Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Experiment Videos

Bacterial reductive dissolution of crystalline Fe(III) oxide in continuous-flow column reactors.

E E Roden1, M M Urrutia, C J Mann

  • 1Department of Biological Sciences, The University of Alabama, Tuscaloosa, Alabama 35487-0206, USA. eroden@biology.as.ua.edu

Applied and Environmental Microbiology
|March 4, 2000
PubMed
Summary

Continuous-flow reactors enabled near-quantitative bacterial reduction of iron (Fe(III)) oxide-coated sand, unlike batch cultures. Removing dissolved iron (Fe(II)) sustained bacterial activity and growth, impacting contaminant fate.

Related Concept Videos

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Microbial acceleration of aerobic pyrite oxidation at circumneutral pH.

Geobiology·2017
Same author

Microbial Fe(III) oxide reduction potential in Chocolate Pots hot spring, Yellowstone National Park.

Geobiology·2016
Same author

The future of emergency medicine.

British journal of hospital medicine (London, England : 2005)·2014
Same author

Molecular signature of the immune and tissue response to non-coding plasmid DNA in skeletal muscle after electrotransfer.

Gene therapy·2011
Same author

Iron isotope fractionation during microbial dissimilatory iron oxide reduction in simulated Archaean seawater.

Geobiology·2011
Same author

Microbial production of isotopically light iron(II) in a modern chemically precipitated sediment and implications for isotopic variations in ancient rocks.

Geobiology·2010

Area of Science:

  • Geochemistry
  • Environmental Microbiology
  • Biogeochemical Cycles

Background:

  • Bacterial reduction of iron (Fe(III)) oxides is crucial in geochemical processes.
  • Surface-bound Fe(II) can passivate Fe(III) oxide reduction activity.
  • Understanding Fe(III) oxide reduction is key for contaminant fate studies.

Purpose of the Study:

  • To compare bacterial Fe(III) oxide reduction in continuous-flow column reactors versus batch cultures.
  • To investigate the role of Fe(II) removal in sustaining microbial activity.
  • To assess the implications for contaminant geochemistry.

Main Methods:

  • Studied bacterial reductive dissolution of synthetic Fe(III) oxide-coated sand.
  • Utilized continuous-flow column reactors and parallel batch cultures.

Related Experiment Videos

  • Analyzed aqueous Fe(II) export and remaining Fe(III) content via wet-chemical analysis.
  • Main Results:

    • Column reactors achieved near-quantitative Fe(III) reduction (95.0 +/- 3.7%) over 6 months.
    • Batch cultures showed limited Fe(III) reduction (13.0 +/- 2.2%) and reached an asymptote.
    • Continuous flow sustained bacterial growth (100-fold increase) by removing passivating Fe(II).

    Conclusions:

    • Aqueous-phase transport of Fe(II) in flow reactors prevents passivation, enhancing Fe(III) oxide reduction.
    • Sustained reduction and bacterial growth are achievable in flow systems.
    • Findings inform the geochemical behavior of contaminants linked to Fe(III) reduction.