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- Stagnosol abstract "A stagnosol in the FAO World Reference Base for Soil Resources is soil with strong mottling of the soil profile due to redox processes caused by stagnating surface water. Stagnosols are periodically wet and mottled in the topsoil and subsoil, with or without concretions and/or bleaching. The topsoil can also be completely bleached (albic horizon). A common name in many national classification systems for most Stagnosols is pseudogley. In the USDA soil taxonomy, many of them belong to the Aqualfs, Aquults, Aquents, Aquepts and Aquolls.They are developed in a wide variety of unconsolidated materials like glacial till, and loamy aeolian, alluvial and colluvial deposits and physically weathered siltstone. Stagnosols occur on flat to gently sloping land in cool temperate to subtropical regions with humid to perhumid climate conditions.The agricultural suitability of Stagnosols is limited because of their oxygen deficiency resulting from stagnating water above a dense subsoil. Therefore, they have to be drained. However, in contrast to Gleysols, drainage with channels or pipes is in many cases insufficient. It is necessary to have a higher porosity in the subsoil in order to improve the hydraulic conductivity. This may be achieved by deep loosening or deep ploughing. Drained Stagnosols can be fertile soils owing to their moderate degree of leaching.Stagnosols cover 150–200 million ha worldwide. For the greater part in humid to perhumid temperate regions of West and Central Europe, North America, southeast Australia and Argentina. Here Stagnosols are associated with Luvisols as well as silty to clayey Cambisols and Umbrisols. They also occur in humid to perhumid subtropical regions, where they are associated with Acrisols and Planosols.with a light-coloured, coarse-textured, surface horizon that shows signs of periodic water stagnation and abruptly overlies a dense, slowly permeable subsoil with significantly more clay than the surface horizon. In the US Soil Classification of 1938 used the name Planosols, whereas its successor, the USDA soil taxonomy, includes most Planosols in the Great Groups Albaqualfs, Albaquults and Argialbolls.".
- Stagnosol thumbnail Pseudogley.jpg?width=300.
- Stagnosol wikiPageID "21192706".
- Stagnosol wikiPageLength "4572".
- Stagnosol wikiPageOutDegree "50".
- Stagnosol wikiPageRevisionID "634529126".
- Stagnosol wikiPageWikiLink Acrisol.
- Stagnosol wikiPageWikiLink Acrisols.
- Stagnosol wikiPageWikiLink Aeolian_processes.
- Stagnosol wikiPageWikiLink Agriculture.
- Stagnosol wikiPageWikiLink Alluvial.
- Stagnosol wikiPageWikiLink Alluvium.
- Stagnosol wikiPageWikiLink Argentina.
- Stagnosol wikiPageWikiLink Australia.
- Stagnosol wikiPageWikiLink Cambisol.
- Stagnosol wikiPageWikiLink Cambisols.
- Stagnosol wikiPageWikiLink Canadian_system_of_soil_classification.
- Stagnosol wikiPageWikiLink Category:Pedology.
- Stagnosol wikiPageWikiLink Category:Types_of_soil.
- Stagnosol wikiPageWikiLink Central_Europe.
- Stagnosol wikiPageWikiLink Clay.
- Stagnosol wikiPageWikiLink Colluvium.
- Stagnosol wikiPageWikiLink Concretion.
- Stagnosol wikiPageWikiLink FAO.
- Stagnosol wikiPageWikiLink Fertile_soil.
- Stagnosol wikiPageWikiLink Food_and_Agriculture_Organization_of_the_United_Nations.
- Stagnosol wikiPageWikiLink Glacial_till.
- Stagnosol wikiPageWikiLink Gley_soil.
- Stagnosol wikiPageWikiLink Gleysol.
- Stagnosol wikiPageWikiLink Gleysols.
- Stagnosol wikiPageWikiLink Humid_subtropical_climate.
- Stagnosol wikiPageWikiLink Hydraulic_conductivity.
- Stagnosol wikiPageWikiLink Loam.
- Stagnosol wikiPageWikiLink Luvisols.
- Stagnosol wikiPageWikiLink North_America.
- Stagnosol wikiPageWikiLink Oxygen.
- Stagnosol wikiPageWikiLink Pedogenesis.
- Stagnosol wikiPageWikiLink Pedology_(soil_study).
- Stagnosol wikiPageWikiLink Permeability_(earth_sciences).
- Stagnosol wikiPageWikiLink Planosol.
- Stagnosol wikiPageWikiLink Planosols.
- Stagnosol wikiPageWikiLink Porosity.
- Stagnosol wikiPageWikiLink Redox.
- Stagnosol wikiPageWikiLink Sediment.
- Stagnosol wikiPageWikiLink Silt.
- Stagnosol wikiPageWikiLink Soil.
- Stagnosol wikiPageWikiLink Soil_classification.
- Stagnosol wikiPageWikiLink Soil_fertility.
- Stagnosol wikiPageWikiLink Soil_horizon.
- Stagnosol wikiPageWikiLink Soil_profile.
- Stagnosol wikiPageWikiLink Soil_texture.
- Stagnosol wikiPageWikiLink Stagnogley.
- Stagnosol wikiPageWikiLink Subtropics.
- Stagnosol wikiPageWikiLink Temperate_climate.
- Stagnosol wikiPageWikiLink Till.
- Stagnosol wikiPageWikiLink USDA_soil_taxonomy.
- Stagnosol wikiPageWikiLink Umbrisol.
- Stagnosol wikiPageWikiLink Umbrisols.
- Stagnosol wikiPageWikiLink Water.
- Stagnosol wikiPageWikiLink Weathering.
- Stagnosol wikiPageWikiLink Western_Europe.
- Stagnosol wikiPageWikiLink World_Reference_Base_for_Soil_Resources.
- Stagnosol wikiPageWikiLink File:Pseudogley.jpg.
- Stagnosol wikiPageWikiLinkText "Stagnosol".
- Stagnosol wikiPageWikiLinkText "stagnosol".
- Stagnosol hasPhotoCollection Stagnosol.
- Stagnosol wikiPageUsesTemplate Template:Cite_journal.
- Stagnosol wikiPageUsesTemplate Template:Reflist.
- Stagnosol wikiPageUsesTemplate Template:Soil_type.
- Stagnosol subject Category:Pedology.
- Stagnosol subject Category:Types_of_soil.
- Stagnosol hypernym Soil.
- Stagnosol type Species.
- Stagnosol comment "A stagnosol in the FAO World Reference Base for Soil Resources is soil with strong mottling of the soil profile due to redox processes caused by stagnating surface water. Stagnosols are periodically wet and mottled in the topsoil and subsoil, with or without concretions and/or bleaching. The topsoil can also be completely bleached (albic horizon). A common name in many national classification systems for most Stagnosols is pseudogley.".
- Stagnosol label "Stagnosol".
- Stagnosol sameAs Pseudoglej.
- Stagnosol sameAs Pseudogley.
- Stagnosol sameAs Pseŭdoglejo.
- Stagnosol sameAs Stagnosol.
- Stagnosol sameAs m.05c1xyz.
- Stagnosol sameAs Q1418118.
- Stagnosol sameAs Q1418118.
- Stagnosol wasDerivedFrom Stagnosol?oldid=634529126.
- Stagnosol depiction Pseudogley.jpg.
- Stagnosol isPrimaryTopicOf Stagnosol.