@article {1564, title = {A field trial of nutrient stimulation of methanotrophs to reduce greenhouse gas emissions from landfill cover soils.}, journal = {J Air Waste Manag Assoc}, volume = {63}, year = {2013}, month = {2013 Mar}, pages = {300-9}, abstract = {

UNLABELLED: Landfills are among the major sources of anthropogenic methane (CH4) estimated to reach 40 x 10(9) kg per year worldwide by 2015 (IPCC, 2007). A 2 1/2-year field experiment was conducted at a closed landfill in western Michigan where methanotrophs, methane-consuming bacteria, were stimulated by nutrient addition to the soil without significantly increasing biogenic nitrous oxide (N2O) production. The effects of the nitrogen amendments (KNO3 and NH4Cl), phenylacetylene (a selective inhibitor of nitrifying bacteria that contribute to N2O production), and a canopy (to reduce direct water infiltration) on the vertical soil gas profiles of CH4, CO2, and O2 were measured in the top meter of the soil. Methane and nitrous oxide fluxes were calculated from the corresponding soil gas concentration gradients with respect to depth and a Millington-Quirk diffusivity coefficient in soil derived empirically from soil porosity, water content, and diffusivity coefficients in air from the literature. Methane flux estimates were as high as 218.4 g m(-2) day(-1) in the fall and 12.8 g/m(-2) day(-1) in the summer. During the spring and summer CH4 fluxes were reduced by more than half by adding KNO3 and NH4Cl into the soil as compared to control plots, while N2O fluxes increased substantially. The concurrent addition of phenylacetylene to the amendment decreased peak N2O production by half and the rate of peak methane oxidation by about one-third. The seasonal average methane and N2O flux data were extrapolated to estimate the reduction of CH4 and N2O fluxes into the atmosphere by nitrogen and inhibitor addition to the cover soils. The results suggest that such additions coupled with soil moisture management may provide a potential strategy to significantly reduce greenhouse gas emissions from landfills.

IMPLICATIONS: The results of a 2 1/2-year study of effects of nutrient stimulation on methane oxidation in landfill cover soils demonstrates that nutrient addition does decrease methane emissions. The work further underscores the control which soil moisture exerts on methane oxidation. Water management is critical to the success of methane oxidation strategies.

}, keywords = {Biodegradation, Environmental, Gases, Greenhouse Effect, Methane, Oxidation-Reduction, Soil, Soil Microbiology, Waste Management}, issn = {1096-2247}, author = {Lizik, William and Im, Jeongdae and Semrau, Jeremy D and Barcelona, Michael J} } @article {1565, title = {Guided cobalamin biosynthesis supports Dehalococcoides mccartyi reductive dechlorination activity.}, journal = {Philos Trans R Soc Lond B Biol Sci}, volume = {368}, year = {2013}, month = {2013 Apr 19}, pages = {20120320}, abstract = {

Dehalococcoides mccartyi strains are corrinoid-auxotrophic Bacteria and axenic cultures that require vitamin B12 (CN-Cbl) to conserve energy via organohalide respiration. Cultures of D. mccartyi strains BAV1, GT and FL2 grown with limiting amounts of 1 {\textmu}g l(-1) CN-Cbl quickly depleted CN-Cbl, and reductive dechlorination of polychlorinated ethenes was incomplete leading to vinyl chloride (VC) accumulation. In contrast, the same cultures amended with 25 {\textmu}g l(-1) CN-Cbl exhibited up to 2.3-fold higher dechlorination rates, 2.8-9.1-fold increased growth yields, and completely consumed growth-supporting chlorinated ethenes. To explore whether known cobamide-producing microbes supply Dehalococcoides with the required corrinoid cofactor, co-culture experiments were performed with the methanogen Methanosarcina barkeri strain Fusaro and two acetogens, Sporomusa ovata and Sporomusa sp. strain KB-1, as Dehalococcoides partner populations. During growth with H2/CO2, M. barkeri axenic cultures produced 4.2 {\textpm} 0.1 {\textmu}g l(-1) extracellular cobamide (factor III), whereas the Sporomusa cultures produced phenolyl- and p-cresolyl-cobamides. Neither factor III nor the phenolic cobamides supported Dehalococcoides reductive dechlorination activity suggesting that M. barkeri and the Sporomusa sp. cannot fulfil Dehalococcoides{\textquoteright} nutritional requirements. Dehalococcoides dechlorination activity and growth occurred in M. barkeri and Sporomusa sp. co-cultures amended with 10 {\textmu}M 5{\textquoteright},6{\textquoteright}-dimethylbenzimidazole (DMB), indicating that a cobalamin is a preferred corrinoid cofactor of strains BAV1, GT and FL2 when grown with chlorinated ethenes as electron acceptors. Even though the methanogen and acetogen populations tested did not produce cobalamin, the addition of DMB enabled guided biosynthesis and generated a cobalamin that supported Dehalococcoides{\textquoteright} activity and growth. Guided cobalamin biosynthesis may offer opportunities to sustain and enhance Dehalococcoides activity in contaminated subsurface environments.

}, keywords = {Bacteriological Techniques, Benzimidazoles, Biodegradation, Environmental, Chloroflexi, Chromatography, High Pressure Liquid, Coculture Techniques, Culture Media, Dichloroethylenes, Halogenation, Oxidation-Reduction, Trichloroethylene, Vitamin B 12}, issn = {1471-2970}, doi = {10.1098/rstb.2012.0320}, author = {Yan, Jun and Im, Jeongdae and Yang, Yi 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 = {

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.

}, 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} }