{ "id": "1503.03273", "version": "v1", "published": "2015-03-11T11:11:56.000Z", "updated": "2015-03-11T11:11:56.000Z", "title": "From atoms to steps: The microscopic origins of crystal evolution", "authors": [ "Paul N. Patrone", "T. L. Einstein", "Dionisios Margetis" ], "comment": "7 pages, 6 figures", "journal": "Surface Science, Vol. 625 (2014), pp. 37-43", "doi": "10.1016/j.susc.2014.02.015", "categories": [ "cond-mat.mes-hall" ], "abstract": "The BCF theory of crystal growth has been successful in describing a wide range of phenomena in surface physics. Typical crystal surfaces are slightly misoriented with respect to a facet plane; thus, the BCF theory views such systems as composed of staircase-like structures of steps separating terraces. Adsorbed atoms (adatoms), which are represented by a continuous density, diffuse on terraces, and steps move by absorbing or emitting these adatoms. Here we shed light on the microscopic origins of the BCF theory by deriving a simple, one-dimensional (1D) version of the theory from an atomistic, kinetic restricted solid-on- solid (KRSOS) model without external material deposition. We define the time-dependent adatom density and step position as appropriate ensemble averages in the KRSOS model, thereby exposing the non-equilibrium statistical mechanics origins of the BCF theory. Our analysis reveals that the BCF theory is valid in a low adatom-density regime, much in the same way that an ideal gas approximation applies to dilute gasses. We find conditions under which the surface remains in a low-density regime and discuss the microscopic origin of corrections to the BCF model.", "revisions": [ { "version": "v1", "updated": "2015-03-11T11:11:56.000Z" } ], "analyses": { "keywords": [ "microscopic origin", "crystal evolution", "ideal gas approximation applies", "bcf theory views", "low adatom-density regime" ], "tags": [ "journal article" ], "note": { "typesetting": "TeX", "pages": 7, "language": "en", "license": "arXiv", "status": "editable" } } }