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Kenneth M. Kemner

Researcher at Argonne National Laboratory

Publications -  164
Citations -  10441

Kenneth M. Kemner is an academic researcher from Argonne National Laboratory. The author has contributed to research in topics: Adsorption & Uranium. The author has an hindex of 47, co-authored 153 publications receiving 9408 citations. Previous affiliations of Kenneth M. Kemner include University of Illinois at Chicago & Georgia Institute of Technology.

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Functionalized Monolayers on Ordered Mesoporous Supports

TL;DR: The surface modification scheme reported in this paper enables rational design of the surface properties of tailored porous materials and may lead to the synthesis of more sophisticated functionalized composites for environmental and industrial applications.
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Formation of sphalerite (ZnS) deposits in natural biofilms of sulfate-reducing bacteria.

TL;DR: These results show how microbes control metal concentrations in groundwater- and wetland-based remediation systems and suggest biological routes for formation of some low-temperature ZnS deposits.
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Reduction of Uranium(VI) by Mixed Iron(II)/Iron(III) Hydroxide (Green Rust): Formation of UO2 Nanoparticles

TL;DR: Results clearly indicate that U(VI) (as soluble uranyl ion) is readily reduced by green rust to U(IV) in the form of relatively insoluble UO2 nanoparticles, suggesting that the presence of green rusts in the subsurface may have significant effects on the mobility of uranium, particularly under iron-reducing conditions.
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Protein Oxidation Implicated as the Primary Determinant of Bacterial Radioresistance

TL;DR: It is presented the case that protein, rather than DNA, is the principal target of the biological action of IR in sensitive bacteria, and extreme resistance in Mn-accumulating bacteria is based on protein protection.
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Nanometre-size products of uranium bioreduction.

TL;DR: It is shown that uraninite (UO2) particles formed from uranium in sediments by bacterial reduction are typically less than 2 nanometres across and that the small size has important implications for uranite reactivity and fate.