Materials Map

Discover the materials research landscape. Find experts, partners, networks.

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The Materials Map is an open tool for improving networking and interdisciplinary exchange within materials research. It enables cross-database search for cooperation and network partners and discovering of the research landscape.

The dashboard provides detailed information about the selected scientist, e.g. publications. The dashboard can be filtered and shows the relationship to co-authors in different diagrams. In addition, a link is provided to find contact information.

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The Materials Map is still under development. In its current state, it is only based on one single data source and, thus, incomplete and contains duplicates. We are working on incorporating new open data sources like ORCID to improve the quality and the timeliness of our data. We will update Materials Map as soon as possible and kindly ask for your patience.

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Bargar, John R.

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in Cooperation with on an Cooperation-Score of 37%

Topics

Publications (3/3 displayed)

  • 2023Environmental impact of solution pH on the formation and migration of iron colloids in deep subsurface energy systems.7citations
  • 2022Chemical and Reactive Transport Processes Associated with Hydraulic Fracturing of Unconventional Oil/Gas Shales.58citations
  • 2009Arsenite sequestration at the surface of nano-Fe(OH)2, ferrous-carbonate hydroxide, and green-rust after bioreduction of arsenic-sorbed lepidocrocite by Shewanella putrefaciens82citations

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Chart of shared publication
Kovscek, Anthony R.
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Wielinski, Jonas
1 / 1 shared
Frouté, Laura
1 / 1 shared
Noël, Vincent
1 / 2 shared
Bland, Garret
1 / 1 shared
Lowry, Gregory V.
1 / 3 shared
Kaszuba, John P.
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Brown, Gordon E.
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Ihme, Matthias
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Druhan, Jennifer L.
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Jew, Adam D.
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Ruby, Christian
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Juillot, Farid
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Calas, Georges
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Guyot, François
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Jr., Gordon E. Brown
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Ona-Nguema, Georges
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Abdelmoula, Mustapha
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Wang, Yuheng
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Aquilanti, Giuliana
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Morin, Guillaume
1 / 7 shared
Menguy, N.
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Olivi, Luca
1 / 12 shared
Chart of publication period
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2022
2009

Co-Authors (by relevance)

  • Kovscek, Anthony R.
  • Wielinski, Jonas
  • Frouté, Laura
  • Noël, Vincent
  • Bland, Garret
  • Lowry, Gregory V.
  • Kaszuba, John P.
  • Brown, Gordon E.
  • Ihme, Matthias
  • Druhan, Jennifer L.
  • Jew, Adam D.
  • Ruby, Christian
  • Juillot, Farid
  • Calas, Georges
  • Guyot, François
  • Jr., Gordon E. Brown
  • Ona-Nguema, Georges
  • Abdelmoula, Mustapha
  • Wang, Yuheng
  • Aquilanti, Giuliana
  • Morin, Guillaume
  • Menguy, N.
  • Olivi, Luca
OrganizationsLocationPeople

article

Arsenite sequestration at the surface of nano-Fe(OH)2, ferrous-carbonate hydroxide, and green-rust after bioreduction of arsenic-sorbed lepidocrocite by Shewanella putrefaciens

  • Bargar, John R.
  • Ruby, Christian
  • Juillot, Farid
  • Calas, Georges
  • Guyot, François
  • Jr., Gordon E. Brown
  • Ona-Nguema, Georges
  • Abdelmoula, Mustapha
  • Wang, Yuheng
  • Aquilanti, Giuliana
  • Morin, Guillaume
  • Menguy, N.
  • Olivi, Luca
Abstract

X-ray Absorption Fine Structure (XAFS) spectroscopy was used in combination with high resolution transmission elec- tron microscopy (HRTEM), electron energy loss spectroscopy (EELS), X-ray energy dispersive spectroscopy (XEDS), X- ray powder diffraction, and Mo ̈ ssbauer spectroscopy to obtain detailed information on arsenic and iron speciation in the products of anaerobic reduction of pure and As(V)- or As(III)-adsorbed lepidocrocite (c-FeOOH) by Shewanella putrefaciens ATCC 12099. We found that this strain of S. putrefaciens is capable of using Fe(III) in lepidocrocite and As(V) in solution or adsorbed on lepidocrocite surfaces as electron acceptors. Bioreduction of lepidocrocite in the absence of arsenic resulted in the formation of hydroxycarbonate green rust 1 [FeII4FeIII2(OH)12CO3: GR1(CO3)], which completely converted into ferrous-car- bonate hydroxide (FeII2(OH)2CO3: FCH) over nine months. This study thus provides the first evidence of bacterial reduction of stoichiometric GR1(CO3) into FCH. Bioreduction of As(III)-adsorbed lepidocrocite also led to the formation of GR1(CO3) prior to formation of FCH, but the presence of As(III) slows down this transformation, leading to the co-occur- rence of both phases after 22-month of aging. At the end of this experiment, As(III) was found to be adsorbed on the surfaces of GR1(CO3) and FCH. After five months, bioreduction of As(V)-bearing lepidocrocite led directly to the formation of FCH in association with nanometer-sized particles of a minor As-rich Fe(OH)2 phase, with no evidence for green rust formation. In this five-month experiment, As(V) was fully converted to As(III), which was dominantly sorbed at the surface of the Fe(OH)2 nanoparticles as oligomers binding to the edges of Fe(OH)6 octahedra at the edges of the octahedral layers of Fe(OH)2. These multinuclear As(III) surface complexes are characterized by As–As pairs at a distance of 3.32 ± 0.02 A ̊ and by As–Fe pairs at a distance of 3.50 ± 0.02 A ̊ and represent a new type of As(III) surface complex. Chemical analyses show that the majority of As(III) produced in the experiments with As present is associated with iron-bearing hydroxycarbonate or hydroxide solids,

Topics
  • nanoparticle
  • impedance spectroscopy
  • surface
  • phase
  • experiment
  • iron
  • aging
  • electron energy loss spectroscopy
  • aging
  • Arsenic
  • microscopy
  • X-ray absorption fine structure spectroscopy