@article {1560,
	title = {Environmental fate of the next generation refrigerant 2,3,3,3-tetrafluoropropene (HFO-1234yf).},
	journal = {Environ Sci Technol},
	volume = {48},
	year = {2014},
	month = {2014 Nov 18},
	pages = {13181-7},
	abstract = {<p>The hydrofluoroolefin 2,3,3,3-tetrafluoropropene (HFO-1234yf) has been introduced to replace 1,1,1,2-tetrafluoroethane (HFC-134a) as refrigerant in mobile, including vehicle, air conditioning systems because of its lower global warming potential. HFO-1234yf is volatile at ambient temperatures; however, high production volumes and widespread handling are expected to release this fluorocarbon into terrestrial and aquatic environments, including groundwater. Laboratory experiments explored HFO-1234yf degradation by (i) microbial processes under oxic and anoxic conditions, (ii) abiotic processes mediated by reactive mineral phases and zerovalent iron (Fe(0), ZVI), and (iii) cobalamin-catalyzed biomimetic transformation. These investigations demonstrated that HFO-1234yf was recalcitrant to microbial (co)metabolism and no transformation was observed in incubations with ZVI, makinawite (FeS), sulfate green rust (GR(SO4)), magnetite (Fe(3)O(4)), and manganese oxide (MnO2). Sequential reductive defluorination of HFO-1234yf to 3,3,3-trifluoropropene and 3,3-dichloropropene with concomitant stoichiometric release of fluoride occurred in incubations with reduced cobalamins (e.g., vitamin B12) indicating that biomolecules can transform HFO-1234yf at circumneutral pH and at ambient temperature. Taken together, these findings suggest that HFO-1234yf recalcitrance in aquifers should be expected; however, HFO-1234yf is not inert and a biomolecule may mediate reductive transformation in low redox environments, albeit at low rates.</p>},
	issn = {1520-5851},
	doi = {10.1021/es5032147},
	author = {Im, Jeongdae and Walshe-Langford, Gillian E and Moon, Ji-Won and L{\"o}ffler, Frank E}
}
@article {1570,
	title = {Effect of nutrient and selective inhibitor amendments on methane oxidation, nitrous oxide production, and key gene presence and expression in landfill cover soils: characterization of the role of methanotrophs, nitrifiers, and denitrifiers.},
	journal = {Appl Microbiol Biotechnol},
	volume = {85},
	year = {2009},
	month = {2009 Nov},
	pages = {389-403},
	abstract = {<p>Methane and nitrous oxide are both potent greenhouse gasses, with global warming potentials approximately 25 and 298 times that of carbon dioxide. A matrix of soil microcosms was constructed with landfill cover soils collected from the King Highway Landfill in Kalamazoo, Michigan and exposed to geochemical parameters known to affect methane consumption by methanotrophs while also examining their impact on biogenic nitrous oxide production. It was found that relatively dry soils (5\% moisture content) along with 15 mg NH (4) (+) (kg soil)(-1) and 0.1 mg phenylacetylene(kg soil)(-1) provided the greatest stimulation of methane oxidation while minimizing nitrous oxide production. Microarray analyses of pmoA showed that the methanotrophic community structure was dominated by Type II organisms, but Type I genera were more evident with the addition of ammonia. When phenylacetylene was added in conjunction with ammonia, the methanotrophic community structure was more similar to that observed in the presence of no amendments. PCR analyses showed the presence of amoA from both ammonia-oxidizing bacteria and archaea, and that the presence of key genes associated with these cells was reduced with the addition of phenylacetylene. Messenger RNA analyses found transcripts of pmoA, but not of mmoX, nirK, norB, or amoA from either ammonia-oxidizing bacteria or archaea. Pure culture analyses showed that methanotrophs could produce significant amounts of nitrous oxide, particularly when expressing the particulate methane monooxygenase (pMMO). Collectively, these data suggest that methanotrophs expressing pMMO played a role in nitrous oxide production in these microcosms.</p>},
	keywords = {Archaea, Bacteria, Base Sequence, DNA, DNA Primers, DNA, Archaeal, DNA, Bacterial, Global Warming, Greenhouse Effect, Inorganic Chemicals, Methane, Nitrites, Nitrogen, Nitrogen Oxides, Nitrous Oxide, Oxidation-Reduction, Polymerase Chain Reaction, Reverse Transcriptase Polymerase Chain Reaction, RNA, Bacterial, RNA, Messenger, Soil, Water Pollutants, Chemical},
	issn = {1432-0614},
	doi = {10.1007/s00253-009-2238-7},
	author = {Lee, Sung-Woo and Im, Jeongdae and Dispirito, Alan A and Bodrossy, Levente and Barcelona, Michael J and Semrau, Jeremy D}
}
