posted on 2015-12-31, 00:00authored byYiwei Zhang, JingYe Yu, Yu-Hao Yeh, Raymond. J. Gorte, Srinivas Rangarajan, Manos Mavrikakis
CH<sub>4</sub> adsorption was studied
experimentally and theoretically
on ZSM-5, MOR, and ZSM-12 zeolites using calorimetric measurements
at 195 K and plane wave DFT calculations. Differential heats measured
on four different H-ZSM-5 samples were determined to be 22.5 ±
1 kJ/mol, independent of Brønsted site density or defect concentration.
However, DFT calculations performed using various functionals and
on the most stable Brønsted site indicated that CH<sub>4</sub> should bind to this site by an additional 1–7 kJ/mol, a discrepancy
that is due to the inability of standard DFT methods to capture hydrogen-bonding
effects accurately with CH<sub>4</sub>. Differential heats for CH<sub>4</sub> in MOR were 30 ± 1 kJ/mol at low coverages, falling
to 25 kJ/mol for coverages above one molecule per 8-membered-ring
side pocket, while differential heats on ZSM-12 were initially 22.5
kJ/mol, decreasing to 21 kJ/mol with coverage. DFT calculations on
the siliceous form of the zeolites were able to predict these values
within 5 kJ/mol in most cases. The results indicate that CH<sub>4</sub> is an excellent probe molecule for characterizing the pore structure
of zeolites.