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Imogolite
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Imogolite is an aluminium with the . It occurs in formed from and was first described in 1962 for an occurrence in Uemura, Kumamoto prefecture, Kyushu Region, Japan. Its name originates from the Japanese word , which refers to the brownish yellow soil derived from volcanic ash. It occurs together with , , , , and .

(1995). 9780962209710, Mineralogical Society of America.

Imogolite consists of a network of with an outer diameter of ca. 2 nm and an inner diameter of ca. 1 nm. The tube walls are formed by continuous () sheets and ( groups). Owing to its tubular structure, natural availability, and low toxicity, imogolite has potential applications in polymer composites, fuel gas storage, absorbents, and as a catalyst support in chemical .


Further reading
  • (Contains structure illustration)

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