Soil structure is the arrangement of the soil solid particles (sand, silt, and clay) allowing for open pore space between the particles. The ideal soil components include: air 25%, water 25%, minerals 45%, and OM 5%. Structure is determined by how the individual units are arranged, bound together, or clumped to form aggregates resulting in the arrangement of soil pore spaces between them. The clumping is the result of OM (carbon) and biology activity such as earthworms and fungi.“ Carbon is the food for the soil that builds the aggregates and makes the glue. Green plants take in carbon dioxide from the air and secrete carbon exudates into the soil.” Jay Fuhrer, Natural Resources Conservation Service, Menoken, ND. “When it comes to the glue, the fungi do most of the work. The fungi are comprised of long filaments that branch through the soil. Tillage breaks the filaments making it hard for the fungi to survive.”
Tillage, one of the leading causes of soil structure breakdown, has been heavily used in the past. The loss of structure reduces the infiltration of water by more than a 10-fold rate and adds to soil compaction. Dr. Stewart Wuest, USDA ARS reported ½” per hour water infiltration on conventionally tilled soils while no-till soils allowed up to 5” per hour infiltration.

Figure 1. A diagrammatic representation of well structure and poorly structured soils. Source: Victorian Department of Agriculture
View the soil aggregate stability test demo (video) by Doug Sieck’s Ranch in North Central South Dakota.
