Calculus of Variations: the Direct Approach
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Mathematics 412 Partial Differential Equations
Mathematics 412 Partial Differential Equations c S. A. Fulling Fall, 2005 The Wave Equation This introductory example will have three parts.* 1. I will show how a particular, simple partial differential equation (PDE) arises in a physical problem. 2. We’ll look at its solutions, which happen to be unusually easy to find in this case. 3. We’ll solve the equation again by separation of variables, the central theme of this course, and see how Fourier series arise. The wave equation in two variables (one space, one time) is ∂2u ∂2u = c2 , ∂t2 ∂x2 where c is a constant, which turns out to be the speed of the waves described by the equation. Most textbooks derive the wave equation for a vibrating string (e.g., Haber- man, Chap. 4). It arises in many other contexts — for example, light waves (the electromagnetic field). For variety, I shall look at the case of sound waves (motion in a gas). Sound waves Reference: Feynman Lectures in Physics, Vol. 1, Chap. 47. We assume that the gas moves back and forth in one dimension only (the x direction). If there is no sound, then each bit of gas is at rest at some place (x,y,z). There is a uniform equilibrium density ρ0 (mass per unit volume) and pressure P0 (force per unit area). Now suppose the gas moves; all gas in the layer at x moves the same distance, X(x), but gas in other layers move by different distances. More precisely, at each time t the layer originally at x is displaced to x + X(x,t). -
Geometric Integration Theory Contents
Steven G. Krantz Harold R. Parks Geometric Integration Theory Contents Preface v 1 Basics 1 1.1 Smooth Functions . 1 1.2Measures.............................. 6 1.2.1 Lebesgue Measure . 11 1.3Integration............................. 14 1.3.1 Measurable Functions . 14 1.3.2 The Integral . 17 1.3.3 Lebesgue Spaces . 23 1.3.4 Product Measures and the Fubini–Tonelli Theorem . 25 1.4 The Exterior Algebra . 27 1.5 The Hausdorff Distance and Steiner Symmetrization . 30 1.6 Borel and Suslin Sets . 41 2 Carath´eodory’s Construction and Lower-Dimensional Mea- sures 53 2.1 The Basic Definition . 53 2.1.1 Hausdorff Measure and Spherical Measure . 55 2.1.2 A Measure Based on Parallelepipeds . 57 2.1.3 Projections and Convexity . 57 2.1.4 Other Geometric Measures . 59 2.1.5 Summary . 61 2.2 The Densities of a Measure . 64 2.3 A One-Dimensional Example . 66 2.4 Carath´eodory’s Construction and Mappings . 67 2.5 The Concept of Hausdorff Dimension . 70 2.6 Some Cantor Set Examples . 73 i ii CONTENTS 2.6.1 Basic Examples . 73 2.6.2 Some Generalized Cantor Sets . 76 2.6.3 Cantor Sets in Higher Dimensions . 78 3 Invariant Measures and the Construction of Haar Measure 81 3.1 The Fundamental Theorem . 82 3.2 Haar Measure for the Orthogonal Group and the Grassmanian 90 3.2.1 Remarks on the Manifold Structure of G(N,M).... 94 4 Covering Theorems and the Differentiation of Integrals 97 4.1 Wiener’s Covering Lemma and its Variants . -
Some Inequalities in the Theory of Functions^)
SOME INEQUALITIES IN THE THEORY OF FUNCTIONS^) BY ZEEV NEHARI 1. Introduction. Many of the inequalities of function theory and potential theory may be reduced to statements regarding the properties of harmonic domain functions with vanishing or constant boundary values, that is, func- tions which can be obtained from the Green's function by means of elementary processes. For the derivation of these inequalities a large number of different techniques and procedures have been used. It is the aim of this paper to show that many of the known inequalities of this type, and also others which are new, can be obtained as simple consequences of the classical minimum prop- erty of the Dirichlet integral. In addition to the resulting simplification, this method has the further advantage of being capable of generalization to a wide class of linear partial differential equations of elliptic type in two or more variables. The idea of using the positive-definite character of an integral as the point of departure for the derivation of function-theoretic inequalities is, of course, not new and it has been successfully used for this purpose by a num- ber of authors [l; 2; 8; 9; 16]. What the present paper attempts is to give a more or less systematic survey of the type of inequality obtainable in this way. 2. Monotonie functionals. 1. The domains we shall consider will be as- sumed to be bounded by a finite number of closed analytic curves and they will be embedded in a given closed Riemann surface R of finite genus. The symbol 5(a) will be used to denote a "singularity function" with the follow- ing properties: 5(a) is real, harmonic, and single-valued on R, with the excep- tion of a finite number of points at which 5(a) has specified singularities. -
Topics on Calculus of Variations
TOPICS ON CALCULUS OF VARIATIONS AUGUSTO C. PONCE ABSTRACT. Lecture notes presented in the School on Nonlinear Differential Equa- tions (October 9–27, 2006) at ICTP, Trieste, Italy. CONTENTS 1. The Laplace equation 1 1.1. The Dirichlet Principle 2 1.2. The dawn of the Direct Methods 4 1.3. The modern formulation of the Calculus of Variations 4 1 1.4. The space H0 (Ω) 4 1.5. The weak formulation of (1.2) 8 1.6. Weyl’s lemma 9 2. The Poisson equation 11 2.1. The Newtonian potential 11 2.2. Solving (2.1) 12 3. The eigenvalue problem 13 3.1. Existence step 13 3.2. Regularity step 15 3.3. Proof of Theorem 3.1 16 4. Semilinear elliptic equations 16 4.1. Existence step 17 4.2. Regularity step 18 4.3. Proof of Theorem 4.1 20 References 20 1. THE LAPLACE EQUATION Let Ω ⊂ RN be a body made of some uniform material; on the boundary of Ω, we prescribe some fixed temperature f. Consider the following Question. What is the equilibrium temperature inside Ω? Date: August 29, 2008. 1 2 AUGUSTO C. PONCE Mathematically, if u denotes the temperature in Ω, then we want to solve the equation ∆u = 0 in Ω, (1.1) u = f on ∂Ω. We shall always assume that f : ∂Ω → R is a given smooth function and Ω ⊂ RN , N ≥ 3, is a smooth, bounded, connected open set. We say that u is a classical solution of (1.1) if u ∈ C2(Ω) and u satisfies (1.1) at every point of Ω. -
THE IMPACT of RIEMANN's MAPPING THEOREM in the World
THE IMPACT OF RIEMANN'S MAPPING THEOREM GRANT OWEN In the world of mathematics, scholars and academics have long sought to understand the work of Bernhard Riemann. Born in a humble Ger- man home, Riemann became one of the great mathematical minds of the 19th century. Evidence of his genius is reflected in the greater mathematical community by their naming 72 different mathematical terms after him. His contributions range from mathematical topics such as trigonometric series, birational geometry of algebraic curves, and differential equations to fields in physics and philosophy [3]. One of his contributions to mathematics, the Riemann Mapping Theorem, is among his most famous and widely studied theorems. This theorem played a role in the advancement of several other topics, including Rie- mann surfaces, topology, and geometry. As a result of its widespread application, it is worth studying not only the theorem itself, but how Riemann derived it and its impact on the work of mathematicians since its publication in 1851 [3]. Before we begin to discover how he derived his famous mapping the- orem, it is important to understand how Riemann's upbringing and education prepared him to make such a contribution in the world of mathematics. Prior to enrolling in university, Riemann was educated at home by his father and a tutor before enrolling in high school. While in school, Riemann did well in all subjects, which strengthened his knowl- edge of philosophy later in life, but was exceptional in mathematics. He enrolled at the University of G¨ottingen,where he learned from some of the best mathematicians in the world at that time. -
FETI-DP Domain Decomposition Method
ECOLE´ POLYTECHNIQUE FED´ ERALE´ DE LAUSANNE Master Project FETI-DP Domain Decomposition Method Supervisors: Author: Davide Forti Christoph Jaggli¨ Dr. Simone Deparis Prof. Alfio Quarteroni A thesis submitted in fulfilment of the requirements for the degree of Master in Mathematical Engineering in the Chair of Modelling and Scientific Computing Mathematics Section June 2014 Declaration of Authorship I, Christoph Jaggli¨ , declare that this thesis titled, 'FETI-DP Domain Decomposition Method' and the work presented in it are my own. I confirm that: This work was done wholly or mainly while in candidature for a research degree at this University. Where any part of this thesis has previously been submitted for a degree or any other qualification at this University or any other institution, this has been clearly stated. Where I have consulted the published work of others, this is always clearly at- tributed. Where I have quoted from the work of others, the source is always given. With the exception of such quotations, this thesis is entirely my own work. I have acknowledged all main sources of help. Where the thesis is based on work done by myself jointly with others, I have made clear exactly what was done by others and what I have contributed myself. Signed: Date: ii ECOLE´ POLYTECHNIQUE FED´ ERALE´ DE LAUSANNE Abstract School of Basic Science Mathematics Section Master in Mathematical Engineering FETI-DP Domain Decomposition Method by Christoph Jaggli¨ FETI-DP is a dual iterative, nonoverlapping domain decomposition method. By a Schur complement procedure, the solution of a boundary value problem is reduced to solving a symmetric and positive definite dual problem in which the variables are directly related to the continuity of the solution across the interface between the subdomains. -
On Liouville Theorems for Harmonic Functions with Finite Dirichlet Integral Udc 517.95
. C6opHHK Math. USSR Sbornik TOM 132(174)(1987), Ban. 4 Vol. 60(1988), No. 2 ON LIOUVILLE THEOREMS FOR HARMONIC FUNCTIONS WITH FINITE DIRICHLET INTEGRAL UDC 517.95 A. A. GRIGOR'YAN ABSTRACT. A criterion for the validity of the D-Liouville theorem is proved. In §1 it is shown that the question of L°°- and D-Liouville theorems reduces to the study of the so-called massive sets (in other words, the level sets of harmonic functions in the classes L°° and L°° Π D). In §2 some properties of capacity are presented. In §3 the criterion of D-massiveness is formulated—the central result of this article—and examples are presented. In §4 a criterion for the D-Liouville theorem is formulated, and corollaries are derived. In §§5-9 the main theorems are proved. Figures: 5. Bibliography: 17 titles. Introduction The classical theorem of Liouville states that any bounded harmonic function on Rn is constant. It is easy to verify that the following assertions are also true: 1) If the harmonic function u on R™ has finite Dirichlet integral then u = const. 2) If u € LP(R") is a harmonic function, 1 < ρ < oo, then «ΞΟ. The list of theorems of this kind can be extended; they are known in the literature under the general category of Liouville-type theorems. After Moser's paper [1], which in particular proved Liouville's theorem for entire solutions of the uniformly elliptic equation it became possible to study the solutions of the Laplace-Beltrami equation^) on arbitrary Riemannian manifolds. The main efforts here are directed towards finding under what geometric conditions one or another Liouville theorem is true. -
Level-Set Volume-Preserving Diffusions
Level-set volume-preserving diffusions Yann Brenier CNRS, Centre de mathématiques Laurent Schwartz Ecole Polytechnique, FR 91128 Palaiseau Fluid Mechanics, Hamiltonian Dynamics, and Numerical Aspects of Optimal Transportation, MSRI, October 14-18, 2013 Yann Brenier (CNRS) Level-set volume-preserving diffusions October 2013 1 / 18 EQUIVALENCE OF TWO DIFFERENT FUNCTIONS WITH LEVEL SETS OF EQUAL VOLUME ' ∼ '0 1.5 volume and topology preservation 1 0.5 0 -0.5 -1 -1.5 -2.5 -2 -1.5 -1 -0.5 0 0.5 1 1.5 2 2.5 Yann Brenier (CNRS) Level-set volume-preserving diffusions October 2013 2 / 18 MOTIVATION: MINIMIZATION PROBLEMS WITH VOLUME CONSTRAINTS ON LEVEL SETS 1.5 volume and topology preservation 1 0.5 0 -0.5 -1 -1.5 -2.5 -2 -1.5 -1 -0.5 0 0.5 1 1.5 2 2.5 This goes back to Kelvin. See Th. B. Benjamin, G. Burton etc.... Yann Brenier (CNRS) Level-set volume-preserving diffusions October 2013 3 / 18 This can be rephrased as Z Z 1 2 inf sup jr'(x)j dx + [F('(x)) − F('0(x))]dx ': ! D R F:R!R 2 D D Optimal solutions are formally solutions to − 4' + F0(') = 0 for some function F : R ! R , and, in 2d, are just stationary solutions to the Euler equations of incompressible fluids. An example in fluid mechanics d d Here D = T = (R=Z) is the flat torus and '0 is a given function on D. We want to minimize the Dirichlet integral among all ' ∼ '0. Yann Brenier (CNRS) Level-set volume-preserving diffusions October 2013 4 / 18 Optimal solutions are formally solutions to − 4' + F0(') = 0 for some function F : R ! R , and, in 2d, are just stationary solutions to the Euler equations of incompressible fluids. -
An Improved Riemann Mapping Theorem and Complexity In
AN IMPROVED RIEMANN MAPPING THEOREM AND COMPLEXITY IN POTENTIAL THEORY STEVEN R. BELL Abstract. We discuss applications of an improvement on the Riemann map- ping theorem which replaces the unit disc by another “double quadrature do- main,” i.e., a domain that is a quadrature domain with respect to both area and boundary arc length measure. Unlike the classic Riemann Mapping Theo- rem, the improved theorem allows the original domain to be finitely connected, and if the original domain has nice boundary, the biholomorphic map can be taken to be close to the identity, and consequently, the double quadrature do- main close to the original domain. We explore some of the parallels between this new theorem and the classic theorem, and some of the similarities between the unit disc and the double quadrature domains that arise here. The new results shed light on the complexity of many of the objects of potential theory in multiply connected domains. 1. Introduction The unit disc is the most famous example of a “double quadrature domain.” The average of an analytic function on the disc with respect to both area measure and with respect to boundary arc length measure yield the value of the function at the origin when these averages make sense. The Riemann Mapping Theorem states that when Ω is a simply connected domain in the plane that is not equal to the whole complex plane, a biholomorphic map of Ω to this famous double quadrature domain exists. We proved a variant of the Riemann Mapping Theorem in [16] that allows the domain Ω = C to be simply or finitely connected. -
A Brief Introduction to Lebesgue Theory
CHAPTER 3 A BRIEF INTRODUCTION TO LEBESGUE THEORY Introduction The span from Newton and Leibniz to Lebesgue covers only 250 years (Figure 3.1). Lebesgue published his dissertation “Integrale,´ longueur, aire” (“Integral, length, area”) in the Annali di Matematica in 1902. Lebesgue developed “measure of a set” in the first chapter and an integral based on his measure in the second. Figure 3.1 From Newton and Leibniz to Lebesgue. Introduction to Real Analysis. By William C. Bauldry 125 Copyright c 2009 John Wiley & Sons, Inc. ⌅ 126 A BRIEF INTRODUCTION TO LEBESGUE THEORY Part of Lebesgue’s motivation were two problems that had arisen with Riemann’s integral. First, there were functions for which the integral of the derivative does not recover the original function and others for which the derivative of the integral is not the original. Second, the integral of the limit of a sequence of functions was not necessarily the limit of the integrals. We’ve seen that uniform convergence allows the interchange of limit and integral, but there are sequences that do not converge uniformly yet the limit of the integrals is equal to the integral of the limit. In Lebesgue’s own words from “Integral, length, area” (as quoted by Hochkirchen (2004, p. 272)), It thus seems to be natural to search for a definition of the integral which makes integration the inverse operation of differentiation in as large a range as possible. Lebesgue was able to combine Darboux’s work on defining the Riemann integral with Borel’s research on the “content” of a set. -
Harmonic Calculus on P.C.F. Self-Similar Sets
transactions of the american mathematical society Volume 335, Number 2, February 1993 HARMONIC CALCULUSON P.C.F. SELF-SIMILAR SETS JUN KIGAMI Abstract. The main object of this paper is the Laplace operator on a class of fractals. First, we establish the concept of the renormalization of difference operators on post critically finite (p.c.f. for short) self-similar sets, which are large enough to include finitely ramified self-similar sets, and extend the results for Sierpinski gasket given in [10] to this class. Under each invariant operator for renormalization, the Laplace operator, Green function, Dirichlet form, and Neumann derivatives are explicitly constructed as the natural limits of those on finite pre-self-similar sets which approximate the p.c.f. self-similar sets. Also harmonic functions are shown to be finite dimensional, and they are character- ized by the solution of an infinite system of finite difference equations. 0. Introduction Mathematical analysis has recently begun on fractal sets. The pioneering works are the probabilistic approaches of Kusuoka [11] and Barlow and Perkins [2]. They have constructed and investigated Brownian motion on the Sierpinski gaskets. In their standpoint, the Laplace operator has been formulated as the infinitesimal generator of the diffusion process. On the other hand, in [10], we have found the direct and natural definition of the Laplace operator on the Sierpinski gaskets as the limit of difference opera- tors. In the present paper, we extend the results in [10] to a class of self-similar sets called p.c.f. self-similar sets which include the nested fractals defined by Lindstrom [13]. -
A Generalization of the Mehler-Dirichlet Integral
MATHEMATICS A GENERALIZATION OF THE MEHLER-DIRICHLET INTEGRAL BY R. L. VAN DE WETERING (Communicated by Prof. H. D. KLOOSTERMAN at the meeting of November 25, 1967) The main results of this paper are the representation of the generalized Legendre's functions PZ'·n(z) of KuiPERS-MEULENBELD by means of integrals which include a generalization of the Mehler-Dirichlet integral [1, pg 267 (127)]. The principal properties of P;:·n(z), which is one of the solutions of the differential equation: d2w dw { m2 n2 } (1) (1-z2) dz2 - 2z dz + k(k+1)- 2(1-z)- 2(1+z) w=O, are found in [2], [3] and [4 ]. In order to obtain these integral representa tions it is necessary to extend a result of KuiPERS-MEULENBELD [5, (10)]. From [5, (7)] we have P;;'·n(z) = F(iX+ 1) (z+ 1)Hn-m) J' e-imu{z+ (z2-1)! cos u}~· (2) 1 2nF(fJ+ 1)2m-n u,-2n · {z + 1 + (z2 -1 )! eiu}m-n du, where for the sake of brevity we write m+n m-n m-n m+n iX=k+ -2-· '{J=k- -2-, y=k+ -2-, b=k- -2-. In (2), u1=n+ix+i log (iz+1jljz-1j-!)1) where X is given by [5, Fig. 1]. This integral representation is valid for Re (z)>O, jarg (z-1)1 <n, Re (fJ)> -1 and iX not a negative integer. From (2) we get: F(iX+ 1)(z+ 1)Hm-n) u, P;:·n(z)= 2nF(fJ+1)2m-n J e-imu{z+(z2-1)icosu}~· u 1 -2n .