Publications des scientifiques de l'IRD

Rossignol Jean-Pierre, Quantin Paul. (1997). Secuencia de transformacion de un suelo ferralitico en tepetate silicificado en la region de Xalapa (Veracruz, Mexico). In : Zebrowski Claude (ed.), Quantin Paul (ed.), Trujillo G. (ed.), Villamar M.D. (collab.). Suelos volcanicos endurecidos. Quito (ECU) ; Quito (ECU) ; Quito (ECU) ; Quito : UE ; ORSTOM ; PUCE ; UCE, p. 73-82. Suelos Volcanicos Endurecidos, 3., Quito (ECU), 1996/12/9-14.

Titre du document
Secuencia de transformacion de un suelo ferralitico en tepetate silicificado en la region de Xalapa (Veracruz, Mexico)
Année de publication
1997
Type de document
Colloque
Auteurs
Rossignol Jean-Pierre, Quantin Paul
In
Zebrowski Claude (ed.), Quantin Paul (ed.), Trujillo G. (ed.), Villamar M.D. (collab.) Suelos volcanicos endurecidos
Source
Quito (ECU) ; Quito (ECU) ; Quito (ECU) ; Quito : UE ; ORSTOM ; PUCE ; UCE, 1997, p. 73-82
Colloque
Suelos Volcanicos Endurecidos, 3., Quito (ECU), 1996/12/9-14
Indurated soils, called tepetates by the farmers, can be seen in the region of Xalapa, Veracruz, Mexico. They are located in the lower part of a topoclimatic sequence of soils developed on volcanic materials. This sequence, located on the slope of the Cofre de Perote volcano toward the Gulf of Mexico, stars at an altitude of 3,500 m. with a successive appearence of andosols and, lower down ferralitic soils and, at an altitude af 1,200 m., tepetate soils. The representative soils were studied within the framework of the morphopedological map of the region. The ferralitic soils are observed in the altitudinal hand between 1,200 and 1,500 m. where there is a subtropical climate with only a short dry season. The tepetate soils appear in the zone where the dry season is 5 to 6 months long. This work presents the changes from ferralitic soils to tepetate soils. This change is progressively developed under two conditions of soils, acidity and alternative redoximorphy according to a climatic transition from an udic to an ustic moisture regime. The silicification of tepetate soils is a result of these environmental conditions, with alternative wet and dry seasons. (Résumé d'auteur).
Plan de classement
Constituants et propriétés des sols [068PROSOL]
Descripteurs
SOL DEGRADE ; EVOLUTION ; MINERALOGIE ; GEOCHIMIE ; TOPOSEQUENCE ; TEPETATE ; CHANGEMENT CLIMATIQUE
Description Géographique
MEXIQUE ; VERACRUZ
Localisation
Fonds IRD [F A010012910] ; Montpellier (Centre IRD)
Identifiant IRD
fdi:010012914
Contact