“…The characteristic pristine FER structures were well synthesized on all the FER zeolites, and their relative crystallinities are summarized in Table . With an increase of Si/Al molar ratios, the most intense characteristic diffraction peaks at 2θ = 9.3 and 25.2° were increased steadily, which suggests an increased crystallinity by forming well-developed 8- and 10-MR micropore structures of the FER zeolite. ,, The relative crystallinities were found to be in the range of 47–100%, where the FER(8) showed a lower crystallinity with the presence of abundant defect sites such as the Lewis acidic extra-framework Al species possibly which were related to preferential formations of amorphous coke precursors. , The surface acidity of the as-prepared FER zeolites was also verified by NH 3 -TPD analysis, and desorption patterns of NH 3 molecules are displayed in Figure D. Two characteristic desorption peaks of NH 3 were clearly observed at the maximum temperature range of 185–200 °C and ∼440 °C, which can be assigned to weak and strong acidic sites, respectively.…”