Spodosols are most extensive in areas of cool, humid or perhumid climates in the Northeastern States, southern Alaska, the Great Lakes States, and the high mountains of the Northwestern …

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 …

Spodosols are ashy gray, acidic soils with a strongly leached surface layer. Their suitability for cultivation is limited to acid-tolerant crops and orchards, provided that sufficient lime and …

Spodosols (from Greek spodos, "wood ash") are acid soils characterized by a subsurface accumulation of humus that is complexed with Al and Fe. These photogenic soils typically form …

Spodosols are acid soils characterized by a subsurface accumulation of humus and Al & Fe oxides. These soils are very photogenic and typically have a light-colored E horizon overlying …

Spodosols are sandy mineral soils low in organic matter and natural fertility in the surface layer that contain an acidic subsurface restrictive layer composed of Al and iron (Fe) “cemented” …

Spodosols are characterized by high acidity, and have a subsoil accumulation of organic matter, along with aluminum and iron oxides, called a spodic horizon.

Oct 22, 2012 · Spodosols are most common in areas with coniferous trees as the primary native vegetation, and where the soil is coarse-textured. The driving force in the development of …

Spodosols are a type of soil characterized by a subsurface horizon that is rich in iron, aluminum, and organic matter, giving it a distinct gray or white color. These soils typically form under …

This lesson will examine each of these 12 soil orders in turn: Entisols, Inceptisols, Andisols, Mollisols, Alfisols, Spodosols, Ultisols, Oxisols, Gelisols, Histosols, Aridisols, and Vertisols.