Type of Document Dissertation Author Weaver, Robert M Author's Email Address email@example.com URN etd-10252001-011455 Title Comparison of the Reactivity of Various Mn-Oxides With CrIIIaq: Microscopic and Spectroscopic Observations of Dissolution, Cr-sorption and Cr and Mn Redox Interactions Degree PhD Department Geological Sciences Advisory Committee
Advisor Name Title Hochella, Michael F. Jr. Committee Chair Cox, David F. Committee Member Gibbs, Gerald V. Committee Member Post, Jeffery E. Committee Member Rimstidt, james Donald Committee Member Keywords
- manganese oxide
Date of Defense 2001-09-19 Availability unrestricted AbstractThe interaction between CrIIIaq and seven different Mn-oxides (6 monomineralic, 1 synthetic) have been observed in pH ~4.4 HNO3 and pH ~4.4 ~10-4M CrIIIaq solutions. For each mineral-solution interaction, the aqueous chemical concentrations (e.g. [Mn]aq, [Cr]aq, [CrVIaq]) were measured with time. Reacted samples were examined by XPS to determine if, and to what extent, the surface chemical states of Cr, Mn and O had changed. Microscopic observations of the reacted surfaces were obtained using AFM and high-resolution, low-voltage FESEM. The solubility of the Mn-oxides in the acidic, non-Cr bearing solutions varied inversely with the average Mn valence, but did not show systematic behavior with respect to the mineral structure type (e.g. tunnel, layer, framework). This trend was interpreted as resulting from the relative ability of an adsorbed proton to polarize surface Mn-O bonds, with the polarizability being in the order Mn2+-O > Mn3+-O > Mn4+-O. For samples reacted with CrIIIaq, the rate and extent of reductive dissolution was always greater than for acidic dissolution during the initial time period. The measured ratios of the [Mn]aq : [CrVI]aq were approximately in agreement with the values expected from the proposed stoichiometric reactions. Cr-uptake was observed to occur in undersaturated solutions as a result of adsorption, absorption and surface catalyzed precipitation. The chromium as detected by XPS was predominately CrIII, however pyrolusite contained both CrIII and CrVI. Previous studies have implicated a chromium surface precipitate to be responsible for the cessation of the CrIIIaq oxidation reaction. Our surface sensitive FESEM and AFM observations tend to suggest that Cr-uptake is by isolated site binding, very small (<30 nm) surface clusters or monolayer scale films. Cr-uptake was followed by slow Cr-release on several of the solids (particularly the layered solids) after a substantial portion of the total aqueous Cr had been converted to CrVIaq.
The oxidizing ability of the different Mn-oxides for CrIIIaq is evaluated with regards to the energy level of the redox couple (i.e. the redox potential) as compared with the Fermi energy level of the Mn-oxide. Although these energies were calculated rather than directly measured, the results indicate that electrons originating from adsorbed CrIII ions may be transferred into the conduction band or more likely, into available surface states. The presence of an initial limited quantity of electron accepting surface states likely explains the observation of a rapid initial CrIII-oxidation followed by much slower oxidation. The Mn-oxides that exhibited the greatest and longest lasting CrIII-oxidizing power were the Mn-oxides containing Mn3+, and in particular those containing Mn3+ and Mn2+. It is believed that the combined presence of a reducible Mn ion (e.g. Mn3+) and a highly soluble Mn2+ ion facilitates a sustained CrIII-oxidation reaction because fresh surface is exposed during the reaction.
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