Every reference with a DOI in the deposited reference list resolved to a known
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withdrawal, or removal notice.
The 60 checked references that resolve
resolves10.1021/cr970105tOccurrence and Constitution of Natural and Synthetic Ferrihydrite, a Widespread Iron Oxyhydroxide
resolves10.1021/es503669uProperties of Fe-Organic Matter Associations via Coprecipitation versus Adsorption
resolves10.1021/es9026248Biogeochemical Redox Processes and their Impact on Contaminant Dynamics
resolves10.2138/am-2003-11-1233Transformation of 2-line ferrihydrite to 6-line ferrihydrite under oxic and anoxic conditions
resolves10.1016/S0927-7757(03)00134-1Effects of Zn(II), Cu(II), Mn(II), Fe(II), NO3−, or SO42− at pH 6.5 and 8.5 on transformations of hydrous ferric oxide (HFO) as evidenced by Mössbauer spectroscopy
resolves10.1021/es050666zCompeting Fe(II)-Induced Mineralization Pathways of Ferrihydrite
resolves10.2138/am.2006.1860The rate of ferrihydrite transformation to goethite via the Fe(II) pathway
resolves10.1016/j.gca.2011.05.033Effect of adsorbed and substituted Al on Fe(II)-induced mineralization pathways of ferrihydrite
resolves10.1016/j.jssc.2008.06.052The transformation of ferrihydrite in the presence of trace Fe(II): The effect of the anionic media
resolves10.1021/es4043275Effect of Solution and Solid-Phase Conditions on the Fe(II)-Accelerated Transformation of Ferrihydrite to Lepidocrocite and Goethite
resolves10.1080/01490450252864271Biomineralization of Poorly Crystalline Fe(III) Oxides by Dissimilatory Metal Reducing Bacteria (DMRB)
resolves10.1016/S0016-7037(03)00276-XSecondary mineralization pathways induced by dissimilatory iron reduction of ferrihydrite under advective flow
resolves10.2136/vzj2008.0090Aggregate‐Scale Heterogeneity in Iron (Hydr)oxide Reductive Transformations
resolves10.1021/es901736tSpatial Patterns and Modeling of Reductive Ferrihydrite Transformation Observed in Artificial Soil Aggregates
resolves10.1016/j.gca.2010.01.032Aggregate-scale spatial heterogeneity in reductive transformation of ferrihydrite resulting from coupled biogeochemical and physical processes
resolves10.1038/38260Mineral control of soil organic carbon storage and turnover
resolves10.1021/es1023898Fractionation of Organic Matter Due to Reaction with Ferrihydrite: Coprecipitation versus Adsorption
resolves10.1016/j.gca.2014.08.026Properties and reactivity of Fe-organic matter associations formed by coprecipitation versus adsorption: Clues from arsenate batch adsorption
resolves10.1021/es800881wCharacterization of Ferrihydrite-Soil Organic Matter Coprecipitates by X-ray Diffraction and Mössbauer Spectroscopy
resolves10.5194/bgd-11-6039-2014Reduction of ferrihydrite with adsorbed and coprecipitated organic matter: microbial reduction by
<i>Geobacter bremensis</i>
vs. abiotic reduction by Na-dithionite
resolves10.1021/es402812jDissimilatory Reduction and Transformation of Ferrihydrite-Humic Acid Coprecipitates
resolves10.1016/j.gca.2011.06.002X-ray absorption spectroscopy study on the effect of hydroxybenzoic acids on the formation and structure of ferrihydrite
resolves10.1038/212645b0Inhibitory Effect of Soil Organic Matter on the Crystallization of Amorphous Ferric Hydroxide
resolves10.1016/0016-7061(70)90020-0Der einfluss einfacher organischer anionen auf die bildung von goethit und hämatit aus amorphen Fe(III) - hydroxid
resolves10.1016/j.chemgeo.2011.02.009Composition and structure of nanocrystalline Fe and Mn oxide cave deposits: Implications for trace element mobility in karst systems
resolves10.1016/j.gca.2011.10.015Schwertmannite and Fe oxides formed by biological low-pH Fe(II) oxidation versus abiotic neutralization: Impact on trace metal sequestration
resolves10.1021/es0505346Coupled Fe(II)−Fe(III) Electron and Atom Exchange as a Mechanism for Fe Isotope Fractionation during Dissimilatory Iron Oxide Reduction
resolves10.1016/j.gca.2009.04.025The effect of silica and natural organic matter on the Fe(II)-catalysed transformation and reactivity of Fe(III) minerals
resolves10.1016/0168-583X(91)95681-3Voigt-based methods for arbitrary-shape static hyperfine parameter distributions in Mössbauer spectroscopy
resolves10.1007/s10533-013-9871-zNitrogen input quality changes the biochemical composition of soil organic matter stabilized in the fine fraction: a long-term study
resolves10.1021/es5059617Organic Matter Remineralization Predominates Phosphorus Cycling in the Mid-Bay Sediments in the Chesapeake Bay
resolves10.1021/la00037a057Transformation of ferric hydroxide into spinel by iron(II) adsorption
resolves10.1038/ngeo870Extracellular electron transfer through microbial reduction of solid-phase humic substances
resolves10.1016/j.gca.2011.03.006Stabilization of extracellular polymeric substances (Bacillus subtilis) by adsorption to and coprecipitation with Al forms
resolves10.1080/00380768.2004.10408528Nutrient leaching from the plow layer by water percolation and accumulation in the subsoil in an irrigated paddy field
resolves10.1016/j.gca.2004.03.012A revised scheme for the reactivity of iron (oxyhydr)oxide minerals towards dissolved sulfide
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