The Knoevenagel condensation constitutes a crucial role in synthetic chemistry, enabling the formation of C−C single bonds and the introduction of various functional groups into organic molecules
[1]. This versatility enables it indispensable for synthesizing complex organic compounds in the pharmaceutical and fine chemical industries
[2−4]. The Knoevenagel condensation is a typical base-catalyzed reaction, commonly employing soluble bases such as piperidine, pyridine and ethylenediamine as catalysts. However, the use of this type of catalysts poses several drawbacks, including difficulty in product separation, poor recyclability and environmental concerns
[5]. Recently, aluminum-rich zeolites (e.g., FAU and LTA zeolites) have demonstrated high catalytic activity and application potential in the Knoevenagel condensation. Their abundant basic sites, excellent stability at reaction temperature below 150 °C, and ease of separation make them being promising alternatives to traditional liquid catalysts. Unfortunately, the inherent microporous structure (pore size below 1 nm) of conventional zeolite restricts the diffusion of reactant and product molecules, especially in the reactions involving bulky molecules, resulting in increased mass-transfer resistance, reduced catalytic efficiency, and even catalyst deactivation. Previous studies
[6−8] have indicated that hierarchical aluminum-rich zeolites not only offer abundant basic sites but also enhance the diffusion efficiency of reactants and products within their pore structure, thereby improving the catalytic activity. For example, Verboekend et al.
[9] demonstrated that the introduction of mesopores into FAU and LTA zeolites could enhance their catalytic efficiency by tenfold in the Knoevenagel condensation of benzaldehyde with malononitrile.
To date, the methods for preparing hierarchical zeolites can be classified into post-treatment and direct synthesis methods
[10]. Post-treatment technique involves primarily desilication and dealumination. In the case of aluminum-rich Y zeolite, the uniform distribution of framework aluminum atoms inhibits the effective desilication, thereby preventing the formation of mesoporous structure
[11]. The removal of aluminum species is a conventional method for creating hierarchical Y zeolite, however, it involves complex operational steps and demanding conditions. Direct synthesis method can be categorized into templating and template-free approaches, depending on whether a template agent is used. Significant progress has been made in synthesizing hierarchical NaY zeolite
via templating method, which enables the pore structure tuning by adjusting template properties and synthesis conditions
[12]. Regrettably, the industrial application of this approach is limited by the high cost of templates and the environmental issues associated with their removal. In view of this, researchers have proposed the template-free approach for the preparation of hierarchical zeolites through. For example, Xiong et al.
[13] reported that the hierarchical Y zeolite with high crystallinity was fabricated by the
in situ crystallization of a kaolinite microsphere and powder component mixture. Moreover, our previous works have successfully synthesized a series of hierarchical zeolites (e.g., hierarchical NaY, Beta and SAPO-11zeolites) using submolten salt (SMS) activated natural aluminosilicate minerals as raw materials, without adding any mesoporous templates
[14−15]. This method relies on a self-assembly growth mechanism driven by the competitive coordination between crystallization and stabilization of oligomeric structural units formed during the depolymerization of aluminosilicate minerals. This can not only eliminate the need for organic templates, but also decrease the raw material cost associated with zeolite synthesis.
Even though hierarchical NaY zeolite was successfully synthesized from natural aluminosilicate minerals, this approach employed diatomite mineral as the main silicon source
[16]. This dependence brings about the following two issues. Firstly, the silicon species in diatomite necessitates activation
via high-temperature calcination above 800 °C due to their low chemical reactivity, thereby resulting in significant energy consumption. Secondly, the diatomite contains some impurities, especially a stable quartz phase, which are difficult to transform during the synthesis of NaY zeolite. These residual impurities are consequently retained in the final product, ultimately reducing its purity. Therefore, searching for a natural aluminosilicate mineral with an appropriate SiO
2/Al
2O
3 molar ratio (SAR) and free of stable crystalline impurities is essential to circumvent the drawbacks of the conventional mineral system and further advance the green synthesis of zeolite.
To the best of our knowledge, the raw perlite is primarily composed of amorphous SiO
2, with a bulk SAR ranging between 8.5 and 10.0. This characteristic enables the use of perlite as the sole source of silicon and aluminum for the synthesis of NaY zeolite. However, the raw perlite has good chemical stability
[17]. When the untreated perlite was used as the raw material, the resulting product is a composite of Y zeolite and perlite rather than a pure-phase Y zeolite
[18]. Based on our previous studies, this work applies the SMS activation method to depolymerize the perlite, and a hierarchical NaY zeolite is synthesized using this SMS activated perlite as the sole source of silicon and aluminum. The synthesis chemistry is systematically analyzed to determine the optimal conditions for preparing hierarchical NaY zeolite. Additionally, the physicochemical properties and crystallization process of the obtained zeolites are characterized and analyzed in detail. The catalytic performance of the synthesized hierarchical NaY zeolite is evaluated in the Knoevenagel condensation of benzaldehyde with ethyl cyanoacetate.