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7.3

The variational method

An approximation that needs no small parameter: guess any wavefunction you like — the energy it gives can never break below the true ground state, so the better the guess, the tighter the squeeze.

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After this section you should be able to

  • Prove the variational principle — the energy expectation of any normalised trial state is an upper bound on the ground-state energy
  • Construct parametrised trial wavefunctions and minimise over the parameters
  • Carry out the screened variational calculation for the helium ground state, obtaining −77.5 eV against the experimental −79.0 eV
  • State the method's strength (ground-state energies) and its blind spots (wavefunction detail, excited states, no error bar)

At the end of the last section, helium still owed us money: the electron repulsion is a third of the main part — hardly “small” — and first-order perturbation theory gives 74.8 eV-74.8\ \text{eV}, 4 eV away from the experimental 79.0 eV-79.0\ \text{eV}. To do better, grinding out second order means summing over infinitely many intermediate states — sheer misery. The root difficulty: perturbation theory needs a small parameter, and helium has none.

This section takes a completely different road. It makes no expansion whatsoever and asks nothing about the size of the perturbation. Its only weapon is a single inequality — and it is an inequality we already know how to prove.

The variational principle

This inequality instantly becomes a machine for computing energies:

  1. Guess a family of parametrised wavefunctions ψα\psi_\alpha (α\alpha can be one or several parameters);
  2. Compute E(α)=ψα|H^ψαE(\alpha)=\braket{\psi_\alpha}{\hat H\psi_\alpha};
  3. Minimise over α\alpha.

The minimum is still an upper bound — but it is the tightest upper bound in that family of guesses. The smarter the family, the closer the answer gets to the truth. This is the variational method: we “vary” over a family of wavefunctions to minimise the energy functional.

Warm-up: deliberately guessing the wrong shape

First, test the blade somewhere the exact answer is known, to see “what happens when the guess is wrong”. For hydrogen (true ground state: the exponential er/a0\ee^{-r/a_0}, E0=13.6 eVE_0=-13.6\ \text{eV}), deliberately pick the wrong shape as a trial — a Gaussian:

ψb(r)ebr2(7.3.5)\psi_b(r)\propto\ee^{-br^2}\tag{7.3.5}

with bb the variational parameter. Work out the kinetic and potential expectation values (both standard Gaussian integrals),

E(b)=32b2me24πε022bπ(7.3.6)E(b)=\frac{3\hbar^2b}{2m}-\frac{e^2}{4\pi\varepsilon_0}\,2\sqrt{\frac{2b}{\pi}}\tag{7.3.6}

Set the derivative in bb to zero and substitute back:

Emin=43πme4(4πε0)2211.5 eV(7.3.7)E_{\min}=-\frac{4}{3\pi}\,\frac{me^4}{(4\pi\varepsilon_0)^2\hbar^2} \approx-11.5\ \text{eV}\tag{7.3.7}

The true value is 13.6 eV-13.6\ \text{eV}. Two observations: the upper-bound promise held (11.5-11.5 really is above 13.6-13.6); and although the shape was completely wrong (a Gaussian is too flat at the origin and falls off too fast at large rr), the energy still captured 85%. That is the power of the “error is second-order small” theorem — and also its trap: an accurate energy does not mean an accurate wavefunction; ψb\psi_b is badly wrong both near the origin and far away.

The main course: the helium ground state

Time to settle the debt owed for two sections. The craft of building a trial wavefunction is writing your physical intuition into the parameters:

Each electron, besides being pulled by the nucleus (Z=2Z=2), is pushed away by the other electron. Seen from one electron’s viewpoint, the other’s cloud of negative charge “shades” part of the nucleus — the effective nuclear charge it feels should be less than 2, greater than 1 (the other electron is sometimes inside it and sometimes outside, so the shading is imperfect). This effect is called screening.

So guess: each electron sits in a hydrogen-like ground state of nuclear charge ZeZ_e, with ZeZ_e the variational parameter,

ψZe(r1,r2)=Ze3πa03eZe(r1+r2)/a0(7.3.8)\psi_{Z_e}(\vec r_1,\vec r_2)=\frac{Z_e^3}{\pi a_0^3}\, \ee^{-Z_e(r_1+r_2)/a_0}\tag{7.3.8}

and let energy minimisation decide “how much screening” for us.

When to use it, and where to be careful

The variational method applies startlingly widely: no small perturbation required, no nearby solvable model required — only the ability to compute ψ|H^ψ\braket{\psi}{\hat H\psi}. But its blind spots are just as sharp.

What comes next

Perturbation theory and the variational method both answer the same kind of question: where are the energy levels? But some questions are not about levels at all — how does an alpha particle escape the nucleus? How does an electron cross a barrier it could classically never climb? The protagonist of those questions is the wavefunction under the barrier, and there the wavefunction decays exponentially — no polynomial-style correction can keep up with it. The WKB approximation of the next section is built for exactly this “semiclassical” situation: when the potential varies slowly enough, the wavefunction is locally a plane wave at every point — and with that we will compute a tunnelling probability for the first time, and explain the lifetime law in nuclear physics that spans thirty orders of magnitude.

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