A common, intuitive, way of defining free energy is as being the internal energy of a thermodynamical system that is available to perform work.
In the thermodynamical thery of surface tension, we can relate this quantity with a free energy per area unit: \begin{equation} \Omega_s=\gamma S \end{equation}
Let's say that I, somehow, create a gradient $\nabla\gamma$ of surface tension on the surface. In the region of "less" surface tension, we could then conclude that there's less internal energy available to perform work on this region, while in the regions of "more" surface tension we have more internal energy available to perform work.
One well-known phenomena where this takes place is the Marangoni Effect. There, the particles tend to move to the region of higher surface tension.
And that's what I want to understand: Why does the particles tend to go to these regions? That is, why does the particles tend to go to the regions where there's more energy available to perform work?
I thought about some chemical aspects of surface tension, but it would be interesting if I could describe this aspect physically, with mathematics.