Incorporation of Organic Molecules in the Tunnels of the Sepiolite Clay Mineral
Sepiolite is a clay mineral, a complex magnesium silicate, a typical formula for which is (OH2)4(OH)4Mg8Si12O30•8H2O. It is formed by blocks and cavities (tunnels) growing in the direction of the fibres. The tunnels, 3.7 x 10.6 Å in cross-section, are responsible for the high specific surface area a...
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| Language: | en |
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2011
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| Online Access: | http://hdl.handle.net/10393/20219 |