Search results for "Particle radiation"

showing 10 items of 677 documents

Search for heavy neutral lepton production in K+ decays to positrons

2020

A search for heavy neutral lepton ($N$) production in $K^+\to e^+N$ decays using the data sample collected by the NA62 experiment at CERN in 2017--2018 is reported. Upper limits of the extended neutrino mixing matrix element $|U_{e4}|^2$ are established at the level of $10^{-9}$ over most of the accessible heavy neutral lepton mass range 144--462 MeV/$c^2$, with the assumption that the lifetime exceeds 50 ns. These limits improve significantly upon those of previous production and decay searches. The $|U_{e4}|^2$ range favoured by Big Bang Nucleosynthesis is excluded up to a mass of about 340 MeV/$c^2$.

AstrofísicaNuclear and High Energy PhysicsHeavy neutral lepton kaon meson kaon decay positronPontecorvo–Maki–Nakagawa–Sakata matrixSocio-culturaleFOS: Physical sciencesNA62 experiment7. Clean energy01 natural sciencesNA62High Energy Physics - ExperimentNuclear physicsHigh Energy Physics - Experiment (hep-ex)Positronkaon decays heavy neutral lepton SM extensionsPE2_2Big Bang nucleosynthesisSM extensionskaon physics0103 physical sciences[PHYS.HEXP]Physics [physics]/High Energy Physics - Experiment [hep-ex]010306 general physicsComputingMilieux_MISCELLANEOUSPhysicsRange (particle radiation)Large Hadron Colliderkaon decays010308 nuclear & particles physicshep-exSettore FIS/04Heavy neutral leptonlepton flavour violationFísicalcsh:QC1-999kaon mesonkaon decaykaon physics; lepton flavour violation; NA62positronProduction (computer science)High Energy Physics::Experimentkaonlcsh:PhysicsParticle Physics - ExperimentLepton
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Multiyear search for a diffuse flux of muon neutrinos with AMANDA-II

2007

A search for TeV - PeV muon neutrinos from unresolved sources was performed on AMANDA-II data collected between 2000 and 2003 with an equivalent livetime of 807 days. This diffuse analysis sought to find an extraterrestrial neutrino flux from sources with non-thermal components. The signal is expected to have a harder spectrum than the atmospheric muon and neutrino backgrounds. Since no excess of events was seen in the data over the expected background, an upper limit of E^{2}\Phi_{90% C.L.} < 7.4 x 10^{-8} GeV cm^{-2} s^{-1} sr^{-1} is placed on the diffuse flux of muon neutrinos with a \Phi \propto E^{-2} spectrum in the energy range 16 TeV to 2.5 PeV. This is currently the most sensitive…

Astroparticle physicsPhysicsNuclear and High Energy PhysicsRange (particle radiation)MuonPhysics::Instrumentation and DetectorsAstrophysics::High Energy Astrophysical PhenomenaAstrophysics (astro-ph)High Energy Physics::PhenomenologyFOS: Physical sciencesFluxCosmic rayAstrophysicsAstrophysicsSpectral lineAstronomiaNeutron detectionddc:530High Energy Physics::ExperimentNeutrino
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Limits to the muon flux from neutralino annihilations in the Sun with the AMANDA detector

2005

A search for an excess of muon-neutrinos from neutralino annihilations in the Sun has been performed with the AMANDA-II neutrino detector using data collected in 143.7 days of live-time in 2001. No excess over the expected atmospheric neutrino background has been observed. An upper limit at 90% confidence level has been obtained on the annihilation rate of captured neutralinos in the Sun, as well as the corresponding muon flux limit at the Earth, both as functions of the neutralino mass in the range 100 GeV-5000 GeV.

Astroparticle physicsPhysicsParticle physicsRange (particle radiation)AMANDAMuonPhysics::Instrumentation and DetectorsAstrophysics::High Energy Astrophysical PhenomenaDetectorDark matterHigh Energy Physics::PhenomenologyAstrophysics (astro-ph)NeutralinoFOS: Physical sciencesAstronomy and AstrophysicsAstrophysicsAMANDA; Dark matter; Neutralino; Neutrino telescopesNuclear physicsNeutrino detectorNeutralinoMuon fluxDark matterHigh Energy Physics::ExperimentNeutrino telescopes
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Vibronic structures in the visible luminescence of silica nanoparticles

2014

Time resolved photoluminescence investigation in air and in vacuum atmosphere of the visible luminescence related to silica surface defects is here reported. Two contributions can be singled out: one, observed both in air and in vacuum, is the well-known blue band, peaked around 2.8 eV decaying in ∼5 ns; the other, only observed in vacuum, is a structured emission in the violet range characterized by two vibronic progressions spaced 1370 cm−1 and 360 cm−1 decaying in ∼100 ns. In contrast with previous attribution, the well distinguishable spectroscopic properties together with the observation of the effects induced by the interaction with nitrogen allow to state that the emission bands orig…

AtmosphereSilica nanoparticlesRange (particle radiation)PhotoluminescencechemistrySilica nanoparticles defects phonon-coupling photoluminescencechemistry.chemical_elementNanoparticleAtomic physicsLuminescenceNitrogenBlue bandAIP Conference Proceedings
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Single-particle characterization of ice-nucleating particles and ice particle residuals sampled by three different techniques

2015

Abstract. In the present work, three different techniques to separate ice-nucleating particles (INPs) as well as ice particle residuals (IPRs) from non-ice-active particles are compared. The Ice Selective Inlet (ISI) and the Ice Counterflow Virtual Impactor (Ice-CVI) sample ice particles from mixed-phase clouds and allow after evaporation in the instrument for the analysis of the residuals. The Fast Ice Nucleus Chamber (FINCH) coupled with the Ice Nuclei Pumped Counterflow Virtual Impactor (IN-PCVI) provides ice-activating conditions to aerosol particles and extracts the activated particles for analysis. The instruments were run during a joint field campaign which took place in January and …

Atmospheric Science550aerosoliceEvaporationAnalytical chemistryMineralogycloud covermedicine.disease_causeevaporationlcsh:Chemistrysize distributionmedicineddc:550chemical compositionChemical compositionRange (particle radiation)Chemistryparticle sizeSootlcsh:QC1-999AerosolFast icelcsh:QD1-999Ice nucleusParticlelcsh:Physics
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Chemical analysis of refractory stratospheric aerosol particles collected within the arctic vortex and inside polar stratospheric clouds

2016

Abstract. Stratospheric aerosol particles with diameters larger than about 10 nm were collected within the arctic vortex during two polar flight campaigns: RECONCILE in winter 2010 and ESSenCe in winter 2011. Impactors were installed on board the aircraft M-55 Geophysica, which was operated from Kiruna, Sweden. Flights were performed at a height of up to 21 km and some of the particle samples were taken within distinct polar stratospheric clouds (PSCs). The chemical composition, size and morphology of refractory particles were analyzed by scanning electron microscopy and energy-dispersive X-ray microanalysis. During ESSenCe no refractory particles with diameters above 500 nm were sampled. I…

Atmospheric ScienceRange (particle radiation)010504 meteorology & atmospheric sciencesChemistry010502 geochemistry & geophysicsmedicine.disease_causeAtmospheric sciences01 natural sciencesSootlcsh:QC1-999AerosolMesospherelcsh:Chemistrylcsh:QD1-99913. Climate actionddc:550medicineParticlePolarStratosphereRefractory (planetary science)lcsh:Physics0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Effects of 20–100 nm particles on liquid clouds in the clean summertime Arctic

2016

Abstract. Observations addressing effects of aerosol particles on summertime Arctic clouds are limited. An airborne study, carried out during July 2014 from Resolute Bay, Nunavut, Canada, as part of the Canadian NETCARE project, provides a comprehensive in situ look into some effects of aerosol particles on liquid clouds in the clean environment of the Arctic summer. Median cloud droplet number concentrations (CDNC) from 62 cloud samples are 10 cm−3 for low-altitude cloud (clouds topped below 200 m) and 101 cm−3 for higher-altitude cloud (clouds based above 200 m). The lower activation size of aerosol particles is  ≤  50 nm diameter in about 40 % of the cases. Particles as small as 20 nm ac…

Atmospheric ScienceRange (particle radiation)010504 meteorology & atmospheric sciencesClean environment010502 geochemistry & geophysicsAtmospheric sciences01 natural scienceslcsh:QC1-999The arcticAerosollcsh:ChemistryArcticlcsh:QD1-99913. Climate actionLiquid water contentAerosol cloudClimatologyCloud condensation nucleiEnvironmental sciencelcsh:Physics0105 earth and related environmental sciences
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2017

Abstract. In situ single particle analysis of ice particle residuals (IPRs) and out-of-cloud aerosol particles was conducted by means of laser ablation mass spectrometry during the intensive INUIT-JFJ/CLACE campaign at the high alpine research station Jungfraujoch (3580 m a.s.l.) in January–February 2013. During the 4-week campaign more than 70 000 out-of-cloud aerosol particles and 595 IPRs were analyzed covering a particle size diameter range from 100 nm to 3 µm. The IPRs were sampled during 273 h while the station was covered by mixed-phase clouds at ambient temperatures between −27 and −6 °C. The identification of particle types is based on laboratory studies of different types of biolo…

Atmospheric ScienceRange (particle radiation)010504 meteorology & atmospheric sciencesMeteorology010401 analytical chemistrySingle particle analysisFraction (chemistry)Atmospheric sciencesMass spectrometrycomplex mixtures01 natural sciences0104 chemical sciencesAerosolParticle type13. Climate actionEnvironmental scienceParticleParticle size0105 earth and related environmental sciencesAtmospheric Chemistry and Physics
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Individual-particle analysis of airborne dust samples collected over Morocco in 2006 during SAMUM 1

2011

During the course of SAMUM 1 in May and June 2006, airborne samples were collected in southern Morocco at altitudes between 830 and 3340 m above ground. We analysed approximately 22 500 particles of 1–30 μm by automated individual-particle analysis with a scanning electron microscope (SEM) and an energy-dispersive X-ray (EDX) analyser. The major difference between samples is due to the presence and amount of chlorine- and sulphur-bearing particles, pointing to a varying maritime influence and to different degrees of aging. In contrast, the desert dust component is very homogeneous independent of altitude, activated local source area, and dust storm intensity, implying very fast mixing of th…

Atmospheric ScienceRange (particle radiation)010504 meteorology & atmospheric sciencesScanning electron microscopePalygorskiteMineralogy010501 environmental sciencesMineral dust01 natural sciencesAerosolAltitudeDust stormmedicineParticleEnvironmental science0105 earth and related environmental sciencesmedicine.drugTellus B: Chemical and Physical Meteorology
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Aircraft-based observation of meteoric material in lower-stratospheric aerosol particles between 15 and 68° N

2021

We analyse aerosol particle composition measurements from five research missions between 2014 and 2018 to assess the meridional extent of particles containing meteoric material in the upper troposphere and lower stratosphere (UTLS). Measurements from the Jungfraujoch mountaintop site and a low-altitude aircraft mission show that meteoric material is also present within middle- and lower-tropospheric aerosol but within only a very small proportion of particles. For both the UTLS campaigns and the lower- and mid-troposphere observations, the measurements were conducted with single-particle laser ablation mass spectrometers with bipolar-ion detection, which enabled us to measure the chemical c…

Atmospheric ScienceRange (particle radiation)010504 meteorology & atmospheric sciencesaerosol compositionmeteoric particles010502 geochemistry & geophysicsAtmospheric sciences01 natural scienceslcsh:QC1-999Aerosollcsh:ChemistryTroposphereEarth scienceslcsh:QD1-99913. Climate actionPolar vortexddc:550Environmental sciencePotential temperatureaerosol mass spectrometerTropopauseChemical compositionStratospherelcsh:Physics0105 earth and related environmental sciences
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