One of the simple examples of a
three-dimensional wave is the plane wave. In order to derive the mathematical
expression of a plane wave moving in direction vector $\vec{k}$ perpendicular
to the plane, we first write the position vector in Cartesian coordinates in
terms of unit vectors
$\hat{\vec{i}},\hat{\vec{j}},\hat{\vec{k}}$ (see Figure 7.1.a):
$\vec{r}=x\hat{\vec{i}}+y\hat{\vec{j}}+z\hat{\vec{k}}$ (7.1)
For a plane anywhere in space,
that begins at some arbitrary origin O and ends at the point (x,y,z) on that plane (see Figure 7.1.b):
$(\vec{r}-{{\vec{r}}_{o}})=(x-{{x}_{o}})\hat{\vec{i}}+(y-{{y}_{o}})\hat{\vec{j}}+(z-{{z}_{o}})\hat{\vec{k}}$ (7.2)
Figure
7.1. (a) Cartesian unit vectors. (b) A plane wave moving in the $\vec{k}$-direction.
We would set the vector $\left( \vec{r}-{{{\vec{r}}}_{o}}
\right)$ to sweep out a plane perpendicular to $\vec{k}$ therefore,
$\left(
\vec{r}-{{{\vec{r}}}_{o}} \right)\bullet \vec{k}=0$ (7.3)
Rewriting directional vector $\vec{k}$ in term of unit
vectors:
$\vec{k}={{k}_{x}}\hat{\vec{i}}+{{k}_{y}}\hat{\vec{j}}+{{k}_{z}}\hat{\vec{k}}$
(7.4)
And Equation (7.3) becomes:
${{k}_{x}}\left( x-{{x}_{o}}
\right)+{{k}_{y}}\left( y-{{y}_{o}} \right)+{{k}_{z}}\left( z-{{z}_{o}}
\right)=0$ (7.5)
Thus, $\vec{k}\bullet \vec{r}=$ constant.
A set of planes over which the wave function $\psi
(\vec{r})$ varies sinusoidally for constant $\vec{k}\bullet \vec{r}$ can be constructed in term of complex
representation:
$\psi
(\vec{r})=A{{e}^{i\vec{k}\bullet \vec{r}}}$ (7.6)
Naturally, these harmonic functions are repetitive,
therefore, they can be expressed by:
$\psi (\vec{r})=\psi
(\vec{r}+\frac{\lambda \vec{k}}{k})$ (7.7)
In this equation, k
is the magnitude of $\vec{k}$ and ${}^{{\vec{k}}}/{}_{k}$ is a unit vector
parallel to it (see Figure 7.2).
Figure
7.2. Plane waves.
Applying Equation (7.7) to Equation (7.6), we obtain the exponential
form of the harmonic wave function:
$\psi (\vec{r})=A{{e}^{i\vec{k}\bullet
\vec{r}}}=A{{e}^{i\vec{k}\bullet (\vec{r}+{}^{\lambda
\vec{k}}/{}_{k})}}=A{{e}^{i\vec{k}\bullet \vec{r}}}{{e}^{i\lambda k}}$ (7.8)
To satisfy Equation (7.6), we must have:
${{e}^{i\lambda k}}=1={{e}^{i2\pi }}$
(7.9)
Therefore $\lambda k=2\pi $ or $k={}^{2\pi }/{}_{\lambda
}$. The vector $\vec{k}$ is called the propagation
vector, whose magnitude is the propagation
number k.
Since $\psi (\vec{r})$ is moving i.e. is varying in time,
we introduce the time dependence ωt
in analogy to that of the one-dimensional wave equation:
$\psi \left( \vec{r},t
\right)=A{{e}^{i(\vec{k}\bullet \vec{r}\mp \omega t)}}$ (7.10)
With A, ω, and k constant. The wave travels in the direction of propagation vector
$\vec{k}$ such that we can assign a phase corresponding to it at each point in
space and time. The surfaces connecting every points of equal phase at any
given time are known as the wavefronts
(see Figure 7.3).
Figure 7.3. Wavefronts for a harmonic plane waves.
The propagation velocity of the wavefront is equal to the
phase velocity of a plane wave given by Equation (7.10). Following from Figure
7.2, rk is the scalar
component of $\vec{r}$ in the direction of $\vec{k}$. Since we assume that the
wave is homogeneous and the disturbance on a wavefront is constant, so that
after a time dt and after the
wavefront moves along $\vec{k}$ by a distance drk, Equation (7.10) should be:
$\psi (\vec{r},t)=\psi (r+d{{r}_{k}},t+dt)=\psi
({{r}_{k}},t)$ (7.11)
Which can be rewritten in exponential form as follows:
$A{{e}^{i(\vec{k}\bullet
\vec{r}\mp \omega t)}}=A{{e}^{i(k{{r}_{k}}+kd{{r}_{k}}\mp \omega t\mp \omega
dt)}}=A{{e}^{i(k{{r}_{k}}\mp \omega t)}}$ (7.12)
So that $kd{{r}_{k}}=\pm \omega dt$ and the wave velocity
${}^{d{{r}_{k}}}/{}_{dt}$ is then:
$\frac{d{{r}_{k}}}{dt}=\pm
\frac{\omega }{k}=\pm v$ (7.13)



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