Search results for "pressure"

showing 10 items of 4493 documents

Aerosol Chemistry Resolved by Mass Spectrometry: Linking Field Measurements of Cloud Condensation Nuclei Activity to Organic Aerosol Composition.

2016

Aerosol hygroscopic properties were linked to its chemical composition by using complementary online mass spectrometric techniques in a comprehensive chemical characterization study at a rural mountaintop station in central Germany in August 2012. In particular, atmospheric pressure chemical ionization mass spectrometry ((-)APCI-MS) provided measurements of organic acids, organosulfates, and nitrooxy-organosulfates in the particle phase at 1 min time resolution. Offline analysis of filter samples enabled us to determine the molecular composition of signals appearing in the online (-)APCI-MS spectra. Aerosol mass spectrometry (AMS) provided quantitative measurements of total submicrometer or…

010504 meteorology & atmospheric sciencesAnalytical chemistryAtmospheric-pressure chemical ionizationGeneral Chemistry010501 environmental sciencesMass spectrometry01 natural sciencesAerosolchemistry.chemical_compoundchemistryEnvironmental ChemistryAerosol mass spectrometryCloud condensation nucleiSulfateChemical compositionMass fraction0105 earth and related environmental sciencesEnvironmental sciencetechnology
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Aerosol Chemistry Resolved by Mass Spectrometry: Insights into Particle Growth after Ambient New Particle Formation

2016

Atmospheric oxidation of volatile organic compounds (VOCs) yields a large number of different organic molecules which comprise a wide range of volatility. Depending on their volatility, they can be involved in new particle formation and particle growth, thus affecting the number concentration of cloud condensation nuclei in the atmosphere. Here, we identified oxidation products of VOCs in the particle phase during a field study at a rural mountaintop station in central Germany. We used atmospheric pressure chemical ionization mass spectrometry ((-)APCI-MS) and aerosol mass spectrometry for time-resolved measurements of organic species and of the total organic aerosol (OA) mass in the size r…

010504 meteorology & atmospheric sciencesChemistryElectrospray ionizationAnalytical chemistryAtmospheric-pressure chemical ionizationGeneral Chemistry010501 environmental sciencesMass spectrometry01 natural sciencesAerosolParticle growthEnvironmental ChemistryCloud condensation nucleiAerosol mass spectrometryVolatility (chemistry)0105 earth and related environmental sciencesEnvironmental Science & Technology
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Modelling and Analysis of Flow Rate and Pressure Head in Pipelines

2019

Currently, various approaches with several utilities are proposed to identify damage in the pipeline. The pipeline system is modeled in the form of a distributed parameter system, such that the state space related to the distributed parameter system contains infinite dimension. In this paper, a novel technique is proposed to analyze and model the flow in the pipeline. Important theorems are proposed for testing the observability as well as controllability of the proposed model.

010504 meteorology & atmospheric sciencesComputer sciencePipeline (computing)05 social sciences01 natural sciencesControllabilityPipeline transportPressure headFlow (mathematics)Distributed parameter systemControl theory0502 economics and businessState spaceObservability050207 economics0105 earth and related environmental sciences2019 16th International Conference on Electrical Engineering, Computing Science and Automatic Control (CCE)
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Bright Hot Impacts by Erupted Fragments Falling Back on the Sun: Magnetic Channelling

2016

Dense plasma fragments were observed to fall back on the solar surface by the Solar Dynamics Observatory after an eruption on 7 June 2011, producing strong EUV brightenings. Previous studies investigated impacts in regions of weak magnetic field. Here we model the $\sim~300$ km/s impact of fragments channelled by the magnetic field close to active regions. In the observations, the magnetic channel brightens before the fragment impact. We use a 3D-MHD model of spherical blobs downfalling in a magnetized atmosphere. The blob parameters are constrained from the observation. We run numerical simulations with different ambient density and magnetic field intensity. We compare the model emission i…

010504 meteorology & atmospheric sciencesField (physics)FOS: Physical sciencesAstrophysics01 natural sciencesAtmosphereSettore FIS/05 - Astronomia E AstrofisicaSun: activity0103 physical sciencesAstrophysics::Solar and Stellar AstrophysicsMagnetic pressureSun: magnetic field010303 astronomy & astrophysicsSolar and Stellar Astrophysics (astro-ph.SR)0105 earth and related environmental sciencesPhysicsSun: coronaAstronomy and AstrophysicsSun: UV radiation Supporting material: animationPlasmaCoronal loopAstronomy and AstrophysicRam pressureMagnetic fieldStarsAstrophysics - Solar and Stellar AstrophysicsSpace and Planetary SciencePhysics::Space Physics
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Chronospeciation of uranium released in soil during a long-term DU shell weathering experiment.

2021

Corrosion process was investigated of depleted uranium (DU) ammunition fragments buried for three years in aerobic soils continuously irrigated with water. The continuing corrosion process was triggered through formation of soluble uranyl oxyhydrate phases such as metaschoepite and becquerelite, which were identified by micro-Raman and X-ray diffraction spectroscopy. The soil was not amended by phosphates and, therefore, no uranyl phosphates were found as corrosion products on the DU surfaces by X-ray photoelectron spectroscopy. A speciation modelling at high temporal sequence (chronospeciation approach) indicated that the abundant Fe oxyhydroxides in the soil immobilized the U(IV) released…

010504 meteorology & atmospheric sciencesHealth Toxicology and Mutagenesischemistry.chemical_elementWeathering010501 environmental sciences01 natural sciencesCorrosionFerrihydritechemistry.chemical_compoundPore water pressureSoilRadiation MonitoringEnvironmental ChemistrySoil Pollutants RadioactiveWaste Management and Disposal0105 earth and related environmental sciencesTotal organic carbonGeneral MedicineUraniumUranylPollutionCorrosionchemistryEnvironmental chemistrySoil waterUraniumJournal of environmental radioactivity
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Persistence of orographic mixed‐phase clouds

2016

Mixed-phase clouds (MPCs) consist of ice crystals and supercooled water droplets at temperatures between 0 and approximately −38°C. They are thermodynamically unstable because the saturation vapor pressure over ice is lower than that over supercooled liquid water. Nevertheless, long-lived MPCs are ubiquitous in the Arctic. Here we show that persistent MPCs are also frequently found in orographic terrain, especially in the Swiss Alps, when the updraft velocities are high enough to exceed saturation with respect to liquid water allowing simultaneous growth of supercooled liquid droplets and ice crystals. Their existence is characterized by holographic measurements of cloud particles obtained …

010504 meteorology & atmospheric sciencesIce crystalsMeteorologyVapor pressure010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesGeophysicsGeneral Earth and Planetary SciencesEnvironmental scienceClimate modelMixed phasePersistence (discontinuity)SupercoolingSaturation (chemistry)0105 earth and related environmental sciencesOrographic liftGeophysical Research Letters
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Magmas near the critical degassing pressure drive volcanic unrest towards a critical state

2016

During the reawaking of a volcano, magmas migrating through the shallow crust have to pass through hydrothermal fluids and rocks. The resulting magma–hydrothermal interactions are still poorly understood, which impairs the ability to interpret volcano monitoring signals and perform hazard assessments. Here we use the results of physical and volatile saturation models to demonstrate that magmatic volatiles released by decompressing magmas at a critical degassing pressure (CDP) can drive volcanic unrest towards a critical state. We show that, at the CDP, the abrupt and voluminous release of H2O-rich magmatic gases can heat hydrothermal fluids and rocks, triggering an accelerating deformation …

010504 meteorology & atmospheric sciencesScienceGeneral Physics and AstronomyPoison control010502 geochemistry & geophysics01 natural sciencesGeneral Biochemistry Genetics and Molecular BiologyHydrothermal circulationArticlePhysics and Astronomy (all)PetrologyVolcanic unrest0105 earth and related environmental sciencesgeographyMultidisciplinarygeography.geographical_feature_categoryBiochemistry Genetics and Molecular Biology (all)QChemistry (all)CrustGeneral ChemistryPhysics and Astronomy (all) Volcano Eruption Unrest Campi FlegreiVolcano13. Climate actionMagmaRock failureGeologyPressure.drive
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Nonlithostatic pressure during subduction and collision and the formation of (ultra)high-pressure rocks

2016

The mechanisms that result in the formation of high-pressure (HP) and ultrahigh-pressure (UHP) rocks are controversial. The usual interpretation assumes that pressure is close to lithostatic, petrological pressure estimates can be transferred to depth, and (U)HP rocks have been exhumed from great depth. An alternative explanation is that pressure can be larger than lithostatic, particularly in continental collision zones, and (U)HP rocks could thus have formed at shallower depths. To better understand the mechanical feasibility of these hypotheses, we performed thermomechanical numerical simulations of a typical subduction and collision scenario. If the subducting crust is laterally homogen…

010504 meteorology & atmospheric sciencesSubductionContinental collisionHomogeneousGeologyCrustGeophysicsUltra high pressure010502 geochemistry & geophysicsCollision01 natural sciencesGeology0105 earth and related environmental sciencesGeology
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The influence of rock heterogeneity on the scaling properties of simulated and natural stylolites

2009

International audience; Stylolites are among the most prominent deformation patterns in sedimentary rocks that document localized pressure solution. Recent studies revealed that stylolite roughness is characterized by two distinct scaling regimes. The main goal of the present study is to decipher whether this complex scaling behavior of stylolites is caused by the composition of the host-rock, i.e. heterogeneities in the material, or is governed by inherent processes on respective scales, namely the transition from a surface energy to an elastic energy dominated regime, as theoretically predicted. For this purpose we have developed a discrete numerical technique, based on a lattice spring m…

010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]CompactionCompaction[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography[SDU.STU]Sciences of the Universe [physics]/Earth SciencesSurface finish010502 geochemistry & geophysics01 natural sciencesScalingPhysics::Geophysics[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeotechnical engineering[PHYS.COND.CM-SM]Physics [physics]/Condensed Matter [cond-mat]/Statistical Mechanics [cond-mat.stat-mech]ScalingComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesQuenched noiseElastic energyGeologyMechanicsRoughnessSurface energyPressure solution13. Climate action[SDU]Sciences of the Universe [physics]StyloliteFinite strain theoryStylolitePressure solutionGeology
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Modelling of stylolite geometries and stress scaling

2012

International audience; In this contribution we present numerical simulations of stylolite growth to decipher the effects of initial rock heterogeneity and stress on their morphology. We show that stylolite growth in a rock with a uniform grain size produces different patterns than stylolite growth in a rock with a bimodal grain size distribution. Strong pinning of large heterogeneities produce stylolite structures that are dominated by pronounced teeth, whereas a uniform grain size leads to spikes and a roughness that shows variable wavelengths. We compare the simulated stylolites with natural examples and show that the model can reproduce the real structures. In addition we show that stro…

010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]stress-gauge[SDE.MCG]Environmental Sciences/Global ChangesCompaction[SDU.STU]Sciences of the Universe [physics]/Earth Sciences[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]Surface finishpressure solution010502 geochemistry & geophysics01 natural sciencesPhysics::Geophysics[PHYS.MECA.MEMA]Physics [physics]/Mechanics [physics]/Mechanics of materials [physics.class-ph]Stress (mechanics)Geochemistry and Petrology[SPI.MECA.MEMA]Engineering Sciences [physics]/Mechanics [physics.med-ph]/Mechanics of materials [physics.class-ph]Earth and Planetary Sciences (miscellaneous)compactionGeotechnical engineeringScaling0105 earth and related environmental sciencesstyloliteMechanicsself-affinityGrain sizeGeophysicsSpace and Planetary ScienceStyloliteParticle-size distributionPressure solutionnumerical modelGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/MineralogyEarth and Planetary Science Letters
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