Partial Di¤erential Equations
Alexander Grigorian Universität Bielefeld
WS 2015/16 2 Contents
0 Introduction 1 0.1 Examples of PDEs and their origin ...... 1 0.1.1 Laplace equation ...... 2 0.1.2 Waveequation ...... 5 0.1.3 Divergence theorem ...... 8 0.1.4 Heatequation...... 9 0.1.5 Schrödinger equation ...... 11 0.2 Quasi-linear PDEs of second order and change of coordinates ...... 12
1 Laplace equation and harmonic functions 19 1.1 Maximum principle and uniqueness in Dirichlet problem ...... 19 1.2 Representation of C2 functions by means of potentials ...... 22 1.3 Greenfunction ...... 26 1.4 The Green function in a ball ...... 28 1.5 Dirichlet problem in a ball and Poisson formula ...... 31 1.6 Properties of harmonic functions ...... 41 1.7 Sequences of harmonic functions ...... 43 1.8 Discrete Laplace operator ...... 46 1.9 Separation of variables in the Dirichlet problem ...... 49 1.10 Variational problem and the Dirichlet principle ...... 51 1.11 Distributions ...... 59 1.12 Euler-Lagrange equation ...... 60 1.13 Dirichlet problem in arbitrary domains (overview) ...... 62
2 Heat equation 67 2.1 Heatkernel ...... 67 2.2 Solution of the Cauchy problem ...... 70 2.3 Maximum principle and uniqueness in Cauchy problem ...... 72 2.4 Mixed problem and separation of variables ...... 77 2.5 Mixed problem with the source function ...... 83 2.6 Cauchy problem with source function and Duhamel’sprinciple . . . . 84 2.7 Brownianmotion...... 89
3 Wave equation 93 3.1 Cauchy problem in dimension 1 ...... 93 3.2 Energy and uniqueness ...... 95 3.3 Mixed problem for the wave equation ...... 99
3 4 CONTENTS
3.4 Sphericalmeans ...... 107 3.5 Cauchy problem in dimension 3 ...... 111 3.6 Cauchy problem in dimension 2 ...... 114 3.7 Cauchy problem in higher dimensions ...... 116
4 The eigenvalue problem 119 4.1 Distributions and distributional derivatives ...... 119 4.2 Sobolevspaces ...... 123 4.3 Weak Dirichlet problem ...... 125 4.4 TheGreenoperator...... 127 4.5 Compact embedding theorem ...... 129 4.6 Eigenvalues and eigenfunctions of the weak Dirichlet problem ...... 135 4.7 Higher order weak derivatives ...... 139 4.7.1 Higher order derivatives in a cube ...... 139 4.7.2 Higher order derivatives in arbitrary domain ...... 145 4.8 Sobolev embedding theorem ...... 148 4.9 Sobolev spaces of fractional orders ...... 155 Chapter 0
Introduction
21.10.15 0.1 Examples of PDEs and their origin
Let u = u (x1; :::; xn) be a real-valued function of n independent real variables x1; :::; xn. Recall that, for any multiindex = ( 1; :::; n) where i are non-negative integers, the expression D u denotes the following partial derivative of u:
@ u D u = j j ; 1 n @x1 :::@xn
where = 1 + ::: + n is the order of the derivative. A partialj j di¤erential equation (PDE) is an equation with an unknown function u = u (x1; ::; xn) of n > 1 independent variables, which contains partial derivatives of u. That is, a general PDE looks as follows:
F D u; D u; D u; ::: = 0 (0.1)
where F is a given function, u is unknown function, ; ; ; ::: are multiindices. Of course, the purpose of studying of any equation is to develop methods of solving it or at least ensuring that it has solutions. For example, in the theory of ordinary di¤erential equations (ODEs) one considers an unknown function u (x) of a single real variable x and a general ODE
F (u; u0; u00; :::) = 0
and proves theorems about solvability of such an equation with initial conditions, under certain assumptions about F (Theorem of Picard-Lindelöf). One also develops methods of solving explicitly certain types of ODEs, for example, linear ODEs. In contrast to that, there is no theory of general PDEs of the form (0.1). The reason for that is that the properties of PDEs depend too much of the function F and cannot be stated within a framework of one theory. Instead one develops theories for narrow classes of PDEs or even for single PDEs, as we will do in this course. Let us give some examples of PDEs that arise in applications, mostly in Physics. These examples have been motivating development of Analysis for more than a century. In fact, a large portion of modern Analysis has emerged in attempts of solving those special PDEs.
1 2 CHAPTER 0. INTRODUCTION
0.1.1 Laplace equation
Let be an open subset of Rn and let u : R be a function that twice continuously di¤erentiable, that is, u C2 ( ) : By u we! denote the following function 2 n
u = @xkxk u; k=1 X that is, u is the sum of all unmixed partial derivatives of u of the second order. The di¤erential operator n
= @xkxk k=1 X is called the Laplace operator, so that u is the result of application to u of the Laplace operator. The Laplace equation is a PDE of the form u = 0: Any function u that satis…es the Laplace equation is called a harmonic function. Of course, any a¢ ne function
u (x) = a1x1 + ::: + anxn + b with real coe¢ cients a1; :::; an; b is harmonic because all second order partial derivatives of u vanish. However, there are more interesting examples of harmonic functions. For example, in Rn with n 3 the function 1 u (x) = n 2 x j j is harmonic away from the origin, where
x = x2 + ::: + x2 j j 1 n q is the Euclidean norm of x: In R2 the function u (x) = ln x j j is harmonic away from the origin. It is easy to see that the Laplace operator is linear, that is, (u + v) = u + v and (cv) = cu for all u; v C2 and c R: It follows that linear combinations of harmonic functions are harmonic.2 2 A more general equation u = f where f : R is a given function, is called the Poisson equation. The Laplace and Poisson equations! are most basic and most important examples of PDEs. Let us discuss some origins of the Laplace and Poisson equations. 0.1. EXAMPLES OF PDES AND THEIR ORIGIN 3
Holomorphic function Recall that a complex valued function f (z) of a complex variable z = x + iy is called holomorphic (or analytic) if it is C-di¤erentiable. Denoting u = Re f and v = Im f, we obtain functions u (x; y) and v (x; y) of two real variables x; y. It is known from the theory of functions of complex variables that if f is holomorphic then u; v satisfy the Cauchy-Riemann equations
@ u = @ v; x y (0.2) @yu = @xv: Assuming that u; v C2 (and this is necessarily the case for holomorphic functions), we obtain from (0.2)2 @xxu = @x@yv = @y@xv = @yyu whence u = @xxu + @yyu = 0: In the same way v = 0: Hence, both u; v are harmonic functions. This observation allows us to produce many examples of harmonic functions in R2 starting from holomorphic functions. For example, for f (z) = ez we have
ez = ex+iy = ex (cos y + i sin y) which yields the harmonic functions u (x; y) = ex cos y and v (x; y) = ex sin y: For f (z) = z2 we have
z2 = (x + iy)2 = x2 y2 + 2xyi; so that the functions u = x2 y2 and v = 2 xy are harmonic. For the function f (z) = ln z that is de…ned away from the negative part of the real axis, we have, using the polar form z = rei of complex numbers that
ln z = ln r + i:
y z r
S x
Since r = z and = arg z = arctan y , it follows that the both functions u = j j x ln z = ln x2 + y2 and u = arctan y are harmonic. j j x p 4 CHAPTER 0. INTRODUCTION
Gravitational …eld By Newton’slaw of gravitation of 1686, any two point masses m; M are attracted each Mm to other by the gravitational force F = r2 where r is the distance between the points and is the gravitational constant. Assume that the point mass M is located constantly at the origin of R3 and that the point mass m is moving and let its current position be x R3: Taking for simplicity = m = 1, we obtain that the force acting 2 at the moving mass is F = M and it is directed from x to the origin. The vector F x 2 ! of the force is then equal to j j
M x x !F = = M : x 2 x x 3 j j j j j j Any function !F de…ned in a domain of Rn and taking values in Rn is called a vector x 3 …eld. The vector …eld !F (x) = M 3 in R is called the gravitational …eld of the x point mass M. j j A real-value function U (x) in Rn is called a potential of a vector …eld !F (x) in Rn if !F (x) = U (x) ; r where U is the gradient of U de…ned by r
U = (@x U; :::; @x U) : r 1 n Not every vector …eld has a potential; if it does then it is called conservative. Conser- vative …elds are easier to handle as they can be described by one scalar function U (x) instead of a vector function !F (x). It can be checked that the following function M U (x) = x j j x is a potential of the gravitational …eld !F = M 3 . It is called the gravitational x potential of the point mass M sitting at the origin. j j If M is located at another point y R3, then the potential of it is 2 M U (x) = : x y j j More generally, potential of a mass distributed in a closed region D is given by
(y) dy U (x) = ; (0.3) x y ZD j j where (y) is the density of the matter at the point y D. In particular, the gravita- tional force of any mass is a conservative vector …eld. 2 1 n As we have mentioned above, the function n 2 is harmonic in away from the x R 1 j j 3 origin. As a particular case, we see that x is harmonic in R away from the origin. M j j It follows that the potential U (x) = x is harmonic away from the origin and the j j 0.1. EXAMPLES OF PDES AND THEIR ORIGIN 5 potential U (x) = M is harmonic away from y. One can deduce that also the x y function U (x) given byj (0.3)j is harmonic away from D. Historically, it was discovered by Pierre-Simon Laplace in 1784-85 that a gravi- tational …eld of any body is a conservative vector …eld and that its potential U (x) satis…es in a free space the equation U = 0, which is called henceforth the Laplace equation. The latter can be used for actual computation of gravitational potentials even without knowledge of the density .
Electric force By Coulomb’slaw of 1784, magnitude of the electric force F between two point electric Qq charges Q; q is equal to k r2 where r is the distance between the points and k is the Coulomb constant. Assume that the point charge Q is located at the origin and the point charge q at a variable position x R3. Taking for simplicity that k = q = 1, we obtain F = Q and that this force is directed2 from the origin to x if Q > 0, and from x 2 x to the originj j if Q < 0 (indeed, if the both charges are positive then the electric force between them is repulsive, unlike the case of gravitation when the force is attractive). Hence, the vector !F of the electric force is given by Q x x !F = = Q : x 2 x x 3 j j j j j j Q This vector …eld is potential, and its potential is given by U (x) = x . If a distributed charge is located in a closed domain D with thej j charge density , then the electric potential of this charge is given by (y) dy U (x) = ; x y ZD j j which is a harmonic function outside D.
0.1.2 Wave equation Electromagnetic …elds In the case of fast moving charges one should take into account not only their electric …elds but also the induced magnetic …elds. In general, an electromagnetic …eld is described by two vector …elds !E (x; t) and !B (x; t) that depend not only on a point 3 x R but also on time t. If a point charge q moves with velocity !v , then the electromagnetic2 …eld exerts the following force on this charge: