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Histosol and landscape BR

Soil profile: A representative soil profile of an Histosol from the Cerado physiographic region--a vast tropical savanna ecoregion of Brazil, particularly in the states of Goiás, Mato Grosso do Sul, Mato Grosso, Tocantins, Minas Gerais and the Federal District of Brazil. (Horizonation is by Brazil soil classification system.)

 

Landscape: Typical landscape and vegetation associated with Histosols occurring in low-lying areas in Brazil.

 

In both the World Reference Base for Soil Resources (WRB) and the USDA soil taxonomy, a Histosol is a soil consisting primarily of organic materials. They are defined as having 40 centimetres (16 in) or more of organic soil material in the upper 80 centimetres (31 in). Organic soil material has an organic carbon content (by weight) of 12 to 18 percent, or more, depending on the clay content of the soil. These materials include muck (sapric soil material), mucky peat (hemic soil material), or peat (fibric soil material). Aquic conditions or artificial drainage are required. Typically, Histosols have very low bulk density and are poorly drained because the organic matter holds water very well. Most are acidic and many are very deficient in major plant nutrients which are washed away in the consistently moist soil.

 

Histosol (Organossolos) and landscape BRAZIL--In the Brazil soil classification system, these soils are classified as Organossolos. Organossolos are soils that are very rich in organic matter and are characterized by an organic carbon level that is greater than 80 g/kg. These soils are usually completely saturated for at least a month out of the year and/or have a large amount of organic matter accumulation.

 

For additional information about these soils, visit:

sites.google.com/site/soil350brazilsoilsla/soil-formation...

 

and...

 

For additional information about U.S. soil classification, visit:

www.nrcs.usda.gov/wps/portal/nrcs/main/soils/survey/class...

 

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Uploaded on June 17, 2021