Concept information
There is no term for this concept in this language.
PREFERRED TERM
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DEFINITION
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Stagnosols are soils with perched water. They show periodically reducing conditions resulting in stagnic properties. Stagnosols have a mottled layer (with oxides predominantly inside the aggregates) with or without an overlying layer with albic material. Redox processes may also be caused by intruding liquids other than water (e.g. gasoline). A common name in many national soil classification systems for most Stagnosols is Pseudogley. In the United States of America many Stagnosols belong to Aquic Suborders and Epiaquic Great Groups of various Orders (Aqualfs, Aquults, Aquents, Aquepts and Aquolls).
(en)Created: 1/20/20
BROADER CONCEPT
IN OTHER LANGUAGES
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Arabic
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Belarusian
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псеўдаглей
Created: 2024-01-19T13:10:13
skos:notation: 128a5d59
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Chinese
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English
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French
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Georgian
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German
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Pseudogley
Created: 2020-01-20T13:44:57.812+01:00
skos:notation: 353e8f07
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Italian
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Russian
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Spanish
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Swahili
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stagnosoller
Created: 2020-02-04T14:47:20.829+01:00
Last modified: 2023-10-27T15:09:23
skos:notation: d9028da2
Turkish
URI
http://aims.fao.org/aos/agrovoc/c_d9028da2
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