Every reference with a DOI in the deposited reference list resolved to a known
work in Crossref or DataCite at the dated check, and none carried a retraction,
withdrawal, or removal notice.
The 39 checked references that resolve
resolves10.1021/es902119uOptimizing Cr(VI) and Tc(VII) Remediation through Nanoscale Biomineral Engineering
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/j.gca.2014.02.040Reduction and immobilization of hexavalent chromium by microbially reduced Fe-bearing clay minerals
resolves10.1016/j.clay.2008.03.002Some effects of microbial activity on the evolution of clay-based buffer properties in underground repositories
resolves10.1016/S0016-7037(99)00372-5Using X-ray photoelectron spectroscopy to discriminate among different sorption sites of micas: with implications for heterogeneous reduction of chromate at the mica-water interface
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
resolves10.2475/ajs.289.2.180Kinetics of chromate reduction by ferrous ions derived from hematite and biotite at 25 degrees C
resolves10.1002/hyp.6408Evaluating the transport and removal of chromate using pyrite and biotite columns
resolves10.1021/es00050a025Batch experiments characterizing the reduction of chromium(VI) using suboxic material from a mildly reducing sand and gravel aquifer
resolves10.1021/es803526gAssessment of Long-Term Performance and Chromate Reduction Mechanisms in a Field Scale Permeable Reactive Barrier
resolves10.1080/00206810009465107Chromium Transformations in Natural Environments: The Role of Biological and Abiological Processes in Chromium(VI) Reduction
resolves10.1016/S0016-7037(02)01081-5Structural and compositional evolution of Cr/Fe solids after indirect chromate reduction by dissimilatory iron-reducing bacteria
resolves10.1021/es981297sInfluence of Mineral Surfaces on Chromium(VI) Reduction by Iron(II)
resolves10.1021/es801840xAssessing the Redox Reactivity of Structural Iron in Smectites Using Nitroaromatic Compounds As Kinetic Probes
resolves10.1128/aem.54.6.1472-1480.1988Novel Mode of Microbial Energy Metabolism: Organic Carbon Oxidation Coupled to Dissimilatory Reduction of Iron or Manganese
resolves10.1128/AEM.68.12.6256-6262.2002Growth of Iron(III)-Reducing Bacteria on Clay Minerals as the Sole Electron Acceptor and Comparison of Growth Yields on a Variety of Oxidized Iron Forms
resolves10.1346/CCMN.2008.0560204Partitioning of Fe(II) in reduced nontronite (NAu-2) to reactive sites: Reactivity in terms of Tc(VII) reduction
resolves10.1021/es2037146Engineering Biogenic Magnetite for Sustained Cr(VI) Remediation in Flow-through Systems
resolves10.1103/PhysRevB.43.13401Strong magnetic x-ray dichroism in 2<i>p</i>absorption spectra of 3<i>d</i>transition-metal ions
resolves10.1088/0953-8984/4/16/019The 2p absorption spectra of 3d transition metal compounds in tetrahedral and octahedral symmetry
resolves10.1021/es102560mSpectroscopic Evidence for Interfacial Fe(II)−Fe(III) Electron Transfer in a Clay Mineral
resolves10.1063/1.1612912Charge transport in micas: The kinetics of FeII/III electron transfer in the octahedral sheet
resolves10.1021/es304744vSpectroscopic Evidence for Fe(II)–Fe(III) Electron Transfer at Clay Mineral Edge and Basal Sites
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