Theory and experiments on the ice-water front propagation in droplets freezing on a subzero surface
Michael Nauenberg

TL;DR
This paper presents an approximate theory and experimental validation of ice-water front propagation in freezing water droplets on various subzero surfaces, highlighting the influence of substrate heat conductivity and challenging previous assumptions.
Contribution
The study introduces a new approximate theoretical model for droplet freezing and provides experimental data comparing different substrates, revealing limitations of prior constant-temperature assumptions.
Findings
The heat conductivity of the substrate affects freezing dynamics.
Experimental results show the base temperature varies during freezing.
Previous models assuming constant base temperature are not accurate.
Abstract
An approximate theory is presented describing the propagation of the ice-water front that develops in droplets of water that are deposited on a planar surface at a temperature below the melting point of ice. A calculation based on this theory is compared with our experimental observations of the time evolution of this front. The results of calculations of this front by Schultz et al7, obtained by integrating numerically the exact differential equations for this problem, were published graphically, but only for the time-dependent velocity of this front. Unfortunately, these theoretical results cannot be compared directly with our experimental observations. Our experiments were performed by freezing water droplets directly on a block of dry ice, and in order to examine the effects of the heat conductivity of a substrate during the freezing process, such droplets were also deposited on a…
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