Spatial variability of iron oxides in soils from the Western Paulista Plateau (Brazil)

Abstract

Iron oxides as goethite (Gt) and hematite (Hm) are key minerals to better understand the soil-landscape relationships. Soil samples were collected at three stages of landscape dissection from the geological formations of Vale do Rio do Peixe (sandstone) and Serra Geral (basalt) in the Western Paulista Plateau (WPP), Brazil. Both iron oxides were quantified by XRD and DRS, and the results were subjected to geostatistical analysis in order to assess the usefulness of DRS for characterizing the spatial variability in Gt and Hm. The prevalence and spatial variability of Hm and Gt in the soils were governed by the sandstone/basalt lithological contrast and landscape dissection. Iron oxides in the clay fraction exhibited high spatial variability over a large area and can be robust indicators of geological diversity and landscape dissection in pedoenvironments with low or high contents of iron oxides. Goethite had the highest spatial variability. Based on the spatial pattern of the differences between DRS and XRD estimates, the saturated red color in soil made DRS less useful for quantifying Hm in environments with high iron oxide contents. The accuracy of maps based on XRD and DRS data was influenced by the spatial variability in Hm and Gt in lithologically contrasting settings, being DRS more sensitive to Gt within landscape dissections. The DRS technique can be useful to characterize the spatial variability in these soil attributes over large, even geomorphologically, complex areas.