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- Bb2324d44c775455e7ee2633bc71ee10e hasDbXref Properties @default.
- Bb2324d44c775455e7ee2633bc71ee10e type Axiom @default.
- Bb2324d44c775455e7ee2633bc71ee10e annotatedProperty comment @default.
- Bb2324d44c775455e7ee2633bc71ee10e annotatedSource ENVO_00000343 @default.
- Bb2324d44c775455e7ee2633bc71ee10e annotatedTarget "The distinction between silt and clay varies by discipline. Geologists and soil scientists usually consider the separation to occur at a particle size of 2 μm (clays being finer than silts), sedimentologists often use 4–5 μm, and colloid chemists use 1 μm. Geotechnical engineers distinguish between silts and clays based on the plasticity properties of the soil, as measured by the soils' Atterberg limits. ISO 14688 grades clay particles as being smaller than 2 μm and silt particles as being larger. Mixtures of sand, silt and less than 40% clay are called loam." @default.