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- B70e7ebbefa0d3684dd46c14a6528dc1d hasDbXref Properties @default.
- B70e7ebbefa0d3684dd46c14a6528dc1d type Axiom @default.
- B70e7ebbefa0d3684dd46c14a6528dc1d annotatedProperty comment @default.
- B70e7ebbefa0d3684dd46c14a6528dc1d annotatedSource ENVO_00000343 @default.
- B70e7ebbefa0d3684dd46c14a6528dc1d 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.