What are Soil Aggregates?

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Soil aggregates retained on a 4.75 mm sieve after wet sieving experiment. Credit: Nall Moonilall

This article by Nall I. Moonilall of Ohio State University is from the excellent site Soils Matter, Get the Scoop! of the Soil Science Society of America, a go-to source for valuable and honest information on the soils we garden in.

The ground beneath your feet might seem like a uniform material, but it’s really a mixture of soil particles, organic matter, and other mineral/organic components. For a soil to be healthy, it must have good structure. Soil is made up of a combination of primary particles—sand, silt and clay. These particles can be bound together into what soil scientists call “aggregates.”

These aggregates are clumps of soil that range from the micro level (less than 0.25 mm in diameter) to the macro level (greater than 0.25 mm in diameter). Furthermore, they can resemble various shapes: granular, blocky, etc. These varied shapes allow for healthy soil to have pores—spaces for air and water—, needed for healthy plant growth.

Aggregate formation is a complex process. Soil aggregates are formed through physical, chemical and biological activity below ground. They are even influenced by human factors, like tilling, walking on the surface, or even how you fertilize your garden. Formation of aggregates begins with finer soil primary particles binding together. You may know that clay particles have a negative charge. And the fertilizers you use include salts that have positively charged cations (things like potassium nitrate, etc.). The positively charged cations allow the negatively charged clay particles to bind together creating “floccules.” The type and amount of clay minerals in the soil often play an influential role in aggregation formation.

Soil crust formation on a soil exposed to simulated rainfall. You can see the crust formation on the surface of the soil as well as how deep the crust extends. (This really is soil—not cement!) Credit: Nall Moonilall

The second part of aggregate formation deals with cementation. Here, the clay floccules and other soil particles are bonded together by some type of cementing agent. (Here the word cementing means “binding”—not cement like in concrete!) Examples of cementing agents include organic matter and liming materials like calcium carbonate. Even types of oxides, like iron and aluminum, can help cement particles together.

In the case of organic matter, it is broken down by the soil microorganisms and soil fauna (earthworms, etc.). When breakdown occurs, these organisms secrete organic compounds that are the “glue” that makes cementation occur. Plant roots also play a role in aggregate formation by secreting organic compounds called root exudates. These help bind soil together near the root zone. Fungal hyphae also contribute to aggregate formation by entangling and weaving around soil particles.

As you can see, aggregate formation is the result of many interactions and feedback loops occurring below ground.

Soil aggregates play a major role in soil structure formation and soil health. In agriculture, the stability of aggregates is critical to how well an agroecosystem will function. The pore spaces in soil influence air and water storage and gaseous exchange. They create habitat for soil microorganisms, and allow for plant root development and penetration. They also assist in nutrient cycling and transport.

Soils that have high aggregate stability are less susceptible to erosion. They hold their shape when exposed to disruptive forces, like water, and do not easily break apart.


Keep soil covered! Crop residues on the soil surface help to protect soil from erosive forces. Credit: Nall Moonilall

Poorly aggregated soils disintegrate easily when exposed to erosive forces. They tend to break down faster, leading to soil degradation. Poor stability can lead to pore spaces being filled in and can ultimately result in the formation of soil crusts. This can lead to reduced infiltration and gaseous exchange. Poorly aggregated soils can reduce crop productivity.

Soil management often influences aggregate size, shape, and stability. Favorable practices that promote and maintain greater stability include:

  • Minimizing soil disturbance, like minimal tillage. This reduces aggregate destruction because they are not physically or mechanically broken apart;
  • Adding organic matter enhances aggregate strength and stability;
  • Keeping soil covered is essential to keeping soil intact. Vegetative cover on the soil reduces the impact of erosive forces;
  • Promoting a diverse cropping system. Systems that promote perennial plants or meadows have expansive rooting systems and require no tillage. Promoting this kind of diversity within a system will ensure that soil’s function is not reduced;
  • Managing for grazing. Grasses have strong root systems, but if animals graze too long, that can be disruptive to the forage system. There are many ways to graze animals and preserve or enhance soil stability;
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  • Managing for pest control. The choice of plants and how they are managed (e.g. annual vs. perennial, cover crops, rotation) are highly influential.

To recap—soil aggregates are the building blocks that make up soil and their stability is extremely important in the long-term. Soils that are well-aggregated exhibit greater soil health, ensure greater agronomic productivity, are less susceptible to soil erosion, and can play a role in carbon sequestration.

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