Influence of Size on Reductive Dissolution of Six-Line Ferrihydrite

This work investigates size dependence of the kinetics of reductive dissolution of six-line ferrihydrite, ranging in average length from 3.4 to 5.9 nm. Empirical rate laws, activation energies, and pre-exponential factors were determined for freshly prepared aqueous suspensions and dried powders of each ferrihydrite sample. Mass-normalized initial rates of reductive dissolution are substantially faster for the freshly prepared suspensions than for reactions using the dried powders, which is consistent with a drop in reactive surface area upon drying. In addition, results demonstrate substantial differences between the empirical rate laws for the freshly prepared and the dried six-line ferrihydrite. Comparing surface-area-normalized rates of reductive dissolution reveals a small dependence on size for the freshly prepared ferrihydrite, no dependence on size for the dried ferrihydrite nanoparticles, and no statistically significant change in the activation energy for reaction in either case. In addition, X-...

[1]  M. Schoonen,et al.  The Structure of Ferrihydrite, a Nanocrystalline Material , 2007, Science.

[2]  S. Lo,et al.  Size effect in reactivity of copper nanoparticles to carbon tetrachloride degradation. , 2007, Water research.

[3]  Sandeep Kumar,et al.  Aggregative growth of silicalite-1. , 2007, The journal of physical chemistry. B.

[4]  Benjamin Gilbert,et al.  Stable cluster formation in aqueous suspensions of iron oxyhydroxide nanoparticles. , 2006, Journal of colloid and interface science.

[5]  Michael F. Hochella,et al.  Insights for size-dependent reactivity of hematite nanomineral surfaces through Cu2+ sorption , 2006 .

[6]  R. Jakobsen,et al.  Release of arsenic associated with the reduction and transformation of iron oxides , 2006 .

[7]  R. L. Penn,et al.  Controlled growth of alpha-FeOOH nanorods by exploiting-oriented aggregation , 2006 .

[8]  R. L. Penn,et al.  Influence of aluminum doping on ferrihydrite nanoparticle reactivity. , 2006, The journal of physical chemistry. B.

[9]  W. Arnold,et al.  Kinetic and microscopic studies of reductive transformations of organic contaminants on goethite. , 2006, Environmental science & technology.

[10]  R. L. Penn,et al.  Reduction of crystalline iron(III) oxyhydroxides using hydroquinone: Influence of phase and particle size , 2005, Geochemical transactions.

[11]  J. Banfield,et al.  Nanoparticulate Iron Oxide Minerals in Soils and Sediments: Unique Properties and Contaminant Scavenging Mechanisms , 2005 .

[12]  D. Sherman Electronic structures of iron(III) and manganese(IV) (hydr)oxide minerals : Thermodynamics of photochemical reductive dissolution in aquatic environments , 2005 .

[13]  J. Banfield,et al.  Size dependence of the kinetic rate constant for phase transformation in TiO2 nanoparticles , 2005 .

[14]  S. C. Parker,et al.  Molecular dynamics simulations of the interactions between water and inorganic solids , 2005 .

[15]  A. S. Madden,et al.  A test of geochemical reactivity as a function of mineral size: Manganese oxidation promoted by hematite nanoparticles , 2005 .

[16]  M. Engelhard,et al.  Reaction of hydroquinone with hematite; I. Study of adsorption by electrochemical-scanning tunneling microscopy and X-ray photoelectron spectroscopy. , 2004, Journal of colloid and interface science.

[17]  P. Cummings,et al.  Ion adsorption at the rutile-water interface: linking molecular and macroscopic properties. , 2004, Langmuir : the ACS journal of surfaces and colloids.

[18]  P. Schurtenberger,et al.  Characterization of the pores in hydrous ferric oxide aggregates formed by freezing and thawing. , 2004, Journal of colloid and interface science.

[19]  J. Leckie,et al.  Variability in goethite surface site density: evidence from proton and carbonate sorption. , 2003, Journal of colloid and interface science.

[20]  S. Stipp,et al.  Behaviour of Fe-oxides relevant to contaminant uptake in the environment , 2002 .

[21]  M. Hochella Nanoscience and technology: the next revolution in the Earth sciences , 2002 .

[22]  K. Straub,et al.  Iron metabolism in anoxic environments at near neutral pH. , 2001, FEMS microbiology ecology.

[23]  P. Persson,et al.  Benzenecarboxylate Surface Complexation at the Goethite (α-FeOOH)/Water Interface: III. The Influence of Particle Surface Area and the Significance of Modeling Parameters , 2000 .

[24]  D. Lovley,et al.  Quinone Moieties Act as Electron Acceptors in the Reduction of Humic Substances by Humics-Reducing Microorganisms , 1998 .

[25]  K. Farley,et al.  Changes in Transition and Heavy Metal Partitioning during Hydrous Iron Oxide Aging , 1997 .

[26]  Timothy L. Johnson,et al.  Kinetics of Halogenated Organic Compound Degradation by Iron Metal , 1996 .

[27]  A. Stone,et al.  Reductive dissolution of goethite by phenolic reductants , 1989 .

[28]  M. McBride,et al.  Electron Transfer Processes Between Hydroquinone and Iron Oxides , 1988 .