Cited by 325

The DOI matches its Crossref record; 3 of the 3 references it cites were found in a registry or an index.

Bacterial reduction of crystalline Fe (super 3+) oxides in single phase suspensions and subsurface materials

Zachara, John M., Fredrickson, James K., Li, Shu-Mei, Kennedy, David W., Smith, Steven C., Gassman, Paul L.·1998·American Mineralogist

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Crossref · 10.2138/am-1998-11-1232

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  • Formate and lactate are established electron donors for DIR by S. putrefaciens CN32 and Shewanella spp. in general.

    “Formate and lactate are established electron donors for DIR by S. putrefaciens CN32 [25,33,44,48] as well as Shewanella spp. in general [16,34,46,52,53,[71][72][73][74][75]77].”

    From Electron Donor Utilization and Secondary Mineral Formation during the Bioreduction of Lepidocrocite by Shewanella putrefaciens CN32 (2019) · cites this paper as [25]

    The Experimental Procedures identify S. putrefaciens CN32 and state that sodium lactate was added as the electron donor; Biogenic mineralization likewise describes lactate-driven Fe reduction. The passages found do not establish formate as an electron donor or extend this result to Shewanella species generally (searched: formate electron donor CN32; formate lactate Shewanella). (LLM, conf=0.87)

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Citations

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Research works printed but not linked: 11

  1. Chao, T.T. and Zhou, L. (1983) Extraction techniques for selective dis- solution of amorphous Fe oxides from soils and sediments. Soil Science Society of America Journal, 47, 225-232.
  2. Cornejo, J. (1987) Porosity evaluation of thermally treated hydrous oxide gel. Journal Colloid Interface Science, 115, 260-263.
  3. Dzombak, D.A. and Morel, F.M. (1990) Surface Complexation Modeling, p. 393. Wiley, New York.
  4. Fredrickson, J.K., McKinley, J.P., Bjornstad, B.N., Long, P.E., Ringelberg, D.B., White, D.C., Krumholz, L.R., Suflita, J.M., Colwell, F.S., Leh- man, R.M., and Phelps, T.J. (1997) Pore-size constraints on the activity and survival of subsurface bacteria in a late Cretaceous shale-sandstone sequence, Northwestern, New Mexico. Geomicrobiology Journal, 14, 183-202.
  5. Kandori, K., Kawashima, Y., and Isikawa, T. (1991) Characterization of monodispersed hematite particles by gas adsorption and Fourier trans- form infra-red spectroscopy. Journal of chemistry Society Faraday Trans. I., 87, 2241-2246.
  6. Lindsay, W.L. (1979) Chemical Equilibria in Soils, p. 449. Wiley-Inter- science, New York.
  7. Naono, H. and Fegiwara, R. (1980) Micropore formation due to thermal decomposition of acicular microcrystals of ␣-FeOOH. Journal Colloid Interface Science, 73, 406-415.
  8. Naono, H., Nakai, K., Sueyoshi, T., and Yagi, H. (1987) Porous texture in hematite derived from goethite: mechanism of thermal decomposition of goethite. Journal Collid Interface Science, 120, 439-450.
  9. Norrish, K. and Taylor, R.M. (1961) The isomorphous replacement of Fe by aluminum in soil goethites. Journal of Soil Science, 12, 294-306.
  10. Stevenson, F.J. (1985) Geochimistry of Soil Humic Substances. In Aiken, G.R., McKnight, D.M., Wershaw, R.L., and MacCarthy, P., Eds., Humic Substances in Soil Sediment and Water, p. 13-52. Wiley, New York.
  11. Stone, A.T. and Ulrich, H.J. (1989) Kinetics and reaction stoichiometry in the reductive dissolution of manganese(IV) dioxide and Co(III) oxide by hydroquinone. Journal of Colloid and Interface Science, 132, 509- 515.

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Metadata

Authors
Zachara, J. M., Fredrickson, J. K., Li, S.-M., Kennedy, D. W., Smith, S. C., & Gassman, P. L.
Venue
American Mineralogist
Published
1998-12-01
Volume
83
Issue
11-12 Part 2
Pages
1426-1443
ISSN
0003-004X
Cited by
325
References
3
Language
en

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