Residence time of inertial particles in 3D thermal convection: implications for magma reservoirs

TL;DR

This study models how inertial particles, like crystals, settle in 3D convective flows, revealing how flow dynamics influence residence times, with implications for understanding magma solidification and crystal distribution in geological formations.

Contribution

It provides a robust 3D numerical model for particle residence time in convective flows, highlighting the transition from tracer-like to free-fall behavior and the effects of flow regimes on settling rates.

Findings

Residence time scales with Stokes velocity in different regimes.

Flow geometry significantly affects particle trapping and settling.

3D simulations are essential for accurate flow-particle interaction modeling.

Abstract

The dynamic behavior of crystals in convecting fluids determines how magma bodies solidify. In particular, it is often important to estimate how long crystals stay in suspension in the host liquid before being deposited at its bottom (or top, for light particles). We perform a systematic 3D numerical study of particle-laden Rayleigh-Benard convection, and derive a robust model for the particle residence time. For Rayleigh numbers higher than 10^7, inertial particles' trajectories exhibit a monotonic transition from fluid tracer-like to free-fall dynamics, the control parameter being the ratio between particle Stokes velocity and the fluid velocity. The average settling rate is proportional to the particle Stokes velocity in both the end-member regimes, but the distribution of the residence times differs markedly from one to the other. For lower Rayleigh numbers (<10^7), an interaction between large-scale circulation and particle motion emerges, increasing the settling rates on average. Nevertheless, the mean residence time does not exceed the terminal time, i.e. the settling time from a quiescent fluid, by a factor larger than four. An exception are simulations with only a slightly super-critical Rayleigh number (~ 10^4), for which stationary convection develops and some particles become trapped indefinitely. 2D simulations of the same problem overestimate the flow-particle interaction - and hence the residence time - for both high and low Rayleigh numbers, which stresses the importance of using 3D geometries for simulating particle-laden flows. We outline how our model can be used to explain depth changes of crystal size distribution in sedimentary layers of magmatic intrusions that are thought to have formed via settling of a crystal cargo, and discuss how the micro-structural observations of solidified intrusions can be used to infer the past convective velocity of magma.