Abstract
An isothermal layer suspended from a surface is gravitationally (Rayleigh-Taylor) unstable. We find that, when a vertical temperature difference above a critical value is imposed across the liquid-gas layer system (heated from below), the restoring force provided by the temperature-dependent surface tension (thermocapillarity) can stabilize the layer. Our measurements of the most unstable wave number for agree well with our linear stability analysis. The instability occurs at long wavelengths: the most unstable wavelength at is infinite.
- Received 18 July 2000
DOI:https://doi.org/10.1103/PhysRevLett.86.1203
©2001 American Physical Society