Dynamics of a reactive spherical particle falling in a linearly stratified fluid

Abstract

Motivated by numerous geophysical applications, we have carried out laboratory experiments of a reactive (i.e. melting) solid sphere freely falling by gravity in a stratified environment, in the regime of large Reynolds ($Re$) and Froude numbers. We compare our results to non-reactive spheres in the same regime. First, we confirm for larger values of $Re$, the stratification drag enhancement previously observed for low and moderate Re (Magnaudet and Mercier, 2020). We also show an even more significant drag enhancement due to melting, much larger than the stratification-induced one. We argue that the mechanism for both enhancements is similar, due to the specific structure of the vorticity field sets by buoyancy effects and associated baroclinic torques, as deciphered for stratification by Zhang et al. (2019). Using particle image velocimetry, we then characterize the long-term evolution (at time $t\gg 1/N$ with $N$ the Brünt-Väisälä frequency) of the internal wave field generated by the wake of the spheres. Measured wave field is similar for both reactive and inert spheres: indeed, each sphere fall might be considered as a quasi impulsive source of energy in time and the horizontal direction, as the falling time (resp. the sphere radius) is much smaller than $N$ (resp. than the tank width). Internal gravity waves are generated by wake turbulence over a broad spectrum, with the least damped component being at the Brünt-Väisälä frequency and the largest admissible horizontal wavelength. About 1% of the initial potential energy of each sphere is converted in to kinetic energy in the internal waves, with no significant dependence on the Froude number over the explored range.

References in corpus (7)

• Generation of Internal Waves by Buoyant Bubbles in Galaxy Clusters and Heating of Intracluster Medium
• Iron Snow in the Martian Core?
• Inertial drag on a sphere settling in a stratified fluid
• Mercury's magnetic field in the MESSENGER era
• Transient stratification force on particles crossing a density interface
• Heat and water vapor transfer in the wake of a falling ice sphere and its implication for secondary ice formation in clouds
• Fe alloy slurry and a compacting cumulate pile across Earth's inner-core boundary

Cited by in corpus (1)

• Solid-liquid phase change in planetary cores