# Creating slabs with ASE

ASE is short for the atomistic simulation environment, a Python package to simplify the process of setting up, running and analysing results from atomistic simulations across different programs. Extremely powerful in this respect are the routines this code provides for setting up complicated systems (including surface-adsorption scenarios, defects, nanotubes, etc). See also the ASE installation instructions.

This example shows how to use ASE to setup a particular gallium arsenide surface and run the resulting calculation in DFTK. If you are less interested in having access to the full playground of options in DFTK, but more interested in performing analysis in ASE itself, have a look at asedftk. This package provides an ASE-compatible calculator based on DFTK, such that one may write the usual Python scripts against ASE, but the calculations are still run in DFTK.

The particular example we consider the (1, 1, 0) GaAs surface separated by vacuum with the setup slightly adapted from ^{[RCW2001]}.

Parameters of the calculation. Since this surface is far from easy to converge, we made the problem simpler by choosing a smaller `Ecut`

and smaller values for `n_GaAs`

and `n_vacuum`

. More interesting settings are `Ecut = 15`

and `n_GaAs = n_vacuum = 20`

.

```
miller = (1, 1, 0) # Surface Miller indices
n_GaAs = 2 # Number of GaAs layers
n_vacuum = 4 # Number of vacuum layers
Ecut = 5 # Hartree
kgrid = (4, 4, 1); # Monkhorst-Pack mesh
```

Use ASE to build the structure:

```
using PyCall
ase_build = pyimport("ase.build")
a = 5.6537 # GaAs lattice parameter in Ångström (because ASE uses Å as length unit)
gaas = ase_build.bulk("GaAs", "zincblende", a=a)
surface = ase_build.surface(gaas, miller, n_GaAs, 0, periodic=true);
```

Get the amount of vacuum in Ångström we need to add

```
d_vacuum = maximum(maximum, surface.cell) / n_GaAs * n_vacuum
surface = ase_build.surface(gaas, miller, n_GaAs, d_vacuum, periodic=true);
```

Write an image of the surface and embed it as a nice illustration:

```
pyimport("ase.io").write("surface.png", surface * (3, 3, 1),
rotation="-90x, 30y, -75z")
```

Use the `load_atoms`

, `load_positions`

and `load_lattice`

functions to convert to DFTK datastructures. These two functions not only support importing ASE atoms into DFTK, but a few more third-party datastructures as well. Typically the imported `atoms`

use a bare Coulomb potential, such that appropriate pseudopotentials need to be attached in a post-step:

```
using DFTK
positions = load_positions(surface)
lattice = load_lattice(surface)
atoms = map(load_atoms(surface)) do el
if el.symbol == :Ga
ElementPsp(:Ga, psp=load_psp("hgh/pbe/ga-q3.hgh"))
elseif el.symbol == :As
ElementPsp(:As, psp=load_psp("hgh/pbe/as-q5.hgh"))
else
error("Unsupported element: $el")
end
end;
```

We model this surface with (quite large a) temperature of 0.01 Hartree to ease convergence. Try lowering the SCF convergence tolerance (`tol`

) or the `temperature`

or try `mixing=KerkerMixing()`

to see the full challenge of this system.

```
model = model_DFT(lattice, atoms, positions, [:gga_x_pbe, :gga_c_pbe],
temperature=0.001, smearing=DFTK.Smearing.Gaussian())
basis = PlaneWaveBasis(model; Ecut, kgrid)
scfres = self_consistent_field(basis, tol=1e-4, mixing=LdosMixing());
```

n Energy log10(ΔE) log10(Δρ) Diag --- --------------- --------- --------- ---- 1 -16.58836257966 -0.58 4.6 2 -16.72543603026 -0.86 -1.01 1.0 3 -16.73068860659 -2.28 -1.58 3.8 4 -16.73127995249 -3.23 -2.16 2.6 5 -16.73133395342 -4.27 -2.61 2.9

`scfres.energies`

Energy breakdown (in Ha): Kinetic 5.8605376 AtomicLocal -105.6248843 AtomicNonlocal 2.3499093 Ewald 35.5044300 PspCorrection 0.2016043 Hartree 49.5752597 Xc -4.5981865 Entropy -0.0000040 total -16.731333953418

- RCW2001D. Raczkowski, A. Canning, and L. W. Wang
*Thomas-Fermi charge mixing for obtaining self-consistency in density functional calculations*Phys. Rev. B**64**, 121101(R).