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Growth and control of suspended ice bridges during sessile droplet freezing
Abstract The growth of in-plane ice tracks that connect supercooled sessile droplets is a physical phenomenon that accelerates large-scale frost propagation. However, the general mechanism of frost propagation through ice bridging, beyond in-plane ice tracks, remains unexplored. Here we observe the formation of suspended, out-of-plane ice bridges that connect freezing droplets.
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