In Computational Physics there are a number of different theoretical approaches to our disposal that are valid on different time and length scales. In this talk I will demonstrate that similar computational  approaches can be used to model rather different physical problems. Moreover, I will illustrate how a combination of different techniques that I have all worked with can be used to describe physical problems that span time and length scales over many orders of magnitude. In fact, such different theoretical techniques are complementary to each other, and form a hierarchy of models.

 

I will focus on two examples in this talk. In the first part, I will show how we can use density-functional theory (DFT) to calculate the vibrational frequencies of small vanadium clusters. DFT is a fully quantum mechanical approach that is essentially a parameter-free theory.  I will show how comparison of calculated spectra with the once measured experimentally allow us to determine the detailed atomistic structure of these small metal clusters.

 

In the second part, I will discuss multiscale modeling of epitaxial growth. Physical processes during epitaxial growth span length and time scales of many orders of magnitude. For example, on the microscopic level, atoms move several Angstroms (the lattice constant), and vibrate with a frequency of approx. 1013 1/s. On the other hand, phenomena and applications of practical interest occur on a timescale of seconds, with system sizes that can be microns or larger. The grand challenge is to link those vastly different time and length scales. DFT allows us to calculate the energetics of microscopic processes with very high accuracy. I will show how DFT can be used to predict the stability of surface reconstructions, and will discuss how microscopic parameters, for example diffusion constants, can be obtained. These microscopic parameters are indispensable input for kinetic Monte Carlo methods, or more coarse grained model.  I will then discuss a new technique, the level-set method, that describes the formation of islands during growth and the evolution of their boundaries. With this method, one can simulate the motion of a boundary that separates the phases of any two phase problem, and I will show how the method is used to describe epitaxial growth.