Faujasite is a mineral from the family of
zeolites. It occurs in natural form and is also synthesized industrially.
History
Faujasite was discovered in 1842 by Damour and is named for
Barthélemy Faujas de Saint-Fond, a French geologist and volcanologist.
1).
Structure
The faujasite framework consists of
sodalite cages which are connected through hexagonal prisms. The pores are arranged perpendicular to each other. The pore, which is formed by a 12-membered ring, has a relatively large diameter of 7.4 Å. The inner cavity has a diameter of 12 Å and is surrounded by 10 sodalite cages. The unit cell is cubic with a length of 24.7 Å. Zeolite Y has a void fraction of 48 % and a Si/Al ratio of 2.43. It thermally decomposes at 793 °C.
2)
Synthesis
Faujasite is synthesized as other zeolites from alumina sources such as
sodium aluminate and silica sources such as
sodium silicate. Other alumosilicates such as
kaolin are used as well. The ingredients are dissolved in a basic environment such as
sodium hydroxide aqueous solution and crystallized at 70 to 300 °C (usually at 100 °C). After crystallization the faujasite is in it is sodium form and must be ion exchanged with
ammonium to improve stability. The ammonium ion is removed later by calcination which renders the zeolite in its acid form.
Use
Faujasite is used above all as a catalyst in
fluid catalytic cracking to convert high-boiling fractions of petroleum crude to more valuable gasoline, diesel and other products. Zeolite Y has superseded zeolite X in this use because it is both more active and more stable at high temperatures due to the higher Si/Al ratio. It is also used in the
hydrocracking units as a platinum/palladium support to increase aromatic content of reformulated refinery products.
External links
Literature
- Subhash Bhatia, Zeolite Catalysis: Principles and Applications, CRC Press, Inc., Boca Raton, Florida, 1990.
- Ribeiro, F. R., et. al., ed., Zeolites: Science and Technology, Martinus Nijhoff Publishers, The Hague, 1984.