Complexes of Fulvic Acid on Hematite Interfaces: Characterization and Photochemical Properties

Fourier transform infrared spectroscopy (FTIR), combined with ultraviolet-visible spectroscopy (UV-Vis) and transmission electron micrograph (TEM), has been used to observe the interaction between fulvic acid (FA) and hematite. The FTIR data have shown that the interaction mechanism corresponds mainly to the ligand-exchange involving carboxylic functional groups of the FA and hematite surface sites. The general trends included an increase in the content of Fe(III)-humate complexes on hematite surfaces accompanied by a decrease in pH and an increasing in the ionic strength. Both UV-Vis spectroscopy and TEM images have shown that hematite can interplay with FA under acidic conditions. In particular, the TEM images have shown that the presence of FA can significantly alter the characteristics of the hematite surfaces. Photochemical experiments have shown that hematite promotes the phototransformation of lindane (-HCH), whereas the presence of FA adversely affects the phototransformation of the target pollutant. The hematite coated with FA displayed a somewhat better catalyzing capability compared to the hematite only.