Access the full text.
Sign up today, get DeepDyve free for 14 days.
Loading next page...
/lp/wiley/importance-of-clay-size-minerals-for-fe-iii-respiration-in-a-petroleum-YtgeV66n8o
References (44)
-
(1996)
Thermodynamically unstable iron hydroxides in soddy-podzolic and brown forest soils -
B. Bekins, I. Cozzarelli, E. Godsy, E. Warren, H. Essaid, M. Tuccillo (2001)
Progression of natural attenuation processes at a crude oil spill site: II. Controls on spatial distribution of microbial populations.Journal of contaminant hydrology, 53 3-4
-
D. Lovley, E. Phillips (1987)
Competitive Mechanisms for Inhibition of Sulfate Reduction and Methane Production in the Zone of Ferric Iron Reduction in SedimentsApplied and Environmental Microbiology, 53
-
Y. Vodyanitskii, S. Lesovaya, A. Sivtsov (2001)
Iron minerals in soils on red-colored depositsEurasian Soil Science, 34
-
M. Baedecker, I. Cozzarelli, R. Eganhouse, D. Siegel, P. Bennett (1993)
Crude oil in a shallow sand and gravel aquifer-III -
P. Bennett, F. Hiebert, J. Rogers (2000)
Microbial control of mineral–groundwater equilibria:Macroscale to microscaleHydrogeology Journal, 8
-
E. Murad, W. Fischer (1988)
The Geobiochemical Cycle of Iron -
D. Lovley, Joan Woodward, F. Chapelle (1994)
Stimulated anoxic biodegradation of aromatic hydrocarbons using Fe(III) ligandsNature, 370
-
(1997)
X-Ray Diffraction and the Identification and Analysis of Clay Minerals, 2nd edn -
G. Heron, C. Crouzet, A. Bourg, T. Christensen (1994)
Speciation of Fe(II) and Fe(III) in Contaminated Aquifer Sediments Using Chemical Extraction Techniques.Environmental science & technology, 28 9
-
C. Weaver (1989)
Clays, muds, and shales -
D. Lovley, E. Phillips (1986)
Organic Matter Mineralization with Reduction of Ferric Iron in Anaerobic SedimentsApplied and Environmental Microbiology, 51
-
J. Kostka, E. Haefele, and Viehweger, J. Stucki (1999)
Respiration and Dissolution of Iron(III)-Containing Clay Minerals by BacteriaEnvironmental Science & Technology, 33
-
(1985)
Surficial and subsurface distribution of aquifer sediments at the Bemidji, Minnesota, research site -
B. Bekins, E. Godsy, E. Warren (1999)
Distribution of Microbial Physiologic Types in an Aquifer Contaminated by Crude OilMicrobial Ecology, 37
-
Robert Anderson, D. Lovley (1999)
Naphthalene and Benzene Degradation under Fe(III)-Reducing Conditions in Petroleum-Contaminated AquifersBioremediation Journal, 3
-
D. Lovley, F. Chapelle, J. Woodward (1994)
Use of dissolved h2 concentrations to determine distribution of microbially catalyzed redox reactions in anoxic groundwater.Environmental science & technology, 28 7
-
W. Röling, B. Breukelen, M. Braster, B. Lin, H. Verseveld (2001)
Relationships between Microbial Community Structure and Hydrochemistry in a Landfill Leachate-Polluted AquiferApplied and Environmental Microbiology, 67
-
(1969)
Soil Chemical Analysis – Advanced Course, 2nd edn -
I. Cozzarelli, B. Bekins, M. Baedecker, George Aiken, R. Eganhouse, M. Tuccillo (2001)
Progression of natural attenuation processes at a crude-oil spill site: I. Geochemical evolution of the plume.Journal of contaminant hydrology, 53 3-4
-
I. Cozzarelli, M. Baedecker, R. Eganhouse, D. Goerlitz (1994)
THE GEOCHEMICAL EVOLUTION OF LOW-MOLECULAR-WEIGHT ORGANIC ACIDS DERIVED FROM THE DEGRADATION OF PETROLEUM CONTAMINANTS IN GROUNDWATERGeochimica et Cosmochimica Acta, 58
-
(1987)
Sedimentary and postdepositional processes related to aquifer properties at the Bemidji research site, north-central Minnesota -
L. Carver (1971)
PARTICLE SIZE ANALYSIS -
W. Huff (1990)
X-ray Diffraction and the Identification and Analysis of Clay MineralsClays and Clay Minerals, 38
-
M. Tuccillo, I. Cozzarelli, J. Herman (1999)
Iron reduction in the sediments of a hydrocarbon-contaminated aquiferApplied Geochemistry, 14
-
M. Strobel, G. Delin, Carissa Munson (1998)
Spatial variation in saturated hydraulic conductivity of sediments at a crude-oil spill site near Bemidji, MinnesotaWater-Resources Investigations Report
-
F. Murphy, W. Herkelrath (1996)
A Sample‐Freezing Drive Shoe for a Wire Line Piston Core SamplerGround Water Monitoring and Remediation, 16
-
Y. Vodyanitskii, S. Lesovaya, A. Sivtsov (2003)
Iron hydroxidogenesis in forest and steppe soils of the Russian plainEurasian Soil Science, 36
-
D. Lovley (1997)
Microbial Fe(III) reduction in subsurface environmentsFems Microbiology Reviews, 20
-
(1999)
Naphtalene and benzene degradation under Fe (III)-reducing conditions in petroleumcontaminated aquifers -
(1999)
1999); extraction time is 1 h. dThis study; 1 h extraction with 0.5 M HCl only followed by 1 h extraction -
D. Lovley, E. Phillips (1986)
Availability of Ferric Iron for Microbial Reduction in Bottom Sediments of the Freshwater Tidal Potomac RiverApplied and Environmental Microbiology, 52
-
A. Manceau, B. Lanson, V. Drits, D. Chateigner, W. Gates, Jun Wu, Dongfang Huo, J. Stucki (2000)
Oxidation-reduction mechanism of iron in dioctahedral smectites: I. Crystal chemistry of oxidized reference nontronitesAmerican Mineralogist, 85
-
D. Lovley, M. Baedecker, D. Lonergan, I. Cozzarelli, E. Phillips, D. Siegel (1989)
Oxidation of aromatic contaminants coupled to microbial iron reductionNature, 339
-
D. Bond, D. Lovley (2002)
Reduction of Fe(III) oxide by methanogens in the presence and absence of extracellular quinones.Environmental microbiology, 4 2
-
(1993)
Crude oil in a shallow sand and gravel aquifer: 3. Biogeochemical reactions and mass balance modeling in anoxic ground water -
R. Eganhouse, M. Baedecker, I. Cozzarelli, G. Aiken, K. Thorn, T. Dorsey (1993)
Crude oil in a shallow sand and gravel aquifer—II. Organic geochemistryApplied Geochemistry, 8
-
Robert Anderson, J. Rooney-Varga, Catherine Gaw, D. Lovley (1998)
Anaerobic Benzene Oxidation in the Fe(III) Reduction Zone of Petroleum-Contaminated AquifersEnvironmental Science & Technology, 32
-
(1988)
The geochemical cycle of iron -
D. Lovley, S. Goodwin (1988)
Hydrogen concentrations as an indicator of the predominant terminal electron-accepting reactions in aquatic sedimentsGeochimica et Cosmochimica Acta, 52
-
D. Lovley, E. Phillips (1987)
Rapid Assay for Microbially Reducible Ferric Iron in Aquatic SedimentsApplied and Environmental Microbiology, 53
-
(1986)
Particle-size analysis. In Methods of Soil Analyses Physical and Mineralogical Methods (ed -
W. Gates, A. Jaunet, D. Tessier, M. Cole, H. Wilkinson, J. Stucki (1998)
Swelling and Texture of Iron-Bearing Smectites Reduced by BacteriaClays and Clay Minerals, 46
-
M. Jackson (1969)
Soil Chemical Analysis - Advanced Course., 2
- Publisher
- Wiley
- Copyright
- Copyright © 2004 Wiley Subscription Services, Inc., A Wiley Company
- ISSN
- 1472-4677
- eISSN
- 1472-4669
- DOI
- 10.1111/j.1472-4677.2004.00018.x
- Publisher site
- See Article on Publisher Site
Abstract
ABSTRACT The availability of Fe(III)‐bearing minerals for dissimilatory Fe(III) reduction was evaluated in sediments from a petroleum‐contaminated sandy aquifer near Bemidji, Minnesota (USA). First, the sediments from a contaminated area of the aquifer, in which Fe(III) reduction was the predominant terminal electron accepting process, were compared with sediments from a nearby, uncontaminated site. Data from 0.5 m HCl extraction of different size fractions of the sediments revealed that the clay size fraction contributed a significant portion of the ‘bio‐available’ Fe(III) in the background sediment and was the most depleted in ‘bio‐available’ Fe(III) in the iron‐reducing sediment. Analytical transmission electron microscopy (TEM) revealed the disappearance of thermodynamically unstable Fe(III) and Mn(IV) hydroxides (ferrihydrite and Fe vernadite), as well as a decrease in the abundance of goethite and lepidocrocite in the clay size fraction from the contaminated sediment. TEM observations and X‐ray diffraction examination did not provide strong evidence of Fe(III)‐reduction‐related changes within another potential source of ‘bio‐available’ Fe(III) in the clay size fraction – ferruginous phyllosilicates. However, further testing in the laboratory with sediments from the methanogenic portion of the aquifer that were depleted in microbially reducible Fe(III) revealed the potential for microbial reduction of Fe(III) associated with phyllosilicates. Addition of a clay size fraction from the uncontaminated sediment, as well as Fe(III)‐coated kaolin and ferruginous nontronite SWa‐1, as sources of poorly crystalline Fe(III) hydroxides and structural iron of phyllosilicates respectively, lowered steady‐state hydrogen concentrations consistent with a stimulation of Fe(III) reduction in laboratory incubations of methanogenic sediments. There was no change in hydrogen concentration when non‐ferruginous clays or no minerals were added. This demonstrated that Fe(III)‐bearing clay size minerals were essential for microbial Fe(III) reduction and suggested that both potential sources of ‘bio‐available’ Fe(III) in the clay size fraction, poorly crystalline Fe(III) hydroxides and structural Fe(III) of phyllosilicates, were important sources of electron acceptor for indigenous iron‐reducing microorganisms in this aquifer.
Journal
Geobiology – Wiley
Published: Jan 1, 2004