Search results for "Names"

showing 10 items of 6843 documents

The role of hydrochlorofluorocarbon densifiers in the formation of clathrate hydrates in deep boreholes and subglacial environments

2007

AbstractClear evidence for the formation of mixed clathrate hydrates of air and hydrochlorofluorocarbon densifier (known as HCFC-141b, sometimes also called R-141b) is found by means of synchrotron X-ray diffraction and Raman spectroscopy on a sample recovered from the bottom of the EPICA Dronning Maud Land deep borehole in Antarctica. Subglacial water (SGW) appears to have reacted with the drilling liquid to build a large lump of clathrate hydrate. The hydrate growth may well have been accelerated by the stirring of the SGW–densifier mixture during drilling. Moreover, dissolved air in the SGW appears to have participated in the formation of mixed hydrates of air and HCFC-141b as evidenced …

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesClathrate hydrateBoreholeDrillingMineralogy02 engineering and technology021001 nanoscience & nanotechnology01 natural sciencesSink (geography)symbols.namesake13. Climate actionsymbols0210 nano-technologyPetrologyRaman spectroscopyHydrateGeology0105 earth and related environmental sciencesEarth-Surface ProcessesAnnals of Glaciology
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Comment on “Effects of different tillage practices on the hydraulic resistance of concentrated flow on the loess plateau in China” by J. Sun et al

2020

Abstract For concentrated flows, which are characterized by small water depth and steep sloping beds, hydraulic conditions different from those typical of streams and rivers occur. In this study a new theoretically deduced flow resistance equation was tested using the experimental data by Sun et al. for three different tilled surfaces (Manual Dibbling, MD, Manual Hoeing, MH, and Contour Drilling, CD). At first, the profile parameter-relationship, which is the relationship between the velocity profile parameter Γ, the channel slope and the flow Froude number, was calibrated using rill flow data by Di Stefano et al. Then, the applicability of this relationship was tested by the measurements o…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesFlow (psychology)Soil science04 agricultural and veterinary sciencesSurface finish01 natural sciencesTillageRillsymbols.namesakeFlow velocity040103 agronomy & agricultureFroude numbersymbolsCalibrationSurface roughness0401 agriculture forestry and fisheriesSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDimensional analysis Flow resistance Self-similarity Soil erosion Velocity profileGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Multiple positive normalized solutions for nonlinear Schrödinger systems

2018

We consider the existence of multiple positive solutions to the nonlinear Schr\"odinger systems sets on $H^1(\mathbb{R}^N) \times H^1(\mathbb{R}^N)$, \[ \left\{ \begin{aligned} -\Delta u_1 &= \lambda_1 u_1 + \mu_1 |u_1|^{p_1 -2}u_1 + \beta r_1 |u_1|^{r_1-2} u_1|u_2|^{r_2}, -\Delta u_2 &= \lambda_2 u_2 + \mu_2 |u_2|^{p_2 -2}u_2 + \beta r_2 |u_1|^{r_1} |u_2|^{r_2 -2} u_2, \end{aligned} \right. \] under the constraint \[ \int_{\mathbb{R}^N}|u_1|^2 \, dx = a_1,\quad \int_{\mathbb{R}^N}|u_2|^2 \, dx = a_2. \] Here $a_1, a_2 >0$ are prescribed, $\mu_1, \mu_2, \beta>0$, and the frequencies $\lambda_1, \lambda_2$ are unknown and will appear as Lagrange multipliers. Two cases are studied, the first …

geographygeography.geographical_feature_categoryApplied Mathematics010102 general mathematicsGeneral Physics and AstronomyStatistical and Nonlinear Physics01 natural sciences010101 applied mathematicsStanding waveSet (abstract data type)Constraint (information theory)Nonlinear systemsymbols.namesakeMathematics - Analysis of PDEsCompact spaceLagrange multipliersymbolsApplied mathematics[MATH.MATH-AP]Mathematics [math]/Analysis of PDEs [math.AP]Mountain pass0101 mathematicsMathematical PhysicsSchrödinger's catComputingMilieux_MISCELLANEOUSMathematics
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The nature of black stains in Lascaux Cave, France, as revealed by surface-enhanced Raman spectroscopy

2011

We used surface-enhanced Raman spectroscopy to investigate the chemical composition of the black stains threatening the rock-art paintings of Lascaux Cave, Montignac, France. The stains are mainly composed of melanin from the fungus Ochroconis sp. and the faecal pellets of the collembolan Folsomia candida. Surface-enhanced Raman spectroscopy is a useful technique for revealing the structure of unknown macromolecules in cultural heritage research. Copyright © 2011 John Wiley & Sons, Ltd.

geographygeography.geographical_feature_categoryChemistryMineralogy02 engineering and technologySurface-enhanced Raman spectroscopy010402 general chemistry021001 nanoscience & nanotechnology01 natural scienceshumanities0104 chemical sciencessymbols.namesakeCaveFolsomia candidaOchroconis sp.Environmental chemistrysymbolsGeneral Materials Science0210 nano-technologyRaman spectroscopySpectroscopyFaecal pelletJournal of Raman Spectroscopy
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Experiments for testing soil texture effects on flow resistance in mobile bed rills

2018

Abstract In this paper a recently theoretically deduced rill flow resistance equation, based on a power-velocity profile, was tested experimentally on plots of varying slopes and soil texture in which mobile bed rills are incised. Measurements of flow velocity, water depth, cross section area, wetted perimeter and bed slope conducted in rill reaches incised on experimental plots, having different slope values (9, 14, 22, 24 and 26%) and soil texture (clay fraction ranging from 42 to 73%), and literature data were used to calibrate the flow resistance equation. In particular, the relationship between the velocity profile parameter Γ, the channel slope, the flow Froude number and texture frac…

geographygeography.geographical_feature_categorySoil textureRill hydraulic0208 environmental biotechnologyFlow (psychology)Soil science02 engineering and technologyPlot measurement020801 environmental engineeringRillWetted perimetersymbols.namesakeVelocity profileFlow resistanceFlow velocitySoil textureSoil waterSoil erosionFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliTexture (crystalline)GeologyEarth-Surface ProcessesCATENA
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A boundary condition for arbitrary shaped inlets in lattice-Boltzmann simulations

2009

We introduce a mass-flux-based inlet boundary condition for the lattice-Boltzmann method. The proposed boundary condition requires minimal amount of boundary data, it produces a steady-state velocity field which is accurate close to the inlet even for arbitrary inlet geometries, and yet it is simple to implement. We demonstrate its capability for both simple and complex inlet geometries by numerical experiments. For simple inlet geometries, we show that the boundary condition provides very accurate inlet velocities when Re less than or similar to 1. Even with moderate Reynolds number, the inlet velocities are accurate for practical purposes. Furthermore, the potential of our boundary condit…

geographygeography.geographical_feature_categorybusiness.industryApplied MathematicsMechanical EngineeringComputational MechanicsLattice Boltzmann methodsReynolds numberGeometryMechanicsComputational fluid dynamicsPhysics::Classical PhysicsInletBoltzmann equationPhysics::GeophysicsComputer Science ApplicationsPhysics::Fluid Dynamicssymbols.namesakeMechanics of MaterialssymbolsVector fieldBoundary value problembusinessLattice model (physics)MathematicsInternational Journal for Numerical Methods in Fluids
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A full‐scale study of Darcy‐Weisbach friction factor for channels vegetated by riparian species

2021

In this article, an open channel flow resistance equation, deduced applying dimensional analysis and incomplete self-similarity condition for the flow velocity distribution, was tested using measurements carried out in a full-scale channel equipped with three types of riparian plants (Salix alba L., Salix caprea L. and Alnus glutinosa L.). In the experimental channel, having banks lined with boulders, the vegetation branches were anchored in a concrete bottom. For each species, the measurements were carried out with plants having different amounts of leaves, different plant density and plant area index. The relationship between the scale factor Γ of the velocity profile and the Froude numbe…

geographygeography.geographical_feature_categoryself-similaritySoil scienceScale factorDarcy–Weisbach equationopen channelOpen-channel flowsymbols.namesakevegetationdimensional analysiVegetation typevelocity profileFroude numbersymbolsmedicineSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalimedicine.symptomflow resistanceVegetation (pathology)ScalingWater Science and TechnologyMathematicsRiparian zoneHydrological Processes
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Comparative tests on different multi-electrode arrays using models in near-surface geophysics

2008

In this paper, the response of different synthetic models to geoelectrical multi-electrode surveys is studied. The models considered are related to two main problems, which are very common in geophysical research regarding hydrogeology and engineering. The first class of models represents buried walls, similar archaeological remains or remains of buried foundations; the other class corresponds to a sea-water intrusion of a fresh water aquifer, which is generally studied in hydrogeophysics. A set of 2D simulations, starting from the synthetic models, was carried out to compare the behaviour of the different arrays when acquiring measurements of electrical resistivity tomography. For each mod…

geographylinear grid dipole–dipole Wenner Wenner–Schlumberger buried wall sea intrusion wedgeHydrogeologygeography.geographical_feature_categoryHydrogeophysicsMineralogyGeologyAquiferManagement Monitoring Policy and LawNear-surface geophysicsIndustrial and Manufacturing EngineeringSynthetic dataSet (abstract data type)symbols.namesakeGeophysicsGaussian noiseSettore GEO/11 - Geofisica ApplicatasymbolsElectrical resistivity tomographyGeologyJournal of Geophysics and Engineering
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Models as Research Tools: Plücker, Klein, and Kummer Surfaces

2018

In the late summer of 1869, 20-year-old Felix Klein made his way to Berlin, where he planned to attend the renowned seminar founded by Ernst Eduard Kummer and Karl Weierstrass. Klein had already taken his doctorate in Bonn and he would soon be recognized as a leading expert on line geometry, a new approach to 3-space launched by his mentor in Bonn, Julius Plucker. Just before Plucker died in 1868, he entrusted Klein to complete the classic monograph, Neue Geometrie des Raumes gegrundet auf die Betrachtung der geraden Linie als Raumelement. Overall responsibility for this project fell to Alfred Clebsch in Gottingen, which was how Klein first came to the prestigious Georgia Augusta. There he …

geographysymbols.namesakegeography.geographical_feature_categoryPhilosophyFellsymbolsArt historyField (mathematics)Kummer surfaceNoether's theoremPluckerLate summer
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Embeddings of graph braid and surface groups in right-angled Artin groups and braid groups

2003

We prove by explicit construction that graph braid groups and most surface groups can be embedded in a natural way in right-angled Artin groups, and we point out some consequences of these embedding results. We also show that every right-angled Artin group can be embedded in a pure surface braid group. On the other hand, by generalising to right-angled Artin groups a result of Lyndon for free groups, we show that the Euler characteristic -1 surface group (given by the relation x^2y^2=z^2) never embeds in a right-angled Artin group.

graph groupBraid group20F36Group Theory (math.GR)Graphright-angled Artin groupCombinatorics20F36 05C25 05C25symbols.namesakeMathematics::Group Theory05C25Euler characteristicFOS: MathematicssymbolsBraidEmbeddingArtin groupGeometry and Topologygraph braid groupMathematics - Group Theoryconfiguration spacecubed complexMathematics
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