Inverse Surface Melting in Confined Clusters: Ar13in Zeolite L

Abstract

Monte Carlo and molecular dynamics simulations on an Ar13 cluster in zeolite L have been carried out at a series of temperatures to understand the rigid−nonrigid transition corresponding to the solid−liquid transition exhibited by the free Ar13 cluster. The icosahedral geometry of the free cluster is no longer preferred when the cluster is confined in the zeolite. The root-mean-squared pair distance fluctuation, δ, exhibits a sharp, well-defined rigid−nonrigid transition at 17 K as compared to 27 K for the free cluster. Multiple peaks in the distribution of short-time averages of the guest−host interaction energy indicate coexistence of two phases. It is shown that this transition is associated with the inner atoms becoming mobile at 17 K even while the outer layer atoms, which are in close proximity to the zeolitic wall, continue to be comparatively immobile. This may be contrasted with the melting of large free clusters of 40 or more atoms which exhibit surface melting. Guest−host interactions seem to play a predominant role in determining the properties of confined clusters. We demonstrate that the volume of the cluster increases rather sharply at 17 and 27 K respectively for the confined and the free cluster. Power spectra suggest that the motion of the inner atoms is generally parallel to the atoms which form the cage wall.