Complexation of silver and dissolved organic matter in soil water extracts

An important aspect of the behaviour and fate of silver (Ag) in soils is the interaction with dissolved organic matter (DOM). The complexation and strength of binding of Ag+ with DOM in soil water extracts was examined and modelled based on a range of chemical and quality DOM measurements. Silver ion binding measured by addition of the 110mAg radioisotope in addition to a cation exchange resin technique were used to determine strongly complexed Ag in solutions. Silver was found to be up to 70% strongly complexed. The variability in Ag+ binding by DOM across different soils was closely related (R2 = 0.8) to the mid-infrared spectra of these extracts. The affinity of Ag+ for DOM was stronger in solutions containing a greater content of humic and aromatic structures. The ability of Ag+ to complex with DOM could result in increased mobilisation of this metal in the soil environment.