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Drop impact on superheated surfaces: short-time dynamics and transition to contact

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arxiv 2104.05354 v1 pith:SDZLU7R7 submitted 2021-04-12 physics.flu-dyn

classification physics.flu-dyn
keywords filmcontactdrainagevapordropimpactlevitationliquid
verification ladder T0 review T1 audit T2 compute T3 formal
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When a volatile drop impacts on a superheated solid, air drainage and vapor generation conspire to create an intermediate gas layer that delays or even prevents contact between the liquid and the solid. In this article, we use high-speed synchronized reflection interference and total internal reflection imaging to measure the short-time dynamics of the intermediate gas film and to probe the transition between levitation and contact. We observe that the substrate temperature strongly affects the vertical position of the liquid-gas interface and that the dynamic Leidenfrost transition is influenced by both air and vapor drainage (\emph{i.e}, gas drainage), and evaporation, the later giving rise to hitherto unreported vertical oscillations of the gas film that can trigger liquid-solid contact. We first derive scaling relations for the height of the gas film trapped under the drop's centerline, called the dimple height, and the minimum film thickness at short times. The former is set by a competition between gas drainage and liquid inertia, similarly as for isothermal impacts, while the later strongly depends on the vapor production. The gas pressure, at the location where the minimum thickness is reached, is determined by liquid inertia and vapor production and ultimately balanced by the increasing interfacial curvature, determining the minimum thickness. We show that, in the low impact velocity limit, the transient stability of the draining gas film remarkably makes dynamic levitation less demanding than static levitation. We characterise the vertical gas film oscillations by measuring their frequency and monitoring their occurrence in the parameter space spanned by surface temperature and impact velocity. Finally, we model the occurrence of these oscillations and account for their frequency through an hydrodynamic mechanism.

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