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author | Prefetch | 2022-01-30 11:27:00 +0100 |
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committer | Prefetch | 2022-01-30 11:27:00 +0100 |
commit | 88537b82784f71104c3a2771330c9e492f57fb03 (patch) | |
tree | 0d5ddb6adaf9e55892f4e7b79adf1e22cf0aee10 /content/know/concept/rayleigh-plateau-instability | |
parent | 8a9fb5fef2a97af3274290e512816e1a4cac0c02 (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.pdc | 1 |
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 $p_i = p_o + \alpha / R_0$: $$\begin{aligned} p_o + \alpha \Big( \frac{1}{R_1} + \frac{1}{R_2} \Big) - %= p_i + p_\epsilon(r\!=\!R) = p_o + \frac{\alpha}{R_0} + p_\epsilon(r\!=\!R) \end{aligned}$$ |