The focus of the review is on zeolite characterization, synthesis, and applications. Zeolite is a hydrated aluminosilicate with a tetrahedral structural framework that contains exchangeable active metal ions and water molecules in channels and cages. Different synthesis methods, including hydrothermal and green synthesis methods, were used to make zeolite.Â
The results of the characterization demonstrate that zeolite has a number of distinct properties, including uniform pore size, acidic qualities, thermal stability, mobile extra cation, hydrophilicity, and hydrophobicity. Catalysis, water purification, adsorption, and agriculture are only a few of the applications.
Zeolites are hydrated aluminosilicates of alkaline or alkaline earth metals that are crystalline, microporous, and hydrated. The frameworks are made up of corner-shared SiO4 and AlO4 tetrahedra that form various open structures. The tetrahedra are coupled together to form cages that are connected by pore holes of varying sizes. The pore sizes vary depending on the structural type. The positive charge of cations within the material’s pores balances out the negative charge on the lattice. These are mainly univalent and bivalent metals, or a mixture, in basic zeolites.
Because of the purity of crystalline products and particle size consistency, synthetic zeolites are employed commercially more frequently than natural zeolites. Standard chemical reagents were used to make the first zeolites. Natural zeolites were used for much of the basic zeolite science research. Synthetic zeolites have several advantages over naturally occurring zeolites, including the ability to construct a wide range of chemical characteristics and pore sizes, as well as higher heat stability.
The hydrothermal crystallization of aluminosilicate gels or solutions in a basic environment is used to make zeolite. Crystallization takes place in a closed hydrothermal system at various temperatures, autogenous pressures, and times (a few hours to several days).
Many studies have been conducted with the goal of producing zeolites from low-cost silica-alumina sources. Under hydrothermal circumstances, zeolites are frequently produced in an alkaline phase.
Fly ash and kaolinite are two sources of silica alumina. Zeolites are comparable to clay minerals in terms of composition (kaolinite). They’re both aluminosilicates. Their crystalline structure, on the other hand, is different. Kaolinite has a poor exchange capacity and a mineral layer charge. It has a small surface area and has a low absorption capability. However, careful treatment can improve kaolin’s characteristics.
The cost of zeolite material generated using the methods described above is anticipated to be somewhere between natural and synthetic zeolite. However, given the fact that rates for garbage storage and disposal are likely to rise, the installation of one is unlikely.
As mentioned in the previous section, a variety of seeding methods have been used in the manufacture of zeolite membranes. Seeding is a key step in the fabrication of zeolite membranes because it gives benefits such as crystal development on the support rather than in the solution and avoidance of nucleus transition into undesired zeolite phases.
The following factors influence the crystalline zeolite structure-
To summarise, zeolite synthesis processes are influenced by a variety of parameters, including the composition of precursors, reaction pH, temperature, pre-treatment of precursors, seeding time, reaction time, and template employed. However, using a two-step crystallization approach in hierarchical porous zeolite synthesis is promising; combining hydrothermal crystallization with microwave heating is another synthesis method that produces smaller, more uniform particles in less time.