This is a small tutorial to illustrate the use of KITE to investigate materials with anisotropic electrical conductivity. To this end, we consider a simplified tight-binding model for single layer phosphorene 1. Even though this model is very simple, it captures the anisotropic band structure of phosphorene, which is Dirac like in one direction and Schrödinger like in the other direction. This behaviour results in highly anisotropic transport properties along the different directions 2.

Here, we calculate the single energy longitudinal conductivity (`singleshot_conductivity_dc`

) in the vicinity of the band gap and show that a fast numerical calculation, that is set to run in a normal laptop for about 3-4 minutes, can reproduce qualitatively the expected anisotropic conductivity along **xx** and **yy** directions.

Here, we highlight parts of the python scripts. The complete scripts can be downloaded here for the xx conductivity and here for the yy conductivity .

After the imports that are necessary for *KITE*, we define the lattice, with Pybinding syntax:

```
def monolayer_4band(num_hoppings=4):
"""Monolayer phosphorene lattice using the four-band model
Parameters
----------
num_hoppings : int
Number of hopping terms to consider: from t2 to t5.
"""
a = 0.222 # nm
ax = 0.438 # nm
ay = 0.332 # nm
theta = 96.79 * (pi / 180)
phi = 103.69 * (pi / 180)
lat = pb.Lattice(a1=[ax, 0], a2=[0, ay])
h = a * sin(phi - pi / 2)
s = 0.5 * ax - a * cos(theta / 2)
lat.add_sublattices(('A', [-s/2, -ay/2, h], 0),
('B', [ s/2, -ay/2, 0], 0),
('C', [-s/2 + ax/2, 0, 0], 0),
('D', [ s/2 + ax/2, 0, h], 0))
lat.register_hopping_energies({'t1': -1.22, 't2': 3.665, 't3': -0.205,
't4': -0.105, 't5': -0.055})
if num_hoppings < 2:
raise RuntimeError("t1 and t2 must be included")
elif num_hoppings > 5:
raise RuntimeError("t5 is the last one")
if num_hoppings >= 2:
lat.add_hoppings(([-1, 0], 'A', 'D', 't1'),
([-1, -1], 'A', 'D', 't1'),
([ 0, 0], 'B', 'C', 't1'),
([ 0, -1], 'B', 'C', 't1'))
lat.add_hoppings(([ 0, 0], 'A', 'B', 't2'),
([ 0, 0], 'C', 'D', 't2'))
if num_hoppings >= 3:
lat.add_hoppings(([ 0, 0], 'A', 'D', 't3'),
([ 0, -1], 'A', 'D', 't3'),
([ 1, 1], 'C', 'B', 't3'),
([ 1, 0], 'C', 'B', 't3'))
if num_hoppings >= 4:
lat.add_hoppings(([ 0, 0], 'A', 'C', 't4'),
([ 0, -1], 'A', 'C', 't4'),
([-1, 0], 'A', 'C', 't4'),
([-1, -1], 'A', 'C', 't4'),
([ 0, 0], 'B', 'D', 't4'),
([ 0, -1], 'B', 'D', 't4'),
([-1, 0], 'B', 'D', 't4'),
([-1, -1], 'B', 'D', 't4'))
if num_hoppings >= 5:
lat.add_hoppings(([-1, 0], 'A', 'B', 't5'),
([-1, 0], 'C', 'D', 't5'))
lat.min_neighbors = 2
return lat
```

This model, as defined above, can be used with different number of hoppings. The user can decide the number that is used in the calculation when defining the lattice:

```
lattice=monolayer_4band(num_hoppings=4)
```

To use the large-scale “single-shot” algorithm for direct evaluation of zero-temperature DC conductivities, the resolvent operator requires a nonzero broadening (resolution) parameter `eta`

, which is given in eV. As this type of calculation is energy dependent, it is also necessary to provide a list of desired energy points to the calculation object. In the single shot calculations, the computational time scales linearly with the energy points. For this example, that is intended to run in a normal desktop, we consider a small number of points and the energy range is set in the vicinity of the band gap.

The number of points and the list of energy points can be created when calling the calculation, as illustrated here:

```
calculation = kite.Calculation(configuration)
calculation.singleshot_conductivity_dc(energy=[(1.0 / 25 * i)*3.5 for i in range(25)],
num_moments=512, num_random=5, num_disorder=1,
direction='xx', eta=0.02)
```

Alternatively, one can define the number of points and the energy list outside calculation

```
npoints=25
epoints=[(1.0 / npoints * i)*3.5 for i in range(npoints)]
calculation.singleshot_conductivity_dc(epoints, num_moments=512, num_random=5,
num_disorder=1, direction='xx', eta=0.02)
```

Now it is time to save the configuration in a hdf file:

```
kite.config_system(lattice, configuration, calculation, modification, 'phxx.h5')
```

It is not possible to request same type of calculation in a single call. In this case, we want to calculate the conductivity in xx and yy directions where the type of the calculation is the same, which means we need another hdf file for yy conductivity.

Let’s repeat the procedure for another direction:

```
calculation.singleshot_conductivity_dc(epoints, num_moments=512, num_random=5,
num_disorder=1, direction='xx', eta=0.02)
kite.config_system(lattice, configuration, calculation, modification, 'phyy.h5')
```

For completeness, we provide the two python scripts for both orientations.

The result of this fast calculation can be seen in the figure below, for `l1=512, l2=512`

. To get a feeling of how KITE works, we suggest modifying parameters like `eta`

and `num_random`

.

In the next figure, we repeat the calculation for 300 energy points and 10 random vectors and a large energy window.

1 Alexander N. Rudenko, Mikhail I. Katsnelson, Phys. Rev. B **89**, 201408 (2014)

2 H. Liu, A. T. Neal, Z. Zhu, X. Xu , D. Tomanek and P. D. Ye, ACS Nano 8, 4033 (2014) .