Retisol

A Retisol is a Reference Soil Group of the World Reference Base for Soil Resources (WRB).^[1] Retisols are characterized by clay migration and an additional specific feature: The clay-poorer and lighter coloured eluvial horizon intercalates netlike into the clay-richer more intensely coloured illuvial horizon. The illuvial horizon is the diagnostic argic horizon, and the intercalation is called retic properties (Latin: rete = net).

Retisols were newly introduced with the third edition of the WRB in 2014. They include the narrower defined Albeluvisols^[2] of the first and second edition (1998 and 2006), which were abolished in 2014. The definition of the Retisols resembles the definition of the Podzoluvisols of the Legend (1974) and the Revised Legend (1988) of the FAO soil classification.

Horizonation

A typical horizon sequence according to Annex 3 of the WRB is:

A – mineral topsoil, usually with relatively low organic matter concentrations
E – horizon that lost clay (eluvial horizon)
Bt/E – intercalating eluvial/illuvial horizon (argic horizon with retic properties)
Bt – horizon that gained clay (illuvial horizon, argic horizon)
C – more or less unweathered material (parent material)

Occurrence and use

Retisols occur mainly in periglacial areas of the last glaciation in Europe and North America. In Europe, they are found along a belt from Belgium through northern Germany, Poland and Belarus to Russia. Because the very specific retic properties are not so widespread, they normally do not cover larger areas.

Most Retisols are dominated by high-activity clays and show a low base saturation. Many are used as forest^[3] or pasture land. Especially their physical conditions are not good for agriculture. The topsoils are often poor in clay minerals and iron oxides. In the subsoil, the rainwater runs downwards predominantly in the clay-poorer parts, whereas the clay-richer and therefore also nutrient-richer parts are often insufficiently humid. The clay-richer parts are relatively dense and difficult to be rooted. These characteristics make the Retisols also unattractive for many soil animals, especially earthworms. Retisols have typically sandy or silty topsoils that are prone to erosion.

Relationships with other Reference Soil Groups

The WRB defines five Reference soil Groups with a compulsory argic horizon. Only the Retisols have retic properties. The other four are differentiated according to the cation exchange capacity per kg clay at pH 7 (CEC / kg clay) in the argic horizon and according to the base saturation calculated per sum of exchangeable cations (BSeff) in the subsoil. For Luvisols both values are high. Alisols have a high CEC and a low BS. Lixisols have a low CEC and a high BS. For Acrisols both values are low. Soils with an argic horizon and retic properties that are dominated by stagnant water are classified as Retic Stagnosols.

References

^ IUSS Working Group WRB (2022). "World Reference Base for Soil Resources, fourth edition" (PDF). International Union of Soil Sciences, Vienna.
^ W. Zech, P. Schad, G. Hintermaier-Erhard: Böden der Welt. 2. Auflage. Springer-Spektrum, Heidelberg 2014, ISBN 978-3-642-36574-4.
^ W.E.H. Blum, P. Schad, S. Nortcliff: Essentials of Soil Science. Soil formation, functions, use and classification (World Reference Base, WRB). Borntraeger Science Publishers, Stuttgart 2018. ISBN 978-3-443-01090-4

External links

profile photos (with classification) WRB homepage
profile photos (with classification) IUSS World of Soils

[1] IUSS Working Group WRB (2022). "World Reference Base for Soil Resources, fourth edition" (PDF). International Union of Soil Sciences, Vienna.

[2] W. Zech, P. Schad, G. Hintermaier-Erhard: Böden der Welt. 2. Auflage. Springer-Spektrum, Heidelberg 2014, ISBN 978-3-642-36574-4.

[3] W.E.H. Blum, P. Schad, S. Nortcliff: Essentials of Soil Science. Soil formation, functions, use and classification (World Reference Base, WRB). Borntraeger Science Publishers, Stuttgart 2018. ISBN 978-3-443-01090-4

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v t e Soil classification
World Reference Base for Soil Resources (1998–)	Acrisols Alisols Andosols Anthrosols Arenosols Calcisols Cambisols Chernozem Cryosols Durisols Ferralsols Fluvisols Gleysols Gypsisols Histosol Kastanozems Leptosols Lixisols Luvisols Nitisols Phaeozems Planosols Plinthosols Podzols Regosols Retisols Solonchaks Solonetz Stagnosol Technosols Umbrisols Vertisols
USDA soil taxonomy	Alfisols Andisols Aridisols Entisols Gelisols Histosols Inceptisols Mollisols Oxisols Spodosols Ultisols Vertisols
Other systems	FAO soil classification (1974–1998) Unified Soil Classification System AASHTO Soil Classification System Référentiel pédologique (French classification system) Canadian system of soil classification Australian Soil Classification Polish Soil Classification 1938 USDA soil taxonomy List of U.S. state soils List of vineyard soil types
Non-systematic soil types	Sand Silt Clay Loam Topsoil Subsoil Soil crust Claypan Hardpan Gypcrust Caliche Parent material Pedosphere Laimosphere Rhizosphere Bulk soil Alkali soil Bay mud Blue goo Brickearth Brown earth Calcareous grassland Dark earth Dry quicksand Duplex soil Eluvium Expansive clay Fill dirt Fuller's earth Hydrophobic soil Loess Lunar soil Martian soil Mud Muskeg Paleosol Peat Prime farmland Quicksand Serpentine soil Spodic soil Stagnogley Subaqueous soil Takir Terra preta Terra rossa Tropical peat Yedoma
Types of soil