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-rw-r--r--source/know/concept/guiding-center-theory/index.md178
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diff --git a/source/know/concept/guiding-center-theory/index.md b/source/know/concept/guiding-center-theory/index.md
index 6de54fa..5368966 100644
--- a/source/know/concept/guiding-center-theory/index.md
+++ b/source/know/concept/guiding-center-theory/index.md
@@ -11,14 +11,14 @@ layout: "concept"
When discussing the [Lorentz force](/know/concept/lorentz-force/),
we introduced the concept of *gyration*:
-a particle in a uniform [magnetic field](/know/concept/magnetic-field/) $\vb{B}$
+a particle in a uniform [magnetic field](/know/concept/magnetic-field/) $$\vb{B}$$
*gyrates* in a circular orbit around a **guiding center**.
Here, we will generalize this result
to more complicated situations,
for example involving [electric fields](/know/concept/electric-field/).
The particle's equation of motion
-combines the Lorentz force $\vb{F}$
+combines the Lorentz force $$\vb{F}$$
with Newton's second law:
$$\begin{aligned}
@@ -28,7 +28,7 @@ $$\begin{aligned}
\end{aligned}$$
We now allow the fields vary slowly in time and space.
-We thus add deviations $\delta\vb{E}$ and $\delta\vb{B}$:
+We thus add deviations $$\delta\vb{E}$$ and $$\delta\vb{B}$$:
$$\begin{aligned}
\vb{E}
@@ -38,10 +38,10 @@ $$\begin{aligned}
\to \vb{B} + \delta\vb{B}(\vb{x}, t)
\end{aligned}$$
-Meanwhile, the velocity $\vb{u}$ can be split into
-the guiding center's motion $\vb{u}_{gc}$
-and the *known* Larmor gyration $\vb{u}_L$ around the guiding center,
-such that $\vb{u} = \vb{u}_{gc} + \vb{u}_L$.
+Meanwhile, the velocity $$\vb{u}$$ can be split into
+the guiding center's motion $$\vb{u}_{gc}$$
+and the *known* Larmor gyration $$\vb{u}_L$$ around the guiding center,
+such that $$\vb{u} = \vb{u}_{gc} + \vb{u}_L$$.
Inserting:
$$\begin{aligned}
@@ -49,7 +49,7 @@ $$\begin{aligned}
= q \big( \vb{E} + \delta\vb{E} + (\vb{u}_{gc} + \vb{u}_L) \cross (\vb{B} + \delta\vb{B}) \big)
\end{aligned}$$
-We already know that $m \: \idv{\vb{u}_L}{t} = q \vb{u}_L \cross \vb{B}$,
+We already know that $$m \: \idv{\vb{u}_L}{t} = q \vb{u}_L \cross \vb{B}$$,
which we subtract from the total to get:
$$\begin{aligned}
@@ -59,8 +59,8 @@ $$\begin{aligned}
This will be our starting point.
Before proceeding, we also define
-the average of $\Expval{f}$ of a function $f$ over a single gyroperiod,
-where $\omega_c$ is the cyclotron frequency:
+the average of $$\Expval{f}$$ of a function $$f$$ over a single gyroperiod,
+where $$\omega_c$$ is the cyclotron frequency:
$$\begin{aligned}
\Expval{f}
@@ -74,19 +74,19 @@ and focus only on the guiding center.
## Uniform electric and magnetic field
-Consider the case where $\vb{E}$ and $\vb{B}$ are both uniform,
-such that $\delta\vb{B} = 0$ and $\delta\vb{E} = 0$:
+Consider the case where $$\vb{E}$$ and $$\vb{B}$$ are both uniform,
+such that $$\delta\vb{B} = 0$$ and $$\delta\vb{E} = 0$$:
$$\begin{aligned}
m \dv{\vb{u}_{gc}}{t}
= q \big( \vb{E} + \vb{u}_{gc} \cross \vb{B} \big)
\end{aligned}$$
-Dotting this with the unit vector $\vu{b} \equiv \vb{B} / |\vb{B}|$
-makes all components perpendicular to $\vb{B}$ vanish,
+Dotting this with the unit vector $$\vu{b} \equiv \vb{B} / |\vb{B}|$$
+makes all components perpendicular to $$\vb{B}$$ vanish,
including the cross product,
leaving only the (scalar) parallel components
-$u_{gc\parallel}$ and $E_\parallel$:
+$$u_{gc\parallel}$$ and $$E_\parallel$$:
$$\begin{aligned}
m \dv{u_{gc\parallel}}{t}
@@ -95,8 +95,8 @@ $$\begin{aligned}
This simply describes a constant acceleration,
and is easy to integrate.
-Next, the equation for $\vb{u}_{gc\perp}$ is found by
-subtracting $u_{gc\parallel}$'s equation from the original:
+Next, the equation for $$\vb{u}_{gc\perp}$$ is found by
+subtracting $$u_{gc\parallel}$$'s equation from the original:
$$\begin{aligned}
m \dv{\vb{u}_{gc\perp}}{t}
@@ -104,11 +104,11 @@ $$\begin{aligned}
= q (\vb{E}_\perp + \vb{u}_{gc\perp} \cross \vb{B})
\end{aligned}$$
-Keep in mind that $\vb{u}_{gc\perp}$ explicitly excludes gyration.
-If we try to split $\vb{u}_{gc\perp}$ into a constant and a time-dependent part,
+Keep in mind that $$\vb{u}_{gc\perp}$$ explicitly excludes gyration.
+If we try to split $$\vb{u}_{gc\perp}$$ into a constant and a time-dependent part,
and choose the most convenient constant,
we notice that the only way to exclude gyration
-is to demand that $\vb{u}_{gc\perp}$ does not depend on time.
+is to demand that $$\vb{u}_{gc\perp}$$ does not depend on time.
Therefore:
$$\begin{aligned}
@@ -116,8 +116,8 @@ $$\begin{aligned}
= \vb{E}_\perp + \vb{u}_{gc\perp} \cross \vb{B}
\end{aligned}$$
-To find $\vb{u}_{gc\perp}$, we take the cross product with $\vb{B}$,
-and use the fact that $\vb{B} \cross \vb{E}_\perp = \vb{B} \cross \vb{E}$:
+To find $$\vb{u}_{gc\perp}$$, we take the cross product with $$\vb{B}$$,
+and use the fact that $$\vb{B} \cross \vb{E}_\perp = \vb{B} \cross \vb{E}$$:
$$\begin{aligned}
0
@@ -125,10 +125,10 @@ $$\begin{aligned}
= \vb{B} \cross \vb{E} + \vb{u}_{gc\perp} B^2
\end{aligned}$$
-Rearranging this shows that $\vb{u}_{gc\perp}$ is constant.
+Rearranging this shows that $$\vb{u}_{gc\perp}$$ is constant.
The guiding center drifts sideways at this speed,
-hence it is called a **drift velocity** $\vb{v}_E$.
-Curiously, $\vb{v}_E$ is independent of $q$:
+hence it is called a **drift velocity** $$\vb{v}_E$$.
+Curiously, $$\vb{v}_E$$ is independent of $$q$$:
$$\begin{aligned}
\boxed{
@@ -138,8 +138,8 @@ $$\begin{aligned}
\end{aligned}$$
Drift is not specific to an electric field:
-$\vb{E}$ can be replaced by a general force $\vb{F}/q$ without issues.
-In that case, the resulting drift velocity $\vb{v}_F$ does depend on $q$:
+$$\vb{E}$$ can be replaced by a general force $$\vb{F}/q$$ without issues.
+In that case, the resulting drift velocity $$\vb{v}_F$$ does depend on $$q$$:
$$\begin{aligned}
\boxed{
@@ -151,18 +151,18 @@ $$\begin{aligned}
## Non-uniform magnetic field
-Next, consider a more general case, where $\vb{B}$ is non-uniform,
-but $\vb{E}$ is still uniform:
+Next, consider a more general case, where $$\vb{B}$$ is non-uniform,
+but $$\vb{E}$$ is still uniform:
$$\begin{aligned}
m \dv{\vb{u}_{gc}}{t}
= q \big( \vb{E} + \vb{u}_{gc} \cross (\vb{B} + \delta\vb{B}) + \vb{u}_L \cross \delta\vb{B} \big)
\end{aligned}$$
-Assuming the gyroradius $r_L$ is small compared to the variation of $\vb{B}$,
-we set $\delta\vb{B}$ to the first-order term
-of a Taylor expansion of $\vb{B}$ around $\vb{x}_{gc}$,
-that is, $\delta\vb{B} = (\vb{x}_L \cdot \nabla) \vb{B}$.
+Assuming the gyroradius $$r_L$$ is small compared to the variation of $$\vb{B}$$,
+we set $$\delta\vb{B}$$ to the first-order term
+of a Taylor expansion of $$\vb{B}$$ around $$\vb{x}_{gc}$$,
+that is, $$\delta\vb{B} = (\vb{x}_L \cdot \nabla) \vb{B}$$.
We thus have:
$$\begin{aligned}
@@ -182,7 +182,7 @@ $$\begin{aligned}
+ \Expval{ \vb{u}_L \cross (\vb{x}_L \cdot \nabla) \vb{B} } \big)
\end{aligned}$$
-Where we have used that $\Expval{\vb{u}_{gc}} = \vb{u}_{gc}$.
+Where we have used that $$\Expval{\vb{u}_{gc}} = \vb{u}_{gc}$$.
The two averaged expressions turn out to be:
$$\begin{aligned}
@@ -198,9 +198,9 @@ $$\begin{aligned}
<label for="proof-nonuniform-B-averages">Proof</label>
<div class="hidden" markdown="1">
<label for="proof-nonuniform-B-averages">Proof.</label>
-We know what $\vb{x}_L$ is,
-so we can write out $(\vb{x}_L \cdot \nabla) \vb{B}$
-for $\vb{B} = (B_x, B_y, B_z)$:
+We know what $$\vb{x}_L$$ is,
+so we can write out $$(\vb{x}_L \cdot \nabla) \vb{B}$$
+for $$\vb{B} = (B_x, B_y, B_z)$$:
$$\begin{aligned}
(\vb{x}_L \cdot \nabla) \vb{B}
@@ -212,7 +212,7 @@ $$\begin{aligned}
\end{pmatrix}
\end{aligned}$$
-Integrating $\sin$ and $\cos$ over their period yields zero,
+Integrating $$\sin$$ and $$\cos$$ over their period yields zero,
so the average vanishes:
$$\begin{aligned}
@@ -220,8 +220,8 @@ $$\begin{aligned}
= 0
\end{aligned}$$
-Moving on, we write out $\vb{u}_L \cross (\vb{x}_L \cdot \nabla) \vb{B}$,
-suppressing the arguments of $\sin$ and $\cos$:
+Moving on, we write out $$\vb{u}_L \cross (\vb{x}_L \cdot \nabla) \vb{B}$$,
+suppressing the arguments of $$\sin$$ and $$\cos$$:
$$\begin{aligned}
\vb{u}_L \cross (\vb{x}_L \cdot \nabla) \vb{B}
@@ -247,7 +247,7 @@ $$\begin{aligned}
\end{pmatrix}
\end{aligned}$$
-Integrating products of $\sin$ and $\cos$ over their period gives us the following:
+Integrating products of $$\sin$$ and $$\cos$$ over their period gives us the following:
$$\begin{aligned}
\Expval{\cos^2} = \Expval{\sin^2} = \frac{1}{2}
@@ -256,7 +256,7 @@ $$\begin{aligned}
\end{aligned}$$
Inserting this tells us that the average
-of $\vb{u}_L \cross (\vb{x}_L \cdot \nabla) \vb{B}$ is given by:
+of $$\vb{u}_L \cross (\vb{x}_L \cdot \nabla) \vb{B}$$ is given by:
$$\begin{aligned}
\Expval{ \vb{u}_L \cross (\vb{x}_L \cdot \nabla) \vb{B} }
@@ -268,11 +268,11 @@ $$\begin{aligned}
\end{pmatrix}
\end{aligned}$$
-We use [Maxwell's equation](/know/concept/maxwells-equations/) $\nabla \cdot \vb{B} = 0$
-to rewrite the $z$-component,
-and follow the convention that $\vb{B}$
-points mostly in the $z$-direction,
-such that $B \equiv |\vb{B}| \approx B_z$:
+We use [Maxwell's equation](/know/concept/maxwells-equations/) $$\nabla \cdot \vb{B} = 0$$
+to rewrite the $$z$$-component,
+and follow the convention that $$\vb{B}$$
+points mostly in the $$z$$-direction,
+such that $$B \equiv |\vb{B}| \approx B_z$$:
$$\begin{aligned}
\Expval{ \vb{u}_L \cross (\vb{x}_L \cdot \nabla) \vb{B} }
@@ -290,6 +290,7 @@ $$\begin{aligned}
\end{pmatrix}
= - \frac{u_L^2}{2 \omega_c} \nabla B
\end{aligned}$$
+
</div>
</div>
@@ -301,11 +302,11 @@ $$\begin{aligned}
= q \bigg( \vb{E} + \vb{u}_{gc} \cross \vb{B} - \frac{u_L^2}{2 \omega_c} \nabla B \bigg)
\end{aligned}$$
-Let us now split $\vb{u}_{gc}$ into
-components $\vb{u}_{gc\perp}$ and $u_{gc\parallel} \vu{b}$,
+Let us now split $$\vb{u}_{gc}$$ into
+components $$\vb{u}_{gc\perp}$$ and $$u_{gc\parallel} \vu{b}$$,
which are respectively perpendicular and parallel
-to the magnetic unit vector $\vu{b}$,
-such that $\vb{u}_{gc} = \vb{u}_{gc\perp} \!+\! u_{gc\parallel} \vu{b}$.
+to the magnetic unit vector $$\vu{b}$$,
+such that $$\vb{u}_{gc} = \vb{u}_{gc\perp} \!+\! u_{gc\parallel} \vu{b}$$.
Consequently:
$$\begin{aligned}
@@ -322,9 +323,9 @@ $$\begin{aligned}
= q \bigg( \vb{E} + \vb{u}_{gc} \cross \vb{B} - \frac{u_L^2}{2 \omega_c} \nabla B \bigg)
\end{aligned}$$
-The derivative of $\vu{b}$ can be rewritten as follows,
-where $R_c$ is the radius of the field's [curvature](/know/concept/curvature/),
-and $\vb{R}_c$ is the corresponding vector from the center of curvature:
+The derivative of $$\vu{b}$$ can be rewritten as follows,
+where $$R_c$$ is the radius of the field's [curvature](/know/concept/curvature/),
+and $$\vb{R}_c$$ is the corresponding vector from the center of curvature:
$$\begin{aligned}
\dv{\vu{b}}{t}
@@ -336,8 +337,8 @@ $$\begin{aligned}
<label for="proof-nonuniform-B-curvature">Proof</label>
<div class="hidden" markdown="1">
<label for="proof-nonuniform-B-curvature">Proof.</label>
-Assuming that $\vu{b}$ does not explicitly depend on time,
-i.e. $\ipdv{\vu{b}}{t} = 0$,
+Assuming that $$\vu{b}$$ does not explicitly depend on time,
+i.e. $$\ipdv{\vu{b}}{t} = 0$$,
we can rewrite the derivative using the chain rule:
$$\begin{aligned}
@@ -346,16 +347,16 @@ $$\begin{aligned}
= u_{gc\parallel} \dv{\vu{b}}{s}
\end{aligned}$$
-Where $\dd{s}$ is the arc length of the magnetic field line,
-which is equal to the radius $R_c$ times the infinitesimal subtended angle $\dd{\theta}$:
+Where $$\dd{s}$$ is the arc length of the magnetic field line,
+which is equal to the radius $$R_c$$ times the infinitesimal subtended angle $$\dd{\theta}$$:
$$\begin{aligned}
\dd{s}
= R_c \dd{\theta}
\end{aligned}$$
-Meanwhile, across this arc, $\vu{b}$ rotates by $\dd{\theta}$,
-such that the tip travels a distance $|\dd{\vu{b}}|$:
+Meanwhile, across this arc, $$\vu{b}$$ rotates by $$\dd{\theta}$$,
+such that the tip travels a distance $$|\dd{\vu{b}}|$$:
$$\begin{aligned}
|\!\dd{\vu{b}}\!|
@@ -363,15 +364,15 @@ $$\begin{aligned}
= \dd{\theta}
\end{aligned}$$
-Furthermore, the direction $\dd{\vu{b}}$ is always opposite to $\vu{R}_c$,
-which is defined as the unit vector from the center of curvature to the base of $\vu{b}$:
+Furthermore, the direction $$\dd{\vu{b}}$$ is always opposite to $$\vu{R}_c$$,
+which is defined as the unit vector from the center of curvature to the base of $$\vu{b}$$:
$$\begin{aligned}
\dd{\vu{b}}
= - \vu{R}_c \dd{\theta}
\end{aligned}$$
-Combining these expressions for $\dd{s}$ and $\dd{\vu{b}}$,
+Combining these expressions for $$\dd{s}$$ and $$\dd{\vu{b}}$$,
we find the following derivative:
$$\begin{aligned}
@@ -380,6 +381,7 @@ $$\begin{aligned}
= - \frac{\vu{R}_c}{R_c}
= - \frac{\vb{R}_c}{R_c^2}
\end{aligned}$$
+
</div>
</div>
@@ -391,8 +393,8 @@ $$\begin{aligned}
= q \bigg( \vb{E} + \vb{u}_{gc} \cross \vb{B} - \frac{u_L^2}{2 \omega_c} \nabla B \bigg)
\end{aligned}$$
-Since both $\vb{R}_c$ and any cross product with $\vb{B}$
-will always be perpendicular to $\vb{B}$,
+Since both $$\vb{R}_c$$ and any cross product with $$\vb{B}$$
+will always be perpendicular to $$\vb{B}$$,
we can split this equation into perpendicular and parallel components like so:
$$\begin{aligned}
@@ -405,7 +407,7 @@ $$\begin{aligned}
The parallel part simply describes an acceleration.
The perpendicular part is more interesting:
-we rewrite it as follows, defining an effective force $\vb{F}_{\!\perp}$:
+we rewrite it as follows, defining an effective force $$\vb{F}_{\!\perp}$$:
$$\begin{aligned}
m \dv{\vb{u}_{gc\perp}}{t}
@@ -416,7 +418,7 @@ $$\begin{aligned}
\end{aligned}$$
To solve this, we make a crude approximation now, and improve it later.
-We thus assume that $\vb{u}_{gc\perp}$ is constant in time,
+We thus assume that $$\vb{u}_{gc\perp}$$ is constant in time,
such that the equation reduces to:
$$\begin{aligned}
@@ -426,8 +428,8 @@ $$\begin{aligned}
\end{aligned}$$
This is analogous to the previous case of a uniform electric field,
-with $q \vb{E}$ replaced by $\vb{F}_{\!\perp}$,
-so it is also solved by crossing with $\vb{B}$ in front,
+with $$q \vb{E}$$ replaced by $$\vb{F}_{\!\perp}$$,
+so it is also solved by crossing with $$\vb{B}$$ in front,
yielding a drift:
$$\begin{aligned}
@@ -436,11 +438,11 @@ $$\begin{aligned}
\equiv \frac{\vb{F}_{\!\perp} \cross \vb{B}}{q B^2}
\end{aligned}$$
-From the definition of $\vb{F}_{\!\perp}$,
-this total $\vb{v}_F$ can be split into three drifts:
-the previously seen electric field drift $\vb{v}_E$,
-the **curvature drift** $\vb{v}_c$,
-and the **grad-$\vb{B}$ drift** $\vb{v}_{\nabla B}$:
+From the definition of $$\vb{F}_{\!\perp}$$,
+this total $$\vb{v}_F$$ can be split into three drifts:
+the previously seen electric field drift $$\vb{v}_E$$,
+the **curvature drift** $$\vb{v}_c$$,
+and the **grad-$$\vb{B}$$ drift** $$\vb{v}_{\nabla B}$$:
$$\begin{aligned}
\boxed{
@@ -454,11 +456,11 @@ $$\begin{aligned}
}
\end{aligned}$$
-Such that $\vb{v}_F = \vb{v}_E + \vb{v}_c + \vb{v}_{\nabla B}$.
+Such that $$\vb{v}_F = \vb{v}_E + \vb{v}_c + \vb{v}_{\nabla B}$$.
We are still missing a correction,
-since we neglected the time dependence of $\vb{u}_{gc\perp}$ earlier.
-This correction is called $\vb{v}_p$,
-where $\vb{u}_{gc\perp} \approx \vb{v}_F + \vb{v}_p$.
+since we neglected the time dependence of $$\vb{u}_{gc\perp}$$ earlier.
+This correction is called $$\vb{v}_p$$,
+where $$\vb{u}_{gc\perp} \approx \vb{v}_F + \vb{v}_p$$.
We revisit the perpendicular equation, which now reads:
$$\begin{aligned}
@@ -466,10 +468,10 @@ $$\begin{aligned}
= \vb{F}_{\!\perp} + q \big( \vb{v}_F + \vb{v}_p \big) \cross \vb{B}
\end{aligned}$$
-We assume that $\vb{v}_F$ varies much faster than $\vb{v}_p$,
-such that $\idv{}{\vb{v}p}{t}$ is negligible.
-In addition, from the derivation of $\vb{v}_F$,
-we know that $\vb{F}_{\!\perp} + q \vb{v}_F \cross \vb{B} = 0$,
+We assume that $$\vb{v}_F$$ varies much faster than $$\vb{v}_p$$,
+such that $$\idv{}{\vb{v}p}{t}$$ is negligible.
+In addition, from the derivation of $$\vb{v}_F$$,
+we know that $$\vb{F}_{\!\perp} + q \vb{v}_F \cross \vb{B} = 0$$,
leaving only:
$$\begin{aligned}
@@ -477,11 +479,11 @@ $$\begin{aligned}
= q \vb{v}_p \cross \vb{B}
\end{aligned}$$
-To isolate this for $\vb{v}_p$,
-we take the cross product with $\vb{B}$ in front,
+To isolate this for $$\vb{v}_p$$,
+we take the cross product with $$\vb{B}$$ in front,
like earlier.
We thus arrive at the following correction,
-known as the **polarization drift** $\vb{v}_p$:
+known as the **polarization drift** $$\vb{v}_p$$:
$$\begin{aligned}
\boxed{
@@ -490,8 +492,8 @@ $$\begin{aligned}
}
\end{aligned}$$
-In many cases $\vb{v}_E$ dominates $\vb{v}_F$,
-so in some literature $\vb{v}_p$ is approximated as follows:
+In many cases $$\vb{v}_E$$ dominates $$\vb{v}_F$$,
+so in some literature $$\vb{v}_p$$ is approximated as follows:
$$\begin{aligned}
\vb{v}_p
@@ -502,7 +504,7 @@ $$\begin{aligned}
The polarization drift stands out from the others:
it has the opposite sign,
-it is proportional to $m$,
+it is proportional to $$m$$,
and it is often only temporary.
Therefore, it is also called the **inertia drift**.