The correct increasing order of the surface areas of soils
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A. clay → sand → silt →gravel
B. silt → sand → clay → gravel
C. clay → silt → sand → gravel
D. silt → clay → sand → gravel
B. silt → sand → clay → gravel
C. clay → silt → sand → gravel
D. silt → clay → sand → gravel
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The correct increasing order of the surface area of soil includes
fine sand, clay, silt colloids.
Explanation:
- Sand is a 'granular material' composed of 'finely divided rock' and mineral particles
- Clay is a 'finely-grained natural rock' or soil material that 'combines' 'one or more' clay minerals.
- Geologic clay 'deposits' are mostly formed of 'phyllosilicate minerals' including changeable 'amounts of water' trapped in the mineral structure.
- The 'clay-sized' and the 'fine silt-sized particles' are distributed as colloids.
- The fine size of the colloidal particles is responsible for their very high surface ratio.
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