Mots-clés
Basalte ; Chronoséquence ; Domaine aride ; Eau du sol ; Etats-Unis ; Hydrologie ; Nappe aquifère ; New Mexico ; Propriétés du sol ; Pédogenèse ; Transport éolien ; Variation spatialeAeolian transport ; Aquifer ; Arid area ; Basalt ; Chronosequence ; Hydrology ; New Mexico ; Pedogenesis ; Soil properties ; Soil water ; Spatial variation ; United States of AmericaSpatial variability of soils developing on basalt flows in the Potrillo volcanic field, southern New Mexico : prelude to a chronosequence study
Auteurs :EPPES, M.C.
HARRISON, J.B.J.
Description :
The spatial variability of swale soils results in part from the significant hydrologic variability of low-lying landscape positions. Depth profiles of chloride concentrations suggest that hydrologic variability systematically correlates with the size and shape of depressions in which soils are forming. The infilling of depressions with aeolian material results in increasingly arid hydrologic conditions. The pre-burial high water flux evident in depressions suggests that basalt flows may play an important role in aquifer recharge in this area of New Mexico.
Type de document :
Article de périodique
Source :
Earth surface processes and landforms, issn : 0197-9337, 1999, vol. 24, n°. 11, p. 1009-1024, Collation : Illustration, Références bibliographiques : 32 ref.
Date :
1999
Editeur :
Pays édition : Royaume-Uni, Chichester, Wiley
Langue :
Anglais
Anglais
Droits :
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)
Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI)