0000000000349962

AUTHOR

Keijo Mönkkönen

0000-0001-7848-8286

showing 9 related works from this author

Inflaatio ja rakenteiden synty

2016

Kosmologian standardimallina tunnettu LCDM-malli on vakiinnuttanut asemansa parhaana mahdollisena selityksenä viimeaikaisille kosmologisille havainnoille. Ilman ns. inflaatiovaihetta malli törmää kuitenkin varhaista maailmankaikkeutta koskeviin vakaviin ongelmiin. Se ei kykene antamaan selitystä avaruuden laakeudelle, taustasäteilyn tasaisuudelle, raskaiden reliikkihiukkasten puuttumiselle ja taustasäteilyn anisotropioille. Edellä mainittujen ongelmien ratkaisuksi on esitetty kosmologista inflaatiota, jonka mukaan hyvin varhainen maailmankaikkeus on käynyt läpi kehitysvaiheen, jossa sen koko kasvoi lähes eksponentiaalisesti. Tässä pro gradu -tutkielmassa perehdytään lähdeaineiston avulla in…

rakenteiden syntykosmologiakosminen inflaatiokosmologinen häiriöteoria
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The Geodesic Ray Transform on Spherically Symmetric Reversible Finsler Manifolds

2023

We show that the geodesic ray transform is injective on scalar functions on spherically symmetric reversible Finsler manifolds where the Finsler norm satisfies a Herglotz condition. We use angular Fourier series to reduce the injectivity problem to the invertibility of generalized Abel transforms and by Taylor expansions of geodesics we show that these Abel transforms are injective. Our result has applications in linearized boundary rigidity problem on Finsler manifolds and especially in linearized elastic travel time tomography.

Mathematics - Differential Geometryinverse problems44A12 53A99 86A22inversio-ongelmatFunctional Analysis (math.FA)Mathematics - Functional Analysisdifferentiaaligeometriageodesic ray transformDifferential Geometry (math.DG)FOS: MathematicsMathematics::Metric GeometryGeometry and TopologyMathematics::Differential GeometryMathematics::Symplectic Geometryintegral geometry
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Partial Data Problems and Unique Continuation in Scalar and Vector Field Tomography

2022

AbstractWe prove that if P(D) is some constant coefficient partial differential operator and f is a scalar field such that P(D)f vanishes in a given open set, then the integrals of f over all lines intersecting that open set determine the scalar field uniquely everywhere. This is done by proving a unique continuation property of fractional Laplacians which implies uniqueness for the partial data problem. We also apply our results to partial data problems of vector fields.

osittaisdifferentiaaliyhtälötvector field tomographyinverse problemstomografiaApplied MathematicsGeneral MathematicsX-ray tomographyregion of interest tomographyunique continuationinversio-ongelmatAnalysisJournal of Fourier Analysis and Applications
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Unique continuation of the normal operator of the x-ray transform and applications in geophysics

2020

We show that the normal operator of the X-ray transform in $\mathbb{R}^d$, $d\geq 2$, has a unique continuation property in the class of compactly supported distributions. This immediately implies uniqueness for the X-ray tomography problem with partial data and generalizes some earlier results to higher dimensions. Our proof also gives a unique continuation property for certain Riesz potentials in the space of rapidly decreasing distributions. We present applications to local and global seismology. These include linearized travel time tomography with half-local data and global tomography based on shear wave splitting in a weakly anisotropic elastic medium.

FOS: Physical sciencesx-ray transformSpace (mathematics)01 natural sciencesTheoretical Computer SciencePhysics - GeophysicsContinuationtomografiaClassical Analysis and ODEs (math.CA)FOS: MathematicsNormal operatorUniqueness0101 mathematicsAnisotropyMathematical PhysicsMathematicsX-ray transformgeophysicsApplied Mathematics010102 general mathematicsMathematical analysisgeofysiikkaShear wave splittingInverse problemFunctional Analysis (math.FA)Geophysics (physics.geo-ph)Computer Science ApplicationsMathematics - Functional Analysis010101 applied mathematicsMathematics - Classical Analysis and ODEsSignal ProcessingInverse Problems
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X-ray Tomography of One-forms with Partial Data

2021

If the integrals of a one-form over all lines meeting a small open set vanish and the form is closed in this set, then the one-form is exact in the whole Euclidean space. We obtain a unique continuation result for the normal operator of the X-ray transform of one-forms, and this leads to one of our two proofs of the partial data result. Our proofs apply to compactly supported covector-valued distributions.

Mathematics - Differential Geometry46F12 44A12 58A10Open set01 natural sciencesinversio-ongelmatintegraaliyhtälötSet (abstract data type)vector field tomographytomografiaFOS: MathematicsNormal operator0101 mathematicsMathematicsx-ray tomographyinverse problemsEuclidean spaceApplied MathematicsMathematical analysisInverse problemunique continuationnormal operatorFunctional Analysis (math.FA)Mathematics - Functional Analysis010101 applied mathematicsComputational MathematicsDifferential Geometry (math.DG)röntgenkuvausTomographyfunktionaalianalyysiAnalysisSIAM Journal on Mathematical Analysis
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The higher order fractional Calderón problem for linear local operators : Uniqueness

2020

We study an inverse problem for the fractional Schr\"odinger equation (FSE) with a local perturbation by a linear partial differential operator (PDO) of order smaller than the order of the fractional Laplacian. We show that one can uniquely recover the coefficients of the PDO from the Dirichlet-to-Neumann (DN) map associated to the perturbed FSE. This is proved for two classes of coefficients: coefficients which belong to certain spaces of Sobolev multipliers and coefficients which belong to fractional Sobolev spaces with bounded derivatives. Our study generalizes recent results for the zeroth and first order perturbations to higher order perturbations.

osittaisdifferentiaaliyhtälötMathematics - Analysis of PDEsGeneral MathematicsSobolev multipliersFractional Calderón problemMathematics::Spectral Theory35R30 35R11Fractional Schrödinger equationinversio-ongelmat
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Boundary rigidity for Randers metrics

2021

If a non-reversible Finsler norm is the sum of a reversible Finsler norm and a closed 1-form, then one can uniquely recover the 1-form up to potential fields from the boundary distance data. We also show a boundary rigidity result for Randers metrics where the reversible Finsler norm is induced by a Riemannian metric which is boundary rigid. Our theorems generalize Riemannian boundary rigidity results to some non-reversible Finsler manifolds. We provide an application to seismology where the seismic wave propagates in a moving medium.

Mathematics - Differential GeometryInverse problemsboundary rigidityMathematical analysisBoundary (topology)Rigidity (psychology)ArticlesInverse problemtravel time tomography53C24 53A35 86A22Seismic waveDifferential Geometry (math.DG)Norm (mathematics)Metric (mathematics)FOS: MathematicsMathematics::Metric GeometryMathematics::Differential GeometryMathematics::Symplectic GeometryMathematicsAnnales Fennici Mathematici
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Unique continuation property and Poincar�� inequality for higher order fractional Laplacians with applications in inverse problems

2020

We prove a unique continuation property for the fractional Laplacian $(-\Delta)^s$ when $s \in (-n/2,\infty)\setminus \mathbb{Z}$. In addition, we study Poincar\'e-type inequalities for the operator $(-\Delta)^s$ when $s\geq 0$. We apply the results to show that one can uniquely recover, up to a gauge, electric and magnetic potentials from the Dirichlet-to-Neumann map associated to the higher order fractional magnetic Schr\"odinger equation. We also study the higher order fractional Schr\"odinger equation with singular electric potential. In both cases, we obtain a Runge approximation property for the equation. Furthermore, we prove a uniqueness result for a partial data problem of the $d$-…

Pure mathematicsControl and Optimizationfractional Schrödinger equationApproximation propertyPoincaré inequalityRadon transform.01 natural sciencesinversio-ongelmatSchrödinger equationsymbols.namesakefractional Poincaré inequalityOperator (computer programming)Mathematics - Analysis of PDEsFOS: MathematicsDiscrete Mathematics and CombinatoricsUniquenesskvanttimekaniikka0101 mathematicsepäyhtälötMathematicsosittaisdifferentiaaliyhtälötPlane (geometry)inverse problemsComputer Science::Information Retrieval010102 general mathematicsOrder (ring theory)Gauge (firearms)Mathematics::Spectral Theoryunique continuationFunctional Analysis (math.FA)010101 applied mathematicsMathematics - Functional AnalysisModeling and Simulationsymbolsfractional LaplacianAnalysis35R30 46F12 44A12Analysis of PDEs (math.AP)
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Kinemaattinen inversio-ongelma pallosymmetrisellä monistolla

2017

Tutkielman pääaiheena on maanjäristysaaltoihin ja Maan sisärakenteen tutkimiseen liittyvä käänteinen kinemaattinen ongelma. Maapalloa mallinnetaan kolmiulotteisella kompaktilla reunallisella monistolla \(\bar{B}^3(0, R)\), jonka säde normitetaan ykköseksi \(R=1\). Aaltorintamat kulkevat pitkin geodeeseja, jotka sijaitsevat kokonaan avoimessa pallossa \(B^3(0, 1)\) lukuun ottamatta päätepisteitä, jotka ovat reunalla \(S^2(0, 1)\). Symmetrioiden nojalla tarkastelu voidaan siirtää tasoon \(\mathbb{R}^2\), jossa riittää tutkia kiekon \(\bar{B}^2(0, 1)\) geodeeseja. Äänennopeus \(v=v(r)\) oletetaan isotrooppiseksi ja aidosti positiiviseksi \(C^{1,1}([0, 1])\)-funktioksi, jolle \(v^{\prime}(0)=0\…

riemannin geometriageometriainversio-ongelmatseismologia
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