Biblio: boulders

biblio/chapters/literature.tex

@@ -426,6 +426,14 @@ porosity induced friction.
 
 \section{Block displacement by waves}
 
+\subsection{Introduction}
+
+Displacement of blocks or boulders by waves has been a major topic in
+understanding the influence of storm and tsunami waves in coastal regions.
+Several approaches have been taken to study this phenomenon. In a first part,
+we will discuss in-situ studies on displaced boulders. In a second part, we
+will review models of block displacements.
+
 \subsection{In-situ studies}
 
 \cite{barbano2010large}
@@ -435,6 +443,7 @@ porosity induced friction.
 \cite{biolchi2016}
 \cite{kennedy2016observations}
 \cite{erdmann2018boulder}
+\cite{cox2018extraordinary}
 
 \subsection{Models}
 
@@ -442,7 +451,7 @@ porosity induced friction.
 
 \cite{nott2003waves} Submerged boulder:
 \begin{equation}
-u^2 \ge \frac{2\left(\rho_s-\frac{\rho_s}{\rho_w}\right)ag}
+u^2 \ge \frac{2\left(\frac{\rho_s}{\rho_w}-1\right)ag}
 {C_d\left(\frac{ac}{b^2}\right)+C_l}
 \end{equation}
 
@@ -467,7 +476,7 @@ u^2 \ge \frac{2\left(\frac{\rho_s}{\rho_w}-1\right) gc
 \cite{kennedy2017extreme}
 \cite{weiss2017toward}
 
-\cite{bressan2018laboratory}
+\cite{bressan2018laboratory} Partially submerged boulders
 \begin{equation}
 u^2 \ge \frac{2b_wW}{\rho_w\left(b_DC_DA_{wfs}+b_LC_LA_{wbs}\right)}
 \end{equation}