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authorPrefetch2021-05-30 15:54:40 +0200
committerPrefetch2021-05-30 15:54:40 +0200
commitaab299218975a8e775cda26ce256ffb1fe36c863 (patch)
tree9483e02b11a629456ce81d5a55ca06cc47a45b5a /content/know/concept/optical-wave-breaking/index.pdc
parent9657833b115c8a61509295d2296c6f89e81fd219 (diff)
Expand knowledge base
Diffstat (limited to 'content/know/concept/optical-wave-breaking/index.pdc')
-rw-r--r--content/know/concept/optical-wave-breaking/index.pdc54
1 files changed, 30 insertions, 24 deletions
diff --git a/content/know/concept/optical-wave-breaking/index.pdc b/content/know/concept/optical-wave-breaking/index.pdc
index 757a633..2ab3ff1 100644
--- a/content/know/concept/optical-wave-breaking/index.pdc
+++ b/content/know/concept/optical-wave-breaking/index.pdc
@@ -75,11 +75,10 @@ the instantaneous frequencies for these separate effects:
$$\begin{aligned}
\omega_i(z,t)
&\approx \omega_\mathrm{GVD}(z,t) + \omega_\mathrm{SPM}(z,t)
- \\
% &= \frac{\beta_2 z / T_0^2}{1 + \beta_2^2 z^2 / T_0^4} \frac{t}{T_0^2}
% + \frac{2\gamma P_0 z}{T_0^2} t \exp\!\Big(\!-\frac{t^2}{T_0^2}\Big)
% \\
- &= \frac{tz}{T_0^2} \bigg( \frac{\beta_2 / T_0^2}{1 + \beta_2^2 z^2 / T_0^4}
+ = \frac{tz}{T_0^2} \bigg( \frac{\beta_2 / T_0^2}{1 + \beta_2^2 z^2 / T_0^4}
+ 2\gamma P_0 \exp\!\Big(\!-\!\frac{t^2}{T_0^2}\Big) \bigg)
\end{aligned}$$
@@ -97,14 +96,14 @@ and $N_\mathrm{sol}$ is the **soliton number**,
which is defined as:
$$\begin{aligned}
- N_\mathrm{sol}^2 = \frac{L_D}{L_N} = \frac{\gamma P_0 T_0^2}{|\beta_2|}
+ N_\mathrm{sol}^2 \equiv \frac{L_D}{L_N} = \frac{\gamma P_0 T_0^2}{|\beta_2|}
\end{aligned}$$
This quantity is very important in anomalous dispersion,
but even in normal dispesion, it is still a useful measure of the relative strengths of GVD and SPM.
As was illustrated earlier, $\omega_i$ overtakes itself at the edges,
-so OWB only occurs when $\omega_i$ is not monotonic,
-which is when its $t$-derivative,
+so OWB occurs when $\omega_i$ oscillates there,
+which starts when its $t$-derivative,
the **instantaneous chirpyness** $\xi_i$,
has *two* real roots for $t^2$:
@@ -122,11 +121,17 @@ leading to the following exact minimum value $N_\mathrm{min}^2$ for $N_\mathrm{s
such that OWB can only occur when $N_\mathrm{sol}^2 > N_\mathrm{min}^2$:
$$\begin{aligned}
- N_\mathrm{min}^2 = \frac{1}{4} \exp\!\Big(\frac{3}{2}\Big) \approx 1.12
+ \boxed{
+ N_\mathrm{min}^2 = \frac{1}{4} \exp\!\Big(\frac{3}{2}\Big) \approx 1.12
+ }
\end{aligned}$$
-Now, consider two times $t_1$ and $t_2$ in the pulse, separated by
-a small initial interval $(t_2 - t_1)$.
+If this condition $N_\mathrm{sol}^2 > N_\mathrm{min}^2$ is not satisfied,
+$\xi_i$ cannot have two roots for $t^2$, meaning $\omega_i$ cannot overtake itself.
+GVD is unable to keep up with SPM, so OWB will not occur.
+
+Next, consider two points at $t_1$ and $t_2$ in the pulse,
+separated by a small initial interval $(t_2 - t_1)$.
The frequency difference between these points due to $\omega_i$
will cause them to displace relative to each other
after a short distance $z$ by some amount $\Delta t$,
@@ -136,21 +141,21 @@ $$\begin{aligned}
\Delta t
&\approx z \Delta\beta_1
\qquad
- &&\Delta\beta_1 = \beta_1(\omega_i(z,t_2)) - \beta_1(\omega_i(z,t_1))
+ &&\Delta\beta_1 \equiv \beta_1(\omega_i(z,t_2)) - \beta_1(\omega_i(z,t_1))
\\
&\approx z \beta_2 \Delta\omega_i
\qquad
- &&\Delta\omega_i = \omega_i(z,t_2) - \omega_i(z,t_1)
+ &&\Delta\omega_i \equiv \omega_i(z,t_2) - \omega_i(z,t_1)
\\
&\approx z \beta_2 \Delta\xi_i \,(t_2 - t_1)
\qquad \quad
- &&\Delta\xi_i = \xi_i(z,t_2) - \xi_i(z,t_1)
+ &&\Delta\xi_i \equiv \xi_i(z,t_2) - \xi_i(z,t_1)
\end{aligned}$$
Where $\beta_1(\omega)$ is the inverse of the group velocity.
OWB takes place when $t_2$ and $t_1$ catch up to each other,
which is when $-\Delta t = (t_2 - t_1)$.
-The distance where this happens, $z = L_\mathrm{WB}$,
+The distance where this happens first, $z = L_\mathrm{WB}$,
must therefore satisfy the following condition
for a particular value of $t$:
@@ -161,7 +166,7 @@ $$\begin{aligned}
\end{aligned}$$
The time $t$ of OWB must be where $\omega_i(t)$ has its steepest slope,
-which is at the minimum value of $\xi_i(t)$, and, by extension $f(x)$.
+which is at the minimum value of $\xi_i(t)$, and by extension $f(x)$.
This turns out to be $f(3/2)$:
$$\begin{aligned}
@@ -170,16 +175,17 @@ $$\begin{aligned}
= 1 - N_\mathrm{sol}^2 / N_\mathrm{min}^2
\end{aligned}$$
-Clearly, $f_\mathrm{min} \ge 0$ when
-$N_\mathrm{sol}^2 \le N_\mathrm{min}^2$, which, when inserted in the
-condition above, confirms that OWB cannot occur in that case. Otherwise,
-if $N_\mathrm{sol}^2 > N_\mathrm{min}^2$, then:
+Clearly, $f_\mathrm{min} \ge 0$ when $N_\mathrm{sol}^2 \le N_\mathrm{min}^2$,
+which, when inserted above, leads to an imaginary $L_\mathrm{WB}$,
+confirming that OWB cannot occur in that case.
+Otherwise, if $N_\mathrm{sol}^2 > N_\mathrm{min}^2$, then:
$$\begin{aligned}
- L_\mathrm{WB}
- = - \frac{T_0^2}{\beta_2 \, \sqrt{f_\mathrm{min}}}
- = \frac{L_D}{\sqrt{N_\mathrm{sol}^2 / N_\mathrm{min}^2 - 1}}
- = \frac{L_D}{\sqrt{4 N_\mathrm{sol}^2 \exp(-3/2) - 1}}
+ \boxed{
+ L_\mathrm{WB}
+ = \frac{T_0^2}{\beta_2 \, \sqrt{- f_\mathrm{min}}}
+ = \frac{L_D}{\sqrt{N_\mathrm{sol}^2 / N_\mathrm{min}^2 - 1}}
+ }
\end{aligned}$$
This prediction for $L_\mathrm{WB}$ appears to agree well
@@ -196,7 +202,7 @@ Filling $L_\mathrm{WB}$ in into $\omega_\mathrm{SPM}$ gives:
$$\begin{aligned}
\omega_{\mathrm{SPM}}(L_\mathrm{WB},t)
- = \frac{2 \gamma P_0 t}{\beta_2 \sqrt{4 N_\mathrm{sol}^2 \exp(-3/2) - 1}} \exp\!\Big(\!-\frac{t^2}{T_0^2}\Big)
+ = \frac{2 \gamma P_0 t}{\beta_2 \sqrt{4 N_\mathrm{sol}^2 \exp(-3/2) - 1}} \exp\!\Big(\!-\!\frac{t^2}{T_0^2}\Big)
\end{aligned}$$
Assuming that $N_\mathrm{sol}^2$ is large in the denominator, this can
@@ -205,8 +211,8 @@ be approximately reduced to:
$$\begin{aligned}
\omega_\mathrm{SPM}(L_\mathrm{WB}, t)
% = \frac{2 \gamma P_0 t \exp(-t^2 / T_0^2)}{\beta_2 \sqrt{N_\mathrm{sol}^2 / N_\mathrm{min}^2 - 1}}
- \approx \frac{2 \gamma P_0 t}{\beta_2 N_\mathrm{sol}} \exp\!\Big(\!-\frac{t^2}{T_0^2}\Big)
- = 2 \sqrt{\frac{\gamma P_0}{\beta_2}} \frac{t}{T_0} \exp\!\Big(\!-\frac{t^2}{T_0^2}\Big)
+ \approx \frac{2 \gamma P_0 t}{\beta_2 N_\mathrm{sol}} \exp\!\Big(\!-\!\frac{t^2}{T_0^2}\Big)
+ = 2 \sqrt{\frac{\gamma P_0}{\beta_2}} \frac{t}{T_0} \exp\!\Big(\!-\!\frac{t^2}{T_0^2}\Big)
\end{aligned}$$
The expression $x \exp(-x^2)$ has its global extrema