The occurrence of concretionary soils in the Central and Northern Brazil is very common. They are found in low areas and on plateau edges, usually constituting dystrophic soils,poor in nutrients. The finding of an eutrophicc concretionary soil in the edge of a plateau in Ouro Verde de Goiás stimulated this research, which had the purpose of verifying the relationship between the soil eutrophic conditions and the underlying lithologic material, the probable source of the exchangeable bases. The pedologic and geochemical […]