Soil samples illustrating horizons (subsoil on right)

A soil horizon is a specific layer in the soil which parallels the soil surface and possesses physical characteristics which differ from the layers above and beneath. Horizon formation is a function of a range of geological, chemical, and biological processes and occurs over long time periods. Identification and description of the horizons present at a given site is the first step in classifying a soil at higher levels, through the use of systems such as the USDA soil taxonomy or the Australian Soil Classification. Image File history File linksMetadata DSCN0384_(Small). ... Image File history File linksMetadata DSCN0384_(Small). ... Loess field in Germany Surface-water-gley developed in glacial till, Northern Ireland Soil is a complex mixture of materials, principally ground up rock and water. ... USDA Soil Taxonomy developed by United States Department of Agriculture and the National Cooperative Soil Survey provides an elaborate classification of soil types according to several parameters (most commonly their properties) and in several levels: Order, Suborder, Great Group, Subgroup, Family, and Series. ... The Australian Soil Classification is the system used to describe and group soils in Australia. ...

The term 'horizon' describes each of the distinctive layers that occur in a soil. Each soil type has at least one, usually three or four different horizons and these are described by soil scientists when seeking to classify soils (Soil-Net). Horizons are defined in most cases by obvious physical features, colour and texture being chief among them. These may be described both in absolute terms (particle size distribution for texture, for instance) and in terms relative to the surrounding material, ie, ‘coarser’ or ‘sandier’ than the horizons above and below.

Most soils conform to a similar general pattern of horizons, often represented as an ‘ideal’ soil in diagrams. Each main horizon is denoted by a capital letter, which may then be followed by several alphanumerical modifiers highlighting particular outstanding features of the horizon. While the general O-A-B-C-R sequence seems fairly universal, some variation exists between the classification systems in different parts of the world. In addition, the exact definition of each main horizon may differ slightly – for instance, the US system uses the thickness of a horizon as a distinguishing feature, while the Australian system does not. It should be emphasised that no one system is more correct – as artificial constructs, their utility lies in their ability to accurately describe local conditions in a consistent manner.

Main Horizons

The following horizons are listed by their position from top to bottom within the soil profile. Not all of these layers are present in every location – for instance, P horizons only form in areas which have been waterlogged for long periods of time. Soils with a history of human interference, for instance through major earthworks or regular deep ploughing, may lack distinct horizons almost completely. When examining soils in the field, attention must be paid to the local geomorphology and the historical uses to which the land has been put in order to ensure that the appropriate names are applied to the observed horizons. A soil profile is a cross section through the soil which reveals its horizons (layers). ...

Layers

Soil generally consists of visually and texturally distinct layers, which can be summarized as follows from top to bottom: Soil texture triangle, showing the 12 major textural classes, and particle size scales. ...

O) Organic matter: Litter layer of plant residues in relatively undecomposed form.

A) Surface soil: Layer of mineral soil with most organic matter accumulation and soil life. This layer eluviates (is depleted of) iron, clay, aluminum, organic compounds, and other soluble constituents. When eluviation is pronounced, a lighter colored "E" subsurface soil horizon is apparent at the base of the "A" horizon.

B) Subsoil: Layer of alteration below an "E" or "A" horizon. This layer accumulates iron, clay, aluminum and organic compounds, a process referred to as illuviation.

C) Substratum: Layer of unconsolidated soil parent material. This layer may accumulate the more soluble compounds that bypass the "B" horizon.

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O Horizon

The “O” stands for Organic, with this surface layer being dominated by the presence of large amounts of organic material in varying stages of decomposition. The O Horizon should be held distinct from the layer of leaf litter covering many heavily vegetated areas – these contain no weathered mineral particles and are thus not part of the soil itself. If desired, O horizons may be divided into O1 and O2 categories, whereby O1 horizons contain decomposed matter whose origin can be spotted by sight (for instance, fragments of rotting leaves), and O2 horizons contain only well-decomposed organic matter whose origin cannot be immediately seen.

P Horizon

These horizons are also heavily organic, but are distinct from O Horizons in that they form under waterlogged conditions. The “P” designation comes from their common name, peats. They may be divided into P1 and P2 in the same way as O Horizons. Peat in Lewis, Scotland Peat is an accumulation of partially decayed vegetation matter. ...

A Horizon

The A Horizon is the top layer of the soil horizon. The technical definition of an A Horizon may vary, but it is most commonly described in terms relative to deeper layers. A Horizons may be darker in color than deeper layers and contain more organic material, or they may be lighter but contain less clay or sesquioxides. The A is a surface horizon, and as such is also known as the zone in which most biological activity occurs. Soil organisms such as worms, nematodes, fungi, and many species of bacteria exist here, often in close association with plant roots. However, since biological activity extends far deeper into the soil, it cannot be used as a chief distinguishing feature of an A Horizon. Organic material or organic matter is informally used to denote a material that originated as a living organism; most such materials contain carbon and are capable of decay. ... For other uses, see Clay (disambiguation). ... An oxide containing three atoms of oxygen with two atoms (or radicals) of some other substance. ... It has been suggested that this article or section be merged with Bioactivity. ... Worms may refer to: The plural form of worm Worms (computer game), a series of turn-based computer games Worms, Germany, a city in the southwest of Germany René Worms, founder of the Institut International de Sociologie in 1893 Worms (family) The common term for an animals condition of... Classes Adenophora    Subclass Enoplia    Subclass Chromadoria Secernentea    Subclass Rhabditia    Subclass Spiruria    Subclass Diplogasteria The roundworms (Phylum Nematoda) are one of the most common phyla of animals, with over 20,000 different described species. ... Divisions Chytridiomycota Zygomycota Ascomycota Basidiomycota The Fungi (singular: fungus) are a large group of organisms ranked as a kingdom within the Domain Eukaryota. ... Phyla Actinobacteria Aquificae Chlamydiae Bacteroidetes/Chlorobi Chloroflexi Chrysiogenetes Cyanobacteria Deferribacteres Deinococcus-Thermus Dictyoglomi Fibrobacteres/Acidobacteria Firmicutes Fusobacteria Gemmatimonadetes Lentisphaerae Nitrospirae Planctomycetes Proteobacteria Spirochaetes Thermodesulfobacteria Thermomicrobia Thermotogae Verrucomicrobia Bacteria (singular: bacterium) are unicellular microorganisms. ... Primary and secondary roots in a cotton plant In vascular plants, the root is that organ of a plant body that typically lies below the surface of the soil (compare with stem). ...

A horizons may be divided into A1, A2, and A3 horizons under the Australian system. A1s contain relatively higher levels of humic matter and will have a darker colour than the A2. A3s are a transitional layer between A and B, whose characteristics are more similar to the overlying A horizons than the B horizons below.

B Horizon

B Horizons are commonly referred to as ‘subsoil’, and consist of mineral layers which may contain concentrations of clay or minerals such as iron or aluminium, or organic material. In addition, they are defined by having a distinctly different structure or consistence to the A horizon above and the horizons below. They may also have ‘stronger’ colours (ie higher chroma) than the A horizon. Chroma may refer to: Chroma, short for Chromatics, the science of color. ...

As with A horizons, B horizons may be divided into B1, B2, and B3 types under the Australian system. B1 is a transitional horizon of the opposite nature to an A3 – dominated by the properties of the B horizons below it, but containing some A-horizon characteristics. B2 horizons have a concentration of clay, minerals, or organics and feature the strongest pedological development within the profile. B3 horizons are transitional between the overlying B layers and the material beneath it, whether C or D horizon.

The A3, B1, and B3 horizons are not tightly defined, and their use is generally at the discretion of the individual worker.

E Horizon

“E” being short for eluviated, this designation is most commonly used in the United States to label a horizon that has been significantly leached of its mineral and/or organic content, leaving a pale layer largely composed of silicates. These are present only in older, well-developed soils, and generally occur between the A and B Horizons. In regions where this designation is not employed, leached layers are classified firstly as an A or B according to other characteristics, and then appended with the designation “e” (see the section below on horizon suffixes).

The above layers may be referred to collectively as the ‘solum’. The layers below have no collective name but are distinct in that they are noticeably less affected by surface soil-forming processes.

C Horizon

C Horizons are simply named so because they come ‘after’ A and B within the soil profile. These layers are little affected by soil forming processes, and their lack of pedological development is one of their defining attributes. C Horizons may contain lumps of unweathered rock, rather than being comprised solely of small fragments as in the solum. ‘Ghost’ rock structure may be present within these horizons.

D Horizon

D horizons are not universally distinguished, but in the Australian system refer to ‘any soil material below the solum that is unlike the solum in general character, is not C horizon, and cannot be given reliable designation… [it] may be recognised by the contrast in pedologic organization between it and the overlying horizons’ (MacDonald et al, 1990, p. 106).

R Horizon

R horizons basically denote the layer of partially-weathered bedrock at the base of the soil profile. Unlike the above layers, R horizons largely comprise continuous masses (as opposed to boulders) of hard rock that cannot be excavated by hand. Soils formed in situ will exhibit strong similarities to this bedrock layer, while depositional will often appear very distinct.

Horizon numbering and suffixes

In addition to the main descriptors above, several modifiers exist to add necessary detail to each horizon. Firstly, each major horizon may be divided into sub-horizons by the addition of a numerical subscript, based on minor shifts in colour or texture with increasing depth (e.g., B21, B22, B23 etc). While this can add necessary depth to a field description, workers should bear in mind that excessive division of a soil profile into narrow sub-horizons should be avoided. Walking as little as ten metres in any direction and digging another hole can often reveal a very different profile in regards to the depth and thickness of each horizon. Over-precise description can be a waste of time, and as a rule of thumb, layers thinner than 5cm (2 inches) or so are best described as pans or segregations within a horizon rather than as a distinct layer.

Suffixes describing particular physical features of a horizon may also be added. These vary considerably between countries, but a limited selection of common ones employed in Australia is listed here:

• c : presence of mineral concretions or nodules, perhaps of iron, aluminium, or manganese.
• e : a bleached horizon.
• h : accumulation of organic matter.
• p : disturbed by ploughing or other tillage practices (A horizon only).
• s : sesquioxide accumulation.

Thus, a bleached A2 horizon would be described as ‘A2e’. An oxide containing three atoms of oxygen with two atoms (or radicals) of some other substance. ...

The US system employs largely similar suffixes, with a few important differences. For instance, 'e' under the US system denotes a horizon containing 'organic material of intermediate decomposition' rather than a bleached horizon. A full list of suffixes is available online as part of the USDA Soil Survey Manual.

Buried Soils

While soil formation is generally described as occurring in situ, as rock breaks down and is mixed with other materials, the process is often far more complicated. For instance, a fully-formed profile may have developed in an area only to be buried by wind- or water-deposited sediments which later formed into another soil profile. This sort of occurrence is most common in coastal areas, and descriptions are modified by numerical prefixes. Thus, a profile containing a buried sequence could be structured O, A1, A2, B2, 2A2, 2B21, 2B22, 2C with the buried profile commencing at 2A2.

References

• McDonald, R. C. et al. 1990. Australian Soil and Land Survey Field Handbook, 2nd Ed. Melbourne: Inkata Press.
• This article incorporates text from http://soils.usda.gov/technical/manual/, a public domain work of the United States Government.
• Soil-Net section on soil horizons.