We present a lattice-gas (generalised Ising) model for liquid droplets on solid surfaces. The time evolution in the model involves two processes: (i) Single-particle moves which are determined by a kinetic Monte Carlo algorithm. These incorporate into the model particle diffusion over the surface and within the droplets and also evaporation and condensation, i.e. the exchange of particles between droplets and the surrounding vapour. (ii) Larger-scale collective moves, modelling advective hydrodynamic fluid motion, determined by considering the dynamics predicted by a thin-film equation. The model enables us to relate how macroscopic quantities such as the contact angle and the surface tension depend on the microscopic interaction parameters between the particles and with the solid surface. We present results for droplets joining, spreading, sliding under gravity, dewetting, the effects of evaporation, the interplay of diffusive and advective dynamics, and how all this behaviour depends on the temperature and other parameters. * Electronic address: A.J. Archer@lboro.ac.uk arXiv:1906.08121v1 [cond-mat.soft] 19 Jun 2019 is to use Monte Carlo methods to simulate the dynamic properties of Hamiltonian systems [18]. However, it is not clear to us that one should enforce detailed balance when constructing coarse grained models of such non-equilibrium systems, since droplets on surfaces are highly dissipative systems, due to the evaporation, the strong coupling to the substrate, etc. Of course, at equilibrium, there should be detailed balance in the model.To model collective hydrodynamic motion in our model, we generate large-scale collective particle moves by considering the dynamics that is predicted by a thin-film equation. This is a time evolution equation for the liquid film thickness profile h, i.e. the height of the liquid-vapour interface above the surface [2,[19][20][21][22]. This equation is derived from the Navier-Stokes equations for a film of liquid on a surface by making a long-wave approximation, which greatly simplifies the analysis. When generating these 'thin-film moves', we first determine the liquid film height profile from the configuration of occupied lattice sites, we then evolve the thin-film equation for a short amount of time, and then map back to the lattice. In our model, an important quantity is the parameter λ, defined below in Eq. (13), which is proportional to the ratio of the number of KMC attempted particle moves to the number of thin-film moves. When λ = 0, our model reduces to just evolving the thin-film equation, whilst in the limit λ → ∞, our model is a pure KMC model. Therefore, this parameter λ ∝ D/η, where D is a single-particle diffusion coefficient and η is the viscosity.Key quantities that characterises how a liquid wets a surface are the spreading parameter S = γ sv − (γ sl + γ lv ), where γ sv , γ sl , and γ lv are the solid-vapour, solid-liquid and liquid-vapour interfacial tensions, respectively [2], and also the contact angle θ, which is given by Young's equation [2]:The...