Concept information
PREFERRED TERM
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void:inDataset: http://aims.fao.org/aos/agrovoc/void.ttl#Agrovoc
Created: 2009-02-13T00:00:00Z
skos:notation: 6492
DEFINITION
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Regosols are very weakly developed mineral soils in unconsolidated materials that do not have a mollic or umbric horizon, are not very thin or very rich in coarse fragments (Leptosols), not sandy (Arenosols), and not with fluvic materials (Fluvisols). Regosols are extensive in eroding lands and accumulation zones, particularly in arid and semiarid areas and in mountainous terrain. Many Regosols correlate with soil taxa that are marked by incipient soil formation such as Entisols (United States of America), Rudosols (Australia), Regosole (Germany), Sols peu évolués régosoliques d’érosion or even Sols minéraux bruts d’apport éolien ou volcanique (France), Pelozems (Russia) and Neossolos (Brazil).
(en)Created: 1/20/20
BROADER CONCEPT
IN OTHER LANGUAGES
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Arabic
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Chinese
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Czech
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Regosols
Created: 1981-01-09T00:00:00Z
Last modified: 2020-01-23T13:47:30.44+01:00
skos:notation: 6492
English
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French
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aol peu évolué régosolique
Created: 1987-04-07T00:00:00Z
Last modified: 2021-05-19T13:07:45
skos:notation: 18856
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Georgian
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German
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Hindi
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Hungarian
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Italian
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Japanese
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Korean
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Lao
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Persian
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Polish
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Gleba inicjalna luźna
Created: 2006-12-19T00:00:00Z
skos:notation: 61880
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Portuguese
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Romanian
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Serbian
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Slovak
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Spanish
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Thai
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Turkish
URI
http://aims.fao.org/aos/agrovoc/c_6492
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