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Numerical Methods in Quantum Mechanics - Dipartimento di Fisica

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potential, we can hope to obta<strong>in</strong> a set of electronic levels that can describe the<br />

ma<strong>in</strong> features of the crystal. A rigorous basis for such approach can be provided<br />

by Hartree-Fock or Density-Functional theory. In the end, the basic step is to<br />

solve to the problem of calculat<strong>in</strong>g the energy levels <strong>in</strong> a perio<strong>di</strong>c potential.<br />

We haven’t yet said anyth<strong>in</strong>g about the composition and the perio<strong>di</strong>city of<br />

our system. Let us simplify further the problem and assume a one-<strong>di</strong>mensional<br />

array of atoms of the same k<strong>in</strong>d, regularly spaced by a <strong>di</strong>stance a. The atomic<br />

position of atom n will thus be given as a n = na, with n runn<strong>in</strong>g on all <strong>in</strong>teger<br />

numbers, positive and negative. In the jargon of solid-state physics, a is the<br />

lattice parameter, while the a n are the vectors of the crystal lattice. The system<br />

has a <strong>di</strong>screte translational <strong>in</strong>variance, that is: it is equal to itself if translated<br />

by a or multiples of a. Called V (x) the crystal potential, formed by the<br />

superposition of atomic-like potentials: V (x) = ∑ n V n(x − a n ), the follow<strong>in</strong>g<br />

symmetry holds: V (x + a) = V (x). Such symmetry plays a very important role<br />

<strong>in</strong> determ<strong>in</strong><strong>in</strong>g the properties of crystall<strong>in</strong>e solids. Our one-<strong>di</strong>mensional space<br />

(the <strong>in</strong>f<strong>in</strong>ite l<strong>in</strong>e) can be decomposed <strong>in</strong>to f<strong>in</strong>ite regions (segments) of space, of<br />

length a, perio<strong>di</strong>cally repeated. A region hav<strong>in</strong>g such property is called unit cell,<br />

and the smallest possible unit cell is called primitive cell. Its def<strong>in</strong>ition conta<strong>in</strong>s<br />

some degree of arbitrarity: for <strong>in</strong>stance, both <strong>in</strong>tervals [0, a[ and ] − a/2, +a/2]<br />

def<strong>in</strong>e a valid primitive cell <strong>in</strong> our case.<br />

9.1.1 Perio<strong>di</strong>c Boundary Con<strong>di</strong>tions<br />

Before start<strong>in</strong>g to look for a solution, we must ask ourselves how sensible it is<br />

to apply such idealized modell<strong>in</strong>g to a real crystal. The latter is formed by a<br />

macroscopically large (<strong>in</strong> the order of the Avogadro number or fractions of it)<br />

but f<strong>in</strong>ite number of atoms. We might consider <strong>in</strong>stead a f<strong>in</strong>ite system conta<strong>in</strong><strong>in</strong>g<br />

N atoms with N → ∞, but this is not a convenient way: translational<br />

symmetry is lost, due to the presence of surfaces (<strong>in</strong> our specific 1D case, the<br />

two ends). A much more convenient and formally correct approach is to <strong>in</strong>troduce<br />

perio<strong>di</strong>c boundary con<strong>di</strong>tions (PBC). Let us consider the system <strong>in</strong> a box<br />

with <strong>di</strong>mensions L = Na and let us consider solutions obey<strong>in</strong>g to the con<strong>di</strong>tion<br />

ψ(x) = ψ(x + L), i.e. perio<strong>di</strong>c solutions with period L >> a. We can imag<strong>in</strong>e<br />

our wave function that arrives at one end “re-enters” from the other side. In the<br />

one-<strong>di</strong>mensional case there is a simple representation of the system: our atoms<br />

are <strong>di</strong>stributed not on a straight l<strong>in</strong>e but on a r<strong>in</strong>g, with atom N between atom<br />

N − 1 and atom 1.<br />

The advantage of PBC is that we can treat the system as f<strong>in</strong>ite (a segment<br />

of length L <strong>in</strong> the one-<strong>di</strong>mensional case) but macroscopically large (hav<strong>in</strong>g N<br />

atoms, with N macroscopically large if a is a typical <strong>in</strong>teratomic <strong>di</strong>stance and<br />

L the typical size of a piece of crystal), still reta<strong>in</strong><strong>in</strong>g the <strong>di</strong>screte translational<br />

<strong>in</strong>variance. Case N → ∞ describes the so-called thermodynamical limit. It is to<br />

be noticed that a crystal with PBC has no surface. As a consequence there is no<br />

“<strong>in</strong>side” and “outside” the crystal: the latter is not contemplated. This is the<br />

price to pay for the big advantage of be<strong>in</strong>g able to use translational symmetry.<br />

In spite of PBC and of translational symmetry, the solution of the Schröd<strong>in</strong>ger<br />

equation for a perio<strong>di</strong>c potential does not yet look like a simple problem.<br />

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