Soil permeability is the
ease with which air, water, or plant roots penetrate or pass through the soil.
The size of pore space and
interconnectivity of the
spaces help
determine permeability, so the shape and arrangement of grains play a role.
Permeability for soils
Type of grain Permeability(cm/s)
Well sorted gravel 102 to 1
silt sands, fine sands 10-5 to 10-3
silt, sandy silts, clayey sands, till 10-6 to 10-4
Clay 10-9 to 10-6
Type of grain Permeability(cm/s)
Well sorted gravel 102 to 1
silt sands, fine sands 10-5 to 10-3
silt, sandy silts, clayey sands, till 10-6 to 10-4
Clay 10-9 to 10-6
Although sandy soils
have lower porosity than clay soils, sandy soils have relatively larger
permeability than clay because pores in clay are not connected together very
well.
The most rapid water
and air movement is in sands because sand soils have relatively larger pores
and loose aggregated structure.
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