Soil structure

What is soil structure?

Soil structure is the arrangement of soil particles (sand, silt, clay and organic matter) into granules, crumbs or blocks. It is the shape that the soil takes based on its physical, chemical and biological properties. Soil structure is often confused with soil texture, both of which affect the soil’s drainage and aeration capabilities.

Well-structured soils, as in the image above, are usually crumbly and friable and have plenty of pore space to allow water and air movement and healthy root development.

The image below on the right shows a poorly structured, cloddy soil, which will be difficult to work.

Why is structure important?

To perform effectively as a growing medium soils need an open structure through the soil profile. A good soil structure is important to allow air and water into the soil which are vital for healthy plant growth. It will improve drainage and reduce soil erosion caused by excess surface run-off.

Info centre - well structured soil
Info centre - soil structure poorly structured soil

Without structure, soils will suffer from anaerobism, waterlogging and nutrient lock-up and, ultimately, plants will die!

Checking your soil structure

Soil structure can be examined quite easily by visual inspection. Dig a hole approximately 30-40cm deep, making sure there are no spade marks along one side. Examine the unmarked side of the hole, inserting a knife or pen at approx 1cm intervals vertically to identify compacted zones where there is greater resistance.

Looking at root development and for evidence of worm activity will also give an indication of how well-structured your soil is. Shallow, restricted rooting and lack of earthworm activity indicate a problem with the soil structure which needs to addressed.

Find out more about improving your soil.