSM5-100 and K-ZSM-5-100 (25) samples, respectively

  • K-ZSM-5 zeolites were prepared by ion-exchange and evaluated for soot combustion

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Summary

Introduction

Soot particulates are one of the main pollutants emitted from diesel engines, which represents a significant threat to environment and human health. Zhao’s group has reported that gold nanoparticles supported on three-dimensionally ordered macroporous oxides exhibit outstanding activity[9]. Kimura et al reported that K2CO3 supported on aluminosilicate zeolite exhibited excellent catalytic activity[24, 25]. No one has reported ion-exchanged K-ZSM-5 as catalysts for soot combustion. K-ZSM-5 was first reported to increase both activity and selectivity to CO2 for soot combustion. This was confirmed by the fact that increasing K+-exchanged amounts via decreasing the Si/Al ratio led to the improved activity, which was attributed to the activation of gaseous oxygen by K+ at the ion-exchanged sites

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