Agrotermos

Preferred term

Stagnosols

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).

World Reference Base soil types

English

Created

2020-01-23T14:25:48.642+01:00

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

Notation

d9028da2

Stagnosols

French

Created

2020-01-23T14:25:48.642+01:00

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

Notation

d9028da2

Stagnosols

Spanish

Created

2024-07-03T16:11:42Z

void:inDataset

http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc

Notation

d9028da2

Stagnosol

URI

http://aims.fao.org/aos/agrovoc/c_d9028da2

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Created 1/20/20, 12:43 PM, last modified 7/3/24, 4:11 PM