Search results for "Metallurgy"

showing 10 items of 1419 documents

The effect of heat treatment on the morphology and mobility of Au nanoparticles

2020

This work was supported by The Centre National de la Recherche Scientifique (CNRS) of France and the French Embassy Program. The authors are also grateful for partial support by COST Action CA15216, the Estonian Science Foundation (grants PUT1689 and PUT1372), the Estonian Centre of Excellence in Zero Energy and Resource Efficient Smart Buildings and Districts, ZEBE, grant 2014-2020.4.01.15.0016 and Latvian Science Council grant lzp-2018/2-0083.

fusionmeltingMaterials scienceAnnealing (metallurgy)General Physics and AstronomyNanoparticle02 engineering and technologylcsh:Chemical technology010402 general chemistrylcsh:Technology01 natural sciencesFull Research PaperLower energyAnnealing:NATURAL SCIENCES:Physics [Research Subject Categories]ManipulationNanotechnologylcsh:TP1-1185atomic force microscopy (AFM)General Materials ScienceKinetic Monte CarloElectrical and Electronic Engineeringlcsh:ScienceFusionlcsh:TAtomic force microscopyNanotribologynanotribologyMeltingDissipation021001 nanoscience & nanotechnologylcsh:QC1-9990104 chemical sciencesNanoscienceChemical engineeringAtomic force microscopy (AFM)microscopie à force atomique (AFM)manipulationNanotribologylcsh:Qannealing[CHIM.OTHE]Chemical Sciences/OtherAu nanoparticles0210 nano-technologynanoparticules d'Aulcsh:PhysicsBeilstein Journal of Nanotechnology
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Positron Studies of Subsurface Zone in Titanium Created in Sliding Wear

2014

Positron annihilation studies of the subsurface zone constituted during dry sliding in pure titanium are reported. A new type of defect depth profile in this zone, which is not an exponential decay usually reported for other metals and alloys, is observed. Two layers in the subsurface zone are present in this metal. In the layer adjacent to the worn surface, the characteristic plateau of the mean positron lifetime that extends to a depth of 60–70 μm was observed. Small vacancy clusters and dislocations were recognized in this layer. At deeper zone, the mean positron lifetime decreased exponentially in the manner typical for the other metals. In this zone, vacancy clusters increase in size a…

geographyMaterials sciencePlateaugeography.geographical_feature_categoryMechanical EngineeringMetallurgychemistry.chemical_elementSurfaces and InterfacesIndentation hardnessSurfaces Coatings and FilmsMetalPositronchemistryMechanics of MaterialsVacancy defectvisual_artvisual_art.visual_art_mediumExponential decayComposite materialLayer (electronics)TitaniumTribology Letters
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Ultraviolet camera measurements of passive and explosive (Strombolian) sulphur dioxide emissions at Yasur volcano, Vanuatu

2020

Here, we present the first ultraviolet (UV) camera measurements of sulphur dioxide (SO2) flux from Yasur volcano, Vanuatu, for the period 6–9 July 2018. These data yield the first direct gas-measurement-derived calculations of explosion gas masses at Yasur. Yasur typically exhibits persistent passive gas release interspersed with frequent Strombolian explosions. We used compact forms of the “PiCam” Raspberry Pi UV camera system [1,2] powered through solar panels to collect images. Our daily median SO2 fluxes ranged from 4 to 5.1 kg s−1, with a measurement uncertainty of −12.2% to +14.7%, including errors from the gas cell calibration drift, uncertainties in plume direction and distance, and…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesExplosive materialultraviolet camerassub-05010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesRemote sensing Strombolian explosions Sulphur dioxide Ultraviolet camerasStrombolian eruptionPlumeStrombolian explosionsremote sensingFlux (metallurgy)VolcanoParticle image velocimetryCalibrationsulphur dioxideGeneral Earth and Planetary SciencesEnvironmental scienceMeasurement uncertaintylcsh:Qlcsh:Science0105 earth and related environmental sciences
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Dynamics of ice mass deformation: Linking processes to rheology, texture, and microstructure

2013

[1] Prediction of glacier and polar ice sheet dynamics is a major challenge, especially in view of changing climate. The flow behavior of an ice mass is fundamentally linked to processes at the grain and subgrain scale. However, our understanding of ice rheology and microstructure evolution based on conventional deformation experiments, where samples are analyzed before and after deformation, remains incomplete. To close this gap, we combine deformation experiments with in situ neutron diffraction textural and grain analysis that allows continuous monitoring of the evolution of rheology, texture, and microstructure. We prepared ice samples from deuterium water, as hydrogen in water ice has …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMineralogyGlacierSlip (materials science)Strain rateNeutron scattering010502 geochemistry & geophysics01 natural sciencesPhysics::GeophysicsGeophysicsRheologyDeformation mechanism13. Climate actionGeochemistry and PetrologyHardening (metallurgy)CrystallitePhysics::Atmospheric and Oceanic PhysicsGeology0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
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First simultaneous mercury and major volatiles characterization of atmospheric hydrothermal emissions at the Pisciarelli's fumarolic system (Campi Fl…

2020

Abstract Hydrothermal systems with active surface expressions are important natural source of atmospheric mercury. Here we report on the first simultaneous assessment of gaseous elemental mercury (GEM) and major volatiles (H2S and CO2) fluxes from the fumarolic system of Pisciarelli, currently the most active at the Campi Flegrei caldera (CFc), Naples (Italy). This was achieved via a GPS-synchronized Lumex and MultiGAS survey which extends similar investigations reported elsewhere. GEM concentrations measured in the fumarolic emissions were consistently above background air level close to the degassing area (mean ~ 8 ± 3 ng m−3 on average) and ranged up to 12,000 ng m−3. Our data evidenced …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMineralogychemistry.chemical_elementAtmospheric dispersion modeling010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationFumarolePlumeMercury (element)GeophysicsFlux (metallurgy)VolcanochemistryGeochemistry and PetrologyCalderaGeology0105 earth and related environmental sciencesJournal of Volcanology and Geothermal Research
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Relationships between diffuse CO 2 emissions and volcanic activity on the island of Vulcano (Aeolian Islands, Italy) during the period 1984-1994

2002

Measurements of CO2 flux from the ground were periodically carried out on the island of Vulcano (Aeolian Islands, Italy) between 1984 and 1994. Three high-flux areas were identified at the foot of the volcanic cone (La Fossa), either inside or very close to the main village. Effect of the choice of the sampling grid was evaluated. A different sampling grid resulted in similar distribution patterns, but with different CO2 fluxes. Therefore, the absolute estimate of the total flux from the investigated area includes a large degree of uncertainty, but repeated measurements with permanent sampling sites are accurate and can detect small changes. No correlation of the flux with atmospheric param…

geographygeography.geographical_feature_categoryAstrophysics::High Energy Astrophysical PhenomenaSoil gasMineralogySampling (statistics)Atmospheric sciencesFumarolePhysics::GeophysicsMediterranean seaFlux (metallurgy)VolcanoGeochemistry and PetrologyAeolian processesVolcanic conePhysics::Atmospheric and Oceanic PhysicsGeologyBulletin of Volcanology
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Emission of bromine and iodine from Mount Etna volcano

2005

[1] Constraining fluxes of volcanic bromine and iodine to the atmosphere is important given the significant role these species play in ozone depletion. However, very few such measurements have been made hitherto, such that global volcanic fluxes are poorly constrained. Here we extend the data set of volcanic Br and I degassing by reporting the first measurements of bromine and iodine emissions from Mount Etna. These data were obtained using filter packs and contemporaneous ultraviolet spectroscopic SO2 flux measurements, resulting in time-averaged emission rates of 0.7 kt yr−1 and 0.01 kt yr−1 for Br and I, respectively, from April to October 2004, from which we estimate global Br and I flu…

geographygeography.geographical_feature_categoryBromineMineralogychemistry.chemical_elementmedicine.disease_causeIodineOzone depletionPlumeAtmosphereGeophysicsFlux (metallurgy)VolcanochemistryGeochemistry and PetrologymedicineGeologyUltravioletGeochemistry, Geophysics, Geosystems
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Multicopter measurements of volcanic gas emissions at Masaya (Nicaragua), Turrialba (Costa Rica) and Stromboli (Italy) volcanoes: Applications for vo…

2017

Abstract. Volcanoes are a natural source of several reactive gases (e.g. sulfur and halogen containing species), as well as non-reactive gases (e.g. carbon dioxide). Besides that, halogen chemistry in volcanic plumes might have important impacts on atmospheric chemistry, carbon to sulfur ratios and sulfur dioxide fluxes are important established parameters to gain information on subsurface processes. In this study we demonstrate the successful deployment of a multirotor UAV (quadcopter) system with custom-made lightweight payloads on board for the compositional analysis and gas flux estimation of volcanic plumes. The various applications and their potential with such new measurement strateg…

geographygeography.geographical_feature_categoryDifferential optical absorption spectroscopyMineralogychemistry.chemical_elementSulfurPlumechemistry.chemical_compoundFlux (metallurgy)VolcanochemistryAtmospheric chemistryGas compositionGeologySulfur dioxide
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First volatile inventory for Gorely volcano, Kamchatka

2012

[1] We report here the very first assessment of volatile flux emissions from Gorely, an actively degassing volcano in Kamchatka. Using a variety of in situ and remote sensing techniques, we determined the bulk plume concentrations of major volatiles (H2O ∼93.5%, CO2, ∼2.6%, SO2 ∼2.2%, HCl 1.1%, HF 0.3%, H20.2%) and trace-halogens (Br, I), therefore estimating a total gas release of ∼11,000 tons·day−1during September 2011, at which time the target was non-eruptively degassing at ∼900°C. Gorely is a typical arc emitter, contributing 0.3% and 1.6% of the total global fluxes from arc volcanism for CO2 and HCl, respectively. We show that Gorely's volcanic gas (H2O/SO2 ∼43, CO2/SO2 ∼1.2, HCl/SO2∼…

geographygeography.geographical_feature_categoryEarth scienceGeochemistryGas releaseVolcanismMantle (geology)PlumeGeophysicsFlux (metallurgy)VolcanoMagmatismGeneral Earth and Planetary SciencesGeologyGeophysical Research Letters
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UV camera measurements of fumarole field degassing (La Fossa crater, Vulcano Island)

2011

Abstract The UV camera is becoming an important new tool in the armory of volcano geochemists to derive high time resolution SO2 flux measurements. Furthermore, the high camera spatial resolution is particularly useful for exploring multiple-source SO2 gas emissions, for instance the composite fumarolic systems topping most quiescent volcanoes. Here, we report on the first SO2 flux measurements from individual fumaroles of the fumarolic field of La Fossa crater (Vulcano Island, Aeolian Island), which we performed using a UV camera in two field campaigns: in November 12, 2009 and February 4, 2010. We derived ~ 0.5 Hz SO2 flux time-series finding fluxes from individual fumaroles, ranging from…

geographygeography.geographical_feature_categoryField (physics)MineralogyFumaroleGeophysicsMediterranean seaFlux (metallurgy)Impact craterVolcanoGeochemistry and PetrologyAeolian processesImage resolutionGeologyJournal of Volcanology and Geothermal Research
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