4.6 Article

Rare-earth ion exchanged Cu-SSZ-13 zeolite from organotemplate-free synthesis with enhanced hydrothermal stability in NH3-SCR of NOx

Journal

CATALYSIS SCIENCE & TECHNOLOGY
Volume 9, Issue 1, Pages 241-251

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/c8cy02033g

Keywords

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Funding

  1. National Natural Science Foundation of China [2187020455, 21603022]
  2. Fundamental Research Funds for the Central Universities in China [DUT16RC(3)002, DUT17TD04]
  3. Open Project Funds of the State Key Laboratory of Catalysis, Dalian Institute of Chemical Physics [N-16-08]
  4. Program for Liaoning Innovative Research Team in University [LT2016001]
  5. INCOE (International Network of Centers of Excellence) project

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The relatively low hydrothermal stability of Al-rich Cu-SSZ-13 catalysts hinders their practical application in ammonia selective catalytic reduction (NH3-SCR) reaction. Rare-earth ions were introduced into the Al-rich SSZ-13 zeolite using an organotemplate-free synthesis prior to the exchange of Cu2+ ions. Among the rare-earth ions tested (Ce, La, Sm, Y, Yb), Y shows significant enhancement of the hydrothermal stability and NH3-SCR activities after severe hydrothermal aging at 800 degrees C for 16 h when compared with Cu-SSZ-13 without Y. Cu-Y-SSZ-13 catalysts with various amounts of Y were prepared, and it is found that with increasing Y content, the low temperature NO conversions can be improved even after hydrothermal aging. SEM-EDX analysis together with two-dimensional multiple quantum magic-angle-spinning nuclear magnetic resonance (Na-23 MQ MAS NMR) confirms that the Y ions are successfully incorporated into the ion-exchange sites of the SSZ-13 zeolite. Results from Al-27 MAS, Si-29 MAS NMR, temperature-programmed desorption of ammonia (NH3-TPD) and quantitative H-1 MAS NMR indicate that Y can stabilize the framework Al and also preserve the BrOnsted acid sites in the Al-rich SSZ-13 zeolite. The hydrogen temperature programmed reduction (H-2-TPR), ultraviolet-visible-near infrared spectroscopy (UV-vis-NIR) and diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS) of nitric oxide (NO) or NH3 adsorption demonstrate that introduction of Y ions causes Cu2+ ions to preferentially occupy the 6-MR, which has high hydrothermal stability. However, too much of Y may lead to activity loss at both low and high temperatures. The optimized Al-rich Cu-Y-SSZ-13 with 2.8 wt% of copper (Cu) and 1.3 wt% of Y displays almost the same deNO(x) activities as the conventional organotemplated high silica Cu-SSZ-13 catalyst in a wide reaction temperature window of 150-650 degrees C after severe hydrothermal treatment. Rare-earth ions could be an effective additive for Cu-SSZ-13 catalysts to further improve their hydrothermal stability for practical applications.

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