Key to Soil Orders
The material below is arranged to give the simplest way of identifying a particular soil in terms of the Orders, and is not a complete definition of each Order. Work successively through the key until an apparent identification is made, then check the full definition of the Order by clicking on the highlighted name. Hyperlinked words or phrases are defined in the glossary.
- Soils resulting from human activities which have caused a profound modification, mixing, truncation or burial of the original soil horizons, or the creation of new soil parent materials.
- Soils that are not regularly inundated by saline tidal waters and either:
- Have more than 0.4 m of organic materials within the upper 0.8 m. The required thickness may either extend down from the surface or be taken cumulatively within the upper 0.8 m; or
- Have organic materials extending from the surface to a minimum depth of 0.1 m; these either overlie a mineral soil horizon or unconsoidated mineral material no thicker than the organic materials above, or directly overlie rock or other hard layers, partially weathered or decomposed rock or saprolite, or overlie fragmental material such as gravel, cobbles or stones in which the interstices are filled or partially filled with organic material. In some soils there may be layers of humose, melacic and/or melanic horizon material underlying the organic materials and overlying the substrate.
- Other soils that have a Bs, Bhs or Bh horizon (see Podosol diagnostic horizons).
These horizons may occur either singly or in combination. PODOSOLS
- Other soils that:
- Have a clay field texture or 35% or more clay throughout the solum except for thin, surface crusty horizons 30 mm or less thick, and
- Unless too moist, have open cracks at some time in most years that are at least 5 mm wide and extend upward to the surface or to the base of any plough layer, peaty horizon, self-mulching horizon, or thin, surface crusty horizon, and
- At some depth in the solum, have slickensides and/or lenticular peds.
- Other soils that are saturated in the major part of the soil profile for at least 2-3 months in most years (ie. includes tidal waters).HYDROSOLS
- Other soils with a clear or abrupt textural B horizon and in which the major part of the upper 0.2 m of the B2t horizon (or the major part of the entire B2t horizon if it is less than 0.2 m thick) is strongly acid.KUROSOLS
- Other soils with a clear or abrupt textural B horizon and in which the major part of the upper 0.2 m of the B2t horizon (or the major part of the entire B2t horizon if it is less than 0.2 m thick) is sodic and is not strongly subplastic.SODOSOLS
- Other soils with a clear or abrupt textural B horizon and in which the major part of the upper 0.2 m of the B2t horizon (or the major part of the entire B2t horizon if it is less than 0.2 m thick) is not strongly acid.CHROMOSOLS
- Other soils that:
- Are either calcareous throughout the solum - or calcareous at least directly below the A1 or Ap horizon, or within a depth of 0.2 m (whichever is shallower). Carbonate accumulations must be judged to be pedogenic, i.e. are a result of soil forming processes in situ (either current or relict). Soils dominated by non-pedogenic calcareous materials such as particles of limestone or shells are excluded. See also calcrete, and
- Do not have deep sandy profiles that have a field texture of sand, loamy sand or clayey sand in 80% or more of the upper 1.0 m.
- Other soils with B2 horizons in which the major part has a free iron oxide content greater than 5% Fe in the fine earth fraction (<2 mm). Soils with a B2 horizon in which at least 0.3m has vertic properties are excluded (see also Comment and footnote in Ferrosols).FERROSOLS
- Other soils with B2 horizons that have grade of pedality greater than weak throughout the major part of the horizon.DERMOSOLS
- Other soils that:
- Have B2 horizons in which the major part has a grade of pedality that is massive or weak , and
- Have a maximum clay content in some part of the B2 horizon which exceeds 15% (ie. heavy sandy loam [SL+] or heavier).
- Other soils that have, within the upper 1.0 m of the soil profile:
- a sandy field texture (i.e. a field texture of sand, loamy sand or clayey sand) in one or more layers or horizons with a combined thickness of at least 0.8 m; and
- no layer with a clay content that exceeds 15% (i.e. heavy sandy loam [SL+] or heavier) excluding argic horizon/s; and
- ≤10% (by visual abundance and weighted average) of coarse fragments and/or hard segregations >2 mm in size; and
- no hard layers (cemented pans, other cemented materials, rock or saprock that do not soften when moist)
- Other soils with negligible (rudimentary), if any, pedologic organisation apart from the minimal development of an A1 horizon or the presence of less than 10% of B horizon material (including pedogenic carbonate) in fissures in the parent rock or saprolite. The soils have a grade of pedality of single grain, massive or weak in the A1 horizon and show no pedological colour change apart from darkening of an A1 horizon. There is little or no texture or colour change with depth unless stratified or buried soils are present. Cemented pans may be present as a substrate material.RUDOSOLS
- Other soils.TENOSOLS