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Hydraulics of Structures: Energy Dissipation via Ski-Jump Bucket Spillways

When downstream tailwater depths are too low for a stable hydraulic jump stilling basin, Ski-Jump (Trajectory) Buckets throw high-velocity spillway flows into the air, dispersing kinetic energy into the atmosphere before impact. The trajectory distance $(x)$ and maximum height $(y_{max})$ of the jet arc are derived from projectile kinematics:

$x = \frac{v_0^2}{g} \cdot \sin(2\theta) \quad \text{and} \quad y_{max} = \frac{v_0^2 \cdot \sin^2\theta}{2 \cdot g}$

​Where $v_0$ is bucket exit velocity and $\theta$ is the lip angle above horizontal (typically $30^\circ \text{ to } 45^\circ).$ To prevent scour hole formation from undercutting the dam, the depth of pre-formed or natural plunge pool scour $(d_s)$ is calculated using Veronese’s Formula:

$d_s = 1.90 \cdot H_T^{0.225} \cdot q^{0.54} - y_t$

​Where $H_T$ is head drop, $q$ is unit discharge, and $y_t$ is downstream tailwater depth.

​Ski-jump buckets are widely deployed in narrow Himalayan river gorges (such as the Tehri and Nathpa Jhakri dam complexes) where high fall heads and narrow channels make wide stilling basins unfeasible.

​Modern hydraulic designs use trajectory CFD models paired with physical scale modeling to shape flip bucket radii and lip angles. Structural engineers line plunge pool plunge zones with heavy concrete armor blocks to absorb dynamic impact pressures and mitigate localized bed erosion.

​Note: This technical content was curated and structured with AI assistance to support technical education. 

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