In this exercise we explore nonlinear effects in ion-acoustic waves (Ex. 21.5), and show that they give rise to solitons that obey the same KdV equation as governs solitonic water waves (Sec. 16.3). This version of the solitons is only mildly nonlinear. In Sec. 23.6 we will generalize to strong nonlinearity.
(a) Introduce a bookkeeping expansion parameter $\varepsilon$ whose numerical value is unity, ${ }^5$ and expand the ion density, ion velocity, and potential in the forms
$$
\begin{aligned}
n & =n_0\left(1+\varepsilon n_1+\varepsilon^2 n_2+\ldots\right), \\
u & =\left(k_B T_e / m_p\right)^{1 / 2}\left(\varepsilon u_1+\varepsilon^2 u_2+\ldots\right), \\
\Phi & =\left(k_B T_e / e\right)\left(\varepsilon \Phi_1+\varepsilon^2 \Phi_2+\ldots\right) .
\end{aligned}
$$
Here $n_1, u_1$, and $\Phi_1$ are small compared to unity, and the factors of $\varepsilon$ tell us that, as the wave amplitude is decreased, these quantities scale proportionally to one another, while $n_2, u_2$, and $\Phi_2$ scale proportionally to the squares of $n_1, u_1$, and $\Phi_1$, respectively. Change independent variables from $(t, z)$ to $(\tau, \eta)$, where
$$
\begin{aligned}
\eta & =\sqrt{2} \varepsilon^{1 / 2} \lambda_D^{-1}\left[z-\left(k_B T_e / m_p\right)^{1 / 2} t\right], \\
\tau & =\sqrt{2} \varepsilon^{3 / 2} \omega_{p p} t .
\end{aligned}
$$
Explain, now or at the end, the chosen powers $\varepsilon^{1 / 2}$ and $\varepsilon^{3 / 2}$. By substituting Eqs. (21.37) and (21.38) into the nonlinear equations (21.35), equating terms of the same order in $\varepsilon$, and then setting $\varepsilon=1$ (bookkeeping parameter!), show that $n_1, u_1$, and $\Phi_1$ each satisfy the $\mathrm{KdV}$ equation (16.32):
$$
\frac{\partial \zeta}{\partial \tau}+\zeta \frac{\partial \zeta}{\partial \eta}+\frac{\partial^3 \zeta}{\partial \eta^3}=0
$$
(b) In Sec. 16.3 we discussed the exact, single-soliton solution (16.33) to this KdV equation. Show that for an ion-acoustic soliton, this solution propagates with the physical speed $\left(1+n_{1 o}\right)\left(k_B T_e / m_p\right)^{1 / 2}$ (where $n_{1 o}$ is the value of $n_1$ at the peak of the soliton), which is greater the larger is the wave's amplitude.