Soils of Azores islands: elemental characterization with an emphasis on rare-earth elements

This work addresses the chemical features of topsoils from Pico, São Jorge and São Miguel islands (Azores, Portugal), resulting from the weathering of more or less recent volcanic materials, namely pyroclastic debris, scoriae and basaltic rocks. The fractions under 64 μm of the surface-soil samples (0–10 cm) were put through k ₀-standardized, instrumental neutron activation analysis (k ₀-INAA), and their contents in 29 chemical elements were determined. Overall, the results show the chemical composition in the top horizon of soils to be correlated with the type of initial material, as well as with the age of formation of the island. The more relevant differences between the surveyed islands are: (1) a positive Ce anomaly in soils from São Miguel, most probably due to the higher age of that island; and (2) a fractionation between heavy and light rare-earth elements (REEs) in São Miguel, not found in the younger Pico and São Jorge. Other than the islands’ age, terrain altitude seems another relevant factor in differentiating the topsoils’ composition.