Journal of Materials Chemistry · 2008 · 117 citations · 27 references
Hydrothermal CrystallizationEngineeringOrganic ChemistryChemistryInorganic MaterialHierarchical Zsm-5Hierarchical PorosityOrganic Moiety NatureSol-gel SynthesisNovel OrganocatalystsZeoliteHybrid MaterialsProtozeolitic UnitsMaterials ScienceInorganic ChemistryCatalysisSynthesis MethodCrystallographyInorganic SynthesisFunctional MaterialsHydrothermal Processing
The synthesis of hierarchical ZSM-5 from silanized protozeolitic units has been accomplished following a three step procedure comprising gel precrystallization at 90 °C, grafting of the seed silanization agent (SSA) and hydrothermal crystallization at 170 °C. The following four organosilanes were tested and investigated as SSAs: 3-aminopropyltrimethoxysilane (APTMS), isobutyltriethoxysilane (IBTES), phenylaminopropyltrimethoxysilane (PHAPTMS) and octadecyltrimethoxysilane (ODTMS). The last agent became anchored to the zeolite seeds to a rather reduced extent (1.3%) and the obtained material presented properties very similar to those of a reference nanocrystalline ZSM-5 (Sext ∼ 100 m2 g−1, SBET ∼ 450 m2 g−1, crystallite size = 20–80 nm). In contrast, silanization of the protozeolitic units with APTMS or IBTES led to ZSM-5 samples having large surface areas (Sext ∼ 200 m2 g−1, SBET ∼ 500 m2 g−1) and exhibiting mesopores (Dp ∼ 8 nm). These materials are formed by 300–400 nm particles consisting of aggregates of ZSM-5 nanounits (10–20 nm). Seed silanization with PHAPTMS caused the greatest enhancement in surface area (SBET = 573 m2 g−1, Sext = 225 m2 g−1), the material so obtained being formed by the smallest nanounits (5–10 nm) within the aggregates. Moreover, this sample presented a hierarchical porosity with pores around 2.0–3.0 nm in addition to those generated by the MFI channels. The strong changes induced in the ZSM-5 crystal size and properties when using PHAPTMS as SSA have been attributed to this agent being very effective in both anchoring onto the protozeolitic units and perturbing the subsequent crystal growth step.
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