Fully conservative hydraulic jumps and solibores in two-layer Boussinesq fluids

TL;DR

This paper investigates special fully conservative hydraulic jumps and solibores in two-layer Boussinesq fluids, revealing conditions for their existence and providing a new analytical solution that aligns with previous numerical results.

Contribution

It identifies specific conditions under which hydraulic jumps conserve energy and circulation, introduces a new analytical solibore solution, and links these to wave dispersion effects.

Findings

Certain large-amplitude jumps are fully conservative.

A new analytical solibore solution matches DNS results.

Wave dispersion is key to the lossy nature of internal bores.

Abstract

We consider a special type of hydraulic jumps (internal bores) which, in the vertically bounded system of two immiscible fluids with slightly different densities, conserve not only the mass and impulse but also the circulation and energy. This is possible only at specific combinations of the upstream and downstream states. Two such combinations are identified with arbitrary upstream and downstream interface heights. The first has a cross symmetry between the interface height and shear on both sides of the jump. This symmetry, which is due to the invariance of the two-layer shallow-water system with swapping the interface height and shear, ensures the automatic conservation of the impulse and energy as well as the continuity of characteristic velocities across the jump. The speed at which such jumps propagate is uniquely defined by the conservation of the mass and circulation. The other possibility is a marginally stable shear flow which can have fully conservative jumps with discontinuous characteristic velocities. Both types of conservative jumps are shown to represent a long-wave approximation to the so-called solibores which appear as smooth permanent-shape solutions in a weakly non-hydrostatic model. A new analytical solution for solibores is obtained and found to agree very well with the previous DNS results for partial-depth lock release flow. The finding that certain large-amplitude hydraulic jumps can be fully conservative, while most are not such even in the inviscid approximation, points toward the wave dispersion as a primary mechanism behind the lossy nature of internal bores.