Ferrierite

The ferrierite group of zeolite minerals (the FER structure) consists of three very similar species: ferrierite-Mg, ferrierite-Na, and ferrierite-K, based on the dominant cation in the A location. Ferrierites are orthorhombic minerals with highly variable cationic composition, (Na,K)₂Mg(Si,Al)₁₈O₃₆(OH)·9H₂O. Calcium and other ions are often also present. They are found in vitreous to pearly, often radiating, spherical aggregates of thin blade-shaped transparent to translucent crystals.

Ferrierite typically occurs as an alteration mineral in basaltic rocks and in tuffaceous sediments. In North America, it is found at Kamloops Lake, BC, Canada (the original Type locality) and Leavitt Lake, California. Ferrierite was named for Canadian geologist and mining engineer Walter Frederick Ferrier (1865-1950).

Use

Synthetic ferrierites have even greater cation variability and have important uses as commercial filters and ion-exchange beds.

Ferrierite-H can be used as a catalyst in the chemical industry for the acid-catalyzed skeletal isomerization of n-butenes to iso-butene, the raw material for production of methyl tert-butyl ether (MTBE).

ee also

*List of minerals
*List of minerals named after people

References

* [http://webmineral.com/data/Ferrierite.shtml Webmineral]
* [http://www.mindat.org/min-6931.html Mindat - Ferrierite-Mg]
* [http://web.clas.ufl.edu/users/neuhoff/zeo/ferrierite.html Univ. Florida images]

Ferrierite-(Mg),_Kamloops_Lake,_British_Columbia,_Canada