Search results for "evaporation"

showing 10 items of 175 documents

Fabrication and characterization of vacuum deposited fluorescein thin films

2011

Simple vacuum evaporation technique for deposition of dyes on various solid surfaces has been developed. The method is compatible with conventional solvent-free nanofabrication processing enabling fabrication of nanoscale optoelectronic devices. Thin films of fluorescein were deposited on glass, fluorine-tin-oxide (FTO) coated glass with and without atomically layer deposited (ALD) nanocrystalline 20 nm thick anatase TiO2 coating. Surface topology, absorption and emission spectra of the films depends on their thickness and the material of supporting substrate. On a smooth glass surface the dye initially formes islands before merging into a uniform layer after 5 to 10 monolayers. On FTO cove…

Absorption spectroscopyta221Analytical chemistryFOS: Physical sciencesSubstrate (electronics)Vacuum evaporationVacuum depositionMesoscale and Nanoscale Physics (cond-mat.mes-hall)Materials ChemistryThin filmta216ta116Surface statesCondensed Matter - Materials ScienceCondensed Matter - Mesoscale and Nanoscale Physicsta114business.industryChemistryMetals and AlloysMaterials Science (cond-mat.mtrl-sci)Surfaces and InterfacesNanocrystalline materialSurfaces Coatings and FilmsElectronic Optical and Magnetic MaterialsOptoelectronicsbusinessLayer (electronics)Thin Solid Films
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Transpiration and Water Use of an Irrigated Traditional Olive Grove with Sap-Flow Observations and the FAO56 Dual Crop Coefficient Approach

2021

The SIMDualKc model was applied to evaluate the crop water use and the crop coefficient (Kc) of an irrigated olive grove (Olea europaea L.) located in Sicily, Italy, using experimental data collected from two crop seasons. The model applies the FAO56 dual Kc approach to compute the actual crop evapotranspiration (ETc act) and its components, i.e., the actual tree transpiration (Tc act), obtained through the basal crop coefficient (Kcb), and soil evaporation according to an evaporation coefficient (Ke). Model calibration was performed by minimizing the difference between the predicted Tc act and the observed daily tree transpiration measured with sap flow instrumentation (TSF field) acquired…

Actual transpiration; Fraction of ground cover; K; cb; from cover fraction and height; Orchard water balance; Sap flow; Soil evaporation; Standard basal crop coefficientStandard basal crop coefficientFraction of ground coverK<sub>cb</sub> from cover fraction and heightGeography Planning and DevelopmentDeficit irrigationAquatic Sciencefrom cover fraction and heightBiochemistryactual transpirationWater balancesap flowSap flowLinear regressionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalisoil evaporationKcb from cover fraction and heightIrrigation managementTD201-500Water Science and TechnologyTranspirationHydrologyActual transpirationWater supply for domestic and industrial purposesIrrigation schedulingActual transpiration Kcb from cover fraction and height soil evaporation Sap flow water balance Standard basal crop coefficientHydraulic engineeringKcbCrop coefficientfraction of ground coverOrchard water balanceEnvironmental sciencestandard basal crop coefficientTC1-978Soil evaporationWater useorchard water balance
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On the Creeping of Saturated Salt Solutions

2013

Creeping is a well-known but annoying phenomenon in the preparation of crystals from solution, where growing crystallites gradually extend up the walls of the growth vessel. In this process, solution is transported toward the tip of the creeping crystallites, where solvent evaporation takes place and solid material is deposited. In this study, the growth of crystal aggregates extending from evaporating droplets of saturated aqueous solutions of ionic salts, placed on different substrate materials, has been investigated using optical microscopy. It is shown that the rate determining step of the crystallization process is the evaporation of solution, following Fick’s laws. Fresh solution, nec…

Aqueous solutionChemistryEvaporationIonic bondingGeneral ChemistrySubstrate (electronics)Solid State ChemistryCondensed Matter Physicslaw.inventionCrystalCrystallographyChemical engineeringOptical microscopelawGeneral Materials ScienceCrystalliteCrystallizationCrystal Growth & Design
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Structural and Vibrational Study of a New Mixed Dipotassium Hydrogenselenate Dihydrogenphosphate K2(HSeO4)1.5 (H2PO4)0.5.

2006

Abstract Ongoing studies of the KHSeO4–KH2PO4 system, aimed at developing novel proton conducting solids, resulted in the new compound K2(HSeO4)1.5(H2PO4)0.5 (dipotassium hydrogenselenate dihydrogenphosphate). The crystals have been prepared by slow evaporation of an aqueous solution at room temperature. The structural properties of the crystals were characterized by X-ray single analysis (performed at room temperature), which revealed that K2(HSeO4)1.5(H2PO4)0.5 (KHSeP) crystallizes in space group P 1 ¯ with lattice parameters: a = 7.417(3) A, b = 7.668(2) A, c = 7.744(5) A, α = 71.59(3)°, β = 87.71(4)° and γ = 86.04(6)°. The compound has a unit cell volume 416.8(3) A3 and two formula unit…

Aqueous solutionProtonHydrogenInfraredHydrogen bondChemistryMechanical EngineeringInorganic chemistryMetals and AlloysEvaporationSpace groupInfrared spectroscopychemistry.chemical_elementGeneral MedicineCrystal structureCrystallographyChemical bondMechanics of MaterialsMaterials ChemistryTetrahedronChemInform
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The Purpose and Age of Underwater Walls in the Bay of Elaia of Western Turkey: A Multidisciplinary Approach

2014

Pergamum (modern: Bergama) was operating an important harbour used by military forces and merchants at the city of Elaia during Hellenistic and Roman Imperial times. Harbour-related facilities such as warehouses, breakwaters and wharfs document the importance of this harbour site not only for the Pergamenians. This paper focuses on the purpose and age of six submerged wall structures situated approximately 1 km south of the ancient closed harbour basin of Elaia. Geoelectric cross-sections and semi-aquatic coring near these walls failed to detect any solid basement under the walls which excludes their possible use as breakwaters or wharfs. Instead, the walls were most likely delineating and …

ArcheologyStructural basinArchaeologyCoringEvaporation pondBasementBreakwaterHarbourEarth and Planetary Sciences (miscellaneous)UnderwatercomputerBayGeologycomputer.programming_languageGeoarchaeology
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Evaporation of Near-Extremal Reissner-Nordström Black Holes

2000

The formation of near-extremal Reissner-Nordstrom black holes in the S-wave approximation can be described, near the event horizon, by an effective solvable model. The corresponding one-loop quantum theory remains solvable and allows to follow analytically the evaporation process which is shown to require an infinite amount of time.

AstrofísicaHigh Energy Physics - TheoryPhysicsEvent horizonMembrane paradigmAstronomyAstronomical PhenomenaEvaporationFOS: Physical sciencesGeneral Physics and AstronomyGeneral Relativity and Quantum Cosmology (gr-qc)Models TheoreticalFuzzballGeneral Relativity and Quantum CosmologyGeneral Relativity and Quantum CosmologyTheoretical physicsHigh Energy Physics - Theory (hep-th)Nonsingular black hole modelsAstronomiaCamps Teoria quàntica deBlack hole thermodynamicsMathematical physicsPhysical Review Letters
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Critical energy flux and mass in solvable theories of 2D dilaton gravity

1998

In this paper we address the issue of determining the semiclassical threshold for black hole formation in the context of a one-parameter family of theories which continuously interpolates between the RST and BPP models. We find that the results depend significantly on the initial static configuration of the spacetime geometry before the influx of matter is turned on. In some cases there is a critical energy density, given by the Hawking rate of evaporation, as well as a critical mass $m_{cr}$ (eventually vanishing). In others there is neither $m_{cr}$ nor a critical flux.

AstrofísicaHigh Energy Physics - TheoryPhysicsGravitacióNuclear and High Energy PhysicsGravity (chemistry)EvaporationFOS: Physical sciencesFluxSemiclassical physicsContext (language use)General Relativity and Quantum Cosmology (gr-qc)General Relativity and Quantum CosmologyGeneral Relativity and Quantum CosmologyHigh Energy Physics - Theory (hep-th)Quantum mechanicsCritical massCritical energyDilatonMathematical physicsPhysical Review D
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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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Lagrangian simulations of stable isotopes in water vapor: An evaluation of nonequilibrium fractionation in the Craig-Gordon model

2009

[1] The Craig-Gordon model is the basis for the parameterization of water isotope fractionation during evaporation from the ocean in many atmospheric isotope models. Its exact formulation (e.g., with respect to the nonequilibrium fractionation factor k) is mainly based on theoretical considerations and not very well constrained by observations. This study addresses this issue by combining a recently developed Lagrangian moisture source analysis with a Craig-Gordon fractionation parameterization for the identified evaporation events in order to model isotope ratios in water vapor. This technique is applied to 45 measurement days of isotopes in water vapor at Rehovot (Israel) during the years…

Atmospheric ScienceEcologyMeteorologyStable isotope ratioEvaporationPaleontologySoil ScienceNon-equilibrium thermodynamicsThermodynamicsForestryAquatic ScienceOceanographyWind speedGeophysicsIsotope fractionationDeuteriumSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Environmental scienceParametrizationPhysics::Atmospheric and Oceanic PhysicsWater vaporEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Air parcel trajectory analysis of stable isotopes in water vapor in the eastern Mediterranean

2008

[1] With the help of a Lagrangian moisture source diagnostic, linkages between stable isotope measurements in water vapor in Rehovot (Israel), with typical sampling times of 8 hours, and the meteorological conditions in the evaporation regions are established. These linkages can be formulated in quantitative terms, and are also quantitatively comparable with other data from isotope measurements over the ocean and with simple theoretical calculations. On the one hand, a strong negative correlation (r = −0.82) between relative humidity with respect to sea surface temperature in the source regions and measured deuterium excess (d) is found, corroborating results from isotope global circulation…

Atmospheric ScienceEcologyMoistureMeteorologyIsotopeStable isotope ratioEvaporationPaleontologySoil ScienceForestryAquatic ScienceOceanographyAtmospheric sciencesSea surface temperatureGeophysicsMediterranean seaSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Environmental scienceRelative humidityWater vaporEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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