Search results for " methane"

showing 10 items of 146 documents

Mild, Fast, and Easy To Conduct MoCl5-Mediated Dehydrogenative Coupling Reactions in Flow

2018

A convenient and straightforward approach to performing oxidative coupling reactions in flow is presented. A collection of electron-rich benzene derivatives was subjected to this protocol, and the distinct utility of molybdenum pentachloride (MoCl5) is established. Using this unexplored protocol, biphenyls could be obtained in 21–91% isolated yield. This simple protocol opens a new chapter in reagent-mediated dehydrogenative coupling reactions, and yields are compared to classical approaches.

010405 organic chemistryChemistryOrganic ChemistryMolybdenum pentachloride010402 general chemistry01 natural sciencesBiochemistryCombinatorial chemistryCoupling reaction0104 chemical sciencesFlow (mathematics)Yield (chemistry)Benzene derivativesOxidative coupling of methanePhysical and Theoretical ChemistryOrganic Letters
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Molybdenum Pentachloride Mediated Synthesis of Spirocyclic Compounds by Intramolecular Oxidative Coupling

2015

The oxidative treatment of (m)ethyl 2-aryl cinnamates equipped with methoxy groups in position 4 of the phenyl moiety promote the formation of cyclohexadienone substructures. This dealkylative oxidative C–C coupling gives access to spirocyclic compounds and avoids the construction of the corresponding phenanthrenes. Furthermore, the transformation can be expanded to other spirocyclic systems.

010405 organic chemistryStereochemistryOrganic Chemistrychemistry.chemical_elementMolybdenum pentachloride010402 general chemistry01 natural sciences0104 chemical sciencesScholl reactionchemistryMolybdenumIntramolecular forceMoietyCinnamatesOxidative coupling of methanePhysical and Theoretical ChemistryPhenanthrenesEuropean Journal of Organic Chemistry
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A novel comprehensive procedure for estimating greenhouse gas emissions from water resource recovery facilities

2017

The emissions of the major greenhouse gases (GHGs), i.e. carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) from water resource recovery facilities (WRRFs) are of increasing concern in the water industry. In order to produce useful and comparable information for monitoring, assessing, and reporting GHG emissions from WRRFs, there is a need for a generally accepted methodology for their quantification. This paper aims at proposing the first protocol for monitoring and accounting for GHG emissions from WRRFs, taking into account both direct and indirect internal emissions and focusing the attention on plant sections known to be primarily responsible for GHG emissions (i.e. oxidation…

010504 meteorology & atmospheric sciences0208 environmental biotechnologyNitrous Oxide02 engineering and technologyWastewater01 natural sciencesMethaneCarbon footprint; Methane; Nitrous oxide; Off-gas; Wastewater; Energychemistry.chemical_compoundBiogasOff-ga0105 earth and related environmental sciencesResource recoveryCarbon FootprintEnergy recoveryEnergyWaste managementSettore ICAR/03 - Ingegneria Sanitaria-AmbientaleEnvironmental engineering020801 environmental engineeringAnaerobic digestionchemistryGreenhouse gasCarbon footprintEnvironmental scienceAerationMethane
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A record of seafloor methane seepage across the last 150 million years

2020

<p>Methane seepage at the seafloor is a source of carbon in the marine environment and has long been recognized as an important window into the deep geo-, hydro-, and bio-spheres. However, the processes and temporal patterns of natural methane emission over multi-million-year time scales are still poorly understood. The microbially-mediated methane oxidation leads to the precipitation of authigenic carbonate minerals within subseafloor sediments, thus providing a potentially extensive record of past methane emission. In this study, we used data on methane-derived authigenic carbonates to build a proxy time series of seafloor methane emission over the last 150 My. We quantitat…

010504 meteorology & atmospheric sciencesEarth scienceCarbonate mineralslcsh:Medicine010502 geochemistry & geophysics01 natural sciencesMethaneArticlechemistry.chemical_compoundlcsh:ScienceSea level0105 earth and related environmental sciencesTotal organic carbonMultidisciplinarylcsh:RBiogeochemistryCretaceousSeafloor spreadingOceanographyOcean scienceschemistryEnvironmental scienceSeawaterlcsh:QArctic methane releaseGeologyScientific Reports
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Applications of a new set of methane line parameters to the modeling of Titan's spectrum in the 1.58 μm window

2012

International audience; In this paper we apply a recently released set of methane line parameters (Wang et al., 2011) to the modeling of Titan spectra in the 1.58 mu m window at both low and high spectral resolution. We first compare the methane absorption based on this new set of methane data to that calculated from the methane absorption coefficients derived in situ from DISR/Huygens (Tomasko et al., 2008a; Karkoschka and Tomasko, 2010) and from the band models of Irwin et al. (2006) and Karkoschka and Tomasko (2010). The Irwin et al. (2006) band model clearly underestimates the absorption in the window at temperature-pressure conditions representative of Titan's troposphere, while the Ka…

010504 meteorology & atmospheric sciencesInfraredCASSINI VIMSHUYGENS PROBEMONODEUTERATED METHANEAtmospheric sciences01 natural sciences7. Clean energyMethaneSpectral lineTropospherechemistry.chemical_compoundsymbols.namesake0103 physical sciencesSpectral resolutionSpectroscopy010303 astronomy & astrophysicsCLOUD STRUCTURE0105 earth and related environmental sciencesPhysics[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][PHYS.PHYS.PHYS-OPTICS]Physics [physics]/Physics [physics]/Optics [physics.optics][ PHYS.PHYS.PHYS-OPTICS ] Physics [physics]/Physics [physics]/Optics [physics.optics]Astronomy and Astrophysics9500 CM(-1)SPECTROSCOPIC DATABASEM TRANSPARENCY WINDOWComputational physicsAerosolchemistry[ PHYS.PHYS.PHYS-AO-PH ] Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]TEMPERATURE-DEPENDENCE13. Climate actionSpace and Planetary SciencesymbolsSHIFT COEFFICIENTSOUTER SOLAR-SYSTEMTitan (rocket family)
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Titan's surface albedo variations over a Titan season from near-infrared CFHT/FTS spectra

2006

International audience; We have observed Titan in a series of campaigns from 1991 to 1996 with the Fourier Transform Spectrometer on the CFH telescope. The data acquired provide a lightcurve from the geometric albedos in the 0.9–View the MathML source spectral region. The 1991–1993 data were previously analyzed in Coustenis et al. [1995. Titan's surface: composition and variability from its near-infrared albedo. Icarus 118, 87–104] with a spherical particle code by McKay et al. [1989. The thermal structure of Titan's atmosphere. Icarus 80, 23–53]. We present here three new datasets from the 1994, 1995 and 1996 observations, with additional information from the 0.94-μm methane window on Tita…

010504 meteorology & atmospheric sciencesSatellitesCFHTAstrophysicsAtmospheric sciences01 natural sciencesMethaneAtmosphereMethane absorption coefficientssymbols.namesakechemistry.chemical_compoundNear-infraredPlanet0103 physical sciencesRadiative transfer010303 astronomy & astrophysicsSpectroscopy0105 earth and related environmental sciencesPhysicsAtmospheric methaneAstronomy and AstrophysicsTholinAlbedochemistry13. Climate actionSpace and Planetary SciencesymbolsTitan (rocket family)Titan
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Methanotrophy in geothermal soils, an overlooked process: The example of Nisyros island (Greece)

2020

Abstract A multidisciplinary field campaign was carried out at Nisyros Island (Greece). Hydrothermal gases were sampled and analysed, and CH4 and CO2 fluxes from the soils were measured with the accumulation chamber method. The sampling area (Lakki plain) covers an area of about 0.08 km2, and includes the main fumarolic areas of Kaminakia, Stefanos, Ramos, Lofos and Phlegeton. Flux values measured at 130 sites range from −3.4 to 1420 mg m−2 d−1 for CH4 and from 0.1 to 383 g m−2 d−1 for CO2. The fumarolic areas show very different CH4 degassing patterns, Kaminakia showing the highest CH4 output values (about 0.8 t a−1 from an area of about 30,000 m2) and Phlegeton the lowest (about 0.01 t a−…

010504 meteorology & atmospheric sciencesSoil testMethanotrophy Soil degassing Hydrothermal systems Methane output Greenhouse gasesSampling (statistics)GeologySoil scienceMethanotrophy Soil degassing Hydrothermal systems Methane output Greenhouse gases010502 geochemistry & geophysics01 natural sciencesSettore GEO/08 - Geochimica E VulcanologiaFlux (metallurgy)Geochemistry and PetrologyChamber methodSoil waterGeothermal gradientGeologyField campaign0105 earth and related environmental sciencesChemical Geology
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New insight to the role of microbes in the methane exchange in trees: evidence from metagenomic sequencing

2021

Methane (CH4) exchange in tree stems and canopies and the processes involved are among the least understood components of the global CH4 cycle. Recent studies have focused on quantifying tree stems as sources of CH4 and understanding abiotic CH4 emissions in plant canopies, with the role of microbial in situ CH4 formation receiving less attention. Moreover, despite initial reports revealing CH4 consumption, studies have not adequately evaluated the potential of microbial CH4 oxidation within trees. In this paper, we discuss the current level of understanding on these processes. Further, we demonstrate the potential of novel metagenomic tools in revealing the involvement of microbes in the C…

0106 biological sciences0301 basic medicinePhysiologyPlant Science01 natural sciencesmetaaniMethaneTreesbakteerit03 medical and health scienceschemistry.chemical_compoundboreal forestsUltraviolet radiationAbiotic componentbiologyNorwayEcologyAtmospheric methaneTaigakasvifysiologiapuut (kasvit)Picea abiesgenomiikka15. Life on landbiology.organism_classificationmethanogenic archaeametsätplant microbiometree030104 developmental biologymethane exchangeboreaalinen vyöhykemikrobistochemistry13. Climate actionMetagenomicsEnvironmental scienceaineiden kiertoMetagenomicsmethanotrophic bacteriaMethanearkeonit010606 plant biology & botanycaptured metagenomicsNew Phytologist
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Oxidation, efflux, and isotopic fractionation of methane during autumnal turnover in a polyhumic, boreal lake

2007

[1] We studied the oxidation and efflux of methane (CH4) in a small, polyhumic lake, Mekkojarvi (southern Finland), during 6 weeks in autumn when the stability of the water mass first weakened, temporarily restabilized, and finally mixed completely. During the summer stratification period, CH4 had accumulated in the anoxic hypolimnion to high concentrations (>150 mmol m−3). Gradual mixing of the water column during the autumn allowed access to both oxygen and CH4 by aerobic methane-oxidizing bacteria (MOB) deeper in the water column. Thus the bulk (∼83–88%) of the CH4 accumulated in the hypolimnion was subsequently consumed by MOB while only 12–17% was lost from the lake to the atmosphere a…

0106 biological sciencesAtmospheric ScienceWater mass010504 meteorology & atmospheric sciencesSoil ScienceAquatic ScienceOceanography01 natural sciencesMethanechemistry.chemical_compoundWater columnIsotope fractionationGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and TechnologyHydrologyEcologyChemistry010604 marine biology & hydrobiologyPaleontologyForestryAnoxic watersGeophysics13. Climate actionSpace and Planetary ScienceIsotopes of carbonEnvironmental chemistryAnaerobic oxidation of methaneHypolimnionJournal of Geophysical Research
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Species disparity response to mutagenesis of marine yeasts for the potential production of biodiesel.

2019

Abstract Background Among the third-generation biodiesel feed stock, oleaginous marine yeasts are the least studied microorganisms for such purpose. Results Wild strains yeasts were isolated from various Tunisian marine sources including fish waste (Candida tenuis CtTun15, Debaryomyces hansenii DhTun2015, Trichosporon asahii TaTun15 and Yarrowia lipolytica YlTun15) and seawater (Rhodotorula mucilaginosa RmTun15). Following incubation with ethyl methanesulfonate (EMS: 75 mM) for various periods of time (T15, T30, T45, T60 min), the cell viability of these strains responded differentially according to yeast species. For instance, mutated CtTun15 did not survive after 30 min of EMS treatment; …

0106 biological sciencesEthyl methanesulfonatelcsh:BiotechnologyMicroorganismManagement Monitoring Policy and Law01 natural sciencesApplied Microbiology and Biotechnologylcsh:Fuel03 medical and health scienceschemistry.chemical_compoundEthyl methanesulfonatelcsh:TP315-360lcsh:TP248.13-248.65010608 biotechnologyDebaryomyces hanseniiFood scienceBiomassIncubationMutagenesis optimization030304 developmental biologychemistry.chemical_classification0303 health sciencesOleaginous yeastbiologyRenewable Energy Sustainability and the EnvironmentFatty acidCorrectionYarrowiaLipidbiology.organism_classificationFatty acidYeastddc:General EnergychemistryBiodiesel productionBiodieselBiotechnologyBiotechnology for biofuels
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