There are a number of definitions and classifications for soil structure. In general terms soil structure describes how the soil particles and aggregates are arranged.

A soil that has a good soil structure will contain adequate pore spaces for root growth and will have aggregates that are of a size and shape that promote a relatively persistent state of the pores and aggregates in the soil.

A poorly structured soil is one that has minimal pore spaces, with soil particles and small aggregates filling the spaces between larger aggregates. A compacted sportspitch is a good example of a structureless soil.

Within a soil profile there are several types of soil ped (individual aggregates) that are recognised. These are as follows:

Soil ped name Sub-division Description Diagrammatic representation of ped
Blocky Angular Vertical and Horizontal cracking are fairly evenly balanced.
The edges of the aggregates are relatively sharp.
When the soil is wet, the aggregates swell and fit together like a jigsaw.
angular
Sub-angular Vertical and Horizontal cracking are fairly evenly balanced.
The edges of the aggregates are more rounded.
When the soil is wet, the aggregates swell and fit together like a jigsaw.
subangular
Laminar (or Platy) Not applicable Cracking of the aggregates is most significant along the Horizontal plane. platy
Prism - like Columnar Cracking of the aggregates is significantly along the Vertical.
The tops of the aggregates have a generally rounded feature.
columnar
Prismatic Cracking of the aggregates is significantly along the Vertical.
The tops of the aggregates are more angular and sharp edged.
prismatic
Spheriodal Crumb These aggregates are more rounded than Blocky aggregates.
Noticeable pore spaces remain between the aggregates when the soil swells.
There is good porosity within the soil profile.
crumbs
Granular These peds are similar to the crumb ped, however, they have fine particles in between the aggregates, resulting in low porosity. Granular

The soil peds are typically made up of smaller aggregates (also called structural units). Four main structural units are recognised.

Structural Units

Unit name Size Description
Domain 5 micron (0.005mm) This is an aggregation of clay particles.
Granule < 500 micron (0.5mm) Clay domains, silt and fine sand form these small units.
Crumb 0.5 - 10mm
It is convenient to sub-divide this unit into aggregates of
(a) 0.5 - 2mm
(b) 2 - 5mm
(c) 5 - 10mm
This is a group of granules.

Having crumb sub-divisions allows a soil to be analysed in more detail following any wet sieving.

Seed bed preparation will have crumbs for the tilth.

Clod > 10mm These are relatively large soil aggregates.

Small clods may be suitable for soil areas that require turfing, but larger clods will need to be broken down into crumbs.