Abstract
AbstractWe describe an experimental study of the forces acting on a square cylinder (of width $\def \xmlpi #1{}\def \mathsfbi #1{\boldsymbol {\mathsf {#1}}}\let \le =\leqslant \let \leq =\leqslant \let \ge =\geqslant \let \geq =\geqslant \def \Pr {\mathit {Pr}}\def \Fr {\mathit {Fr}}\def \Rey {\mathit {Re}}b$) which occupies 10–40 % of a channel (of width $w$), fixed in a free-surface channel flow. The force experienced by the obstacle depends critically on the Froude number upstream of the obstacle, ${\mathit{Fr}}_1$ (depth $h_1$), which sets the downstream Froude number, ${\mathit{Fr}}_2$ (depth $h_2$). When ${\mathit{Fr}}_1<{\mathit{Fr}}_{1c}$, where ${\mathit{Fr}}_{1c}$ is a critical Froude number, the flow is subcritical upstream and downstream of the obstacle. The drag effect tends to decrease or increase the water depth downstream or upstream of the obstacle, respectively. The force is form drag caused by an attached wake and scales as $\overline{F_{D}}\simeq C_D \rho b u_1^2 h_1/2$, where $C_D$ is a drag coefficient and $u_1$ is the upstream flow speed. The empirically determined drag coefficient is strongly influenced by blocking, and its variation follows the trend $C_D=C_{D0}(1+C_{D0}b/2w)^2$, where $C_{D0}=1.9$ corresponds to the drag coefficient of a square cylinder in an unblocked turbulent flow. The r.m.s. lift force is approximately 10–40 % of the mean drag force and is generated by vortex shedding from the obstacle. When ${\mathit{Fr}}_1={\mathit{Fr}}_{1c}\, (<1)$, the flow is choked and adjusts by generating a hydraulic jump downstream of the obstacle. The drag force scales as $\overline{F}_D\simeq C_K \rho b g (h_1^2-h_2^2)/2$, where experimentally we find $C_K\simeq 1$. The r.m.s. lift force is significantly smaller than the mean drag force. A consistent model is developed to explain the transitional behaviour by using a semi-empirical form of the drag force that combines form and hydrostatic components. The mean drag force scales as $\overline{F_{D}}\simeq \lambda \rho b g^{1/3} u_1^{4/3} h_1^{4/3}$, where $\lambda $ is a function of $b/w$ and ${\mathit{Fr}}_1$. For a choked flow, $\lambda =\lambda _c$ is a function of blocking ($b/w$). For small blocking fractions, $\lambda _c= C_{D0}/2$. In the choked flow regime, the largest contribution to the total drag force comes from the form-drag component.
Highlights
The Japan (2011) and Indian Ocean (2004) tsunami led to significant loss of life and destruction of city infrastructure, including businesses and homes
Experimental results To examine the influence of the channel flow on the force acting on the obstacle, both the channel volume flux Q and the initial channel water depth hI were varied
As the Froude number Fr1 approaches a critical value, we observe that the water depth decreases rapidly around the sides of the obstacle and a hydraulic jump is generated just downstream
Summary
The Japan (2011) and Indian Ocean (2004) tsunami led to significant loss of life and destruction of city infrastructure, including businesses and homes. While the initial damage in coastal regions was largely caused by slamming forces, significant damage was caused by the quasi-steady flow of sea water around buildings, which generated stress on the building panels, torque on the buildings and buoyancy forces that carried wooden buildings away. Theoretical studies by Nagler (1918) and the large-scale experiments of Yarnell (1934a,b) focused on predicting changes in the upstream water depth – the backwater effect – caused by streamlined piers. The key concept these authors introduced was a classification of the flow types observed, which we describe here as being either subcritical or choked. The change in water depth is quite dramatic and is characterised by a hydraulic jump downstream
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