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Diatomaceous earth

soft diatomite variety

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionAug 21, 2026
Entity authorityQ193414
Source-derived summary

Diatomaceous earth ( DY-ə-tə-MAY-shəs), also known as diatomite ( dy-AT-ə-myte), celite, or kieselgur, is a naturally occurring, soft, siliceous sedimentary rock that can be crumbled into a fine white to off-white powder. It has a particle size ranging from more than 3 mm to less than 1 μm, but typically 10 to 200 μm. Depending on the granularity, this powder can have an abrasive feel, like that of pumice powder, and has a low density as a result of its high porosity. The typical chemical composition of oven-dried diatomaceous earth is 80–90% silica, with 2–4% alumina (attributed mostly to clay minerals), and 0.5–2% iron oxide.

Diatomaceous earth consists of the fossilized remains of diatoms, a type of hard-shelled microalgae, that have accumulated over millions of years. It is used as a filtration aid, mild abrasive in products including metal polishes and toothpaste, mechanical insecticide, absorbent for liquids, matting agent for coatings, reinforcing filler in plastics and rubber, anti-block in plastic films, porous support for chemical catalysts, cat litter, activator in coagulation studies, stabilizing component of dynamite, thermal insulator, and soil for potted plants and trees as in the art of bonsai. It is also used in gas chromatography packed columns made with glass or metal as stationary phase.

Composition

Diatomaceous earth consists of the fossilized remains of diatoms that accumulated over millions of years. It is usually composed of 80% to 90% silica, 2% to 4% alumina minerals, and 0.5% to 2% iron oxide, although the precise composition of every deposit is different. Deposits may contain different amounts of silica depending on the sedimentation conditions, the presence of other sediments (clay, sand, volcanic ashes), and the age of the deposit (diagenesis, silica (SiO2) dissolution/precipitation, diatoms tests ageing).

Editorial summary

The public source identifies “Diatomaceous earth” as soft diatomite variety. This brief keeps that definition visible, then builds a research path around Diatomaceous, earth and soft.

Editorial reviewA practical starting point whose main value is the path it opens into stronger specialist and primary sources. The current 287-word lead offers orientation but no explicit four-digit date, so chronology should not be assumed. The selected authority fields contribute no independent date. Its value is orientation rather than verdict, with Diatomaceous, earth and soft providing the first useful test.
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A short description can identify a subject without explaining its stakes. For “Diatomaceous earth”, the useful work is to connect “soft diatomite variety” to the records capable of establishing context and consequence.

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Vocabulary and entity names are the principal evidence signals here, because they determine the precision of every later search. The source revision retrieved here is dated Aug 21, 2026. The linked authority identifier is Q193414. The Library of Congress control number is sh85037626. 1 of 1 selected statements include explicit references; 1 carry qualifiers and 0 use preferred rank.

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Source & attribution

This entry incorporates text from Diatomaceous earth” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.