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Aeolian transport ; Aquifer ; Arid area ; Basalt ; Chronosequence ; Hydrology ; New Mexico ; Pedogenesis ; Soil properties ; Soil water ; Spatial variation ; United States of America
(supprimer)
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