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- B26b5349b490d98d06d0cdb84c4a4e8c7 type Axiom @default.
- B26b5349b490d98d06d0cdb84c4a4e8c7 comment "https://en.wikipedia.org/wiki/Diatomaceous_earth#Geology_and_occurrence" @default.
- B26b5349b490d98d06d0cdb84c4a4e8c7 annotatedProperty comment @default.
- B26b5349b490d98d06d0cdb84c4a4e8c7 annotatedSource ENVO_01000963 @default.
- B26b5349b490d98d06d0cdb84c4a4e8c7 annotatedTarget "Diatomite is easily crumbled into a fine white to off-white powder. The powder has a particle size ranging from less than 3 micrometres to more than 1 millimetre, but typically 10 to 200 micrometres. The diatoms in each deposit contain different amounts of silica, depending on the age of the deposit. The species of diatom may differ among deposits. The species of diatom is dependent upon the age and paleo-environment of the deposit. In turn, the shape of a diatom is determined by its species. The typical chemical composition of oven-dried diatomaceous earth is 80 to 90% silica, with 2 to 4% alumina (attributed mostly to clay minerals) and 0.5 to 2% iron oxide." @default.