What is Compaction?
Compaction is a change in soil structure, not just an increase in soil density. Healthy soils have a diversity of pore sizes, while compacted soils have mostly small pores.
During the compaction process soil aggregates are pushed closer together. This reduces the size of pores, the continuity of pores, and the size and stability of aggregates. Only under severe compaction will aggregates break down.
Because the change in soil structure is complex, there is not a simple relationship between increased soil density and decreased crop yield. The changes in soil structure affect the movement of water, air, roots, and soil organisms through the soil, so the effect on yield depends on the weather, the amount and depth of compaction, and the crop type.
What causes compaction?
Wheel traffic is the main cause of compaction on most farms, though rain, drying, and animal traffic also contribute on certain soils. The amount of compaction depends on the size and weight of the equipment, the moisture level of the soil, and the type of soil (soils high in clay or low in organic matter compact more readily).
How does compaction occur?
A typical chain of events begins in the fall when heavy harvest equipment pushes soil aggregates closer together and reduces soil drainage. The next spring, the soil will not drain as quickly, and the short window of opportunity for spring field work becomes even shorter. Farmers are forced to work wet soils and more compaction occurs.
Spring tillage will loosen surface soil, but seeds in the tire tracks may have trouble emerging from the packed soil, and roots will not spread as easily. To compensate for the poor root growth, a farmer may increase the amount of fertilizer or use split applications. The extra fertilizer may mean more traffic, and may discourage extensive root growth deep into subsoil where they can help alleviate compaction.
The process of loosening soil might begin when soil swells from a good rainfall, and then shrinks during a dry spell. The swelling and shrinking causes cracks that can be filled by roots or soil organisms that further improve soil structure. Freezing and thawing also creates cracks, especially near the surface where soil may freeze and thaw several times in a season. But all of this is a slower process than the compaction caused by a 20-ton combine or grain cart.