Buoyancy-driven flow regimes for a melting vertical ice cylinder in saline water

Abstract

The presence of salt in seawater significantly affects the melt rate and morphological evolution of ice. This study investigates the melting process of a vertical cylinder in saline water using a combination of laboratory experiments and direct numerical simulations. The two-dimensional (2D) direct numerical simulations and 3D experiments achieve thermal Rayleigh numbers up to ${\text{Ra}}_T=\mathcal{O}\left(10^9\right)$ and saline Rayleigh numbers up to ${\text{Ra}}_S=\mathcal{O}\left(10^{12}\right)$. Some 3D simulations of the vertical ice cylinder are conducted at ${\text{Ra}}_T=\mathcal{O}\left(10^5\right)$ to confirm that the results in 2D simulations are qualitatively similar to those in 3D simulations. The mean melt rate exhibits a non-monotonic relationship with ambient salinity. With increasing salinity, the mean melt rate initially decreases towards the point where thermal and saline effects balance, after which it increases again. Based on the ambient salinity, the flow can be categorized into three regimes: temperature-driven flow, salinity-driven flow, and thermal-saline competing flow. In the temperature-driven and competing flow regimes, we find that the mean melt rate follows a ${\text{Ra}}_{T_d}^{1/4}$ scaling. In contrast, in the salinity-driven flow regime, we see a transition from a ${\text{Ra}}_{T_d}^{1/4}$ to a ${\text{Ra}}_{T_d}^{1/3}$ scaling. Additionally, the mean melt rate follows a ${\text{Ra}}_{S_d}^{1/3}$ scaling in this regime. The ice cylinder develops distinct morphologies in different flow regimes. In the thermal-saline competing flow regime, distinctive scallop (dimpled) patterns emerge along the ice cylinder due to the competition between thermal buoyancy and saline buoyancy. We observe these scallop patterns to migrate downwards over time, due to local differences in the melt rate, for which we provide a qualitative explanation.

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Cited by in corpus (3)

• Melting of floating ice cylinders in fresh and saline environments
• Collective effects of neighbouring melting ice objects
• Freezing and ice aging dynamics in saline water under natural convection