Search results for " Boundary"

showing 10 items of 686 documents

Mobility, interdiffusion, and tracer diffusion in lattice-gas models of two-component alloys

1989

The transport properties of lattice-gas models of alloys with two particle species are studied. The numbers of the particles and vacancies are conserved, and the two particle species have different exchange rates with the vacancies. The mobility and interdiffusion is described by the linear Onsager theory of transport. The Onsager coefficients are estimated from numerical simulations of the mobilities. A recently proposed relation between the Onsager coefficients of the random-alloy model is verified. The interdiffusion of the two species is directly monitored in the simulations; it is well described by the estimated Onsager coefficients. The results on interdiffusion are compared with simu…

Condensed Matter::Soft Condensed MatterCondensed Matter::Materials ScienceMaterials scienceLattice (order)TRACERGrain boundary diffusion coefficientEffective diffusion coefficientInverseThermodynamicsComputer Science::OtherPhysical Review B
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Heterogeneous nucleation at a wall near a wetting transition: a Monte Carlo test of the classical theory

2009

While for a slightly supersaturated vapor the free energy barrier ΔF(hom)(*), which needs to be overcome in a homogeneous nucleation event, may be extremely large, nucleation is typically much easier at the walls of the container in which the vapor is located. While no nucleation barrier exists if the walls are wet, for incomplete wetting of the walls, described via a nonzero contact angle Θ, classical theory predicts that nucleation happens through sphere-cap-shaped droplets attracted to the wall, and their formation energy is ΔF(het)(*) = ΔF(hom)(*)f(Θ), with f(Θ) = (1-cosΘ)(2)(2+cosΘ)/4. This prediction is tested through simulations for the simple cubic lattice gas model with nearest-nei…

Condensed matter physicsChemistryEvaporationNucleationThermodynamicsCondensed Matter PhysicsPhysics::Fluid DynamicsContact angleWetting transitionPhenomenological modelPeriodic boundary conditionsGeneral Materials ScienceIsing modelWettingJournal of Physics: Condensed Matter
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A symmetric nonlocal damage theory

2003

The paper presents a thermodynamically consistent formulation for nonlocal damage models. Nonlocal models have been recognized as a theoretically clean and computationally efficient approach to overcome the shortcomings arising in continuum media with softening. The main features of the presented formulation are: (i) relations derived by the free energy potential fully complying with nonlocal thermodynamic principles; (ii) nonlocal integral operator which is self-adjoint at every point of the solid, including zones near to the solid's boundary; (iii) capacity of regularizing the softening ill-posed continuum problem, restoring a meaningful nonlocal boundary value problem. In the present app…

Continuum (measurement)Applied MathematicsMechanical EngineeringMathematical analysisNonlocal boundaryTangentLocalization limiterCondensed Matter PhysicsNonlocal damageAssociative damageModuliQuantum nonlocalityMechanics of MaterialsModeling and SimulationThermodynamicsGeneral Materials ScienceTangent stiffness matrixSettore ICAR/08 - Scienza Delle CostruzioniSofteningAssociative propertyMathematicsInternational Journal of Solids and Structures
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A Parametric Dirichlet Problem for Systems of Quasilinear Elliptic Equations With Gradient Dependence

2016

The aim of this article is to study the Dirichlet boundary value problem for systems of equations involving the (pi, qi) -Laplacian operators and parameters μi≥0 (i = 1,2) in the principal part. Another main point is that the nonlinearities in the reaction terms are allowed to depend on both the solution and its gradient. We prove results ensuring existence, uniqueness, and asymptotic behavior with respect to the parameters.

Control and Optimization01 natural sciencesElliptic boundary value problemsymbols.namesakeDirichlet eigenvalueSettore MAT/05 - Analisi MatematicaDirichlet's principleBoundary value problemparametric problem0101 mathematicssystem of elliptic equationsMathematicsDirichlet problemDirichlet problem010102 general mathematicsMathematical analysisDirichlet's energyMathematics::Spectral Theory(pq)-LaplacianComputer Science Applications010101 applied mathematicsGeneralized Dirichlet distributionDirichlet boundary conditionSignal ProcessingsymbolsAnalysis
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Infinitely many solutions for a perturbed p-Laplacian boundary value problem with impulsive effects

2017

In this paper, we deal with the existence of weak solutions for a perturbed p-Laplacian boundary value problem with impulsive effects. More precisely, the existence of an exactly determined open interval of positive parameters for which the problem admits infinitely many weak solutions is established. Our proofs are based on variational methods.

Control and OptimizationApplied MathematicsPerturbed p-Laplacian boundary value problemCritical point theory; Impulsive effects; Infinitely many solutions; Perturbed p-Laplacian boundary value problem; Variational methods; Analysis; Geometry and Topology; Control and Optimization; Applied MathematicsVariational methodAnalysiImpulsive effectsInfinitely many solutionsImpulsive effectVariational methodsCritical point theoryInfinitely many solutionGeometry and TopologyAnalysis
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Probabilistic interpretation of the Calderón problem

2017

In this paper, we use the theory of symmetric Dirichlet forms to give a probabilistic interpretation of Calderon's inverse conductivity problem in terms of reflecting diffusion processes and their corresponding boundary trace processes. This probabilistic interpretation comes in three equivalent formulations which open up novel perspectives on the classical question of unique determinability of conductivities from boundary data. We aim to make this work accessible to both readers with a background in stochastic process theory as well as researchers working on deterministic methods in inverse problems.

Control and OptimizationStochastic processComputer science010102 general mathematicsProbabilistic logicBoundary (topology)Inverse problem01 natural sciencesDirichlet distributionInterpretation (model theory)010104 statistics & probabilitysymbols.namesakeModeling and SimulationNeumann boundary conditionsymbolsDiscrete Mathematics and CombinatoricsApplied mathematics0101 mathematicsAnalysisTRACE (psycholinguistics)Inverse Problems & Imaging
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Initiation of deep convection at marginal instability in an ensemble of mesoscale models: a case-study from COPS

2011

The present study investigates the initiation of precipitating deep convection in an ensemble of convection-resolving mesoscale models. Results of eight different model runs from five non-hydrostatic models are compared for a case of the Convective and Orographically-induced Precipitation Study (COPS). An isolated convective cell initiated east of the Black Forest crest in southwest Germany, although convective available potential energy was only moderate and convective inhibition was high. Measurements revealed that, due to the absence of synoptic forcing, convection was initiated by local processes related to the orography. In particular, the lifting by low-level convergence in the planet…

Convection021110 strategic defence & security studiesAtmospheric ScienceConvective inhibition010504 meteorology & atmospheric sciencesMeteorologyPlanetary boundary layer0211 other engineering and technologiesMesoscale meteorologyOrography02 engineering and technologyForcing (mathematics)01 natural sciencesConvective available potential energyFree convective layerPhysics::Fluid Dynamics13. Climate actionClimatologyPhysics::Atmospheric and Oceanic PhysicsGeology0105 earth and related environmental sciencesQuarterly Journal of the Royal Meteorological Society
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Uncertainties in future climate predictions due to convection parameterisations

2013

Abstract. In the last decades several convection parameterisations have been developed to consider the impact of small-scale unresolved processes in Earth System Models associated with convective clouds. Global model simulations, which have been performed under current climate conditions with different convection schemes, significantly differ among each other in the simulated transport of trace gases and precipitation patterns due to the parameterisation assumptions and formulations, e.g. the computation of convective rainfall rates, calculation of entrainment and detrainment rates etc. Here we address sensitivity studies comparing four different convection schemes under alternative climate…

ConvectionCloud forcingAtmospheric SciencePlanetary boundary layerEntrainment (meteorology)Atmospheric sciencesFree convective layerlcsh:QC1-999Tropospherelcsh:Chemistrylcsh:QD1-999ClimatologyEnvironmental sciencePrecipitationStratospherelcsh:PhysicsAtmospheric Chemistry and Physics
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Variable exponent p(x)-Kirchhoff type problem with convection

2022

Abstract We study a nonlinear p ( x ) -Kirchhoff type problem with Dirichlet boundary condition, in the case of a reaction term depending also on the gradient (convection). Using a topological approach based on the Galerkin method, we discuss the existence of two notions of solutions: strong generalized solution and weak solution. Strengthening the bound on the Kirchhoff type term (positivity condition), we establish existence of weak solution, this time using the theory of operators of monotone type.

ConvectionKirchhoff type termApplied MathematicsWeak solutionMathematical analysisWeak solutionGeneralized solutionType (model theory)ConvectionTerm (time)Pseudomonotone operatorNonlinear systemsymbols.namesakeMonotone polygonGalerkin basisSettore MAT/05 - Analisi MatematicaDirichlet boundary conditionsymbolsGalerkin methodAnalysisMathematics
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Multiple solutions with sign information for semilinear Neumann problems with convection

2019

We consider a semilinear Neumann problem with convection. We assume that the drift coefficient is indefinite. Using the theory of nonlinear operators of monotone type, together with truncation and comparison techniques and flow invariance arguments, we prove a multiplicity theorem producing three nontrivial smooth solutions (positive, negative and nodal).

ConvectionTruncationGeneral Mathematics010102 general mathematicsMathematical analysisMultiplicity (mathematics)Type (model theory)Convection01 natural sciencesIndefinite drift coefficientExtremal constant sign solution010101 applied mathematicsMonotone polygonFlow (mathematics)Settore MAT/05 - Analisi MatematicaConstant sign and nodal solutionNeumann boundary conditionFlow invariance0101 mathematicsSign (mathematics)MathematicsRevista Matemática Complutense
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