Ice accretion on
economically valuable and strategically important
surfaces poses significant challenges. Current anti-/de-icing techniques
often have critical issues regarding their efficiency, convenience,
long-term stability, or sustainability. As an emerging ice mitigation
strategy, the thin-film surface acoustic wave (SAW) has great potentials
due to its high energy efficiency and effective integration on structural
surfaces. However, anti-/de-icing processes activated by SAWs involve
complex interfacial evolution and phase changes, and it is crucial
to understand the nature of dynamic solid–liquid–vapor
phase changes and ice nucleation, growth, and melting events under
SAW agitation. In this study, we systematically investigated the accretion
and removal of porous rime ice from structural surfaces activated
by SAWs. We found that icing and de-icing processes are strongly linked
with the dynamical interfacial phase and structure changes of rime
ice under SAW activation and the acousto-thermally induced localized
heating that facilitate the melting of ice crystals. Subsequently,
interactions of SAWs with the formed thin water layer at the ice/structure
interface result in significant streaming effects that lead to further
damage and melting of ice, liquid pumping, jetting, or nebulization.