@article {453,
	title = {Electrode-based approach for monitoring in situ microbial activity during subsurface bioremediation.},
	journal = {Environ Sci Technol},
	volume = {44},
	year = {2010},
	month = {2010 Jan 1},
	pages = {47-54},
	abstract = {Current production by microorganisms colonizing subsurface electrodes and its relationship to substrate availability and microbial activity was evaluated in an aquifer undergoing bioremediation. Borehole graphite anodes were installed downgradient from a region of acetate injection designed to stimulate bioreduction of U(VI); cathodes consisted of graphite electrodes embedded at the ground surface. Significant increases in current density (< or =50 mA/m2) tracked delivery of acetate to the electrodes, dropping rapidly when acetate inputs were discontinued. An upgradient control electrode not exposed to acetate produced low, steady currents (< or =0.2 mA/m2). Elevated current was strongly correlated with uranium removal but minimal correlation existed with elevated Fe(II). Confocal laser scanning microscopy of electrodes revealed firmly attached biofilms, and analysis of 16S rRNA gene sequences indicated the electrode surfaces were dominated (67-80\%) by Geobacter species. This is the first demonstration that electrodes can produce readily detectable currents despite long-range (6 m) separation of anode and cathode, and these results suggest that oxidation of acetate coupled to electron transfer to electrodes by Geobacter species was the primary source of current. Thus it is expected that current production may serve as an effective proxy for monitoring in situ microbial activity in a variety of subsurface anoxic environments.},
	keywords = {Electrodes, Environmental Monitoring, Environmental Remediation, Geobacter, RNA, Ribosomal, 16S, Water Pollutants, Chemical},
	issn = {0013-936X},
	doi = {10.1021/es9017464},
	author = {Williams, Kenneth H and Nevin, Kelly P and Franks, Ashley and Englert, Andreas and Long, Philip E and Lovley, Derek R}
}
@article {575,
	title = {Anaerobic, sulfate-dependent degradation of polycyclic aromatic hydrocarbons in petroleum-contaminated harbor sediment.},
	journal = {Environ Sci Technol},
	volume = {36},
	year = {2002},
	month = {2002 Nov 15},
	pages = {4811-7},
	abstract = {It has previously been demonstrated that [14C]-labeled polycyclic aromatic hydrocarbons (PAHs) can be oxidized to 14CO2 in anoxic, PAH-contaminated, marine harbor sediments in which sulfate reduction is the terminal electron-accepting process. However, it has not previously been determined whether this degradation of [14C]-PAHs accurately reflects the degradation of the in situ pools of contaminant PAHs. In coal tar-contaminated sediments from Boston Harbor, [14C]-naphthalene was readily oxidized to 14CO2, but, after 95 d of incubation under anaerobic conditions, there was no significant decrease in the detectable pool of in situ naphthalene in these sediments. Therefore, to better evaluate the anaerobic biodegradation of the in situ PAH pools, the concentrations of these contaminants were monitored for ca. 1 year during which the sediments were incubated under conditions that mimicked those found in situ. There was loss of all of the PAHs that were monitored (2-5 ring congeners), including high molecular weight PAHs, such as benzo[a]pyrene, that have not previously been shown to be degraded under anaerobic conditions. There was no significant change in the PAH levels in the sediments amended with molybdate to inhibit sulfate-reducing bacteria or in sediments in which all microorganisms had been killed with glutaraldehyde. In some instances, over half of the detectable pools of in situ 2-3 ring PAHs were degraded. In general, the smaller PAHs were degraded more rapidly than the larger PAHs. A distinct exception in the Boston Harbor sediment was naphthalene which was degraded very slowly at a rate comparable to the larger PAHs. In a similar in situ-like study of fuel-contaminated sediments from Liepaja Harbor, Latvia, there was no decline in PAH levels in samples that were sulfate-depleted. However, when the Latvia sediments were supplemented with sufficient sodium sulfate or gypsum to elevate pore water levels of sulfate to approximately 14-25 mM there was a 90\% decline in the naphthalene and a 60\% decline in the 2-methylnaphthalene pool within 90 days. These studies demonstrate for the first time that degradation by anaerobic microorganisms can significantly impact the in situ pools of PAHs in petroleum-contaminated, anoxic, sulfate-reducing harbor sediments and suggest that the self-purification capacity of contaminated harbor sediments is greater than previously considered.},
	keywords = {Bacteria, Anaerobic, Biodegradation, Environmental, Environmental Monitoring, Geologic Sediments, Molecular Weight, Petroleum, Polycyclic Hydrocarbons, Aromatic, Ships, Sulfur-Reducing Bacteria, Transportation, Water Pollutants, Chemical},
	issn = {0013-936X},
	author = {Rothermich, Mary M and Hayes, Lory A and Lovley, Derek R}
}
@article {578,
	title = {Fulvic acid oxidation state detection using fluorescence spectroscopy.},
	journal = {Environ Sci Technol},
	volume = {36},
	year = {2002},
	month = {2002 Jul 15},
	pages = {3170-5},
	abstract = {Humic substances are a heterogeneous class of moderate molecular weight, yellow-colored biomolecules present in all soils, sediments, and natural waters. Although humic substances are generally resistant to microbial degradation under anaerobic conditions, some microorganisms in soils and sediments can use quinone moieties in humic substances as electron acceptors. Laboratory experiments have shown that humic substances can act as electron shuttles in the microbial reduction of ferric iron. Field studies of electron shuttling processes have been constrained by the lack of methods to characterize the oxidation state of quinone moieties in humic substances at natural concentrations. All humic substances have fluorescent properties, and fluorescence spectroscopy can indicate differences in precursor organic source of humic substances. Here we show that the quinone moieties responsible for electron transfer reactions contribute significantly to the fluorescence of humic substances. Further we use fluorescence spectroscopy to elucidate the oxidation state of quinone moieties in humic substances at natural concentrations found in sediment interstitial waters.},
	keywords = {Benzopyrans, Environmental Monitoring, Iron, Oxidation-Reduction, Spectrometry, Fluorescence},
	issn = {0013-936X},
	author = {Klapper, Lisa and McKnight, Diane M and Fulton, J Robin and Blunt-Harris, Elizabeth L and Nevin, Kelly P and Lovley, Derek R and Hatcher, Patrick G}
}
