percolation
percolation
Percolation
percolation
percolation
The last step is percolation. Percolation is when the water on the surface of the Earth seeps down underground. It later forms aquifers in the lowlying regions.
percolation
Percolation
Percolation
Percolation
loamy soil has the lowest percolation rate . to get the mm you will have to use following formula percolation rate = amount of water[ml] percolation rate
percolation rate of water is different in different types of soil . it is the highest in the sandy soil and least in the clayey soil. to calculate the percolation rate use this formula- percolation rate (ml/min)amount of water(ml)/percolation time percolation refers to the ability of the soil to absorb water or liquids