Browsing by Author "Rosso, Kevin M."

Now showing 1 - 4 of 4
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    Cell adhesion of Shewanella oneidensis to iron oxide minerals: Effect of different single crystal faces
    Neal, Andrew L.; Bank, Tracy L.; Hochella, Michael F. Jr.; Rosso, Kevin M. (American Institute of Physics, 2005-12-30)
    The results of experiments designed to test the hypothesis that near-surface molecular structure of iron oxide minerals influences adhesion of dissimilatory iron reducing bacteria are presented. These experiments involved the measurement, using atomic force microscopy, of interaction forces generated between Shewanella oneidensis MR-1 cells and single crystal growth faces of iron oxide minerals. Significantly different adhesive force was measured between cells and the (001) face of hematite, and the (100) and (111) faces of magnetite. A role for electrostatic interactions is apparent. The trend in relative forces of adhesion generated at the mineral surfaces is in agreement with predicted ferric site densities published previously. These results suggest that near-surface structure does indeed influence initial cell attachment to iron oxide surfaces; whether this is mediated via specific cell surface-mineral surface interactions or by more general interfacial phenomena remains untested. (C) 2005 American Institute of Physics.
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    Detection limits of CO₂in fluid inclusions using microthermometry and Raman spectroscopy and the spectroscopic characterization of CO₂
    Rosso, Kevin M. (Virginia Tech, 1994)
    In many geologic environments, dominantly aqueous solutions contain low concentrations of CO₂. At ambient temperature, in fluid inclusions which trap these solutions, the typical phase assemblage consists of a CO₂-rich vapor (where PCO₂ ≈ PinternaI) and an aqueous phase containing dissolved salts and CO₂. In this study, the CO₂ minimum detection limits (MDLs) using microthermometry and laser Raman spectroscopy are established in terms of PCO₂ using synthetic H₂O-CO₂ inclusions. The purpose of the microthermometric experiments was to examine the diagnostic CO₂ phase changes and determine the quantity of CO₂ necessary to result in observable solid CO₂ melting. The results of these experiments show that an observable solid CO₂ melting event requires PCO₂ ≥ 45 bar at 25°C. The Raman spectroscopic detection limits were investigated using a multichannel Raman spectrometer. Because the Raman spectroscopic MDLs are a function of counts, the CO₂ MDLs were determined by collecting signal-to-noise ratios for both the upper and lower v₁-2v₂ bands as a function of CO₂ pressure (5-60 bars) and over a range of integration times and incident laser power to predict the optimal instrument settings. The resulting CO₂ MDLs are on the order of 1 bar for our instrument. The band splitting of the v₁-2v₂ diad as a function of CO₂ pressure was measured up to 500 bar at ambient temperature. The CO₂ pressures were converted to ρCO₂ and the results are given in terms of the frequency separation between the upper and lower bands. These results are compared to those of previous studies. An analysis of the estimated errors indicates that the technique can be used to determine CO₂ densities in fluid inclusions containing a homogenous, free CO₂ phase to a precision of approximately ± 0.02 g/cm³. The temperature dependence of the intensity ratio of the hot bands to the v₁-2v₂ diad was measured from 270 to 315 K. The close agreement between the calculated and observed results indicate that laser induced sample heating is not significant. The intensity ratio can be used to estimate the CO₂ temperature and, combined with the Raman density determination, allows calculation of the CO₂ pressure.
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    Interfacial and long-range electron transfer at the mineral-microbe interface
    Wigginton, Nicholas Scott (Virginia Tech, 2008-04-21)
    The electron transfer mechanisms of multiheme cytochromes were examined with scanning tunneling microscopy (STM). To simulate bacterial metal reduction mediated by proteins in direct contact with mineral surfaces, monolayers of purified decaheme cytochromes from the metal-reducing bacterium Shewanella oneidensis were prepared on Au(111) surfaces. Recombinant tetracysteine sequences were added to two outermembrane decaheme cytochromes (OmcA and MtrC) from S. oneidensis MR-1 to ensure chemical immobilization on Au(111). STM images of the cytochrome monolayers showed good coverage and their shapes/sizes matched that predicted by their respective molecular masses. Current-voltage (I-V) tunneling spectroscopy revealed that OmcA and MtrC exhibit characteristic tunneling spectra. Theoretical modeling of the single-molecule tunneling spectra revealed a distinct tunneling mechanism for each cytochrome: OmcA mediates tunneling current coherently whereas MtrC temporarily traps electrons via orbital-mediated tunneling. These mechanisms suggest a superexchange electron transfer mechanism for OmcA and a redox-specific (i.e. heme-mediated) electron transfer mechanism for MtrC at mineral surfaces during bacterial metal reduction. Additionally, a novel electrochemical STM configuration was designed to measure tunneling current from multiheme cytochromes to hematite (001) surfaces in various electrolyte solutions. Current-distance (I-s) profiles on hematite (001) reveal predictable electric double layer structure that changes with ionic strength. The addition of the small tetraheme cytochrome c (STC) from S. oneidensis on insulated Au tips resulted in modified tunneling profiles that suggest STC significantly modulates the double layer. This observation is relevant to understanding metal reduction in cases where terminal metal-reducing enzymes are unable to come in direct contact with reducible mineral surfaces. Electronic coupling to the mineral surface might therefore be mediated by a localized ion swarm specific to the mineral surface.
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    Natural, incidental, and engineered nanomaterials and their impacts on the Earth system
    Hochella, Michael F. Jr.; Mogk, David W.; Ranville, James; Allen, Irving C.; Luther, George W.; Marr, Linsey C.; McGrail, B. Peter; Murayama, Mitsuhiro; Qafoku, Nikolla P.; Rosso, Kevin M.; Sahai, Nita; Schroeder, Paul A.; Vikesland, Peter J.; Westerhoff, Paul; Yang, Yi (2019-03-29)
    Nanomaterials are critical components in the Earth system's past, present, and future characteristics and behavior. They have been present since Earth's origin in great abundance. Life, from the earliest cells to modern humans, has evolved in intimate association with naturally occurring nanomaterials. This synergy began to shift considerably with human industrialization. Particularly since the Industrial Revolution some two-and-a-half centuries ago, incidental nanomaterials (produced unintentionally by human activity) have been continuously produced and distributed worldwide. In some areas, they now rival the amount of naturally occurring nanomaterials. In the past half-century, engineered nanomaterials have been produced in very small amounts relative to the other two types of nanomaterials, but still in large enough quantities to make them a consequential component of the planet. All nanomaterials, regardless of their origin, have distinct chemical and physical properties throughout their size range, clearly setting them apart from their macroscopic equivalents and necessitating careful study. Following major advances in experimental, computational, analytical, and field approaches, it is becoming possible to better assess and understand all types and origins of nanomaterials in the Earth system. It is also now possible to frame their immediate and long-term impact on environmental and human health at local, regional, and global scales.