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notebooks:peclet_number [2025/02/14 10:41] – rishabhstein | notebooks:peclet_number [Unknown date] (current) – external edit (Unknown date) 127.0.0.1 | ||
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\text{Pe} = \frac{\tau_D}{\tau_A} = \frac{v_0 l_0}{D} | \text{Pe} = \frac{\tau_D}{\tau_A} = \frac{v_0 l_0}{D} | ||
\end{equation} | \end{equation} | ||
- | For larger length scales ($\text{Pe} \gg 1$), flow in the system is naturally advection-dominated, | + | For larger length scales ($\text{Pe} \gg 1$), flow in the system is naturally advection-dominated, |