Zeolite materials were first established in the eighteenth century when Baron Axel Fredrik Cronstedt, a Swedish scientist and pioneer of modern mineralogy, observed that when mineral “stilbite” is heated, moisture forms on its surface.
Zeolites are crystalline aluminosilicates with open 3D-framework structures made up of SiO4 and AlO4 tetrahedra joined together by sharing all of their oxygen atoms, resulting in regular intra-crystalline voids and channels with molecular dimensions.
Chemical structure of zeolites:
Zeolites are three-dimensional, micro – porous, crystalline materials with very well structures that comprise aluminium, silicon, and oxygen in a regular framework, with cations and water in the pores.
Through shared oxygen atoms, the silicon and aluminium atoms are tetrahedrally coordinated. Zeolites are comparable to clay minerals in terms of composition. Both are alumino-silicates, to be precise. Their crystalline structure, on the other hand, is different.
Many varieties of clay have a layered crystalline structure (like a deck of cards) that shrinks and swells when water is absorbed and removed between the layers. Zeolites have a solid, three-dimensional crystalline structure (similar to a honeycomb) with a network of interconnecting tunnels and cages.
Properties of zeolites:
Zeolites have a number of unique qualities due to their unusual structure. The following are the most important features in terms of potential applications:
• it has low density and large volume of free spaces;
• The presence of channels and chambers with precisely defined dimensions (shape-selectivity);
• High degree of hydration;
• High degree of crystallinity
• Ion exchange capacity;
• Catalytic characteristics;
• Possibility of molecule and ion sorption
Applications of zeolites:
Zeolites can be used for a variety of purposes. The following are mentioned below:
Catalysis: Zeolites are excellent catalysts for a variety of key organic molecular processes. Acid-base and metal-induced reactions are among the catalytic reactions that zeolites can promote. Zeolites can be employed as supports for active metals or reagents, as well as acid catalysts.
They’ve also been used as catalysts for oxidation. The processes can take place within the pores of the zeolite, giving you more control over the end result.
Adsorbent: This comprises drying, purification, and separation applications. The ability of zeolites to separate gases is an extensively used attribute. Zeolites’ porous structure can be utilised to “sieve” molecules of a given size and allow them to enter the pores. This feature can be fine-tuned by adjusting the size and amount of cations surrounding the pores in the structure. Polymerisation of semiconducting materials and conducting polymers to produce materials with extraordinary physical and electrical properties are examples of other uses that can take place within the pore.
Ion exchange: When in aqueous media, hydrated cations within the zeolite pores are loosely attached to the zeolite structure and can quickly interchange with other cations. The use of zeolites in detergents and soaps are examples.
Alumina (Al2O3)
It is a crystalline substance that is white or almost colourless and is utilised as an engineering ceramic. It provides outstanding performance at a low cost. It’s created from bauxite, a naturally occurring mineral that contains varying proportions of water-soluble Aluminium Oxides. Aluminium Oxide is found in the mineral Corundum, as well as the gemstones Sapphire and Ruby. Synthetically, alumina is utilised to make these gemstones.
Low electric conductivity, chemical resistance, great strength, and extreme hardness are all characteristics of this material, making it excellent for the products described above. Modifying and toughening it using Zirconia can result in a stronger grade. Pressing, extrusion, slip casting, and injection moulding are all methods used to make alumina components.
Conclusion:
Aluminosilicate minerals, such as zeolites, are aluminosilicate minerals. They’re a type of microporous substance employed as adsorbents and catalysts.
They can hold cations like K+, Na+, Ca2+ and Mg2+. Stilbite, phillipsite, natrolite, heulandite, chabazite, and analcime are the most prevalent zeolite minerals.