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Biblio: submerged blocks equations

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Edgar P. Burkhart 2022-02-17 16:00:22 +01:00
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@ -439,11 +439,24 @@ porosity induced friction.
\subsection{Models}
\cite{nott1997extremely}
\cite{nott2003waves}
\cite{nott2003waves} Submerged boulder:
\begin{equation}
u^2 \ge \frac{2\left(\rho_s-\frac{\rho_s}{\rho_w}\right)ag}
{C_d\left(\frac{ac}{b^2}\right)+C_l}
\end{equation}
\cite{imamura2008numerical}
\cite{barbano2010large}
\cite{nandasena2011numerical}
\cite{nandasena2011reassessment}
\begin{equation}
u^2 \ge \frac{2\left(\frac{\rho_s}{\rho_w}-1\right) gc
\left(\cos\theta+\frac{c}{b}\sin\theta\right)}
{C_d\frac{c^2}{b^2}+C_l}
\end{equation}
\cite{buckley2012inverse}
\cite{weiss2012mystery}
\cite{nandasena2013boulder}
@ -453,7 +466,12 @@ porosity induced friction.
\cite{kennedy2016observations}
\cite{kennedy2017extreme}
\cite{weiss2017toward}
\cite{bressan2018laboratory}
\begin{equation}
u^2 \ge \frac{2b_wW}{\rho_w\left(b_DC_DA_{wfs}+b_LC_LA_{wbs}\right)}
\end{equation}
\cite{lodhi2020role}
\cite{oetjen2020significance}