# Crystals and band structure¶

In this tutorial we calculate properties of crystals.

## Setting up bulk structures¶

ASE provides three frameworks for setting up bulk structures:

Let’s run a simple bulk calculation.

Exercise

Use ase.build.bulk() to get a primitive cell of silver, then visualize it.

Silver is known to form an FCC structure, so presumably the function returned a primitive FCC cell. But it’s always nice to be sure what we have in front of us. Can you recognize it as FCC? You can e.g. use the ASE GUI to repeat the structure and recognize the A-B-C stacking. ASE should also be able to verify that it really is a primitive FCC cell and tell us what lattice constant was chosen:

print(atoms.cell.get_bravais_lattice())


Periodic structures in ASE are represented using atoms.cell and atoms.pbc. The cell is a Cell object which represents the crystal lattice with three vectors. pbc is an array of three booleans indicating whether the system is periodic in each direction.

## Bulk calculation¶

For periodic DFT calculations we should generally use a number of k-points which properly samples the Brillouin zone. Many calculators including GPAW and Aims accept the kpts keyword which can be a tuple such as (4, 4, 4). In GPAW, the planewave mode is very well suited for smaller periodic systems. Using the planewave mode, we should also set a planewave cutoff (in eV):

from gpaw import GPAW, PW
calc = GPAW(mode=PW(600), kpts=(8, 8, 8),
setups={'Ag': '11'}, ...)


Here we have used the setups keyword to specify that we want the 11-electron PAW dataset instead of the default which has 17 electrons, making the calculation faster.

(In principle, we should be sure to converge both kpoint sampling and planewave cutoff – I.e., write a loop and try different samplings so we know both are good enough to accurately describe the quantity we want.)

Exercise

Run a single-point calculation of bulk silver with GPAW. Save the ground-state in GPAW’s own format using calc.write('Ag.gpw').

## Density of states¶

Having saved the ground-state, we can reload it for ASE to extract the density of states:

import matplotlib.pyplot as plt
from ase.dft.dos import DOS
from gpaw import GPAW

calc = GPAW('groundstate.gpw')
dos = DOS(calc, npts=500, width=0)
energies = dos.get_energies()
weights = dos.get_dos()
plt.plot(energies, weights)
plt.show()


Calling the DOS class with width=0 means ASE well calculate the DOS using the linear tetrahedron interpolation method, which takes time but gives a nicer representation. We could also have given it a nonzero width such as the default value of 0.1 (eV). In that case it would have used a simple Gaussian smearing with that width, but we would need more k-points to get a plot of the same quality.

Note that the zero point of the energy axis is the Fermi energy.

Exercise

Plot the DOS.

You probably recall that an Ag atom has 10 d electrons and one s electron.

Which parts of the spectrum do you think originate (mostly) from s electrons? And which parts (mostly) from d electrons?

Time for analysis. As we probably know, the d-orbitals in a transition metal atom are localized close to the nucleus while the s-electron is much more delocalized.

In bulk systems, the s-states overlap a lot and therefore split into a very broad band over a wide energy range. d-states overlap much less and therefore also split less: They form a narrow band with a very high DOS. Very high indeed because there are 10 times as many d electrons as there are s electrons.

So to answer the question, the d-band accounts for most of the states forming the big, narrow chunk between -6.2 eV to -2.6 eV. Anything outside that interval is due to the much broader s band.

The DOS above the Fermi level may not be correct, since the SCF convergence criterion (in this calculation) only tracks the convergenece of occupied states. Hence, the energies over the Fermi level 0 are probably wrong.

What characterises the noble metals Cu, Ag, and Au, is that the d-band is fully occupied. I.e.: The whole d-band lies below the Fermi level (energy=0). If we had calculated any other transition metal, the Fermi level would lie somewhere within the d-band.

Note

We could calculate the s, p, and d-projected DOS to see more conclusively which states have what character. In that case we should look up the GPAW documentation, or other calculator-specific documentation. So let’s not do that now.

## Band structure¶

Let’s calculate the band structure of silver.

First we need to set up a band path. Our favourite image search engine can show us some reference graphs. We might find band structures from both Exciting and GPAW with Brillouin-zone path $$\mathrm{W L \Gamma X W K}$$. Luckily ASE knows these letters and can also help us visualize the reciprocal cell:

lat = atoms.cell.get_bravais_lattice()
print(lat.description())
lat.plot_bz(show=True)


In general, the ase.lattice module provides BravaisLattice classes used to represent each of the 14 + 5 Bravais lattices in 3D and 2D, respectively. These classes know about the high-symmetry k-points and standard Brillouin-zone paths (using the AFlow conventions).

Exercise

Build a band path for $$\mathrm{W L \Gamma X W K}$$. You can use path = atoms.cell.bandpath(...) — see the Cell documentation for which parameters to supply. This gives us a BandPath object.

You can print() the band path object to see some basic information about it, or use its write() method to save the band path to a json file such as path.json. Then visualize it using the command:

$ase reciprocal path.json  Once we are sure we have a good path with a reasonable number of k-points, we can run the band structure calculation. How to trigger a band structure calculation depends on which calculator we are using, so we would typically consult the documentation for that calculator (ASE will one day provide shortcuts to make this easier with common calculators): calc = GPAW('groundstate.gpw') atoms = calc.get_atoms() path = atoms.cell.bandpath(<...>) calc.set(kpts=path, symmetry='off', fixdensity=True)  We have here told GPAW to use our bandpath for k-points, not to perform symmetry-reduction of the k-points, and to fix the electron density. Then we trigger a new calculation, which will be non-selfconsistent, and extract and save the band structure: atoms.get_potential_energy() bs = calc.band_structure() bs.write('bs.json')  Again, the ASE command-line tool offers a helpful command to plot the band structure from a file: $ ase band-structure bs.json


Exercise

Calculate, save, and plot the band structure of silver for the path $$\mathrm{W L \Gamma X W K}$$.

You may need to zoom around a bit to see the whole thing at once. The plot will show the Fermi level as a dotted line (but does not define it as zero like the DOS plot before). Looking at the band structure, we see the complex tangle of what must be mostly d-states from before, as well as the few states with lower energy (at the $$\Gamma$$ point) and higher energy (crossing the Fermi level) attributed to s.

## Equation of state¶

We can find the optimal lattice parameter and calculate the bulk modulus by doing an equation-of-state calculation. This means sampling the energy and lattice constant over a range of values to get the minimum as well as the curvature, which gives us the bulk modulus.

The online ASE docs already provide a tutorial on how to do this, using the empirical EMT potential: https://wiki.fysik.dtu.dk/ase/tutorials/eos/eos.html

Exercise

Run the EOS tutorial.

## Complex crystals and cell optimisation¶

(If time is scarce, please consider skipping ahead to do the remaining exercises before returning here.)

For the simple FCC structure we only have a single parameter, a, and the EOS fit tells us everything there is to know.

For more complex structures we first of all need a more advanced framework to build the atoms, such as the ase.spacegroup.crystal() function.

The documentation helpfully tells us how to build a rutile structure, saving us the trouble of looking up the atomic basis and other crystallographic information. Rutile is a common mineral form of TiO2

Exercise

Build and visualize a rutile structure.

Let’s uptimise the structure. In addition to the positions, we must optimise the unit cell which, being tetragonal, is characterised by the two lengths a and c.

Optimising the cell requires the energy derivatives with respect to the cell parameters accessible through the stress tensor. atoms.get_stress() calculates and returns the stress as a vector of the 6 unique components (Voigt form). Using it requires that the attached calculator supports the stress tensor. GPAW’s planewave mode does this.

The ase.constraints.ExpCellFilter allows us to optimise cell and positions simultaneously. It does this by exposing the degrees of freedom to the optimiser as if they were additional positions — hence acting as a kind of filter. We use it by wrapping it around the atoms:

from ase.optimize import BFGS
from ase.constraints import ExpCellFilter
opt = BFGS(ExpCellFilter(atoms), ...)
opt.run(fmax=0.05)


Exercise

Use GPAW’s planewave mode to optimize the rutile unit cell. You will probably need a planewave cutoff of at least 500 eV. What are the optimised lattice constants a and c?

Exercise

Calculate the band structure of rutile. Does it agree with your favourite internet search engine?

## Solutions¶

Ag ground state:

from ase.build import bulk
from gpaw import GPAW, PW

atoms = bulk('Ag')
calc = GPAW(mode=PW(350), kpts=[8, 8, 8], txt='gpaw.bulk.Ag.txt',
setups={'Ag': '11'})
atoms.calc = calc
atoms.get_potential_energy()
calc.write('bulk.Ag.gpw')


Ag DOS:

import matplotlib.pyplot as plt
from gpaw import GPAW
from ase.dft.dos import DOS

calc = GPAW('bulk.Ag.gpw')
#energies, weights = calc.get_dos(npts=800, width=0)

dos = DOS(calc, npts=800, width=0)
energies = dos.get_energies()
weights = dos.get_dos()

ax = plt.gca()
ax.plot(energies, weights)
ax.set_xlabel('Energy [eV]')
ax.set_ylabel('DOS [1/eV]')
plt.savefig('dos.png')
plt.show()


Ag band structure:

from gpaw import GPAW
calc = GPAW('bulk.Ag.gpw')
atoms = calc.get_atoms()
path = atoms.cell.bandpath('WLGXWK', density=10)
path.write('path.json')

calc.set(kpts=path, fixdensity=True, symmetry='off')

atoms.get_potential_energy()
bs = calc.band_structure()
bs.write('bs.json')


Rutile cell optimisation:

from ase.constraints import ExpCellFilter
from ase.io import write
from ase.optimize import BFGS
from ase.spacegroup import crystal
from gpaw import GPAW, PW

a = 4.6
c = 2.95

# Rutile TiO2:
atoms = crystal(['Ti', 'O'], basis=[(0, 0, 0), (0.3, 0.3, 0.0)],
spacegroup=136, cellpar=[a, a, c, 90, 90, 90])
write('rutile.traj', atoms)

calc = GPAW(mode=PW(800), kpts=[2, 2, 3],
txt='gpaw.rutile.txt')
atoms.calc = calc

opt = BFGS(ExpCellFilter(atoms), trajectory='opt.rutile.traj')
opt.run(fmax=0.05)

calc.write('groundstate.rutile.gpw')

print('Final lattice:')
print(atoms.cell.get_bravais_lattice())


Rutile band structure:

from gpaw import GPAW

calc = GPAW('groundstate.rutile.gpw')
atoms = calc.get_atoms()
path = atoms.cell.bandpath(density=7)
path.write('path.rutile.json')

calc.set(kpts=path, fixdensity=True,
symmetry='off')

atoms.get_potential_energy()
bs = calc.band_structure()
bs.write('bs.rutile.json')