Search results for "Dynamics"

showing 10 items of 9782 documents

Esa's SMOS Mission – Supporting Agricultural Applications

2018

The European Space Agency's (ESA) SMOS mission, in orbit since more than 8 years, carries a passive microwave interferometric radiometer measuring in L-Band and provides accurate global observations of emitted radiation originating from the Earth's surfaces since the atmosphere is almost transparent in this spectral range. In addition, over land the effect of vegetation on the measurements is smaller than for shorter wavelengths. The scientific objectives of the SMOS mission directly respond to the need for global observations of soil moisture and ocean salinity, two key variables used in predictive hydrological, oceanographic and atmospheric models. SMOS observations also provide informati…

geographygeography.geographical_feature_categoryAtmospheric modelsVegetationSnowPhysics::GeophysicsAtmosphereBrightness temperatureOrbit (dynamics)Sea iceEnvironmental scienceAstrophysics::Earth and Planetary AstrophysicsPhysics::Atmospheric and Oceanic PhysicsInterferometric radiometerRemote sensingIGARSS 2018 - 2018 IEEE International Geoscience and Remote Sensing Symposium
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On the Rifting Dynamics of Plate Divergence and Magma Accumulation at Oceanic Ridge Axes

1995

Rifting dynamics at spreading axes is governed by two processes: the large-scale plate divergence and the local magma accumulation in the crust-mantle transition layer. Both evolve simultaneously. A model is developed particularly for the situation in Iceland where a well studied rifting episode occurred in the Krafla volcanic system 1975–1984. Both the divergence and the buoyant rise of magma create tensile deviatoric stress in the axial region, but while divergence generates an altogether extensional stress field, uprising of buoyant melt produces tension only near the axis but compression of the sides. The buoyant rise is driven by the differential pressure gradient in rock and melt. The…

geographygeography.geographical_feature_categoryBuoyancyMid-ocean ridgeCrustGeophysicsGeodynamicsengineering.materialMantle (geology)Stress (mechanics)Stress fieldStress relaxationengineeringPetrologyGeology
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Clastic injection dynamics during ice front oscillations: A case example from Sólheimajökull (Iceland).

2015

18 pages; International audience; Soft-sediment deformation structures are being increasingly used as a tool for reconstructing palaeoenvironments and porewater pressure conditions in glacial settings. However, the potential of hydrofractures and clastic injections in the reconstruction of ice dynamics remains poorly constrained. This paper presents the results of a detailed study of a clastic injection network outcropping in the Sólheimajökull forefield (South Iceland). Sedimentological descriptions are combined with microscopic to macroscopic analyses of clastic injection geometries, sediment-fills, and cross-cutting relationships. The 250 m long and 20 m high exposure observed along the …

geographygeography.geographical_feature_categoryDeformation (mechanics)OutcropStratigraphyFront (oceanography)Iceland[ SDU.STU.GL ] Sciences of the Universe [physics]/Earth Sciences/GlaciologyGeologyOverburden pressure[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyPalaeo-ice dynamicsGlacial sedimentologySillClastic rockMicromorphologyClastic injectionsGlacial periodHydrofracturePetrologyGeomorphologyGeologyHolocene
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CO 2 output and δ 13 C(CO 2 ) from Mount Etna as indicators of degassing of shallow asthenosphere

1997

An estimated average CO2 output from Etna's summit craters in the range of 13±3 Mt/a has recently been determined from the measured SO2 output and measured CO2/SO2 molar ratios. To this amount the CO2 output emitted diffusely from the soil (≈ 1 Mt/a) and the amount of CO2 dissolved in Etna's aquifers (≈ 0.25 Mt/a) must be added. Data on the solubility of CO2 in Etnean magmas at high temperature and pressure allow the volume of magma involved in the release of such an amount of this gas to be estimated. This volume of magma (≈ 0.7 km3/a) is approximately 20 times greater than the volume of magma erupted annually during the period 1971–1995. On the basis of C-isotopic data of CO2 collected in…

geographygeography.geographical_feature_categoryStable isotope ratioMineralogyAquiferchemistry.chemical_compoundImpact craterVolume (thermodynamics)VolcanochemistryGeochemistry and PetrologyAsthenosphereMagmaCarbon dioxideGeologyBulletin of Volcanology
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Hinterland-Verging Thrusting in the Northern Sicily Continental Margin: Evidences for a Late Collisional Stage of the Sicilian Fold and Thrust Belt?

2018

The Sicilian Fold and Thrust Belt developed during Neogene-Quaternary times characterized by main African-wards tectonic transport direction. Recent investigations highlighted extensive hinterland-verging tectonic structures active during late Pliocene-Pleistocene time suggesting a late collisional stage of the Sicilian Fold and Thrust Belt that could be a precursor of a change in the subduction polarity in the central belt of Mediterranean.

geographygeography.geographical_feature_categorySubductionPolarity (physics)Central beltlanguage.human_languageBackthrusting Subduction polarity Sicilian Fold and Thrust Belt Central Mediterranean geodynamicsPaleontologyTectonicsContinental marginStage (stratigraphy)Fold and thrust beltlanguageSicilianGeology
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Chapter 16 Pre-eruptive vapour and its role in controlling eruption style and longevity at Soufrière Hills Volcano

2014

We use volatiles in melt inclusions and nominally anhydrous phenocrysts, with volcanic gas flux and composition, and textural analysis of mafic inclusions to estimate the mass of exsolved vapour prior to eruption at Soufriere Hills Volcano (SHV). Pre-eruptive andesite coexists with exsolved vapour comprising 1.6–2.4 wt% of the bulk magma. The water content of orthopyroxenes indicates a zone of magma storage at pressures of approximately 200–300 MPa, whereas melt inclusions have equilibrated at shallower pressures. Inclusions containing >3 wt% H2O are enriched in CO2, suggesting flushing with CO2-rich gases. Intruding mafic magma contains >8 wt% H2O at 200–300 MPa. Rapid quenching is accompa…

geographygeography.geographical_feature_categoryVolcanoVolume (thermodynamics)AndesiteMagmaGeochemistryNucleationPhenocrystGeologyMaficGeologyMelt inclusionsGeological Society, London, Memoirs
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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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Translocation of Cations During Sorption of Copper in the System Solution - Algae (Spirogyra sp.)/Translokacja Kationów Podczas Procesu Sorpcji Miedz…

2014

Zbadano kinetykę procesu sorpcji kationów miedzi w glonach Spirogyra sp. oraz towarzyszące mu procesy sorpcji kationów wodorowych i procesy uwalniania do roztworu kationów związanych w glonach: Na+, Mg2+, K+ i Ca2+. Stwierdzono, że w układzie statycznym, przy stałym stosunku masy glonów do objętości roztworu, procesy te zachodzą równocześnie, przy czym należy przypuszczać, że ilość uwalnianych soli ma wpływ na parametry heterofazowej równowagi wymiany jonowej. W warunkach prowadzenia eksperymentu ilość uwolnionych kationów była blisko 10-krotnie większa niż ilość kationów sorbowanych. Porównano parametry równowagi wyznaczone z modelu reakcji pseudo-drugiego rzędu z parametrami uzyskanymi po…

glonyalgaeEnvironmental EngineeringOrder of reactionIon exchangebiologyHydrogenChemistryInorganic chemistryKineticskationy miedzichemistry.chemical_elementSorptioncopper cationsbiology.organism_classificationCopperrównowaga wymiany jonowejVolume (thermodynamics)AlgaeEnvironmental Chemistryion exchange equilibriumbiosorpcjabiosorptionEcological Chemistry and Engineering S
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Diffractive Processes at Next-to-Leading Order in the Dipole Picture

2023

Diffraktiiviset prosessit ovat korkean energian rajalla sensitiivisiä kohdehiukkasen gluonijakaumalle, mistä johtuen niiden avulla voidaan tutkia kohdetta kvanttiväridynamiikan epälineaarisessa alueessa. Näiden epälineaaristen ilmiöiden odotetaan johtavan gluonisaturaatioon, jota voidaan kuvata luontevasti värilasikondensaatiksi kutsutun efektiivisen kenttäteorian avulla. Vaikka saatavilla olevassa kokeellisessa datassa onkin vahvoja viitteitä gluonisaturaatiosta, yksiselitteistä merkkiä saturaatiosta ei ole havaittu. Tämän vuoksi on tärkeää parantaa saturaatiolle sensitiivisten prosessien teoreettista ymmärrystä, jotta pystytään löytämään selkeitä eroja kvanttiväridynamiikan lineaarisen ja…

gluonitquantum chromodynamicsscattering (physics)elementary particleskvanttiväridynamiikkasirontaparticle physicshiukkasfysiikkagluonsalkeishiukkaset
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HSV-1 Glycoprotein D and Its Surface Receptors: Evaluation of Protein–Protein Interaction and Targeting by Triazole-Based Compounds through In Silico…

2023

Protein–protein interactions (PPI) represent attractive targets for drug design. Thus, aiming at a deeper insight into the HSV-1 envelope glycoprotein D (gD), protein–protein docking and dynamic simulations of gD-HVEM and gD-Nectin-1 complexes were performed. The most stable complexes and the pivotal key residues useful for gD to anchor human receptors were identified and used as starting points for a structure-based virtual screening on a library of both synthetic and designed 1,2,3-triazole-based compounds. Their binding properties versus gD interface with HVEM and Nectin-1 along with their structure-activity relationships (SARs) were evaluated. Four [1,2,3]triazolo[4,5-b]pyridines were i…

glycoprotein DOrganic Chemistrymolecular dynamics simulationsGeneral MedicineHSV-1Settore CHIM/08 - Chimica FarmaceuticaCatalysisComputer Science ApplicationsInorganic Chemistryprotein–protein interactionprotein–protein interaction; HSV-1; 123-triazoles; docking; molecular dynamics simulations; glycoprotein Ddocking123-triazolesPhysical and Theoretical ChemistryMolecular BiologySpectroscopyInternational Journal of Molecular Sciences
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