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Diatomaceous earth (also known as diatomite, DE or kieselguhr) is a naturally occurring, light-colored, solid material that is easily crumbled into a fine dust. It consists primarily of the fossilized remains of diatoms (a type of hard-shelled algae). Its typical chemical composition is 86% silicon, 5% sodium, 3% magnesium, and 2% iron.
Commercial applicationsThe high absorbency and porosity and low density of diatomaceous earth make it an appealing material to use in a number of commercial applications.
GeologyBecause diatomaceous earth forms from the remains of water-borne diatoms, it is found in proximity to either current or former bodies of water. Diatomaceous earth is generally divided into two categories based upon source: freshwater and saltwater. Freshwater diatomaceous earth is mined from dry lakebeds and is characteristically low in crystalline silica content. Saltwater diatomaceous earth, in contrast, contains a high crystalline silica content making it a useful material for filters due to the sieve-like features of the crystals. Specific varieties
Safety ConsiderationsThe absorbent qualities of diatomaceous earth can result in a significant drying of the hands if handled without gloves. The saltwater form contains the highly crystalline form of silica resulting in sharp edges. The sharpness of this version of the material makes it dangerous to breathe and a dust mask is recommended when working with it. External links
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