Kinetics of Microbial and Chemical Reduction of Humic Substances: Implications for Electron Shuttling

2008 ◽  
Vol 42 (10) ◽  
pp. 3563-3569 ◽  
Author(s):  
Jie Jiang ◽  
Andreas Kappler
2007 ◽  
Vol 40 (1) ◽  
pp. 19-24 ◽  
Author(s):  
Pedro M. David Gara ◽  
Gabriela N. Bosio ◽  
Mónica C. Gonzalez ◽  
Daniel O. Mártire

2006 ◽  
Vol 72 (9) ◽  
pp. 5933-5941 ◽  
Author(s):  
Man Jae Kwon ◽  
Kevin T. Finneran

ABSTRACT The potential for humic substances to stimulate the reduction of hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) was investigated. This study describes a novel approach for the remediation of RDX-contaminated environments using microbially mediated electron shuttling. Incubations without cells demonstrated that reduced AQDS transfers electrons directly to RDX, which was reduced without significant accumulation of the nitroso intermediates. Three times as much reduced AQDS (molar basis) was needed to completely reduce RDX. The rate and extent of RDX reduction differed greatly among electron shuttle/acceptor amendments for resting cell suspensions of Geobacter metallireducens and G. sulfurreducens with acetate as the sole electron donor. AQDS and purified humic substances stimulated the fastest rate of RDX reduction. The nitroso metabolites did not significantly accumulate in the presence of AQDS or humic substances. RDX reduction in the presence of poorly crystalline Fe(III) was relatively slow and metabolites transiently accumulated. However, adding humic substances or AQDS to Fe(III)-containing incubations increased the reduction rates. Cells of G. metallireducens alone reduced RDX; however, the rate of RDX reduction was slow relative to AQDS-amended incubations. These data suggest that extracellular electron shuttle-mediated RDX transformation is not organism specific but rather is catalyzed by multiple Fe(III)- and humic-reducing species. Electron shuttle-mediated RDX reduction may eventually become a rapid and effective cleanup strategy in both Fe(III)-rich and Fe(III)-poor environments.


2006 ◽  
Vol 422 (1-2) ◽  
pp. 109-115 ◽  
Author(s):  
Zi-Zhou Yuan ◽  
Xue-Ding Chen ◽  
Hui Xu ◽  
Xiao-Li Qu ◽  
Bing-Xia Wang

2014 ◽  
Vol 118 (34) ◽  
pp. 19524-19528 ◽  
Author(s):  
Christian Kuss ◽  
Murielle Carmant-Dérival ◽  
Ngoc Duc Trinh ◽  
Guoxian Liang ◽  
Steen Brian Schougaard

Soil Science ◽  
1996 ◽  
Vol 161 (8) ◽  
pp. 509-520 ◽  
Author(s):  
X. Jin ◽  
G. W. Bailey ◽  
Y. S. Yu ◽  
A. T. Lynch

2015 ◽  
Vol 1130 ◽  
pp. 450-453 ◽  
Author(s):  
Laura Castro ◽  
J.A. Muñoz ◽  
F. González ◽  
M. Luisa Blázquez ◽  
Antonio Ballester

The anaerobic bioreduction of three Fe (III) ores by a type strain of Shewanella putrefaciens has been investigated. The release of ferrous ion indicated the microbial reduction of jarosite and promotes the subsequent secondary mineralization, leading to the formation of various iron-nearing minerals. In addition, the influence of citrate and EDTA in the medium acting as chelating agents, and an electron shuttling molecule were studied. While the citrate and humic substances increased the iron reduction rate, AQDS inhibit the mineral bioreduction and dissolution. S. putrefaciens do not have the necessity of the direct contact between cells and jarosites and, in consequence, cell attachment and biofilm formation on the mineral surface is scant.


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