which type of soil facilitates easy procolation of water?
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Single-grained soils (sands) and massive soils (loams and clays) are called “structureless.” In single-grained soils like sand, water percolates very quickly through the soil, while in massive soils such as dense clays, water movement is very slow.
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Sandy Soil
This level of groundwater is called water table. Sandy soil is quite loose, so the percolation rate of water is highest in sandy soil but lowest in the clay soil because it is very compact.
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