Facile Fabrication of Graphene-Containing Foam as a High-Performance Anode for Microbial Fuel Cells.

Facile fabrication of novel three-dimensional anode materials to increase the bacterial loading capacity and improve substrate transport in microbial fuel cells (MFCs) is of great interest and importance. Herein, a novel graphene-containing foam (GCF) was fabricated easily by freeze-drying and pyrolysis of a graphene oxide-agarose gel. Owing to the involvement of graphene and stainless-steel mesh in the GCF, the GCF shows high electrical conductivity, enabling the GCF to be a conductive electrode for MFC applications. With the aid of agarose, the GCF electrode possesses a supermacroporous structure with pore sizes ranging from 100-200 µm and a high surface area, which greatly increase the bacterial loading capacity. Cell viability measurements indicate that the GCF possesses excellent biocompatibility. The MFC, equipped with a 0.4 mm-thick GCF anode, shows a maximum area power density of 786 mW m(-2) , which is 4.1 times that of a MFC equipped with a commercial carbon cloth anode. The simple fabrication route in combination with the outstanding electrochemical performance of the GCF indicates a promising anode for MFC applications.

Secondary bacterial flagellar system improves bacterial spreading by increasing the directional persistence of swimming.

As numerous bacterial species, Shewanella putrefaciens CN-32 possesses a complete secondary flagellar system. A significant subpopulation of CN-32 cells induces expression of the secondary system under planktonic conditions, resulting in formation of one, sometimes two, filaments at lateral positions in addition to the primary polar flagellum. Mutant analysis revealed that the single chemotaxis system primarily or even exclusively addresses the main polar flagellar system. Cells with secondary filaments outperformed their monopolarly flagellated counterparts in spreading on soft-agar plates and through medium-filled channels despite having lower swimming speed. While mutant cells with only polar flagella navigate by a "run-reverse-flick" mechanism resulting in effective cell realignments of about 90°, wild-type cells with secondary filaments exhibited a range of realignment angles with an average value of smaller than 90°. Mathematical modeling and computer simulations demonstrated that the smaller realignment angle of wild-type cells results in the higher directional persistence, increasing spreading efficiency both with and without a chemical gradient. Taken together, we propose that in S. putrefaciens CN-32, cell propulsion and directional switches are mainly mediated by the polar flagellar system, while the secondary filament increases the directional persistence of swimming and thus of spreading in the environment.

Flavin mononucleotide mediated electron pathway for microbial U(VI) reduction.

Microbial reduction of U(VI) is an important phenomenon affecting uranium mobility in the subsurface environments. Elucidation of its mechanism is necessary for predicting uranium migration and for applying environmental remediation. In this study, we have examined the electron pathway for the U(VI) reduction mediated by flavin mononucleotide (FMN), which is secreted by Shewanella species. The cyclic voltammetry (CV) and photo-electrochemical methods with an optically transparent thin-layer electrode (OTTLE) cell were utilized in investigating in vitro the electron transfer reactions that take place between FMN and U(VI). The CV measurements of U(VI) were carried out in a citrate and Tris-HCl buffer both with and without FMN. A scarce U(VI) reduction current was observed in the absence of the FMN. To the contrary, a catalytic U(VI) reduction current was observed in the presence of FMN at the redox potential of the FMN. The reduction current increased with an increase in the concentration of the U(VI). The reduced form of the U was confirmed to be U(VI) by the photo-electrochemical analysis using the OTTLE cell. The results demonstrated that FMN acts as a mediator in the electro-reduction of U(VI) to U(iv). In addition, in vivo bio-reduction experiments on U(VI) with Shewanella putrefaciens revealed that the addition of FMN accelerated the reduction rate of U(VI). These results indicate that the bio-reduction of U(VI) by the Shewanella species can be catalyzed by FMN secreted from the cells.

Effects of oxyanions, natural organic matter, and bacterial cell numbers on the bioreduction of lepidocrocite (gamma-FeOOH) and the formation of secondary mineralization products.

Microbial reduction of Fe(III) oxides results in the production of Fe(II) and may lead to the subsequent formation of Fe(II)-bearing secondary mineralization products including magnetite, siderite, vivianite, chukanovite (ferrous hydroxy carbonate (FHC)), and green rust; however, the factors controlling the formation of specific Fe(II) phases are often not well-defined. This study examined effects of (i) a range of inorganic oxyanions (arsenate, borate, molybdate, phosphate, silicate, and tungstate), (ii) natural organic matter (citrate, oxalate, microbial extracellular polymeric substances [EPS], and humic substances), and (iii) the type and number of dissimilatory iron-reducing bacteria on the bioreduction of lepidocrocite and formation of Fe(II)-bearing secondary mineralization products. The bioreduction kinetics clustered into two distinct Fe(II) production profiles. "Fast" Fe(II) production kinetics [19-24 mM Fe(II) d(-1)] were accompanied by formation of magnetite and FHC in the unamended control and in systems amended with borate, oxalate, gellan EPS, or Pony Lake fulvic acid or having "low" cell numbers. Systems amended with arsenate, citrate, molybdate, phosphate, silicate, tungstate, EPS from Shewanella putrefaciens CN32, or humic substances derived from terrestrial plant material or with "high" cell numbers exhibited comparatively slow Fe(II) production kinetics [1.8-4.0 mM Fe(II) d(-1)] and the formation of green rust. The results are consistent with a conceptual model whereby competitive sorption of more strongly bound anions blocks access of bacterial cells and reduced electron-shuttling compounds to sites on the iron oxide surface, thereby limiting the rate of bioreduction.

Competitive binding of CU2+ and Zn2+ to live cells of shewanella putrefaciens.

Binding of Cu2+ and Zn2+ to live cells of Shewanella putrefaciens was measured at pH 4, 5.5, and 7 for dissolved metal concentrations ranging from 0.1 to 100 microM. Release of organic compounds by the cells resulted in concentrations of dissolved organic carbon (DOC) between 0.5 and 1.6 mM. A discrete site, nonelectrostatic model was used to describe Cu2+ and Zn2+ binding to the cells. Binding of Zn2+, which increased with increasing pH over the entire range of dissolved Zn2+ concentration, could be explained by invoking two types of cell wall binding sites: acidic and neutral functional groups. Binding of Cu2+ exhibited a more complex pH dependence: at dissolved metal concentrations below 1 microM, binding to the cells actually increased with decreasing pH. This behavior could be reproduced by (1) assuming the existence of a small fraction of high-affinity binding sites in the cell wall (approximately 5%) and (2) including metal complexation by dissolved organic ligands. The latter compete with the neutral cell wall groups and decrease Zn2+ and Cu2+ binding at pH 5.5 and 7. The observed isotherms implied that binding of the metals was only weakly affected by cell wall charging. Model parameters derived from the single-metal binding isotherms were able to account for the observed competition of Zn2+ and Cu2+ for cell wall sites when both metals were present.

Microbial activity at gigapascal pressures.

We observed physiological and metabolic activity of Shewanella oneidensis strain MR1 and Escherichia coli strain MG1655 at pressures of 68 to 1680 megapascals (MPa) in diamond anvil cells. We measured biological formate oxidation at high pressures (68 to 1060 MPa). At pressures of 1200 to 1600 MPa, living bacteria resided in fluid inclusions in ice-VI crystals and continued to be viable upon subsequent release to ambient pressures (0.1 MPa). Evidence of microbial viability and activity at these extreme pressures expands by an order of magnitude the range of conditions representing the habitable zone in the solar system.