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authorPrefetch2022-01-30 11:27:00 +0100
committerPrefetch2022-01-30 11:27:00 +0100
commit88537b82784f71104c3a2771330c9e492f57fb03 (patch)
tree0d5ddb6adaf9e55892f4e7b79adf1e22cf0aee10 /content/know/concept/rayleigh-plateau-instability
parent8a9fb5fef2a97af3274290e512816e1a4cac0c02 (diff)
Expand knowledge base, remove comments
Diffstat (limited to 'content/know/concept/rayleigh-plateau-instability')
-rw-r--r--content/know/concept/rayleigh-plateau-instability/index.pdc1
1 files changed, 0 insertions, 1 deletions
diff --git a/content/know/concept/rayleigh-plateau-instability/index.pdc b/content/know/concept/rayleigh-plateau-instability/index.pdc
index 59407d6..ccb2e7c 100644
--- a/content/know/concept/rayleigh-plateau-instability/index.pdc
+++ b/content/know/concept/rayleigh-plateau-instability/index.pdc
@@ -146,7 +146,6 @@ so, by inserting the definition of $p_i = p_o + \alpha / R_0$:
$$\begin{aligned}
p_o + \alpha \Big( \frac{1}{R_1} + \frac{1}{R_2} \Big)
- %= p_i + p_\epsilon(r\!=\!R)
= p_o + \frac{\alpha}{R_0} + p_\epsilon(r\!=\!R)
\end{aligned}$$