Every reference with a DOI in the deposited reference list resolved to a known
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withdrawal, or removal notice.
The 81 checked references that resolve
resolves10.1346/CCMN.1996.0440411Reduction of Structural Fe(III) in Smectite by a Pure Culture of <i>Shewanella Putrefaciens</i> Strain MR-1
resolves10.1021/es801840xAssessing the Redox Reactivity of Structural Iron in Smectites Using Nitroaromatic Compounds As Kinetic Probes
resolves10.1346/CCMN.2000.0480214Reduction and Sorption of Chromium by Fe(II)-Bearing Phyllosilicates: Chemical Treatments and X-Ray Absorption Spectroscopy (XAS) Studies
resolves10.1016/0016-7037(94)90113-9Chromium sorption by phlogopite and biotite in acidic solutions at 25°C: Insights from X-ray photoelectron spectroscopy and electron microscopy
resolves10.1016/S0016-7037(97)00185-3The catalytic effect of sodium and lithium ions on coupled sorption-reduction of chromate at the biotite edge-fluid interface
resolves10.1021/es020935aEffect of Coupled Dissolution and Redox Reactions on Cr(VI)<sub>a</sub><sub>q</sub> Attenuation during Transport in the Sediments under Hyperalkaline Conditions
resolves10.1021/es802658xPathways of Aqueous Cr(VI) Attenuation in a Slightly Alkaline Oxic Subsurface
resolves10.1016/j.gca.2006.10.025Reduction of pertechnetate [Tc(VII)] by aqueous Fe(II) and the nature of solid phase redox products
resolves10.1016/j.gca.2012.05.041Pertechnetate (TcO4−) reduction by reactive ferrous iron forms in naturally anoxic, redox transition zone sediments from the Hanford Site, USA
resolves10.1021/es950627vReduction of Pertechnetate in Solution by Heterogeneous Electron Transfer from Fe(II)-Containing Geological Material
resolves10.1021/es960672iKinetics and pH Dependence of Chromium(VI) Reduction by Iron(II)
resolves10.2475/ajs.289.2.180Kinetics of chromate reduction by ferrous ions derived from hematite and biotite at 25 degrees C
resolves10.1016/j.gca.2014.02.040Reduction and immobilization of hexavalent chromium by microbially reduced Fe-bearing clay minerals
resolves10.1346/CCMN.2000.0480606Chromate Removal by Dithionite-Reduced Clays: Evidence from Direct X-Ray Adsorption Near Edge Spectroscopy (XANES) of Chromate Reduction at Clay Surfaces
resolves10.1346/CCMN.1996.0440603Morphology of Lead(II) and Chromium(III) Reaction Products on Phyllosilicate Surfaces As Determined By Atomic Force Microscopy
resolves10.1021/es0515147Reduction of Nitroaromatic Compounds by Fe(II) Species Associated with Iron-Rich Smectites
resolves10.2138/am-1998-11-1232Bacterial reduction of crystalline Fe (super 3+) oxides in single phase suspensions and subsurface materials
resolves10.1021/es981297sInfluence of Mineral Surfaces on Chromium(VI) Reduction by Iron(II)
resolves10.1021/es0345569Reactivity of Fe(II)-Bearing Minerals toward Reductive Transformation of Organic Contaminants
resolves10.1016/S0009-2541(98)00072-2N-compound reduction and actinide immobilisation in surficial fluids by Fe(II): the surface FeIIIOFeIIOH° species, as major reductant
resolves10.1021/es304744vSpectroscopic Evidence for Fe(II)–Fe(III) Electron Transfer at Clay Mineral Edge and Basal Sites
resolves10.1021/es501887qFe(II) Uptake on Natural Montmorillonites. I. Macroscopic and Spectroscopic Characterization
resolves10.1021/es102560mSpectroscopic Evidence for Interfacial Fe(II)−Fe(III) Electron Transfer in a Clay Mineral
resolves10.1021/jp3110776Electron Exchange and Conduction in Nontronite from First-Principles
resolves10.1021/jp4073125Insights into the Mechanism of Fe(II) Adsorption and Oxidation at Fe–Clay Mineral Surfaces from First-Principles Calculations
resolves10.1021/es403824xRedox Properties of Structural Fe in Clay Minerals: 3. Relationships between Smectite Redox and Structural Properties
resolves10.1128/AEM.07404-11Distribution of Microbial Biomass and Potential for Anaerobic Respiration in Hanford Site 300 Area Subsurface Sediment
resolves10.1346/CCMN.1998.0460106Improvements to the Quantitative Assay of Nonrefractory Minerals for Fe(II) and Total Fe Using 1,10-Phenanthroline
resolves10.1063/1.2008027Design and performance of an eight-pole resistive magnet for soft x-ray magnetic dichroism measurements
resolves10.2136/vzj2006.0180Geochemical Processes Controlling Migration of Tank Wastes in Hanford's Vadose Zone
resolves10.1180/mono-5Crystal Structures of Clay Minerals and their X-Ray Identification
resolves10.1180/claymin.2008.043.1.02Mössbauer spectroscopy of phyllosilicates: effects of fitting models on recoil-free fractions and redox ratios
resolves10.1021/es050717sPyrite Oxidation by Hexavalent Chromium: Investigation of the Chemical Processes by Monitoring of Aqueous Metal Species
resolves10.1021/es034720sEvidence for the Interaction of Technetium Colloids with Humic Substances by X-ray Absorption Spectroscopy
resolves10.1021/es5031849Redox Interactions Between Cr(VI) and Fe(II) in Bioreduced Biotite and Chlorite
resolves10.1021/acs.est.5b03463Redox Interactions of Tc(VII), U(VI), and Np(V) with Microbially Reduced Biotite and Chlorite
resolves10.1016/j.gca.2006.10.019Reversible surface-sorption-induced electron-transfer oxidation of Fe(II) at reactive sites on a synthetic clay mineral
resolves10.1016/j.apgeochem.2012.04.013Geochemical, mineralogical and microbiological characteristics of sediment from a naturally reduced zone in a uranium-contaminated aquifer
resolves10.1016/j.apgeochem.2013.12.001Geochemical and mineralogical investigation of uranium in multi-element contaminated, organic-rich subsurface sediment
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