Podzol
Podzol | |
---|---|
Podsol, Podosol, Spodosol, Espodossolo | |
illuviation C: common |
In soil science, podzols are the typical soils of coniferous or boreal forests and also the typical soils of eucalypt forests and heathlands in southern Australia. In Western Europe, podzols develop on heathland, which is often a construct of human interference through grazing and burning. In some British moorlands with podzolic soils, cambisols are preserved under Bronze Age barrows.[2]
Term
Podzol means "under-ash" and is derived from the Russian под (pod) + зола́ (zola); the full form is подзо́листая по́чва (podzolistaya pochva), meaning "under-ashed soil". The term was first given in mid-1875 by Vasily Dokuchaev.[3][4] It refers to the common experience of Russian peasants of plowing up an apparent under-layer of ash (leached or E horizon) during first plowing of a virgin soil of that type.[5]
Characteristics
Podzols can occur on almost any parent material but generally derive from either quartz-rich sands and sandstone or sedimentary debris from magmatic rocks, provided there is high precipitation.[6] Most Podzols are poor soils for agriculture due to the sandy portion, resulting in a low level of moisture and nutrients. Some are sandy and excessively drained. Others have shallow rooting zones and poor drainage due to subsoil cementation. A low pH further compounds issues, along with phosphate deficiencies and aluminum toxicity. The best agricultural use of Podzols is for grazing, although well-drained loamy types can be very productive for crops if lime and fertilizer are used.
The E horizon (or Ae in Canadian soil classification system), which is usually 4 to 8 centimetres (1.6 to 3.1 in) thick, is low in Fe and Al oxides and humus. It is formed under moist, cool and acidic conditions, especially where the parent material, such as
In some Podzols, the E horizon is absent—either masked by biological activity or obliterated by disturbance. Podzols with little or no E horizon development are often classified as brown Podzolic soils, also called
Geographic distribution
Podzols cover about 4,850,000 square kilometres (1,870,000 sq mi) worldwide and are usually found under sclerophyllous woody vegetation. By extent Podzols are most common in temperate and boreal zones of the Northern Hemisphere but they can also be found in other settings including both temperate rainforests and tropical areas.[7]
In South America Podzols occur beneath Nothofagus betuloides forests in Tierra del Fuego.[8]
Podzolization
Podzolization (or Podsolization
Preconditions
Podzolization usually occurs under
Key steps
The soil-forming process of podzolization can be broken down into two main steps:
- Mobilization and translocation of organic matter, Fe and Al from the surface horizon, and
- Immobilization and stabilization of organic matter, Fe and Al into the subsoil.[11][13][14]
In the topsoil of acidic soils, organic matter (mostly from
There are several reasons why these organo-mineral complexes immobilize in the B horizon: If during the eluviation process more Al- or Fe-ions bind to the organic compounds, the complex can flocculate as the solubility of it decreases with increasing metal to carbon ratio. Apart from that, a higher
The relocated substances can sometimes separate in the illuvial horizons. Then, organic substances are mostly enriched in the uppermost part of the illuvial horizon, whereas Fe- and Al-oxides are mostly found in the lower parts of the illuvial horizon.[10]
Podzolization also promotes the relocation of some nutrients (Cu, Fe, Mn, Mo and P) that sometimes brings them closer to plant roots.[10]
In different soil classification systems
The definitions in different soil classification systems are quite different. Especially soils that show pronounced other soil-forming processes in addition to podzolization are handled in different ways. The following correlations refer to soils, which have undergone advanced podzolization but lack prominent other soil-forming processes.
The term Podzols is used in the World Reference Base for Soil Resources[15] (WRB) and in many national soil classification systems (in some of them, spelled Podsols).
- The USDA soil taxonomy[16] and the Chinese soil taxonomy[17] call these soils Spodosols.[18]
- The Canadian system of soil classification matches Podzols with soils under the Podzolic order (e.g. Humo-Ferric Podzol).[19][20]
- The Australian Soil Classification[21] uses the term Podosols.
- The Brazilian Soil Classification System[22] calls them Espodossolos.
See also
References
- ^ Podzols by Otto Spaargaren in Encyclopedia of Soil Science, pp. 580-582
- OCLC 3814746.[page needed]
- ^ Докучаев В. В. О подзоле Смоленской губернии // Труды Санкт-Петербургского общества естествоиспытателей. 1875. T. 6. Отд. минерал. и геол. Протоколы. С. XXI—XXII.
- ^ Докучаев В. В. О подзоле // Труды Императорского Вольного экономического общества. 1880. T. 1. Вып. 2. С. 142—150.
- ^ Rode A. A. To the problem of the degree of podzolization of soils // Studies in the genesis and geography of soils. M.: Acad. Sci. USSR, 1935. P. 55-70.
- ^ Chesworth, W. (Eds.), 2008. Encyclopedia of soil science, The Netherlands.
- ^ Spaargaren, Otto. Podzols. Encyclopedia of Soil Science, pp. 580–581.
- ^ )
- ^ OCLC 506415938.
- ^ ISSN 0016-7061.
- ^ ISSN 0008-4271.
- ISSN 0016-7061.
- ISSN 0016-7061.
- ^ IUSS Working Group WRB (2022). "World Reference Base for Soil Resources, fourth edition" (PDF). International Union of Soil Sciences, Vienna. Retrieved 2023-08-18.
- ^ "Keys to Soil Taxonomy 2014". Archived from the original on 2018-11-28. Retrieved 2018-11-27.
- ^ Institute of Soil Science, Chinese Academy of Sciences (2001). Chinese Soil Taxonomy. Science Press, Beijing, New York.
- ^ "Spodosols". geo.msu.edu. Archived from the original on 2018-03-30. Retrieved 2018-05-04.
- ^ "Podzolic - Soils of Canada". www.soilsofcanada.ca. Archived from the original on 2018-04-22. Retrieved 2018-05-07.
- OCLC 44961488.
- ^ R.F. Isbell and the National Committee on Soil and Terrain (2016). "Australian Soil Classification, second edition (as Online Interactive Key)". CSIRO. Archived from the original on 29 February 2016. Retrieved 11 February 2016.
- ^ dos Santos, Humberto Gonçalves; et al. (2018). Sistema Brasileira de Classificação de Solos, quinta edição. Embrapa, Brasilia.
Further reading
- W. Zech, P. Schad, G. Hintermaier-Erhard: Soils of the World. Springer, Berlin 2022, Chapter 3.3.3. ISBN 978-3-540-30460-9
External links
- "Spodosols". USDA-NRCS. Archived from the original on 2006-05-09. Retrieved 2006-05-14.[dead link]
- "Spodosols". University of Florida. Archived from the original on September 18, 2004. Retrieved 2006-05-14.
- "Spodosols". University of Idaho. Archived from the original on 2006-03-27. Retrieved 2006-05-14.
- The Podzolic Order
- Podzol http://classification.soilweb.ca/podzol/
- http://edafologia.ugr.es/revista/tomo9b/a107text.pdf
- profile photos (with classification) WRB homepage
- profile photos (with classification) IUSS World of Soils