Solid−Solution Speciation and Phytoavailability of Copper and Zinc in Soils

Publisher Website
Google Scholar
Abstract
The soil solution speciation and solid-phase fractionation of copper (Cu) and zinc (Zn) in 11 typical uncontaminated soils of South Australia were assessed in relation to heavy metal phytoavailability. The soils were analyzed for pH (4.9−8.4), soil organic matter content (3.5 to 23.8 g of C kg-1), total soil solution metal concentrations, Cus (49−358 μg kg-1) and Zns (121−582 μg kg-1), and dissolved organic matter (DOM) (69−827 mg of C L-1). The solid−liquid partition coefficient (Kd) ranged from between 13.9 and 152.4 L kg-1 for Cu and 22.6 to 266.3 L kg-1 for Zn. The phytoavailability of Cu and Zn could be predicted significantly using an empirical model with the solid-phase fractions of Cu and Zn, as obtained from selective sequential extraction scheme, as components. Phytoavailable Cu and Zn were found to significantly correlate with fulvic complex Cu (r = 0.944, P < 0.0001) and exchangeable Zn (r = 0.832, P = 0.002), respectively. The fulvic complex Cu was found to explain 89.2% of the variation in phytoavailable Cu, where as, the exchangeable Zn together with fulvic complex Zn could explain 78.9% of the variation in phytoavailable Zn. The data presented demonstrate the role of solid-phase metal fractions in understanding the heavy metal phytoavailability. The assessment of the role of solid-phase fractions in heavy metal phytoavailability is a neglected area of study and deserves close attention.