Cutans (original) (raw)

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Cutans are the modification of the soil texture, or soil structure, at natural surfaces (particle, pore, or ped) in soil materials due to illuviation. Cutans are oriented deposits which can be composed of any of the component substances of the soil material. Cutans are common features in soil and represent focuses of chemical and biological reactions. Cutans may include clay skins or coatings of silica, sesquioxide, manganese, ferromanganese, soil organic matter or carbonate. Clay skins are also called argillans, and soil horizons with sufficient clay illuviation are termed argillic horizons.

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dbo:abstract Cutans are the modification of the soil texture, or soil structure, at natural surfaces (particle, pore, or ped) in soil materials due to illuviation. Cutans are oriented deposits which can be composed of any of the component substances of the soil material. Cutans are common features in soil and represent focuses of chemical and biological reactions. Cutans may include clay skins or coatings of silica, sesquioxide, manganese, ferromanganese, soil organic matter or carbonate. Clay skins are also called argillans, and soil horizons with sufficient clay illuviation are termed argillic horizons. (en)
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dbo:wikiPageWikiLink dbr:Carbonate dbc:Pedology dbr:Pedogenesis dbr:Clay dbr:Manganese dbr:Silica dbr:Alfisols dbr:Soil_horizons dbc:Sedimentology dbr:Soil_texture dbr:Soil_structure dbr:Ferromanganese dbr:Soil_organic_matter dbr:Illuvium dbr:Soil_morphology dbr:Sesquioxide dbr:Paleopedology dbr:Soil_profile
dcterms:subject dbc:Pedology dbc:Sedimentology
gold:hypernym dbr:Modification
rdf:type dbo:VideoGame
rdfs:comment Cutans are the modification of the soil texture, or soil structure, at natural surfaces (particle, pore, or ped) in soil materials due to illuviation. Cutans are oriented deposits which can be composed of any of the component substances of the soil material. Cutans are common features in soil and represent focuses of chemical and biological reactions. Cutans may include clay skins or coatings of silica, sesquioxide, manganese, ferromanganese, soil organic matter or carbonate. Clay skins are also called argillans, and soil horizons with sufficient clay illuviation are termed argillic horizons. (en)
rdfs:label Cutans (en)
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