In soil science, podzols, also known as podosols, spodosols, or espodossolos, 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.

Podzol, one of the 30 soil groups in the classification system of the Food and Agriculture Organization (FAO). Podzols form under forested landscapes on coarse parent material that is high in quartz. They have a characteristic subsurface layer known as the spodic horizon made up of accumulated humus and metal oxides, usually iron and aluminum.

There are three main British soils; podzol, brown earth and gley. Podzols are easily recognisable by their distinct layers or horizons. A grey or light-coloured 'E' horizon is the result of...

The meaning of PODZOL is any of a group of zonal soils that develop in a moist climate especially under coniferous or mixed forest and have an organic mat and a thin organic-mineral layer above a light gray leached layer resting on a dark horizon that is marked by illuviation and enriched with amorphous clay.

Podsol is an acid soil type characterized by an organic surface horizon, a leached underlying horizon depleted of nutrients, and sometimes a hard layer of iron and other metal oxides known as a 'pan'.

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Podzols oc-cur in humid areas in the Boreal and Temperate Zones and locally also in the tropics. The name ‘Podzol’ is used in most national and international soil classification systems; the USDA Soil Taxonomy refers to these soils as ‘Spodosols’.

Podosols are typically found in close proximity to the coast and on islands comprised of quartz sand. Distribution of Podosols in Australia. Soil Profile (View type example photo of Aeric Podosol).

Learn about the unique properties and formation of podsol soils, their importance in ecosystems, and sustainable management practices to improve soil fertility and reduce waterlogging.

Podsole zeichnen sich durch die Verlagerung von Eisen oder Humus aus, die sogenannte Podsolierung. Charakteristisch sind diagnostische Verarmungs- (Sauerbleichungs-) und Anreicherungshorizonte in der Abfolge Ah/Ae/Bs,Bh/C. Diese Böden sind in den Verbreitungsgebieten von Gesteinen zu finden, die leicht versauern.