Due to the coupled nature of Schrödinger equation and the sheer difficulty of solving the differential equations analytically we often rely on numerical solutions

🗒️ Note: Computers can solve differential equations very efficiently but

Variational methods: ground state

💼 Case: we know the Hamiltonian of a bound system but not the wave function or the ground state energy

💫 The variation principle: If we guess the wave function, the expectation value of the Hamiltonian in that wave function will be greater than the true ground state energy

$$ \frac{\braket{\Psi |\hat H|\Psi}}{\braket{\Psi|\Psi}}\ge E_0 $$

🧙‍♂️ Proof: If we consider expanding the normalized $|\Psi\rang$ in the true energy eigenstate $\ket{n}$ we get $\braket{\hat H} =\sum_n P_ n E_n$ since $P_n>0$ and all $E_n \ge E_0$ ($\sum_nP_n=1$)

🗒️ Note: better guesses will be closer to $E_0$

💃 Example: Consider the infinite square well with $V=0$ for $0<x<a$ and $V=\infin$ elsewhere


In practice we run a minimization algorithm say a Bayesian optimization to try different parameters until we get a good result. Here a better guess would be $\Psi(x)=x(a-x)+bx^2(a-x)^2$ were we let an algorithm try values of $b$ until it reaches a convergence.

This method gives the following precision

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🗒️ Note: again however a minimization algorithm could minimize to a local minima and there would be hard to tell

Variational methods: excited states

⚽ Goal: find a way to get a condition to find $E_1$ and potentially higher

Going back to the expression $\braket{\hat H} =\sum_n P_ n E_n$ here $P_n=|\lang \psi_n |\Psi \rang |^2$ represents the probability of the trial wavefunction $\Psi$ overlapping with the eigenstates $\psi_n$.