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Variational Method

Why approximations are needed

The variational method provides a systematic approach for making approximations and a quantitative way to assess the convergence of predictions toward exact values. Its core idea is simple:

Variational theorem

Consequences of the variational theorem

  1. Ground-state energy is the lowest possible energy for the system.

  2. By minimizing the energy functional we obtain the most accurate prediction for a given trial function.

  3. More parameters give us more handles to vary, and hence more accurate solutions.

Worked examples

The helium atom is tough

H^=22me(Δ1+Δ2)Kinetic energy14πϵ0(Ze2r1+Ze2r2e2r12Tough!)Potential energy{\hat{H} = \underbrace{-\frac{\hbar^2}{2m_e}\left(\Delta_1 + \Delta_2\right)}_{\textnormal{Kinetic energy}} \underbrace{- \frac{1}{4\pi\epsilon_0}\left(\frac{Ze^2}{r_1} + \frac{Ze^2}{r_2} \overbrace{- \frac{e^2}{r_{12}}}^{\textnormal{Tough!}}\right)}_{\textnormal{Potential energy}}}

Independent-electron approximation

H^=H^1+H^2{\hat{H} = \hat{H}_1 + \hat{H}_2}
H^1=22meΔ1Ze24πϵ0r1{\hat{H}_1 = -\frac{\hbar^2}{2m_e}\Delta_1 - \frac{Ze^2}{4\pi\epsilon_0r_1}}
H^2=22meΔ2Ze24πϵ0r2{\hat{H}_2 = -\frac{\hbar^2}{2m_e}\Delta_2 - \frac{Ze^2}{4\pi\epsilon_0r_2}}
H^1ψ(r1)=E1ψ(r1){\hat{H}_1\psi(r_1) = E_1\psi(r_1)}
H^2ψ(r2)=E2ψ(r2){\hat{H}_2\psi(r_2) = E_2\psi(r_2)}

The total energy is a sum of E1E_1 and E2E_2, and the total wavefunction is a product of ψ(r1)\psi(r_1) and ψ(r2)\psi(r_2). Based on our previous wavefunction table for hydrogen-like atoms:

E=E1+E2=RZ2(1n12+1n22){E = E_1 + E_2 = -RZ^2\left(\frac{1}{n_1^2} + \frac{1}{n_2^2}\right)}
ψ(r1)ψ(r2)=1π(Za0)3/2eZr1/a01π(Za0)3/2eZr2/a0=1π(Za0)3eZ(r1+r2)/a0{\psi(r_1)\psi(r_2) = \frac{1}{\sqrt{\pi}}\left(\frac{Z}{a_0}\right)^{3/2}e^{-Zr_1/a_0}\frac{1}{\sqrt{\pi}}\left(\frac{Z}{a_0}\right)^{3/2}e^{-Zr_2/a_0} =\frac{1}{\pi}\left(\frac{Z}{a_0}\right)^3e^{-Z(r_1 + r_2)/a_0}}

Consequences of the independent-electron approximation

A better approximation

E=ψH^ψ=...=[Z227Z8]e24πϵ0a0{E = \langle\psi |\hat{H}|\psi\rangle = ... = \left[ Z^2 - \frac{27Z}{8}\right]\frac{e^2}{4\pi\epsilon_0a_0}}
dEdZ=(2Z278)e24πϵ0a0=0{\frac{dE}{dZ} = \left(2Z - \frac{27}{8}\right)\frac{e^2}{4\pi\epsilon_0a_0} = 0}

The linear variational method

ϕ(r)=nNcnfn(r)\phi(r) = \sum_n^N c_nf_n(r)

A two-function example

ϕ=c1f1+c2f2\phi = c_1f_1 + c_2f_2
Eϕ=ϕH^ϕϕϕ=c1f1+c2f2H^c1f1+c2f2c1f1+c2f2c1f1+c2f2E_\phi = \frac{\langle\phi|\hat{H}|\phi\rangle}{\langle\phi|\phi\rangle} = \frac{\langle c_1f_1 + c_2f_2|\hat{H}|c_1f_1 + c_2f_2 \rangle}{\langle c_1f_1 + c_2f_2|c_1f_1 + c_2f_2 \rangle}
Hij=fiH^fj,Sij=fifjH_{ij} = \langle f_i|\hat{H}|f_j\rangle, \qquad S_{ij} = \langle f_i|f_j\rangle

so that

Eϕ=c12H11+2c1c2H12+c22H22c12S11+2c1c2S12+c22S22E_\phi = \frac{c_1^2 H_{11} + 2 c_1 c_2 H_{12} + c_2^2 H_{22}}{c_1^2 S_{11} + 2 c_1 c_2 S_{12} + c_2^2 S_{22}}

Minimization leads to a generalized eigenvalue problem

Eϕc1=0=c1(H11ES11)+c2(H12ES12)\frac{\partial E_\phi}{\partial c_1} = 0 = c_1(H_{11} - ES_{11}) + c_2(H_{12} - ES_{12})
Eϕc2=0=c1(H12ES12)+c2(H22ES22)\frac{\partial E_\phi}{\partial c_2} = 0 = c_1(H_{12} - ES_{12}) + c_2(H_{22} - ES_{22})

Problems

Problem 1

Problem 2

Problem 3

Problem 4

Problem 5