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-rw-r--r--source/know/concept/rayleigh-plateau-instability/index.md86
1 files changed, 43 insertions, 43 deletions
diff --git a/source/know/concept/rayleigh-plateau-instability/index.md b/source/know/concept/rayleigh-plateau-instability/index.md
index 2ba060c..5dcf77f 100644
--- a/source/know/concept/rayleigh-plateau-instability/index.md
+++ b/source/know/concept/rayleigh-plateau-instability/index.md
@@ -16,11 +16,11 @@ It is the reason why a smooth stream of water (e.g. from a tap)
eventually breaks into droplets as it falls.
Consider an infinitely long cylinder of liquid
-with radius $R_0$ and surface tension $\alpha$.
+with radius $$R_0$$ and surface tension $$\alpha$$.
In this case, the [Young-Laplace equation](/know/concept/young-laplace-law/)
states that its internal pressure
-is a constant $p_i$ expressed as follows,
-where $p_o$ is the exterior air pressure:
+is a constant $$p_i$$ expressed as follows,
+where $$p_o$$ is the exterior air pressure:
$$\begin{aligned}
p_i
@@ -28,12 +28,12 @@ $$\begin{aligned}
\end{aligned}$$
We assume that the liquid is at rest.
-Alternatively, if it is moving in the $z$-direction,
+Alternatively, if it is moving in the $$z$$-direction,
we can also let our coordinate system travel at the same speed.
Anyway, for convenience,
we neglect any motion or acceleration of the liquid column.
-Next, we add a perturbation $p_\epsilon$, assumed to be small,
+Next, we add a perturbation $$p_\epsilon$$, assumed to be small,
to the internal pressure, which we allow to vary with time and space.
We use cylindrical coordinates:
@@ -42,7 +42,7 @@ $$\begin{aligned}
\end{aligned}$$
This internal pressure difference will cause the liquid to start to flow.
-We express the flow velocity as a vector $\vec{u} = (u_r, u_\phi, u_z)$,
+We express the flow velocity as a vector $$\vec{u} = (u_r, u_\phi, u_z)$$,
which obeys the following Euler equations:
$$\begin{aligned}
@@ -53,7 +53,7 @@ $$\begin{aligned}
\end{aligned}$$
The latter equation states that the fluid is incompressible.
-We assume that $\vec{u}$ is so small that we can ignore
+We assume that $$\vec{u}$$ is so small that we can ignore
the quadratic term in the former equation, leaving:
$$\begin{aligned}
@@ -62,7 +62,7 @@ $$\begin{aligned}
\end{aligned}$$
Taking the divergence and using incompressibility
-yields the Laplace equation for $p_\epsilon$:
+yields the Laplace equation for $$p_\epsilon$$:
$$\begin{aligned}
- \frac{1}{\rho} \nabla^2 p_\epsilon
@@ -81,7 +81,7 @@ $$\begin{aligned}
= 0
\end{aligned}$$
-Finally, we add a perturbation $R_\epsilon \ll R_0$
+Finally, we add a perturbation $$R_\epsilon \ll R_0$$
to the radius of the surface of the liquid column:
$$\begin{aligned}
@@ -89,13 +89,13 @@ $$\begin{aligned}
= R_0 + R_\epsilon(z, t)
\end{aligned}$$
-Note that there is no dependence on the angle $\phi$;
+Note that there is no dependence on the angle $$\phi$$;
the deformation is assumed to be symmetric.
Imagine the cross-section of the cylinder,
and convince yourself that all asymmetric deformations
will be removed by surface tension, which prefers a circular shape.
-We thus assume that $R_\epsilon$, $p_\epsilon$ and $\vec{u}$
-do not depend on $\phi$.
+We thus assume that $$R_\epsilon$$, $$p_\epsilon$$ and $$\vec{u}$$
+do not depend on $$\phi$$.
The Laplace equation then reduces to:
$$\begin{aligned}
@@ -105,9 +105,9 @@ $$\begin{aligned}
\end{aligned}$$
Before solving this, we need boundary conditions.
-The radial fluid velocity $u_r$ (the $r$-component of $\vec{u}$)
-at the column surface $r\!=\!R$ is the
-[material derivative](/know/concept/material-derivative/) of $R_\epsilon$:
+The radial fluid velocity $$u_r$$ (the $$r$$-component of $$\vec{u}$$)
+at the column surface $$r\!=\!R$$ is the
+[material derivative](/know/concept/material-derivative/) of $$R_\epsilon$$:
$$\begin{aligned}
u_r(r\!=\!R)
@@ -115,17 +115,17 @@ $$\begin{aligned}
= \pdv{R_\epsilon}{t} + u_z(r\!=\!R) \pdv{R_\epsilon}{z}
\end{aligned}$$
-We linearize this by assuming that the deformation $R_\epsilon$
-varies slowly with respect to $z$:
+We linearize this by assuming that the deformation $$R_\epsilon$$
+varies slowly with respect to $$z$$:
$$\begin{aligned}
u_r(r\!=\!R)
\approx \pdv{R_\epsilon}{t}
\end{aligned}$$
-Meanwhile, we can write the boundary condition of the pressure $p$
+Meanwhile, we can write the boundary condition of the pressure $$p$$
in two ways, respectively from the Young-Laplace equation
-and the definition of the perturbation $p_\epsilon$:
+and the definition of the perturbation $$p_\epsilon$$:
$$\begin{aligned}
p(r\!=\!R)
@@ -135,32 +135,32 @@ $$\begin{aligned}
= p_i + p_\epsilon(r\!=\!R)
\end{aligned}$$
-Where $R_1$ and $R_2$ are the principal curvature radii of the column surface.
+Where $$R_1$$ and $$R_2$$ are the principal curvature radii of the column surface.
These two expressions must be equivalent,
-so, by inserting the definition of $p_i = p_o + \alpha / R_0$:
+so, by inserting the definition of $$p_i = p_o + \alpha / R_0$$:
$$\begin{aligned}
p_o + \alpha \Big( \frac{1}{R_1} + \frac{1}{R_2} \Big)
= p_o + \frac{\alpha}{R_0} + p_\epsilon(r\!=\!R)
\end{aligned}$$
-Isolating this equation for $p_\epsilon$ yields the desired boundary condition:
+Isolating this equation for $$p_\epsilon$$ yields the desired boundary condition:
$$\begin{aligned}
p_\epsilon(r\!=\!R)
= \alpha \Big( \frac{1}{R_1} + \frac{1}{R_2} \Big) - \frac{\alpha}{R_0}
\end{aligned}$$
-The principal radius around the circumference is $R_0 + R_\epsilon$,
+The principal radius around the circumference is $$R_0 + R_\epsilon$$,
while the curvature along the length can be approximated
-using the second $z$-derivative of $R_\epsilon$:
+using the second $$z$$-derivative of $$R_\epsilon$$:
$$\begin{aligned}
p_\epsilon(r\!=\!R)
\approx \alpha \Big( \frac{1}{R_0 + R_\epsilon} - \pdvn{2}{R_\epsilon}{z} \Big) - \frac{\alpha}{R_0}
\end{aligned}$$
-This can be simplified a bit by using the assumption that $R_\epsilon$ is small:
+This can be simplified a bit by using the assumption that $$R_\epsilon$$ is small:
$$\begin{aligned}
p_\epsilon(r\!=\!R)
@@ -170,8 +170,8 @@ $$\begin{aligned}
At last, we have all the necessary boundary condition.
We now make the following ansatz,
-where $k$ is the wavenumber
-and $\sigma$ describes exponential growth or decay:
+where $$k$$ is the wavenumber
+and $$\sigma$$ describes exponential growth or decay:
$$\begin{aligned}
\vec{u}(r, z, t)
@@ -187,7 +187,7 @@ $$\begin{aligned}
This is justified by the fact that we can Fourier-expand any perturbation;
this ansatz is simply the dominant term of the resulting series.
-Inserting this into the Laplace equation for $p_\epsilon$ yields
+Inserting this into the Laplace equation for $$p_\epsilon$$ yields
Bessel's modified equation of order zero:
$$\begin{aligned}
@@ -195,8 +195,8 @@ $$\begin{aligned}
= 0
\end{aligned}$$
-This has well-known solutions: the modified Bessel functions $I_0$ and $K_0$.
-However, because $K_0$ diverges at $r = 0$, we must set the constant $B = 0$:
+This has well-known solutions: the modified Bessel functions $$I_0$$ and $$K_0$$.
+However, because $$K_0$$ diverges at $$r = 0$$, we must set the constant $$B = 0$$:
$$\begin{aligned}
p_\epsilon(r)
@@ -204,7 +204,7 @@ $$\begin{aligned}
= A I_0(kr)
\end{aligned}$$
-Inserting the ansatz into the boundary condition for $p_\epsilon$
+Inserting the ansatz into the boundary condition for $$p_\epsilon$$
gives us the following relation:
$$\begin{aligned}
@@ -213,8 +213,8 @@ $$\begin{aligned}
= A I_0(k R)
\end{aligned}$$
-Meanwhile, the linearized Euler equation governing $\vec{u}$
-states that $u_r$ is given by:
+Meanwhile, the linearized Euler equation governing $$\vec{u}$$
+states that $$u_r$$ is given by:
$$\begin{aligned}
\sigma u_r
@@ -222,7 +222,7 @@ $$\begin{aligned}
= - \frac{A k}{\rho} I_0'(kr)
\end{aligned}$$
-Now that we have an expression for $u_r$,
+Now that we have an expression for $$u_r$$,
we can revisit its boundary condition:
$$\begin{aligned}
@@ -231,8 +231,8 @@ $$\begin{aligned}
= \sigma R_\epsilon
\end{aligned}$$
-Isolating this for $R_\epsilon$ and inserting it
-into the boundary condition for $p_\epsilon$ yields:
+Isolating this for $$R_\epsilon$$ and inserting it
+into the boundary condition for $$p_\epsilon$$ yields:
$$\begin{aligned}
p_\epsilon(r\!=\!R)
@@ -240,18 +240,18 @@ $$\begin{aligned}
= \alpha \Big( \frac{1}{R_0^2} + k^2 \Big) \Big( \frac{A k}{\rho \sigma^2} I_0'(k R) \Big)
\end{aligned}$$
-Isolating this for the exponential growth/decay parameter $\sigma$
+Isolating this for the exponential growth/decay parameter $$\sigma$$
gives us the desired result,
-where we have also used the fact that $R \approx R_0$:
+where we have also used the fact that $$R \approx R_0$$:
$$\begin{aligned}
\sigma^2
= \frac{\alpha k}{\rho R_0^2} (1 - k^2 R_0^2) \frac{I_0'(kR_0)}{I_0(kR_0)}
\end{aligned}$$
-To get exponential growth (i.e. instability), we need $\sigma^2 > 0$.
-Since $(1 - k^2 R_0^2)$ is the only factor that can be negative,
-we need $k R_0 < 1$, leading us to the **critical wavelength** $\lambda_c$:
+To get exponential growth (i.e. instability), we need $$\sigma^2 > 0$$.
+Since $$(1 - k^2 R_0^2)$$ is the only factor that can be negative,
+we need $$k R_0 < 1$$, leading us to the **critical wavelength** $$\lambda_c$$:
$$\begin{aligned}
\boxed{
@@ -261,12 +261,12 @@ $$\begin{aligned}
}
\end{aligned}$$
-If the perturbation wavelength $\lambda$ is larger than $\lambda_c$,
+If the perturbation wavelength $$\lambda$$ is larger than $$\lambda_c$$,
surface tension creates a higher pressure in the narrower sections
compared to the wider ones, thereby pumping the liquid into the bulges,
further increasing their size until they become droplets.
-Else, if $\lambda < \lambda_c$, the tighter curvatures
+Else, if $$\lambda < \lambda_c$$, the tighter curvatures
dominate the action of surface tension,
which will then try to smoothen the surface by shrinking the bulges
and widening the constrictions.