text: The previous two sections focused on two approaches to describe the experimentally observed 
  
  patterning dynamics in the ultrathin postcursor ﬁlm left behind by a mesoscopic receding dewet- 
  
  ting front. Although both the kinetic Monte Carlo model and the dynamical density functional 
  
  theory are able to describe well the processes in the ultrathin ﬁlm, they can not be employed to 
  
  describe mesoscale hydrodynamics. A relatively simple model for the latter can be derived in the 
  
  framework of a long-wave or lubrication equation [8, 63]. We will illustrate here the approach 
  
  by considering an isothermal situation where the nanoparticles are not surface active, i.e., they do 
  
  not act as surfactants. For a model incorporating the effects of latent heat generation and surface- 
  
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              [html]<thead><tr><td>active particies residing in bermal and solutar Maragonistresies, seeker, [ My ]. A lescripton of spreading particle solutions incorporating a structural disjoining pressure has also been considered</td><td>[ 89 ]. For related work on particle - laden film flow on an incline see Refs. [ 90.91 ].</td></tr></thead><tbody><tr><td>One starts from the Stokes equations, together with continuity, no - slip boundary conditions at the</td></tr><tr></tr><tr></tr></tbody>
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  18 