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Clare E. Reimers

Researcher at Oregon State University

Publications -  92
Citations -  7835

Clare E. Reimers is an academic researcher from Oregon State University. The author has contributed to research in topics: Organic matter & Benthic zone. The author has an hindex of 46, co-authored 88 publications receiving 7390 citations. Previous affiliations of Clare E. Reimers include Scripps Institution of Oceanography & University of California, San Diego.

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Harnessing microbially generated power on the seafloor

TL;DR: These results demonstrate in real marine environments a new form of power generation that uses an immense, renewable energy reservoir (sedimentary organic carbon) and has near-immediate application.
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Harvesting Energy from the Marine Sediment−Water Interface

TL;DR: In this paper, the authors proposed that the sediment/anode−seawater/cathode configuration constitutes a microbial fuel cell in which power results from the net oxidation of sediment organic matter by dissolved seawater oxygen.
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Microbial Communities Associated with Electrodes Harvesting Electricity from a Variety of Aquatic Sediments

TL;DR: Future studies designed to help optimize the harvesting of electricity from aquatic sediments or waste organic matter should focus on the electrode interactions of these microorganisms which are most competitive in colonizing anodes and cathodes.
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Microbial fuel cell energy from an ocean cold seep

TL;DR: While cold seeps have the potential to provide more power than neighbouring ocean sediments, the limits of mass transport as well as the proclivity for passivation must be considered when developing new benthic microbial fuel cell designs to meet specific power requirements.
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Carbon fluxes and burial rates over the continental slope and rise off central California with implications for the global carbon cycle

TL;DR: In situ microelectrode, box-core pore water gradient, and in situ benthic chamber estimates of organic carbon degradation and CaCO3 dissolution are combined with organic-C and carbonate-C accumulation rates to approximate the total carbon flux to the seafloor along two transects of the continental slope and rise off central California as discussed by the authors.