The process of dewetting of a thin liquid film is usually described using a
long-wave approximation yielding a single evolution equation for the film
thickness. This equation incorporates an additional pressure term-the disjo
ining pressure-accounting for the molecular forces. Recently a disjoining p
ressure was derived coupling hydrodynamics to the diffuse interface model [
L. M. Pismen and Y. Pomeau. Phys. Rev. E 62, 2480 (2000)]. Using the result
ing evolution equation as a generic example for the evolution of unstable t
hin films, we examine the thickness ranges for linear instability and metas
tability for flat films, the families of stationary periodic and localized
solutions. and their linear stability. The results are compared to simulati
ons of the nonlinear time evolution. From this we conclude that. within the
linearly unstable thickness range, there exists a well defined subrange wh
ere finite perturbations are crucial for the time evolution and the resulti
ng structures. In the remainder of the linearly unstable thickness range th
e resulting structures are controlled by the fastest flat film mode assumed
up to now for the entire linearly unstable thickness range. Finally, the i
mplications for other forms of disjoining pressure in dewetting and for spi
nodal decomposition are discussed.