Imogolite

imogolite

gibbsite

allophane

halloysite

Images

Formula: Al2SiO3(OH)4
Phyllosilicate (sheet silicate), allophane group
Crystal System: Monoclinic
Specific gravity: 2.70 measured and calculated
Hardness: 2 to 3
Streak: White
Colour: Yellowish white, light brownish yellow, blue, green, brown
Environments:

Sedimentary environments

Imogolite occurs principally in soils derived from volcanic ash. It has been found associated with allophane, halloysite, vermiculite, goethite, gibbsite, cristobalite, limonite and quartz. Imogolite has been observed in cracks in weathered plagioclase (Dana, HOM).

Imogolite consists of a network of nanotubes with an outer diameter of ~2 nm and an inner diameter of ~1 nm. The tube walls are formed by continuous Al(OH)3 (gibbsite) sheets and orthosilicate anions (O3SiOH 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 catalysis (Wiki).

Localities

At the type locality, Uemura, Kumamoto, Japan, imogolite occurs as a decomposition product of volcanic ash in soils in a humid environment (Mindat).

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