Wavefunction and Schrödinger Equation

Key idea: H3 Quantum Mechanics: what the wavefunction ψ means, why |ψ|² is a probability density, and how the Schrödinger equation constrains allowed energies.

  • Advanced Physics
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Learning objectives

  • Use state functions, boundary conditions, stationary states, and measurement to analyse introductory quantum systems.

Quantum mechanics describes a particle using a wavefunction (rather than a single trajectory). The Schrödinger equation is the wave equation that tells you what wavefunctions are allowed in a given potential energy V(x).

1. Meaning of the wavefunction

  • The wavefunction Ψ(x,t) is a (generally complex) function that encodes the state of the particle.
  • The wavefunction itself is not measured directly. Predictions come from its modulus squared.
  • In one dimension, dP = |Ψ(x,t)|² dx; in three dimensions, dP = |Ψ(r,t)|² dV.
  • Normalisation: total probability is 1: ∫_(-∞)^∞ |Ψ(x,t)|² dx = 1

The diagram below separates the sign-changing wavefunction from the measurable density and shows interval probability as an area under |ψ|².

Wavefunction and probability density comparisonTop panel shows an oscillatory psi(x); bottom panel shows positive probability density with a highlighted interval area.Wavefunction ψ(x)Probability density |ψ(x)|²xxx₁x₂P(x₁ to x₂) = ∫ |ψ|² dx
Scroll diagram horizontally to read all labels.
Top: ψ(x) can change sign. Bottom: |ψ(x)|² is non-negative, and interval probability is the area under the curve between x₁ and x₂.

Particles show wave behaviour. For a non-relativistic particle with momentum p:

λ = h/p

It is often useful to write momentum in “wave” form:

p = ħ k ⇒ k = 2π/λ

This connection is why quantised wavelengths in a bound system lead to quantised momenta/energies.

3. Schrödinger equations

Time-dependent equation in one dimension

iħ (∂ Ψ)/(∂ t) = -(ħ²/2m)(∂² Ψ)/(∂ x²) + V(x)Ψ

It tells you how the state evolves in time for a given potential energy V(x).

Time-independent equation for stationary states

If V(x) does not depend on time, many exam problems focus on stationary states with:

Ψ(x,t) = ψ(x)e^(-iEt/ħ)

Substituting this into the time-dependent equation gives the time-independent form:

-(ħ²/2m)d²ψ/dx² + V(x)ψ = Eψ

This is an eigenvalue equation: for bound systems, only certain values of E produce acceptable (normalisable) solutions.

4. Physical constraints and boundary conditions

In typical 1D H3 problems, acceptable wavefunctions must satisfy:

  • ψ is finite and single-valued.
  • ψ is continuous.
  • dψ/dx is continuous wherever V(x) is finite.
  • ψ is normalisable: ∫ |ψ|² dx is finite.
  • At an infinite wall, the wavefunction must vanish at the boundary (e.g., ψ = 0 at the wall).

5. Problem workflow

  1. Sketch V(x) and split space into regions where V is simple/constant.
  2. Solve the differential equation in each region:
    • If E > V: solutions are oscillatory (sin/cos).
    • If E < V: solutions are exponential (decaying/growing).
  3. Apply boundary conditions (continuity + wall conditions) to determine constants and quantise allowed E.
  4. Normalise (if asked).
  5. Interpret results using |ψ|² and sanity-check units.

6. Quick check

A. If you scale the wavefunction by a constant A, what happens to the probability density?

Answer

If ψ → Aψ, then |ψ|² → |A|²|ψ|². You must renormalise to keep total probability equal to 1.

B. In a region of constant potential, what kind of wavefunction do you expect for E > V vs E < V?

Answer
  • E > V: oscillatory (sinusoidal) solutions.
  • E < V: exponential solutions (decaying/growing), which is the mathematical basis for tunnelling in finite barriers.

Continue with the next resource in this course.

Course and syllabus information
Course
Advanced Physics
Edition
Advanced Physics