A hydrated aluminum silicate. Generalized formula Al2O3SiO2•xH2O. Component of soils in varying percentages.| Properties: |
| Fine, irregularly shaped crystals ranging from 150 microns to less than 1 micron (colloidal); reddish-brown to pale buff color, depending on iron oxide content; odorless. D approximately 2.50. Insoluble in water and organic solvents. Absorbs water to form a plastic, moldable mass and in some cases a thixotropic gel (bentonite). Refractory material; strong ion-exchange capability; important in soil chemistry and construction engineering. |
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| Derivation: |
| Weathering of rocks. |
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| Occurrence: |
| Southeastern U.S., Wyoming, Texas, Canada, England, France, the former U.S.S.R.. |
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| Available forms: |
| Kaolinite, montmorillonite, atapulgite, illite, bentonite, halloysite. |
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| Grade: |
| Natural, refined, air floated. |
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| Hazard: |
| Dusts may irritating to nose and throat. Suspensions of dust are a fire hazard. |
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| Use: |
| Ceramic products, refractories, colloidal suspensions, oil-well drilling fluids, filler for rubber and plastic products, films, paper coating, decolorizing oils, temporary molds, filtration, carrier in insecticidal sprays, catalyst support. |
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