Spatial variability of iron oxides in soils from Brazilian sandstone and basalt

Autor(es)

Silva, Laercio Santos ^[1] ; Marques Junior, Jose ^[1] ; Barron, Vidal ^[2] ; Gomes, Romario Pimenta ^[1] ; Teixeira, Daniel De Bortoli ^[3] ; Siqueira, Diego Silva ^[1] ; Vasconcelos, Vinicius ^[4]

Afiliação do(s) autor(es)

^[1] Sao Paulo State Univ, Fac Agr & Vet Sci, Res Grp CSME Soil Characterizat Specif Management, Dept Soils & Fertilizers, FCAV, UNESP, Jaboticabal, SP - Brazil

^[2] Cordoba Univ, Dept Agron, Cordoba - Spain

^[3] Univ Marilia, Unimar, Ctr Agr Sci, Sao Paulo, SP - Brazil

^[4] Univ Brasilia, UnB, Dept Geog, Brasilia, DF - Brazil

• Tipo de documento: Artigo Científico
• Fonte: CATENA; v. 185, FEB 2020.
• Citações Web of Science: 0

Resumo

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 X-ray diffraction (XRD) and diffuse reflectance spectroscopy (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 maps indicate the sensitivity of XRD and DRS techniques to represent Hm and Gt spatial variability patterns. Gt was more sensitive to landscape dissection while Hm sensitive to lithology. Thus, the DRS technique is efficient in characterizing the spatial variability of these soil oxides in large areas, even considering the complex relations between soil and landscape. (AU)

• Processo FAPESP: 18/15694-1 - Variabilidade espacial dos óxidos de ferro e emissão de gases de nitrogênio (NOx) em solos do Planalto Ocidental Paulista
• Beneficiário: Laércio Santos Silva
• Modalidade de apoio: Bolsas no Exterior - Estágio de Pesquisa - Doutorado
• Processo FAPESP: 17/01704-2 - Variabilidade espacial dos óxidos de ferro e fósforo adsorvido nos solos do Planalto Ocidental Paulista
• Beneficiário: Laércio Santos Silva
• Modalidade de apoio: Bolsas no Brasil - Doutorado