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- B4e879d64f2a2cc48efc5af2c77acf43a hasDbXref Properties @default.
- B4e879d64f2a2cc48efc5af2c77acf43a type Axiom @default.
- B4e879d64f2a2cc48efc5af2c77acf43a annotatedProperty comment @default.
- B4e879d64f2a2cc48efc5af2c77acf43a annotatedSource ENVO_01003003 @default.
- B4e879d64f2a2cc48efc5af2c77acf43a 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.