Dynamics of finger-type convection in double-diffusive instability

TL;DR

This study investigates finger-type double-diffusive convection through experiments and simulations, revealing growth stages, vortex formation, and transport mechanisms across different salinity contrasts.

Contribution

It provides a comprehensive, finger-resolved analysis of transient growth, transport, and saturation pathways in finger-type DDI, validated by experiments and high-resolution DNS.

Findings

Fingertip growth follows three stages: acceleration, steady propagation, and decay.

Peak growth rates increase with salinity contrast and match linear stability analysis.

Vortex ring formation at fingertips influences vertical and lateral transport modes.

Abstract

Finger-type convection in double-diffusive instability (DDI) controls mixing and scalar transport in many stratified flows, yet a quantitative, finger-resolved description of the transient growth, transport, and saturation pathways has been limited. Here, finger-type DDI is analyzed in a sealed-surface laboratory facility using synchronized planar laser-induced fluorescence (PLIF) and particle image velocimetry (PIV) at fixed thermal contrast $\Delta T=5^\circ$C and three salinity contrasts, $\Delta S=350$, 450, and 550 ppm, complemented by a matched high-resolution three-dimensional DNS. A systematic fingertip detection and tracking framework generates ensemble growth curves. Fingertip growth follows a sequence of three stages (acceleration, quasi-steady propagation, and decay). The peak growth rates increase monotonically with $\Delta S$, and nondimensional fingertip-height histories collapse onto a common trend. The peak growth rates are reproduced by DNS and agree with linear stability analysis, establishing experiment--DNS--theory consistency in the intermediate regime. The mixed-material area increases with time, initially following a common nondimensional trend before transitioning to $\Delta S$-dependent interaction and breakdown. Finger-scale measurements reveal the formation of a symmetric vortex ring at the fingertips for $\Delta S=450$ ppm, inducing vertical-aligned transport. At $\Delta S=550$ ppm the roll-up becomes asymmetric: stronger buoyancy amplifies shear, destabilizes the vortex ring, and produces a zig-zag/lateral-drift mode that enhances the lateral transport. Finally, the evolution of the buoyancy anomaly links the growth-rate phases to a time-dependent force balance in which increasing buoyancy drives acceleration, shear-induced resistance regulates quasi-steady propagation, and dilution with top-boundary influence yields late-stage fingertip deceleration.