Agrotermos

Término preferido

Lixisol

Lixisols have a higher clay content in the subsoil than in the topsoil, as a result of pedogenetic processes (especially clay migration) leading to an argic subsoil horizon. Lixisols have low-activity clays in the argic horizon and a high base saturation in the 50–100 cm depth. Many Lixisols are included in Red yellow podzolic soils (e.g. Indonesia), Chromosols (Australia), Argissolos (Brazil), Sols ferralitiques faiblement desaturés appauvris (France) and Alfisols with low-activity clays (United States of America).

Tipo de base referencial mundial para recursos de suelos

francés

Creado

2021-05-19T13:14:44

void:inDataset

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

skos:notation

7283bd0a

Lixisol

inglés

Creado

2020-01-20T14:26:41.026+01:00

void:inDataset

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

skos:notation

7283bd0a

Lixisols

portugués

Creado

2020-01-20T14:26:41.026+01:00

void:inDataset

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

skos:notation

7283bd0a

Lixisols

portugués (Brasil)

Creado

2020-01-20T14:26:41.026+01:00

void:inDataset

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

skos:notation

7283bd0a

Lixisols

URI

http://aims.fao.org/aos/agrovoc/c_7283bd0a

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Creado 1/20/20, 13:26, última modificación 6/2/25, 10:31