“…Previous work on surface diffusion has focused on such nucleation, growth and coalescence aspects, analyzing the time evolution of the monomer and island densities, characterizing the island size distributions, and describing the origin of the island capture numbers and capture zones. − Similarly, much effort has been invested on clarifying the differences and similarities between the tracer and collective diffusion coefficients, and describing them for various systems. − The tracer diffusivity, D T , which is the relevant transport coefficient when the particles can be followed, can be determined using three alternative formulations, e.g., eqs 1, 3, and 19 in ref . In this study, we present a fourth expression, describing D T in terms of the total hop rate, R h , defined as the sum of all distinct hop rates accessible to the adparticles, each multiplied by the corresponding hop multiplicity (the number of hops that share a given rate).…”