Halloysite

Halloysite is a 1:1 aluminosilicate clay mineral with the empirical formula Al₂Si₂O₅(OH)₄. Its main constituents are aluminium (20.90%), silicon (21.76%), and hydrogen (1.56%). Halloysite typically forms by hydrothermal alteration of alumino-silicate minerals. [Paul F. Kerr, FORMATION AND OCCURRENCE OF CLAY MINERALS, Clays and Clay Minerals, Volume 1, page 19-32, 1952] It can occur intermixed with dickite, kaolin, montmorillonite and other clay minerals. X-ray diffraction studies are required for positive identification. It was first described in 1826 and named for the Belgian geologist Omalius d'Halloy.

tructure

Two common forms are found, when hydrated the clay exhibits a 1 nm spacing of the layers and when dehydrated (meta-halloysite) the spacing is 0.7 nm. Halloysite naturally occurs as small cylinders which average 30 nm in diameter with lengths between 0.5 and 10 micrometres. [George W. Brindley, STRUCTURAL MINERALOGY OF CLAYS, Clays and Clay Minerals, Volume 1, page 33-43, 1952]

Geological Occurrence

The formation of halloysite is due to hydrothermal alteration, and it is often found near carbonate rocks. For example, halloysite samples found in Wagon Wheel Gap, Colorado, are suspected to be the weathering product of rhyolite by downward moving waters. [Kerr P. F. (1952) Formation and Occurrence of Clay Minerals Clays and Clay Minerals 1, 19-23] In general the formation of clay minerals is highly favored in tropical and sub-tropical climates due to the immense amounts of water flow. Halloysite has also been found overlaying basaltic rock, showing no gradual changes from rock to mineral formation. [Papke K.G. (1970) Halloysite Deposits in the tarraced Hills Washoe County, Nevada Clays and Clay Minerals 19, 2, 71-74] Halloysite occurs primarily in youthful volcanic-derived soils, but it also forms from primary minerals in tropical soils or pre-glacially weathered materials. [ Wilson M. J. (1999) The Origin and Formation of Clay Minerals in Soils: Past Present and Future Perspectives Clay Minerals 34, 7-25] Igneous rocks, especially glassy basaltic rocks are more susceptible to weathering and alteration forming halloysite.

Often as is the case with halloysite found in Juab County, Utah, the clay is found in close association with goethite and limonite and often interspersed with alunite. Feldspars are also subject to decomposition by water saturated with carbon dioxide. When feldspar occurs near the surface of lava flows, the CO₂ concentration is high, and reaction rates are rapid. With increasing depth, the leaching solutions become saturated with silica, aluminium, sodium, and calcium. Once the solutions are depleted of CO₂ they precipitate as secondary minerals. The decomposition is dependent on the flow of water. In the case that halloysite is formed from plagioclase it will not pass through intermediate stages. [Kerr P. F. (1952) Formation and Occurrence of Clay Minerals, Clays and Clay Minerals 1, 19-23]

Applications

A very pure halloysite is mined from an highly altered rhyolite occurrence in New Zealand uses include porcelain and bone china. [ [http://www.halloysite.com/index.htm Home Page ] ] Various patents exist for the use of hallosyite as nanofillers [US patent #3467618, http://www.google.com/patents?id=tbh0AAAAEBAJ] and in controlled release technology for a range of active agents. [ [http://www.azonano.com/news.asp?newsID=1935 Biophan Files Patent on Novel Drug Delivery Using Halloysite Nanotubes ] ] [US patent #5651976, http://www.google.com/patents?KTkcAAAAEBAJ&dq=us+5651976] It is also used for other high-tech ceramic applications.

Halloysite also has been used as a petroleum cracking catalyst in the past, [US Patent #3515682, http://www.google.com/patents?id=Gs8hAAAAEBAJ] . Exxon has also developed a cracking catalyst based on synthetic halloysite [US Patent #4150099, http://www.google.com/patents?id=ROY8AAAAEBAJ] .

Due to its structure, it can be used as filler in either natural or modified forms in nanocomposites.

References

Links

* [http://webmineral.com/data/Halloysite.shtml Webmineral]
* [http://www.mindat.org/show.php?id=1808&ld=1&pho= Mindat w/ location data]
* [http://www.uwrf.edu/~wc01/halloysite.htm Univ. Wisconsin]
* [http://www.reciprocalnet.org/recipnet/showsample.jsp?sampleId=27344589&sampleHistoryId=17234&level=65536&applet=minijamm&setLevel=1 New Zealand halloysite]