Agrotermos

Preferred term

Regosols

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).

World Reference Base soil types

French

Created

1981-01-21T00:00:00Z

void:inDataset

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

Notation

6492

Régosol
Created

1987-04-07T00:00:00Z

Last modified

2021-05-19T13:07:45

void:inDataset

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

Notation

18856

aol peu évolué régosolique

Portuguese

Created

1998-08-04T00:00:00Z

void:inDataset

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

Notation

6492

Regossolo

Spanish

Created

2024-07-03T16:11:42Z

void:inDataset

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

Notation

6492

Regosol

URI

http://aims.fao.org/aos/agrovoc/c_6492

Download this concept

Created 11/20/11, 8:22 PM, last modified 7/20/24, 7:28 PM