Surface reactivity of iron, manganese minerals and their environmental implications

The focus of the thesis research was to investigate the surface reactivity of three different minerals, pyrite (FeS2), an ordered form of ferrihydrite (an iron oxyhydroxide phase), and birnessite (MnO2), toward environmentally relevant aqueous reactants. In particular, research was carried out with the goals of 1) understanding the redox chemistry of nitrite (NO2-) and nitrate (NO3-) on pyrite and 2) understanding the redox (photo) chemistry of arsenite (AsO2-, As(III)) on ordered ferrihydrite and birnessite. A motivation for all these studies stemmed in part from the recognition that NO2-, NO3-, and As(III) are all environmental pollutants when they are present at sufficiently high concentration in the environment. The removal of these species or conversion of each of them on mineral surfaces to more benign chemical species is of importance in the realm of environmental chemistry. In the case of NO2- and NO3- on pyrite, an additional and primary motivation for the research was that it has been hypothesized in the "origin-of-life" community that the reaction of NO2- and NO3- with iron sulfide (e.g., pyrite) may have played a role in the production of ammonia (NH3) on early Earth. Such prebiotic chemistry had been hypothesized to an essential step in the production of biomolecules that included proteins. With regard to the NO2- reaction with pyrite, results detailed in this thesis showed that ammonia in µmol/kg quantities could be produced by reacting NO2- in the presence of pyrite under anaerobic conditions. The concentration of NH3 (detected as ammonium, NH4+, in solution) was a strong function of the reaction temperature. At the lower temperatures studied (22oC and 70oC), a small amount of NH4+ was formed, but µmol.kg-1 amounts of NH4+ were formed at a reaction temperature of 120oC. Only about 5% of the initial NO2- concentration was converted to NH4+. In the NO3-/pyrite system, the NO3- reactant concentration remained unchanged at all the three reaction temperatures studied, consistent with the low amounts of NH4+ formed in these experiments. Finally, it was shown using in situ infrared spectroscopy that surface-bound NO formed on pyrite during the conversion of the nitrogen oxides to ammonia. Overall, it was shown that the kinetics of NH4+ formation was slower for NO3- than that observed for NO2-. Studies presented in this thesis that focused on the surface reactivity of As(III) on ordered ferrihydrite and birnessite nano particles showed that As(III) could be oxidized to arsenate (referred to as As(V)) in the presence of simulated solar radiation. In the ordered ferrihydrite circumstance the adsorption of As(III) and photo-induced oxidation to As(V) was compared to the same reaction on the more disordered and smaller ferrihydrite particles (known as "2-line" ferrihydrite). A comparison of the adsorption rate of As(III) on the two surfaces in the presence of light after normalizing for differences in surface area showed that the ordered ferrihydrite exhibited a higher arsenic adsorption rate. Also, the oxidation rate of As(III) to As(V) in the presence of light on the ordered ferrihydrite showed a strong dependence on the amount of dissolved oxygen in solution while the oxidation rate on the more disordered form showed no such dependence. It was proposed that differences in the rates of the heterogeneous oxidation rate of ferrous iron with dissolved oxygen on the two surfaces were the reason for this behavior. Finally, the photo-induced oxidation of As(III) to As(V) on Na- and K-birnessite at solution pHs of 5.0 and 7.4 was investigated. It was shown that the oxidation rate of As(III) to As(V) occurred at a faster rate on birnessite in the presence of light when compared to the same system in the dark. Mn(II) formed during the reductive dissolution of birnessite during the oxidation of As(III) was experimentally observed at pH 5.0, but not at pH 7.4. Experiments were also conducted that investigated the reductive dissolution of Na- and K-birnessite (having different sizes and average oxidation states) by As(III) under more alkaline conditions. These experiments were conducted at pH 8.5 and the post-reaction samples were analyzed with X-ray diffraction (XRD) and X-ray photoelectron spectroscopy (XPS). It was shown under these alkaline conditions using X-ray diffraction that structural changes occurred in/on both the Na- and K-birnessite during the As(III) oxidation reaction.