PlanetMath (more info)
 Math for the people, by the people. Sponsor PlanetMath
Encyclopedia | Requests | Forums | Docs | Wiki | Random | RSS  
Login
create new user
name:
pass:
forget your password?
Main Menu
Viewing Version 6 of 'wave equation'
[ view 'wave equation' | back to history ]

Title of object: wave equation
Canonical Name: WaveEquation
Type: Definition

Created on: 2002-11-21 09:12:58
Modified on: 2007-06-26 12:44:15

Creator: Mathprof
Modifier: Mathprof
Author: Mathprof
Author: pbruin

Classification: msc:35L05
Keywords: partial differential equation
Defines: d'Alembert's solution to the wave equation

Revision comment (for changes between this and next version):

Changes for correction #14254 ('initial conditions pro starting').

Preamble:

% this is the default PlanetMath preamble. as your knowledge
% of TeX increases, you will probably want to edit this, but
% it should be fine as is for beginners.

% almost certainly you want these
\usepackage{amssymb}
\usepackage{amsmath}
\usepackage{amsfonts}

% used for TeXing text within eps files
%\usepackage{psfrag}
% need this for including graphics (\includegraphics)
%\usepackage{graphicx}
% for neatly defining theorems and propositions
%\usepackage{amsthm}
% making logically defined graphics
%\usepackage{xypic}

% there are many more packages, add them here as you need them

% define commands here
Content:

The \emph{wave equation} is a partial differential equation which
describes certain kinds of waves. It arises in various physical
situations, such as vibrating \PMlinkescapetext{strings}, \PMlinkescapetext{sound} waves, and
electromagnetic waves.

The wave equation in one \PMlinkescapetext{dimension} is
$$
\frac{\partial^2 u}{\partial t^2}=c^2\frac{\partial^2 u}{\partial
x^2}.
$$
The general solution of the one-dimensional wave equation can be
obtained by a change of coordinates: $(x,t)\longrightarrow(\xi,\eta)$,
where $\xi=x-ct$ and $\eta=x+ct$. This gives $\frac{\partial^2 u}{\partial\xi\partial\eta}=0$, which we can integrate to get \emph{d'Alembert's solution}:
$$
u(x,t)=F(x-ct)+G(x+ct)
$$
where $F$ and $G$ are twice differentiable functions. $F$ and $G$
represent waves traveling in the positive and negative $x$
directions, respectively, with velocity $c$. These functions can be
obtained if appropriate starting or boundary conditions are given. For example, if $u(x,0)=f(x)$ and $\frac{\partial u}{\partial t}(x,0)=g(x)$ are given, the solution is
$$
u(x,t)=\frac{1}{2}[f(x-ct)+f(x+ct)]+\frac{1}{2c}\int_{x-ct}^{x+ct}g(s)\mathrm d s.
$$

In general, the wave equation in $n$ \PMlinkescapetext{dimensions} is
$$
\frac{\partial^2 u}{\partial t^2}=c^2\nabla^2 u.
$$
where $u$ is a function of the location variables
$x_1,x_2,\ldots,x_n$, and time $t$. Here, $\nabla^2$ is the Laplacian
with respect to the location variables, which in Cartesian coordinates is given by $
\nabla^2=\frac{\partial^2}{\partial x_1^2}+\frac{\partial^2}{\partial x_2^2}+\cdots+\frac{\partial^2}{\partial x_n^2}$.