Search results for "Instability"

showing 10 items of 724 documents

Application of modulated calorimetry to the Liquid metals using electromagnetic levitation and static magnetic field

2018

Measurement of the thermophysical properties of liquid metals is challenging because of their high chemical activity and high temperatures. The electromagnetic levitation allows one to hold the electrically conductive liquid sample containerless in an inert atmosphere in thermal equilibrium while measurements on the sample can be taken in a non-contact way followed by extraction of some thermophysical properties. Yet, the electromagnetic forces within the skin layer inside the sample cause convective flow of the liquid thus disabling the data extraction. A static magnetic field imposed over a sample is known to damp the convective flow. With these ideas, an experimental set-up with a DC mag…

Thermal equilibriumMaterials scienceCalorimetryMechanicsMagnetostatics01 natural sciencesInstability010305 fluids & plasmasMagnetic fieldPhysics::Fluid Dynamics010309 optics[SPI]Engineering Sciences [physics]0103 physical sciencesPerpendicularInert gasMagnetic levitationComputingMilieux_MISCELLANEOUS
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Gis-analysis to assess landslide susceptibility in a fluvial basin of NW Sicily (Italy).

2008

Abstract Landslide hazard assessment, effected by means of geostatistical methods, is based on the analysis of the relationships between landslides and the spatial distributions of some instability factors. Frequently such analyses are based on landslide inventories in which each record represents the entire unstable area and is managed as a single instability landform. In this research, landslide susceptibility is evaluated through the study of a variety of instability landforms: landslides, scarps and areas uphill from crown . The instability factors selected were: bedrock lithology, steepness, topographic wetness index and stream power index. The instability landform densities computed f…

Topographic Wetness Indexgeographygeography.geographical_feature_categoryLandformTopographic attributeLandslide classificationBedrockSettore GEO/04 - Geografia Fisica E GeomorfologiaGIS-analysiFluvialLandslideInstability landformLandslide susceptibilitySlope stabilityGeomorphologySicilySettore GEO/05 - Geologia ApplicataGeologyStream powerEarth-Surface Processes
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A Teaching Experience: Aeroelasticity and the Finite Element Method

2015

[EN] The aeroelastic modelling of aircraft structures is a fundamental area for the students of Aerospace Engineering Degree. This subject has a strongly multidisciplinary character and involves other several subjects like mechanics, vibrations, aerodynamics, structural analysis. Consequently, the students find stimulating the challenge of merging their knowledge at different areas. In this paper, a teaching experience on the solution of the aeroelastic problem of a 3D-wing through six different computer tasks is presented. The main objective is to attempt a relatively complex problem using a simple version of the Finite Element Method with only four degrees of freedom. The students begin c…

TorsionEngineeringFinite element methodBendingMechanical engineeringAerodinámicalcsh:Education (General)DivergencevibrationsAerodynamicsMultidisciplinary approachCalculusAeroelasticitywingVibracionesDivergenciabusiness.industryAlaAerodynamicsFlutterAeroelasticityFinite element methodFlameoFlutter instabilityVibrationFlexiónbusinesslcsh:L7-991AeroelasticidadMétodo elementos finitosTorsión
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Transverse instability of periodic and generalized solitary waves for a fifth-order KP model

2017

We consider a fifth-order Kadomtsev-Petviashvili equation which arises as a two-dimensional model in the classical water-wave problem. This equation possesses a family of generalized line solitary waves which decay exponentially to periodic waves at infinity. We prove that these solitary waves are transversely spectrally unstable and that this instability is induced by the transverse instability of the periodic tails. We rely upon a detailed spectral analysis of some suitably chosen linear operators.

Transverse instabilitymedia_common.quotation_subjectFOS: Physical sciences35Q53 (Primary) 76B15 76B25 35B35 35P15 (Secondary)Pattern Formation and Solitons (nlin.PS)01 natural sciencesInstabilityMathematics - Analysis of PDEsgeneralized solitary wavesdispersive equationsFOS: Mathematics[MATH.MATH-AP]Mathematics [math]/Analysis of PDEs [math.AP]Spectral analysistransverse stability0101 mathematicsperiodic wavesNonlinear Sciences::Pattern Formation and SolitonsMathematical Physicsmedia_commonPhysicsApplied Mathematics010102 general mathematicsMathematical analysisOrder (ring theory)Mathematical Physics (math-ph)InfinityNonlinear Sciences - Pattern Formation and Solitons010101 applied mathematicsClassical mechanicsNonlinear Sciences::Exactly Solvable and Integrable SystemsLine (geometry)Mechanical waveAnalysisLongitudinal waveAnalysis of PDEs (math.AP)
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Boundary-layer Flows Past an Hemispherical Roughness Element: DNS, Global Stability and Sensitivity Analysis

2015

Abstract We investigate the full three-dimensional instability mechanism arising in the wake of an hemispherical roughness element immersed in a laminar Blasius boundary layer. The inherent three-dimensional flow pattern beyond the critical Reynolds number is characterized by coherent vortical structures called hairpin vortices. Direct numerical simulation is used to analyze the formation and the shedding of hairpin packets inside the shear layer. The first bifurcation characteristics are investigated by global stability tools. We show the spatial structure of the linear direct and adjoint global eigenmodes of the linearized Navier-Stokes operator and use structural sensitivity analysis to …

TriGlobal Linear StabilityDirect numerical simulation02 engineering and technologyWake01 natural sciencesInstability010305 fluids & plasmasPhysics::Fluid Dynamicssymbols.namesake0203 mechanical engineeringHairpin vortices0103 physical sciencesPhysics020301 aerospace & aeronauticsRoughness ElementHairpin vortices; Roughness Element; TriGlobal Linear Stability; Mechanical EngineeringMechanical EngineeringReynolds numberLaminar flowGeneral MedicineMechanicsVortexBoundary layerClassical mechanicsBlasius boundary layersymbolsProcedia IUTAM
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Type II Odontoid Fracture: a case series highlighting the treatment strategies

2019

Background: A type II odontoid fracture, if unstable, can cause spinal cord damage. In this case, it is essential to choose the correct treatment—but the issues of what the correct treatment is and which of the different surgical options is best are quite controversial. In this paper we present strategies for treatment of type II odontoid fracture. Materials and Methods: Thirty consecutive cases of type II odontoid fracture were treated at the Division of Neurosurgery at Villa Sofia Hospital in Palermo (23 cases) and at the Neurosurgical Clinic, University Hospital of Palermo (seven cases), from January 2011 to August 2016. Four patients were treated with external immobilization. Twenty-six…

Type II odontoid fracturemedicine.medical_specialtyC1–C2 instabilitySettore MED/27 - Neurochirurgiabusiness.industryBone ScrewExternal FixatorSpinal cord030218 nuclear medicine & medical imagingSurgeryFracture Fixation InternalOdontoid Proce03 medical and health sciences0302 clinical medicinemedicine.anatomical_structureC1–C2 articular screwFracture FixationmedicineSpinal FracturesTreatment strategybusinessOdontoid screw030217 neurology & neurosurgeryHumanOdontoid fracture
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Growth and geomorphic evolution of the Ustica volcanic complex at the Africa-Europe plate margin (Tyrrhenian Sea)

2021

18 pages, 13 figures, 1 table

Tyrrhenian SeaSettore GEO/02 - Geologia Stratigrafica E Sedimentologica010504 meteorology & atmospheric sciencesLavaPyroclastic rockSeamountsMass wastingEscarpmentFault (geology)Geo-hazard010502 geochemistry & geophysics01 natural sciencesUstica IslandPaleontologyContinental marginSlope instabilityActive tectonics Geo-hazard Seamounts Slope instability Submarine geomorphology Tyrrhenian Sea Ustica IslandActive tectonics; Geo-hazard; Seamounts; Slope instability; Submarine geomorphology; Tyrrhenian Sea; Ustica Island0105 earth and related environmental sciencesEarth-Surface ProcessesgeographySubmarine geomorphologygeography.geographical_feature_categoryActive tectonicsTectonicsVolcanoGeology
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Thymidylate synthase polymorphism and microsatellite instability: association in colorectal cancer.

2005

5-Fluorouracil (5FU) is the main drug used for the treatment of colorectal cancer (CRC) and Thymidilate Synthase (TS) is its target enzyme. TS gene has regulatory tandemly repeated sequences in its 5'' and 3''untraslated region (5''-3'' UTR). CRC often shows a kind of genomic instability called Microsatellite Instability (MSI) that is associated with TS levels and survival. Our data show that the genotype 2R/2R (homozygosity for 2 tandem repeat sequences in the 5''UTR) is more frequently associated with MSI+ and lower TS levels. More over we did not find any significant association between the 2R/3R (heterozygosity for 2 and 3 tandem repeat sequences in the 5''UTR) and 3R/3R (homozygosity f…

Untranslated regionGenome instabilityHeterozygoteGenotypeTranscription GeneticColorectal cancerBiologyBiochemistryThymidylate synthaseLoss of heterozygosityCell Line TumorGenotypeGeneticsmedicineHumansRNA MessengerneoplasmsGeneGeneticsPolymorphism GeneticChemistryMicrosatellite instabilityHeterozygote advantageGeneral MedicineThymidylate Synthasemedicine.diseaseMolecular biologydigestive system diseasesPhenotypeDrug Resistance NeoplasmProtein Biosynthesisbiology.proteinMolecular MedicineColorectal NeoplasmsMicrosatellite RepeatsNucleosides, nucleotidesnucleic acids
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Linear instability of mixed convection of cold water in a porous layer induced by viscous dissipation

2009

Accepted version of an article published in the journal: International Journal of Thermal Sciences, Elsevier Published version available on Science Direct: http://dx.doi.org/10.1016/j.ijthermalsci.2008.06.012 An analysis of linear stability of the stationary laminar Darcy flow in a horizontal porous layer is performed. The porous layer is saturated with cold water. The upper plane boundary is assumed to be subject to heat transfer with finite conductance to an environment at the temperature of maximum density of cold water. The lower plane boundary is adiabatic. Convective instabilities are caused by flow viscous dissipation, inducing a basic temperature distribution that decreases in the u…

VDP::Mathematics and natural science: 400::Mathematics: 410::Applied mathematics: 413Materials scienceDarcy's lawLINEAR STABILITYGeneral EngineeringThermodynamicsLaminar flowCondensed Matter PhysicsInstabilityVISCOUS DISSIPATIONVDP::Mathematics and natural science: 400::Physics: 430Physics::Fluid DynamicsDARCY LAWPOROUS MEDIUMCombined forced and natural convectionHeat transferThermalPorous mediumBUOYANT FLOWLinear stability
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Stability of Flow with Viscous Dissipation in a Horizontal Porous Layer with an Open Boundary Having a Prescribed Temperature Gradient

2010

Published version of an article in the journal: Transport in Porous Media. The original publication is available at www.springerlink.com, http://dx.doi.org/10.1007/s11242-010-9588-6 A buoyancy-induced stationary flow with viscous dissipation in a horizontal porous layer is investigated. The lower boundary surface is impermeable and subject to a uniform heat flux. The upper open boundary has a prescribed, linearly varying, temperature distribution. The buoyancy-induced basic velocity profile is parallel and non-uniform. The linear stability of this basic solution is analysed numerically by solving the disturbance equations for oblique rolls arbitrarily oriented with respect to the basic velo…

VDP::Mathematics and natural science: 400::Mathematics: 410::Applied mathematics: 413PhysicsBuoyancyOPEN BOUNDARYGeneral Chemical EngineeringBoundary (topology)MechanicsRayleigh numberPOROUS LAYERengineering.materialCritical valueVISCOUS DISSIPATIONInstabilityCatalysisTHERMAL INSTABILITYPhysics::Fluid DynamicsTemperature gradientClassical mechanicsHeat fluxPRESCRIBED TEMPERATURE GRADIENTengineeringVDP::Technology: 500::Materials science and engineering: 520Linear stabilityTransport in Porous Media
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