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  • 1
    Keywords: Differential equations, Partial. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (441 pages)
    Edition: 1st ed.
    ISBN: 9781483181363
    Language: English
    Note: Front Cover -- Partial Differential Equations of Mathematical Physics -- Copyright Page -- Table of Contents -- TRANSLATON EDITOR'S PREFACE -- AUTHOR'S PREFACES TO THE FIRST AND THIRD EDITIONS -- LECTURE 1. DERTVATON OF THE FUNDAMENTAL EQUATONS -- 1. Ostrogradski's Formula -- 2. Equation for Vibrations of a String -- 3. Equation for Vibrations of a Membrane -- 4. Equation of Continuity for Motion of a Fluid. Laplace's Equation -- 5. Equation of Heat Conduction -- 6. Sound Waves -- LECTURE 2. THE FORMULATION OF PROBLEMS OF MATHEMATICAL PHYSICS HADAMARD'S EXAMPLE -- 1. Initial Conditions and Boundary Conditions -- 2. The Dependence of the Solution on the Boundary Conditions. Hadamard's Example -- LECTURE 3. THE CLASSIFICATION OF LINEAR EQUATIONS OF THE SECOND ORDER -- 1. Linear Equations and Quadratic Forms. Canonical Form of an Equation -- 2. Canonical Form of Equations in Two Independent Variables -- 3. Second Canonical Form of Hyperbolic Equations in Two Independent Variables -- 4. Characteristics -- LECTURE 4. THE EQUATION FOR A VIBRATING STRING AND ITS SOLUTION BY D'ALEMBERT'S METHOD -- 1. D'Alembert's Formula. Infinite String -- 2. String with Two Fixed Ends -- 3. Solution of the Problem for a Non-Homogeneous Equation and for More General Boundary Conditions -- LECTURE 5. RIEMANN'S METHOD -- 1. The Boundary-Value Problem of the First Kind for Hyperbolic Equations -- 2. Adjoint Differential Operators -- 3. Riemann's Method -- 4. Riemann's Function for the Adjoint Equation -- 5. Some Qualitative Consequences of Riemann's Formula -- LECTURE 6. MULTIPLE INTEGRALS: LEBESGUE INTEGRATION -- 1. Closed and Open Sets of Points -- 2. Integrals of Continuous Functions on Open Sets -- 3. Integrals of Continuous Functions on Bounded Closed Sets -- 4. Summable Functions. , 5. The Indefinite Integral of a Function of One Variable. Examples -- 6. Measurable Sets. Egorov's Theorem -- 7. Convergence in the Mean of Summable Functions -- 8. The Lebesgue-Fubini Theorem -- LECTURE 7. INTEGRALS DEPENDENT ON A PARAMETER -- 1. Integrals which are Uniformly Convergent for a Given Value of Parameter -- 2. The Derivative of an Improper Integral with respect to a Parameter -- LECTURE 8. THE EQUATION OF HEAT CONDUCTION -- 1. Principal Solution -- 2. The Solution of Cauchy's Problem -- LECTURE 9. LAPLACE'S EQUATION AND POISSON'S EQUATION -- 1. The Theorem of the Maximum -- 2. The Principal Solution. Green's Formula -- 3. The Potential due to a Volume, to a Single Layer, and to a Double Layer -- LECTURE 10. SOME GENERAL CONSEQUENCES OF GREEN'S FORMULA -- 1. The Mean-Value Theorem for a Harmonic Function -- 2. Behaviour of a Harmonic Function near a Singular Point -- 3. Behaviour of a Harmonic Function at Infinity. Inverse Points -- LECTURE 11. POISSON'S EQUATION IN AN UNBOUNDED MEDIUM. NEWTONIAN POTENTIAL -- LECTURE 12. THE SOLUTION OF THE DIRICHLET PROBLEM FOR A SPHERE -- LECTURE 13. THE DIRICHLET PROBLEM AND THE NEUMANN PROBLEM FOR A HALF-SPACE -- LECTURE 14. THE WAVE EQUATION AND THE RETARDED POTENTIAL -- 1. The Characteristics of the Wave Equation -- 2. Kirchhoff's Method of Solution of Cauchy's Problem -- LECTURE 15. PROPERTIES OF THE POTENTIALS OF SINGLE AND DOUBLE LAYERS -- 1. General Remarks -- 2. Properties of the Potential of a Double Layer -- 3. Properties of the Potential of a Single Layer -- 4. Regular Normal Derivative -- 5. Normal Derivative of the Potential of a Double Layer -- 6. Behaviour of the Potentials at Infinity -- LECTURE 16. REDUCTION OF THE DIRICHLET PROBLEM AND THE NEUMANN PROBLEM TO INTEGRAL EQUATIONS. , 1. Formulation of the Problems and the Uniqueness of their Solutions -- 2. The Integral Equations for the Formulated Problems -- LECTURE 17. LAPLACE'S EQUATON AND POISSON'S EQUATION IN A PLANE -- 1. The Principal Solution -- 2. The Basic Problems -- 3. The Logarithmic Potential -- LECTURE 18. THE THEORY OF INTEGRAL EQUATIONS -- 1. General Remarks -- 2. The Method of Successive Approximations -- 3. Volterra Equations -- 4. Equations with Degenerate Kernel -- 5. A Kernel of Special Type. Fredhohn's Theorems -- 6. Generalization of the Results -- 7. Equations with Unbounded Kernels of a Special Form -- LECTURE 19. APPLICATION OF THE THEORY OF FREDHOLM EQUATIONS TO THE SOLUTION OF THE DIRICHLET AND NEUMANN PROBLEMS -- 1. Derivation of the Properties of Integral Equations -- 2. Investigation of the Equations -- LECTURE 20. GREEN'S FUNCTION -- 1. The Difíerential Operator with One Independent Variable -- 2. Adjoint Operators and Adjoint Families -- 3. The Fundamental Lemma on the Integrals of Adjoint Equations -- 4. The Influence Function -- 5. Definition and Construction of Green's Function -- 6. The Generalized Green's Function for a Linear Second-Order Equation -- 7. Examples -- LECTURE 21. GREEN'S FUNCTION FOR THE LAPLACE OPERATOR -- 1. Green's Function for the Dirichlet Problem -- 2. The Concept of Green's Function for the Neumann Problem -- LECTURE 22. CORRECTNESS OF FORMULATION OF THE BOUNDARY-VALUE PROBLEMS OF MATHEMATICAL PHYSICS -- 1. The Equation of Heat Conduction -- 2. The Concept of the Generalized Solution -- 3. The Wave Equation -- 4. The Generalized Solution of the Wave Equation -- 5. A Property of Generalized Solutions of Homogeneous Equations -- 6. Bunyakovski's Inequality and Minkovski's Inequality -- 7. The Riesz-Fischer Theorem -- LECTURE 23. FOURIER'S METHOD. , 1. Separation of the Variables -- 2. The Analogy between the Problems of Vibrations of a Continuous Medium and Vibrations of Mechanical Systems with a Finite Number of Degrees of Freedom -- 3. The Inhomogeneous Equation -- 4. Longitudinal Vibrations of a Bar -- LECTURE 24. INTEGRAL EQUATONS WTIH REAL, SYMMETRIC KERNELS -- 1. Elementary Properties. Completely Continuous Operators -- 2. Proof of the Existence of an Eigenvalue -- LECTURE 25. THE BILINEAR FORMULA AND THE HILBERT-SCHMIDT THEOREM -- 1. The Bilinear Formula -- 2. The Hilbert-Schmidt Theorem -- 3. Proof of the Fourier Method for the Solution of the Boundary-Value Problems of Mathematical Physics -- 4. An Application of the Theory of Integral Equations with Symmetric Kernel -- LECTURE 26. THE INHOMOGENEOUS INTEGRAL EQUATION WTTH A SYMMETRIC KERNEL -- 1. Expansion of the Resolvent -- 2. Representation of the Solution by means of Analytical Functions -- LECTURE 27. VIBRATIONS OF A RECTANGULAR PARALLELEPIPED -- LECTURE 28. LAPLACE'S EQUATON IN CURVILINEAR COORDINATES. EXAMPLES OF THE USE OF FOURIER'S METHOD -- 1. Laplace's Equation in Curvilinear Coordinates -- 2. Bessel Functions -- 3. Complete Separation of the Variables in the Equation V2u= O in Polar Coordinates -- LECTURE 29. HARMONIC POLYNOMIALS AND SPHERICAL FUNCTIONS -- 1. Definition of Spherical Functions -- 2. Approximation by means of Spherical Harmonics -- 3. The Dirichlet Problem for a Sphere -- 4. The Differential Equations for Spherical Functions -- LECTURE 30. SOME ELEMENTARY PROPERTIES OF SPHERICAL FUNCTIONS -- 1. Legendre Polynomials -- 2. The Generating Function -- 3. Laplace's Formula -- INDEX -- OTHER VOLUMES IN THIS SERIES.
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  • 2
    Publication Date: 2020-02-12
    Description: The data are the numerical modeling results to investigate plume-induced subduction initation on which the figures of the paper "Plume-induced subduction initiation: single- or multi-slab subduction?" by Baes, Sobolev, Gerya and Brune are based. Detailed description on how they are obtained is given in that article (Baes et al., 2020). The naming of the files is based on the number of figures in the paper. Each zipped file contains input files (init.t3c and mode.t3c) and output files (*.vtr).
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 3
    Publication Date: 2020-07-10
    Description: This data publication is supplementary material to the paper " Subduction initiation by plume-plateau interaction: Insights from numerical models" (Baes et al., 2020). In this study, using 3-d numerical models, we explore the effect of relative distance of plume head and plateau edge, age of the lithosphere and strength of the lower crust on plume-induced subduction initiation. We use I3ELVIS code which solves the momentum, continuity and energy equations based on a staggered finite difference scheme combined with a marker-in-cell technique (Gerya, 2010; Gerya et al., 2015; Baes et al., 2016). Our numerical results show four different responses (shown in Figures 2-5 in the paper of Baes et al, 2020) that are: (a) oceanic trench formation, (b) circular plateau-oceanic trench formation, (c) plateau trench formation and (d) no trench formation. The results of models in which plume head is far away from the plateau edge are compatible with the outcomes of models with uniform lithospheres. The current data set contains the figures of five models representing five different deformation regimes (shown in Fig. 7 in the paper), which result from interaction of a plume with a homogenous lithosphere. Note that in all figures the upper panels show the logarithm of viscosity within the lithosphere. The middle and lower panels illustrate compositional field of a 2d cross-section cutting through center of model and surface topography, respectively. The color bars of temperature field and surface topography are shown at the top of the figure and colour code of compositional field is at bottom of the figure.
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 4
    Publication Date: 2023-01-19
    Description: The Central Andes (~21°S) is a subduction-type orogeny formed in the last ~50 Ma from the subduction of the Nazca oceanic plate beneath the South American continental plate. However, the most important phases of deformation occur in the last 20 Ma. Pulses of shortening have led to the sudden growth of the by the Altiplano-Puna plateau. Previous studies have provided insights on the importance of various mechanisms on the overall shortening such as the weakening of the overriding plate from crustal eclogitization and delamination, or the importance of a relatively high friction at the subduction interface, and weak sediments in foreland. However none of them has addressed the mechanism behind these shortening pulses yet. Therefore, we built a series of high resolution 2D visco-plastic subduction models using the ASPECT geodynamic code, in which the oceanic plate is buoyancy-driven and the velocity of the continent is prescribed. We have also implemented a realistic geometry for the south American plate at ~30 Ma. We propose a new plausible mechanism (buckling and steepening of the slab) as the cause of these pulses. The buckling leads to the blockage of the trench. Consequently, the difference of velocity between the South American plate and the trench is accommodated by shortening. The data presented here includes the parameters files, for the reference model (S1) and the following alternative simulations: models with variation of the friction at the subduction interface (S2a-c), a model without eclogitization of the lower crust (S3) and a model with higher thermal conductivity of the upper crust (S4). Additionally, this publication includes the initial composition and thermal state of the lithosphere used for the models and a Readme file that gives all the instructions to run them.
    Language: English
    Type: info:eu-repo/semantics/workingPaper
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  • 5
    Publication Date: 2023-12-18
    Description: In the southern Central Andes (~32°S), subduction of the Nazca oceanic plate beneath the South American continental plate becomes horizontal. The growth of the Altiplano-Puna Plateau is covalently related to the southward migration of the flat subduction, but the role of subduction geometry and the plate strength on current and long-term deformation of the Andes remains poorly explored. This study takes a data-driven approach of integrating the previous structural and thermal model of the lithosphere of the southern central Andes into a 3D geodynamic model to explore the different parameters contributing to the localization of deformation. We simulate visco-plastic deformation using the geodynamic code ASPECT. The repository includes parameter files and input files for the reference model (S1) and the following alternative simulations: a series of models with variation in friction at the subduction interface (S2a-d), a series of models with variation in sedimentary strength (S3a-d), a series that studies the effect of topography (S4), and a series that studies the effect of plate velocities. In addition, a readme file gives all the instructions to run them.
    Type: info:eu-repo/semantics/workingPaper
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