Search results for "water vapor"

showing 10 items of 179 documents

An ultrathin suspended hydrophobic porous membrane for high-efficiency water desalination

2017

Abstract An ultrathin highly fluorinated porous membrane was designed for a large production of desalted water at very low energy consumption. Imprinting water droplets were used through a low thermally conductive tetra-fluoroethylene (TFE)/2,2,4-trifluoro-5-tri-fluorometoxy-1,3-dioxol (TIT) (HYFLON AD 60) solution and the generated porous nanofilm was suspended onto a polyethersulfone (PES) honeycomb texture. The very tiny fluorinated thickness together with a large number of small-shaped pores provided the membrane for enhanced anti-wetting surface properties, extremely reduced resistance to water vapor transfer and outstanding thermal efficiency. Fine materials structure-transport relati…

Thermal efficiencyMaterials scienceMembrane distillation; Nanostructured membrane; PES honeycomb texture; Porous HYFLON AD nanofilm; Thermal efficiency; Water desalinationMembrane distillation02 engineering and technologySuper-hydrophobic interface010402 general chemistryMembrane distillation01 natural sciencesSettore CHIM/04 - Chimica IndustrialeWater desalinationhoneycombPorous membranePES honeycomb textureGeneral Materials SciencePorosityWater desalinationElectrical conductorKeywordChromatographyNanostructured membranePorous HYFLON AD nanofilmNanofilm021001 nanoscience & nanotechnology0104 chemical sciencesMembraneChemical engineeringnanostructured membranesHYFLON AD0210 nano-technologyWater vaporThermal efficiency
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Finite Size Scaling Tools for the Study of Interfacial Phenomena and Wetting

2019

In this chapter, we use the word “interface” in the sense of a boundary between coexisting bulk phases (in thermal equilibrium). An example is the interface between liquid (e.g. water) and gas phases (water vapor) but also interfaces between fluid and solid phases (e.g. water and ice) can be considered, as well as interfaces between coexisting solid phases. The generic example are “domain walls” in magnets, separating domains with opposite orientation of the magnetization, a case that can already be studied in the framework of the simple Ising model (Chaps. 2 and 3) where one has spins on the sites of a rigid perfect lattice pointing up or down.

Thermal equilibriumMagnetizationMaterials scienceCondensed matter physicsSpinsLattice (order)Ising modelWettingScalingWater vapor
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Water vapor effect on high-temperature oxidation behavior of Fe3Al intermetallics

2009

Fe3Al intermetallics (Fe3Al, Fe3Al-Zr, Fe3Al-Zr,Mo and Fe3Al-Zr, Mo, Nb) were oxidized at 950 °C in dry and humid (11 vol% water) synthetic air. Thermogravimetric measurements showed that the oxidation rates of the tested intermetallics were lower in humid air than in dry air (especially for Fe3Al-Zr, Mo and Fe3Al-Zr, Mo, Nb). The addition of small amounts of Zr, Mo or Nb improved the kinetics compared with that of the undoped Fe3Al. Fe3Al showed massive spallation, whereas Fe3Al-Zr, Fe3Al-Zr, Mo and Fe3Al-Zr, Mo, Nb produced a flat, adherent oxide layer. The rapid transformation of transient alumina into alpha alumina may explain the decrease in the oxidation rate in humid air.

Thermogravimetric analysisMaterials scienceMetallurgyKineticsOxideAnalytical chemistryIntermetallicchemistry.chemical_compoundchemistryGeneral Materials ScienceSpallationLayer (electronics)Water vaporOxidation rateScience and Technology of Advanced Materials
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The pattern of radiative heating and cooling in the troposphere and lower stratosphere

1956

For any meteorological effects of radiation, only those constituents of the air which have a very strong absorption in the infra-red are involved; these are water vapour and carbon dioxide. Several methods have been developed (Mügge & Möller 1932 a, b ; Elsasser 1942; Yamamoto 1952) for computing the radiation flux, and numerous calculations of these fluxes and of the cooling rates have been performed in the last 25 years (Ludwig 1935; Kortiim 1939; Thompson & Neiburger 1955). The results are summarized in figure 1, which shows the distribution of the tem­perature and of the cooling rate by water vapour in some characteristic atmospheres. The lower levels of the tropical atmosphere…

TroposphereAtmosphereRadiation fluxGeneral EnergyPrecipitable waterChemistryClimatologyMiddle latitudesAtmospheric sciencesStratosphereWater vaporLatitudeProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences
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2015

In 2011, the MOZAIC (Measurement of Ozone by AIRBUS In-Service Aircraft) successor programme IAGOS (In-service Aircraft for a Global Observing System) started to equip their long-haul passenger aircraft with the modified capacitive hygrometer Vaisala HUMICAP ® of type H. The assurance of the data quality and the consistency of the data set during the transition from MOZAIC Capacitive Hygrometers to IAGOS Capacitive Hygrometers were evaluated within the CIRRUS-III and AIRTOSS-ICE field studies. During these performance tests, the capacitive hygrometers were operated aboard a Learjet 35A aircraft together with a closed-cell Lyman-α fluorescence hygrometer, an open-path tunable diode laser (TD…

TroposphereAtmospheric ScienceField (physics)HygrometerMeteorologyChemistryQuality assessmentCapacitive sensingRelative humidityStratosphereWater vaporRemote sensingTellus B
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The Influence of Trace Substances on the Atmospheric Energy Budget

1979

ABSTRACT The most effective absorbers of solar radiation in the system earth-atmosphere are the earth's surface layer, the atmospheric water vapor, ozone and oxygen. In the troposphere water vapor is dominant, in the lower stratosphere ozone. The absorption contribution due to carbon dioxide may be neglected in both regions of the atmosphere. The contribution of aerosol particles is significant only close to the earth's surface. Here the absorption by aerosol particles equals the effect by water vapor. This fact and the following properties of aerosol particles motivate a special treatment. Particles absorb; particles scatter and elongate the optical path of solar radiation through the abso…

TroposphereEarth's energy budgetAtmosphereChemistryParticleAstrophysics::Earth and Planetary AstrophysicsAlbedoAtmospheric sciencesStratospherePhysics::Atmospheric and Oceanic PhysicsWater vaporAerosol
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Low-temperature atomic layer deposition of SiO2/Al2O3 multilayer structures constructed on self-standing films of cellulose nanofibrils

2018

In this paper, we have optimized a low-temperature atomic layer deposition (ALD) of SiO 2 using AP-LTO® 330 and ozone (O 3 ) as precursors, and demonstrated its suitability to surface-modify temperature-sensitive bio-based films of cellulose nanofibrils (CNFs). The lowest temperature for the thermal ALD process was 80°C when the silicon precursor residence time was increased by the stop-flow mode. The SiO 2 film deposition rate was dependent on the temperature varying within 1.5–2.2 Å cycle −1 in the temperature range of 80–350°C, respectively. The low-temperature SiO 2 process that resulted was combined with the conventional trimethyl aluminium + H 2 O process in order to prepare thin mul…

Water sensitivityMaterials scienceDiffusion barrierSiliconGeneral Mathematicsta221General Physics and Astronomychemistry.chemical_element02 engineering and technology01 natural sciencesOxygenAtomic layer depositionchemistry.chemical_compoundnanorakenteetHybrid multilayersSiO0103 physical sciencesCelluloseta216diffusion barrierta218low-temperature atomic layer depositionDiffusion barrierLow-temperature atomic layer deposition010302 applied physicsta214ta114water sensitivityta111General Engineeringcellulose nanofibrilsAtmospheric temperature range021001 nanoscience & nanotechnologyhybrid multilayerschemistryChemical engineeringCellulose nanofibrilsohutkalvotSiO20210 nano-technologyLayer (electronics)Water vaporPhilosophical Transactions of the Royal Society A : Mathematical Physical and Engineering Sciences
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Atmospheric correction for land surface temperature using NOAA-11 AVHRR channels 4 and 5

1991

Abstract In this work, a theoretical model that permits relating the land surface temperature with the temperatures measured by thermal infrared sensors has been developed. The model has been derived by linearization of Planck's function and atmospheric trasmittance. In this way a split-window equation is obtained, which depends on atmospheric water vapor, viewing angle, and channel surface emissivities. Simulations of satellite measurements of land surface temperatures are made using the atmospheric transmittance-radiance model LOWTRAN-7 for NOAA-11 AVHRR Channels 4 and 5. From these simulations the accuracies of linearizations have been checked. The dependence of the split-window coeffici…

Work (thermodynamics)Atmospheric correctionSoil ScienceGeologyViewing angleAtmosphereSea surface temperatureEmissivityEnvironmental scienceSatelliteComputers in Earth SciencesPhysics::Atmospheric and Oceanic PhysicsWater vaporRemote sensingRemote Sensing of Environment
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Airborne observations of far-infrared upwelling radiance in the Arctic

2016

Abstract. The first airborne measurements of the Far-InfraRed Radiometer (FIRR) were performed in April 2015 during the panarctic NETCARE campaign. Vertical profiles of spectral upwelling radiance in the range 8–50 μm were measured in clear and cloudy conditions from the surface up to 6 km. The clear-sky profiles highlight the strong dependence of radiative fluxes to the temperature inversion typical of the Arctic. Measurements acquired for total column water vapor from 1.5 to 10.5 mm also underline the sensitivity of the far-infrared greenhouse effect to specific humidity. The cloudy cases show that optically thin ice clouds increase the cooling rate of the atmosphere by a factor up to thr…

[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]Atmospheric ScienceRadiometer010504 meteorology & atmospheric sciencesmedia_common.quotation_subjectAtmospheric sciences01 natural scienceslcsh:QC1-999lcsh:Chemistry010309 opticsAtmospherelcsh:QD1-999Arctic13. Climate actionSky0103 physical sciencesRadianceRadiative transferEnvironmental scienceRadiometrylcsh:PhysicsWater vapor0105 earth and related environmental sciencesmedia_commonRemote sensingAtmospheric Chemistry and Physics
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Convective hydration in the tropical tropopause layer during the StratoClim aircraft campaign: pathway of an observed hydration patch

2018

The source and pathway of the hydration patch in the TTL (tropical tropopause layer) that was measured during the Stratospheric and upper tropospheric processes for better climate predictions (StratoClim) field campaign during the Asian summer monsoon in 2017 and its connection to convective overshoots are investigated. During flight no. 7, two remarkable layers are measured in the TTL, namely (1) the moist layer (ML) with a water vapour content of 4.8–5.7 ppmv in altitudes of 18–19 km in the lower stratosphere and (2) the ice layer (IL) with ice content up to 1.9 eq. ppmv (equivalent parts per million by volume) in altitudes of 17–18 km in the upper tropo…

[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph][SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereAtmospheric ScienceTurbulent diffusion010504 meteorology & atmospheric sciencesCloud top0208 environmental biotechnology02 engineering and technologyAtmospheric sciences01 natural scienceslcsh:QC1-999020801 environmental engineeringTropospherelcsh:ChemistryDeposition (aerosol physics)lcsh:QD1-99913. Climate actionIce nucleusEnvironmental scienceStratosphereWater vaporAir masslcsh:Physics0105 earth and related environmental sciences
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