Search results for "Mixture"

showing 10 items of 1178 documents

"Table 25" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged particles only.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesDijet ProductionE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentE+ E- --> 2JETR measurementhuman activitiescirculatory and respiratory physiology
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"Table 26" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged particles only.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 3JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
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"Table 30" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged and neutral particles.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 3JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
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"Table 31" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged and neutral particles.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 4JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
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"Table 27" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged particles only.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 4JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
researchProduct

"Table 28" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged particles only.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 5JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
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"Table 32" of "Properties of hadronic Z decays and test of QCD generators"

1992

N-jet production rates (in percent) corrected for charged and neutral particles.

Astrophysics::High Energy Astrophysical PhenomenaE+ E- --> HADRONSE+ E- --> Z0Integrated Cross Section91.2Jet Productionrespiratory systemCross Sectionequipment and suppliesSIGcomplex mixturesE+ E- --> 5JETE+ E- ScatteringExclusiveHigh Energy Physics::ExperimentR measurementhuman activitiescirculatory and respiratory physiology
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2017

Abstract. Concurrent in situ analyses of interstitial aerosol and cloud droplet residues have been conducted at the Schmücke mountain site during the Hill Cap Cloud Thuringia campaign in central Germany in September and October 2010. Cloud droplets were sampled from warm clouds (temperatures between −3 and +16 °C) by a counterflow virtual impactor and the submicron-sized residues were analyzed by a compact time-of-flight aerosol mass spectrometer (C-ToF-AMS), while the interstitial aerosol composition was measured by an high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS). During cloud-free periods, the submicron out-of-cloud aerosol was analyzed using both instruments, all…

Atmospheric Science010504 meteorology & atmospheric sciences010501 environmental sciencescomplex mixtures01 natural sciencesAerosolAmmoniachemistry.chemical_compoundchemistryNitrateNitric acidEnvironmental chemistryAmmoniumsense organsSulfateScavengingMass fraction0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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African volcanic emissions influencing atmospheric aerosols over the Amazon rain forest

2018

Long-range transport (LRT) plays an important role in the Amazon rain forest by bringing in different primary and secondary aerosol particles from distant sources. The atmospheric oxidation of dimethyl sulfide (DMS), emitted from marine plankton, is considered an important sulfate source over the Amazon rain forest, with a lesser contribution from terrestrial soil and vegetation sulfur emissions. Volcanic sulfur emissions from Africa could be a source of particulate sulfate to the Amazonian atmosphere upon transatlantic transport but no observations have been published. By using satellite observations, together with ground‑based and airborne aerosol particle observations, this paper provide…

Atmospheric Science010504 meteorology & atmospheric sciencesAmazonian[SDE.MCG]Environmental Sciences/Global Changes010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencescomplex mixtureslcsh:ChemistryAtmospherechemistry.chemical_compoundparasitic diseasesCloud condensation nucleiSulfate0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_category15. Life on landParticulateslcsh:QC1-999Trace gasAerosollcsh:QD1-999Volcanochemistry13. Climate actionEnvironmental sciencegeographic locationslcsh:Physics
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2016

Abstract. Cloud residues and out-of-cloud aerosol particles with diameters between 150 and 900 nm were analysed by online single particle aerosol mass spectrometry during the 6-week study Hill Cap Cloud Thuringia (HCCT)-2010 in September–October 2010. The measurement location was the mountain Schmücke (937 m a.s.l.) in central Germany. More than 160 000 bipolar mass spectra from out-of-cloud aerosol particles and more than 13 000 bipolar mass spectra from cloud residual particles were obtained and were classified using a fuzzy c-means clustering algorithm. Analysis of the uncertainty of the sorting algorithm was conducted on a subset of the data by comparing the clustering output with parti…

Atmospheric Science010504 meteorology & atmospheric sciencesChemistryMineralogy010501 environmental sciencesAtmospheric sciencesmedicine.disease_causecomplex mixtures01 natural sciencesSootAerosolchemistry.chemical_compoundLiquid water contentmedicineCloud condensation nucleiParticleAerosol mass spectrometrysense organsSulfateSea salt aerosol0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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