Search results for "isoprene"

showing 10 items of 47 documents

Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in th…

2017

Mineral dust and secondary organic aerosols (SOA) account for a major fraction of atmospheric particulate matter, affecting climate, air quality and public health. How mineral dust interacts with SOA to influence cloud chemistry and public health, however, is not well understood. Here, we investigated the formation of reactive oxygen species (ROS), which are key species of atmospheric and physiological chemistry, in aqueous mixtures of SOA and mineral dust by applying electron paramagnetic resonance (EPR) spectrometry in combination with a spin-trapping technique, liquid chromatography-tandem mass spectrometry (LC-MS/MS), and a kinetic model. We found that substantial amounts of ROS includi…

010504 meteorology & atmospheric sciencesRadicalInorganic chemistry010501 environmental sciencesMineral dustbehavioral disciplines and activities01 natural scienceschemistry.chemical_compoundKaolinitePhysical and Theoretical ChemistryIsoprene0105 earth and related environmental sciencesAerosolsAir PollutantsMineralsAqueous solutionAtmosphereWaterParticulatesDecompositionDeposition (aerosol physics)chemistryEnvironmental chemistryParticulate MatterPublic HealthReactive Oxygen SpeciesFaraday Discussions
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Proton Transfer versus Hydrogen Bonding: The Reduction of Ubiquinone Q2Incorporated in a Self-Assembled Monolayer in Unbuffered Aqueous Solution

2014

The electrochemical reduction of ubiquinone Q2 (UQ2) in unbuffered aqueous media was investigated over a pH range of 2 to 11, and the results were compared to those obtained in our previous work in buffered solutions. The short isoprene chains of UQ2 were incorporated in a self-assembled monolayer. Analysis of the mechanism and a study in D2O solutions allowed us to demonstrate the important role of hydrogen bonding in the stabilization of the reduced species, also in water. If the concentration of H+ is low relative to that of the quinone, the electrochemical reaction does not proceed through proton-coupled electron transfer, as it does in buffered medium or at low pH values (pH<4.4). We p…

Aqueous solutionHydrogenHydrogen bondInorganic chemistrychemistry.chemical_elementPhotochemistryElectrochemistryTautomerCatalysischemistry.chemical_compoundElectron transferchemistryMonolayerElectrochemistryIsopreneChemElectroChem
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Aircraft-based observations of isoprene-epoxydiol-derived secondary organic aerosol (IEPOX-SOA) in the tropical upper troposphere over the Amazon reg…

2018

During the ACRIDICON-CHUVA field project (September–October 2014; based in Manaus, Brazil) aircraft-based in situ measurements of aerosol chemical composition were conducted in the tropical troposphere over the Amazon using the High Altitude and Long Range Research Aircraft (HALO), covering altitudes from the boundary layer (BL) height up to 14.4&thinsp;km. The submicron non-refractory aerosol was characterized by flash-vaporization/electron impact-ionization aerosol particle mass spectrometry. The results show that significant secondary organic aerosol (SOA) formation by isoprene oxidation products occurs in the upper troposphere (UT), leading to increased organic aerosol mass concentratio…

Atmospheric Science010504 meteorology & atmospheric sciences010501 environmental sciencesMass spectrometry01 natural sciencesTropospherelcsh:Chemistrychemistry.chemical_compoundAltitudeNitrateddc:550WolkenphysikAerosolNOxIsoprene0105 earth and related environmental sciencesaerosol chemical compositionisoprene oxidationAtmosphärische SpurenstoffeACRIDICON15. Life on landOberpfaffenhofenlcsh:QC1-999Aerosolchemistrylcsh:QD1-99913. Climate actionEnvironmental chemistryHALOMass spectrumEnvironmental sciencesecondary organic aerosol (SOA)lcsh:PhysicsAtmospheric Chemistry and Physics
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A machine learning examination of hydroxyl radical differences among model simulations for CCMI-1

2020

The hydroxyl radical (OH) plays critical roles within the troposphere, such as determining the lifetime of methane (CH4), yet is challenging to model due to its fast cycling and dependence on a multitude of sources and sinks. As a result, the reasons for variations in OH and the resulting methane lifetime (τCH4), both between models and in time, are difficult to diagnose. We apply a neural network (NN) approach to address this issue within a group of models that participated in the Chemistry-Climate Model Initiative (CCMI). Analysis of the historical specified dynamics simulations performed for CCMI indicates that the primary drivers of τCH4 differences among 10 models are the flux of UV li…

Atmospheric ScienceAtmospheric chemistry010504 meteorology & atmospheric sciencesneural networkAnalytical chemistry010501 environmental sciences01 natural sciencesTropospherelcsh:Chemistrychemistry.chemical_compoundMESSyErdsystem-ModellierungMixing ratioTropospheric ozoneIsopreneNOx0105 earth and related environmental sciencesEMAChydroxyl radicalPhotodissociationlcsh:QC1-999Atmospheric chemistry neural networkmachine learningchemistrylcsh:QD1-99913. Climate actionCCMI[SDE]Environmental SciencesHydroxyl radicalWater vaporlcsh:Physicsmethane lifetime
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2012

Abstract. Ambient total OH reactivity was measured at the Finnish boreal forest station SMEAR II in Hyytiälä (Latitude 61°51' N; Longitude 24°17' E) in July and August 2010 using the Comparative Reactivity Method (CRM). The CRM – total OH reactivity method – is a direct, in-situ determination of the total loss rate of hydroxyl radicals (OH) caused by all reactive species in air. During the intensive field campaign HUMPPA-COPEC 2010 (Hyytiälä United Measurements of Photochemistry and Particles in Air – Comprehensive Organic Precursor Emission and Concentration study) the total OH reactivity was monitored both inside (18 m) and directly above the forest canopy (24 m) for the first time. The c…

Atmospheric ScienceDaytimeTree canopy010504 meteorology & atmospheric sciencesChemistryRadicalTaiga010501 environmental sciences15. Life on land01 natural sciencesLatitudechemistry.chemical_compoundBoreal13. Climate actionEnvironmental chemistryLongitudeIsoprene0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Measurement report: Photochemical production and loss rates of formaldehyde and ozone across Europe

2021

Various atmospheric sources and sinks regulate the abundance of tropospheric formaldehyde (HCHO), which is an important trace gas impacting the HOx (≡ HO2 + OH) budget and the concentration of ozone (O3). In this study, we present the formation and destruction terms of ambient HCHO and O3 calculated from in situ observations of various atmospheric trace gases measured at three different sites across Europe during summertime. These include a coastal site in Cyprus, in the scope of the Cyprus Photochemistry Experiment (CYPHEX) in 2014, a mountain site in southern Germany, as part of the Hohenpeißenberg Photochemistry Experiment (HOPE) in 2012, and a forested site in Finland, where measurement…

Atmospheric ScienceOzonePhysicsQC1-999PhotodissociationFormaldehydePhotochemistryMethaneTrace gasTropospherechemistry.chemical_compoundChemistrychemistryEnvironmental scienceQD1-999IsopreneNOx
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2016

Abstract. We found that ambient and laboratory-generated secondary organic aerosols (SOA) form substantial amounts of OH radicals upon interaction with liquid water, which can be explained by the decomposition of organic hydroperoxides. The molar OH yield from SOA formed by ozonolysis of terpenes (α-pinene, β-pinene, limonene) is  ∼  0.1 % upon extraction with pure water and increases to  ∼  1.5 % in the presence of Fe2+ ions due to Fenton-like reactions. Upon extraction of SOA samples from OH photooxidation of isoprene, we also detected OH yields of around  ∼  0.1 %, which increases upon addition of Fe2+. Our findings imply that the chemical reactivity and aging of SOA particles is strongl…

Atmospheric ScienceOzonolysis010504 meteorology & atmospheric sciencesRadicalInorganic chemistryExtraction (chemistry)010501 environmental sciencesPhotochemistry01 natural sciencesDecompositionAerosolchemistry.chemical_compoundDeposition (aerosol physics)chemistryYield (chemistry)Isoprene0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Organosulfates in atmospheric aerosol: synthesis and quantitative analysis of pm&amp;lt;sub&amp;gt;2.5&amp;lt;/sub&amp;gt; from xi'an, northwestern c…

2018

Abstract. The sources, formation mechanism and amount of organosulfates (OS) in atmospheric aerosol are not yet well understood, partly due to the lack of authentic standards for quantification. In this study, we report an improved robust procedure for the synthesis of organosulfates with different functional groups. Nine authentic organosulfate standards were synthesized and four standards (benzyl sulfate, phenyl sulfate, glycolic acid sulfate, and hydroxyacetone sulfate) were used to quantify their ambient concentrations. The authentic standards and ambient aerosol samples were analyzed using an optimized ultra performance liquid chromatography–electrospray ionization-tandem mass spectrom…

Atmospheric Scienceparticulate organosulfates010504 meteorology & atmospheric sciences010501 environmental sciences01 natural scienceschemistry.chemical_compoundambient aerosolhaze eventsSulfateGlycolic acid0105 earth and related environmental sciencesDetection limitTotal organic carbondicarboxylic-acidsHydroxyacetonemass-spectrometryAerosolaromatic organosulfateschemistryEnvironmental chemistrychemical-compositionarctic aerosolsisopreneQuantitative analysis (chemistry)secondary organic aerosolOrganosulfate
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Enthalpies of formation of isoprene’s major oxidation byproducts

2005

Abstract The theoretical enthalpies of formation ( Δ f H 298 . 15 ∘ ) of methyl vinyl ketone (MVK, CH 2 CHC(O)CH 3 ), methacrolein (MACR, CH 2 C(CH 3 )CHO), and the radical products formed in their corresponding OH radical oxidations have been calculated with DFT (MPW1K/6-31+G(d,p)) and multilevel (MCCM-UT-CCSD(T)//MPW1K/6-31+G(d,p)) methods. The bond dissociation energies ( BDE , DH 298 . 15 0 ) of the H-atoms that can be abstracted from the MVK and MACR molecules, and the C–O forming bonds of the OH addition products are also calculated. The regioselectivity of the global reaction is discussed in terms of bond strength.

Bond strengthGeneral Physics and AstronomyRegioselectivityMethacroleinPhotochemistryBond-dissociation energyMedicinal chemistryStandard enthalpy of formationchemistry.chemical_compoundchemistryMethyl vinyl ketoneMoleculePhysical and Theoretical ChemistryIsopreneChemical Physics Letters
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Size, Form and Flexibility of the Rubber Molecule

1962

Abstract Natural rubber can be brominated in dilute cyclohexane solution, whereby the molecular weight, corresponding to the bromine content, increases. For brominated rubber, increasing bromine content makes cyclohexane an increasingly poorer solvent, which is shown by a contraction of the molecule coils and a decrease in the second virial coefficient. Quantitative results were obtained through viscosity and light scattering measurements. Cyclohexane solutions of brominated rubber containing about 43% bromine have a θ point at room temperature. Here the second virial coefficient is zero and the coil has an ideal Gaussian density distribution. In this state the coil diameter is about 1.6 ti…

BrominePolymers and PlasticsCyclohexaneScatteringChemistryAnalytical chemistrychemistry.chemical_elementBranching (polymer chemistry)Light scatteringchemistry.chemical_compoundNatural rubberVirial coefficientvisual_artPolymer chemistryMaterials Chemistryvisual_art.visual_art_mediumIsopreneRubber Chemistry and Technology
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