English

Scaling limit and cube-root fluctuations in SOS surfaces above a wall

Probability 2013-02-28 v1 Mathematical Physics math.MP

Abstract

Consider the classical (2+1)(2+1)-dimensional Solid-On-Solid model above a hard wall on an L×LL\times L box of \bbZ2\bbZ^2. The model describes a crystal surface by assigning a non-negative integer height ηx\eta_x to each site xx in the box and 0 heights to its boundary. The probability of a surface configuration η\eta is proportional to exp(βH(η))\exp(-\beta \mathcal{H}(\eta)), where β\beta is the inverse-temperature and H(η)\mathcal{H}(\eta) sums the absolute values of height differences between neighboring sites. We give a full description of the shape of the SOS surface for low enough temperatures. First we show that with high probability the height of almost all sites is concentrated on two levels, H(L)=(1/4β)logLH(L)=\lfloor (1/4\beta)\log L\rfloor and H(L)1H(L)-1. Moreover, for most values of LL the height is concentrated on the single value H(L)H(L). Next, we study the ensemble of level lines corresponding to the heights (H(L),H(L)1,...)(H(L),H(L)-1,...). We prove that w.h.p. there is a unique macroscopic level line for each height. Furthermore, when taking a diverging sequence of system sizes LkL_k, the rescaled macroscopic level line at height H(Lk)nH(L_k)-n has a limiting shape if the fractional parts of (1/4β)logLk(1/4\beta)\log L_k converge to a noncritical value. The scaling limit is an explicit convex subset of the unit square QQ and its boundary has a flat component on the boundary of QQ. Finally, the highest macroscopic level line has Lk1/3+o(1)L_k^{1/3+o(1)} fluctuations along the flat part of the boundary of its limiting shape.

Keywords

Cite

@article{arxiv.1302.6941,
  title  = {Scaling limit and cube-root fluctuations in SOS surfaces above a wall},
  author = {Pietro Caputo and Eyal Lubetzky and Fabio Martinelli and Allan Sly and Fabio Lucio Toninelli},
  journal= {arXiv preprint arXiv:1302.6941},
  year   = {2013}
}

Comments

54 pages, 8 figures

R2 v1 2026-06-21T23:33:52.658Z