Clinoptilolite

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Clinoptilolite
Clinoptilolite-Na-269082.jpg
Clinoptilolite-Na
General
Category Tectosilicates
Zeolites
Formula
(repeating unit)
(Na,K,Ca)2-3Al3(Al,Si)2Si13O36·12H2O
Strunz classification 09.GE.05
Identification
Crystal system Monoclinic
Mohs scale hardness 3½ - 4
Luster Vitreous

Clinoptilolite is a natural zeolite comprising a microporous arrangement of silica and alumina tetrahedra. It has the complex formula: (Na,K,Ca)2-3Al3(Al,Si)2Si13O36·12H2O. It forms as white to reddish tabular monoclinic tectosilicate crystals with a Mohs hardness of 3.5 to 4 and a specific gravity of 2.1 to 2.2. It commonly occurs as a devitrification product of volcanic glass shards in tuff and as vesicle fillings in basalts, andesites and rhyolites. It was described in 1969 from an occurrence in Owl Canyon, San Bernardino County, California.

It forms a series with heulandite:

  • Clinoptilolite-Ca – heulandite-Ca solid solution series
  • Clinoptilolite-K – heulandite-K solid solution series
  • Clinoptilolite-Na – heulandite-Na solid solution series

Use of clinoptilolite in industry and academia focuses on its ion exchange properties having a strong exchange affinity for ammonia (NH4+). A typical example of this is in its use as an enzyme based urea sensor. It is also used as fertiliser, and sold as a deodorizer in the form of pebble-sized chunks contained in a mesh bag.

Research is generally focussed around the shores of the Aegean Sea due to the abundance of natural clinoptilolite in easily accessible surface deposits.

The name is derived from the Greek words klino (κλίνω;"oblique"), ptylon (φτερών;"feather"), and lithos (λίθος;"stone").

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