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