We study the convective motion forced by lateral heating on a liquid layer. The movement is caused by two forces: buoyancy and thermocapillarity on the free surface, which is open to the air. As soon as a temperature gradient is imposed along the liquid layer, the fluid begins to move. When a certain threshold of the temperature di erence is attained, this flow destabilizes and oscillations appear. We have performed an experiment to characterize the thermocapillary waves in a rectangular container whose dimensions can be continuously changed. This way, we are able to investigate how boundaries a ect the threshold for the instability, as well as their consequences on other features of the waves
The instabilities of thermocapillary liquid layers with two free surfaces are examined by linear sta...
This work is devoted to the theoretical study of the stability of two superposed horizontal liquid l...
A thin liquid layer draining on a heated inclined plane is susceptible to long surface waves, and ca...
We study the convective motion forced by lateral heating on a liquid layer. The movement is caused ...
We report experiments on buoyant-thermocapillary instabilities in differentially heated liquid layer...
The stability of a liquid layer with an undeformable interface open to the atmosphere, subjected to ...
The stability of a liquid layer with an undeformable interface open to the atmosphere, subjected to ...
When a liquid layer is heated from the side, a monocellular flow develops immediately, no matter ho...
A shallow planar layer of liquid bounded from above by gas is set into motion via the thermocapillar...
This work is devoted to the theoretical study of the stability of two superposed horizontal liquid l...
This work is devoted to the theoretical study of the stability of two superposed horizontal liquid l...
Fluid motion driven by a temperature gradient imposed along a free liquid-gas interface is a well do...
This work is devoted to the theoretical study of the stability of two superposed horizontal liquid l...
We report experiments on buoyant-thermocapillary instabilities in differentially heated liquid layer...
The instabilities of thermocapillary liquid layers with two free surfaces are examined by linear sta...
The instabilities of thermocapillary liquid layers with two free surfaces are examined by linear sta...
This work is devoted to the theoretical study of the stability of two superposed horizontal liquid l...
A thin liquid layer draining on a heated inclined plane is susceptible to long surface waves, and ca...
We study the convective motion forced by lateral heating on a liquid layer. The movement is caused ...
We report experiments on buoyant-thermocapillary instabilities in differentially heated liquid layer...
The stability of a liquid layer with an undeformable interface open to the atmosphere, subjected to ...
The stability of a liquid layer with an undeformable interface open to the atmosphere, subjected to ...
When a liquid layer is heated from the side, a monocellular flow develops immediately, no matter ho...
A shallow planar layer of liquid bounded from above by gas is set into motion via the thermocapillar...
This work is devoted to the theoretical study of the stability of two superposed horizontal liquid l...
This work is devoted to the theoretical study of the stability of two superposed horizontal liquid l...
Fluid motion driven by a temperature gradient imposed along a free liquid-gas interface is a well do...
This work is devoted to the theoretical study of the stability of two superposed horizontal liquid l...
We report experiments on buoyant-thermocapillary instabilities in differentially heated liquid layer...
The instabilities of thermocapillary liquid layers with two free surfaces are examined by linear sta...
The instabilities of thermocapillary liquid layers with two free surfaces are examined by linear sta...
This work is devoted to the theoretical study of the stability of two superposed horizontal liquid l...
A thin liquid layer draining on a heated inclined plane is susceptible to long surface waves, and ca...