Soil Permeability and Infiltration

A soil’s permeability is a measure of the ability of air and water to move through it. Permeability is influenced by the size, shape, and continuity of the pore spaces, which in turn are dependent on the soil bulk density, structure and texture. Most soil series are assigned to a single permeability class based on the most restrictive layer in the upper 5 feet of the soil profile. However, soil series with contrasting textures in the soil profile are assigned to more than one permeability class. In most cases, soils with a slow, very slow, rapid or very rapid permeability classification are considered poor for irrigation.

Infiltration is the downward flow of water from the surface through the soil. The infiltration rate (sometimes called intake rate) of a soil is a measure of its ability to absorb an amount of rain or irrigation water over a given time period. It is commonly expressed in inches per hour. It is dependent on the permeability of the surface soil, moisture content of the soil and surface conditions such as roughness (tillage and plant residue), slope, and plant cover.

Coarse textured soils such as sands and gravel usually have high infiltration rates. The infiltration rates of medium and fine textured soils such as loams, silts, and clays are lower than those of coarse textured soils and more dependent on the stability of the soil aggregates. Water and plant nutrient losses may be greater on coarse textured soils, so the timing and quantity of chemical and water applications is particularly critical on these soils.

 

 

 
Just as the porosity of a soil affects how much water it can hold, it also affects how quickly water can flow through the soil.

So we know that the ability of water to flow through a type of soil is  commonly referred to as permeability. As you can probably guess, the permeability of gravel is higher than that of clay. But can you guess how much higher? Click the button below to see how long it might take water to travel 1 meter in different soil types….


Special Thanks to MTU.edu for the diagram!

 

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One Response to Soil Permeability and Infiltration

  1. Jeffrey Smith says:

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