The Time-Dependent Schrodinger Equation

A sodium atom absorbs a photon. Its electron cloud begins to slosh back and forth between two orbitals. This oscillation occurs at a frequency set exactly by the energy gap. Nothing "jumps" instantaneously. The wavefunction evolves smoothly, continuously, deterministically. It obeys one equation that governs every quantum system. This includes a free electron in a wire. It also includes a chlorophyll molecule funneling excitation energy through a photosynthetic antenna. That equation is the time-dependent Schrödinger equation (TDSE). It plays the role in quantum mechanics that Newton's second law plays in classical mechanics. Given the state now and the forces at play, it tells you the state an instant later. This matters because chemistry is not static. Bonds break and form. Electrons transfer between donor and acceptor. Spins precess in a magnetic field. Wavepackets spread and interfere. All of this is time-dependent quantum behavior. All of it is governed by the same differential equation. That equation acts on the wavefunction introduced through the Wavefunction and Born Interpretation. Where the de Broglie Relation gave us the idea that matter has a wavelength, the TDSE is the equation that wave actually obeys. It is a first-order equation in time, linear, and deterministic. The quantum wavefunction itself never behaves probabilistically in its evolution. Only the measurement outcomes drawn from it are probabilistic. The big picture is this: the Hamiltonian operator H^\hat H is built from kinetic and potential energy. It acts as the generator of time evolution. Once you know H^\hat H for a system, the TDSE tells you how any initial wavefunction morphs in time. This applies to a hydrogen atom, a vibrating diatomic, or a spin in a magnetic field. When the Hamiltonian has no explicit time dependence, the equation factors beautifully. It splits into a spatial part and a universal phase oscillation. This is precisely the bridge to the Time-Independent Schrodinger Equation. It also connects to the whole edifice of stationary-state quantum chemistry — orbitals, energy levels, spectroscopy. This article builds the TDSE from the physical requirements of a wave equation. That equation must be consistent with the de Broglie relations. It shows how stationary states emerge as its simplest solutions. It works through the full machinery of superposition and quantum beats, foreshadowing Superposition of States. It applies all of this to problems ranging from a particle in a box to a two-level system in a laser field. This is the same mathematics used to describe NMR, laser spectroscopy, and coherent control of chemical reactions.

Key takeaways
  • The TDSE, iℏ ∂Ψ/∂t=H^Ψi\hbar \,\partial\Psi/\partial t = \hat H \Psi, is the fundamental law of quantum time evolution — one equation, all of chemistry's dynamics.
  • The Hamiltonian H^\hat H is the total-energy operator; it generates time evolution the way it generates energy eigenvalues in the static picture.
  • Stationary states Ψ(x,t)=ψ(x)e−iEt/ℏ\Psi(x,t) = \psi(x)e^{-iE t/\hbar} solve the TDSE whenever H^\hat H has no explicit time dependence — this is the seed of the time-independent equation.
  • Superpositions of stationary states oscillate at beat frequencies (E2−E1)/ℏ(E_2-E_1)/\hbar — this is literally why spectroscopy works.
  • Probability is conserved automatically: ∫∣Ψ∣2dτ\int|\Psi|^2 d\tau never changes in time, guaranteed by the Hermiticity of H^\hat H.
  • The TDSE reduces to Newton's equations in the classical limit (Ehrenfest's theorem), so it does not contradict macroscopic mechanics — it contains it.
  • Key idea: the wavefunction evolves smoothly and deterministically under H^\hat H; only the acts of measurement introduce probability, never the evolution itself.

Where this lives today

The TDSE is not a historical curiosity confined to textbooks — it is the working equation behind entire modern subfields. In ultrafast spectroscopy, femtosecond and attosecond laser pulses prepare exactly the kind of coherent superpositions worked through above, and pump–probe experiments directly measure the beat frequencies (Ej−Ek)/ℏ(E_j-E_k)/\hbar as oscillating signals in real time, watching chemical bonds vibrate and electrons redistribute on their natural timescales. In magnetic resonance (NMR and MRI), nuclear spins precess under a time-dependent Hamiltonian containing static and radiofrequency magnetic fields; the Rabi-flopping mathematics of the second worked example is literally the equation solved to design the radiofrequency pulses (π/2\pi/2- and π\pi-pulses) that make every NMR and MRI pulse sequence work. In photosynthesis research, the TDSE governs how excitonic coherences move energy through light-harvesting antenna complexes with remarkable efficiency, a topic of intense study in quantum biology. In quantum computing, qubits are literally two-level systems whose state vector is propagated by the TDSE (or its extension including decoherence), and gate operations are engineered pulse sequences that drive precisely controlled Rabi oscillations. In computational chemistry, real-time TDSE propagation (real-time TDDFT) is used to simulate absorption spectra, nonlinear optical response, and photochemical reaction dynamics directly in the time domain, complementing the energy-domain picture from the Time-Independent Schrodinger Equation. And in coherent control, chemists shape laser pulses to steer superpositions of vibrational and electronic states — quantum "steering wheels" built entirely from solving the TDSE for a chosen molecular Hamiltonian to select which bond breaks.

Ask the tutor: How does the time-dependent Schrödinger equation reduce to the time-independent one, and why do chemists usually start with the latter?

The physical picture

Consider a free particle described, as motivated by the de Broglie Relation, by a plane wave Ψ(x,t)=Aei(kx−ωt)\Psi(x,t) = A e^{i(kx - \omega t)}, with p=ℏkp = \hbar k and E=ℏωE = \hbar \omega. This wave is not a static snapshot; it is explicitly a function of time, oscillating in place as it also propagates. If quantum mechanics is to describe how any wavefunction changes from one instant to the next, we need a differential equation whose solutions include this plane wave and, more generally, any physically allowed Ψ\Psi. Schrödinger's insight (1925–1926) was to demand that this equation be linear — so that superpositions of solutions are also solutions, which is essential for interference — and that it link the time derivative of Ψ\Psi to the energy of the particle, since E=ℏωE=\hbar\omega links frequency to energy. Differentiating the plane wave with respect to time brings down a factor of −iω-i\omega, and differentiating twice with respect to position brings down −k2-k^2. Since E=p2/2mE = p^2/2m for a free particle, and p=ℏkp = \hbar k, matching the two derivative relations forces a very specific structure: a first time derivative must equal iℏi\hbar times a second spatial derivative (up to sign and constants), because ℏω\hbar\omega is linear in EE but E∝k2∝(second spatial derivative)E \propto k^2 \propto (\text{second spatial derivative}). This is why the Schrödinger equation is first-order in time (unlike the classical wave equation, which is second-order) and why it necessarily involves the imaginary unit ii — a real equation of this structure could not support traveling, oscillating solutions with the right dispersion relation. Once a potential energy V(x,t)V(x,t) is present, the total energy operator — the Hamiltonian — is kinetic plus potential, and the same structural equation holds with H^\hat H in place of the free-particle kinetic operator alone. The resulting equation is the master law: H^\hat H acting on Ψ\Psi equals iℏi\hbar times the time derivative of Ψ\Psi. Crucially, this equation is exact — it is not an approximation, a rule of thumb, or a model. Every non-relativistic quantum system, from an electron in a Coulomb field to a nuclear spin in an oscillating magnetic field, obeys exactly this equation, differing only in what H^\hat H is. The picture that emerges is one of a wavefunction as a vector rotating (in an abstract, infinite-dimensional space) under a "rotation generator" H^\hat H. If Ψ\Psi is initially an eigenstate of H^\hat H (a stationary state), it does not change its shape at all — only a uniform, physically unobservable overall phase factor accumulates. If Ψ\Psi is a superposition of eigenstates with different energies, the relative phases between components drift apart at rates proportional to their energy differences, and this relative dephasing is what produces all observable time dependence — oscillating dipole moments, spectral line shapes, wavepacket motion.

Figure
Time evolution of a stationary state vs. a superposition: phase spirals and beats
Stationary state: |Ψ|² frozen, phase rotates e^{-iEt/ħ}: phase spins, |Ψ|² = ψ*ψ unchanged Superposition: probability density oscillates t = 0 t = 2π/ω₂₁ beat frequency ω₂₁ = (E₂ − E₁)/ħ
Figure
Building the TDSE: matching plane-wave derivatives to the free-particle energy
Ψ(x,t) = A e^{i(kx − ωt)}, E = ħω, p = ħk, E = p²/2m ∂Ψ/∂t = −iω Ψ → iħ ∂Ψ/∂t = ħω Ψ = E Ψ ∂²Ψ/∂x² = −k² Ψ → −(ħ²/2m) ∂²Ψ/∂x² = (ħ²k²/2m) Ψ = E Ψ ⇒ iħ ∂Ψ/∂t = −(ħ²/2m) ∂²Ψ/∂x² + V(x,t)Ψ ≡ ĤΨ Both routes give E Ψ — consistency forces the first-order-in-time, second-order-in-space, complex structure of the equation.

The core ideas

The general, exact statement, valid for any potential (even time-dependent ones, as in a molecule driven by a laser field):

iℏ ∂Ψ(r,t)∂t=H^(t) Ψ(r,t)i\hbar \, \frac{\partial \Psi(\mathbf{r},t)}{\partial t} = \hat H(t)\, \Psi(\mathbf{r},t)

where:

  • Ψ(r,t)\Psi(\mathbf r, t) — the time-dependent wavefunction, whose modulus-squared gives the probability density (Born interpretation, now time-dependent).
  • H^(t)=T^+V^(r,t)=−ℏ22m∇2+V(r,t)\hat H(t) = \hat T + \hat V(\mathbf r, t) = -\dfrac{\hbar^2}{2m}\nabla^2 + V(\mathbf r, t) — the Hamiltonian operator, kinetic plus potential energy.
  • ℏ=h/2π\hbar = h/2\pi — the reduced Planck constant.
  • i=−1i = \sqrt{-1} — the imaginary unit; the wavefunction is intrinsically complex.

Reading: the rate of change of the state is proportional to the Hamiltonian acting on that state; H^\hat H literally is the time-evolution generator, not merely an energy bookkeeping device. When H^\hat H has no explicit time dependence (no external field turning on and off, no moving nuclei in the Born–Oppenheimer sense), separation of variables gives the single most important special solution:

Ψ(r,t)=ψ(r) e−iEt/ℏ\Psi(\mathbf r, t) = \psi(\mathbf r)\, e^{-iEt/\hbar}

where:

  • ψ(r)\psi(\mathbf r) — a time-independent spatial function satisfying H^ψ=Eψ\hat H \psi = E\psi, the eigenvalue equation that becomes the Time-Independent Schrodinger Equation.
  • EE — the (real, conserved) energy eigenvalue associated with that eigenstate.
  • e−iEt/ℏe^{-iEt/\hbar} — a pure phase factor of unit modulus; it never affects ∣Ψ∣2|\Psi|^2.

Reading: for a stationary state, all time dependence is an unobservable global phase — the probability density, and every expectation value of a time-independent operator, is frozen in time. This is precisely why we can speak of "the 2p orbital" as a fixed spatial shape. For a general initial state expanded in energy eigenstates,

Ψ(r,t)=∑ncn ψn(r) e−iEnt/ℏ,cn=∫ψn∗(r) Ψ(r,0) dτ\Psi(\mathbf r, t) = \sum_n c_n\, \psi_n(\mathbf r)\, e^{-iE_n t/\hbar}, \qquad c_n = \int \psi_n^*(\mathbf r)\,\Psi(\mathbf r,0)\, d\tau

where:

  • cnc_n — fixed (time-independent) expansion coefficients, determined entirely by the initial wavefunction at t=0t=0.
  • ψn\psi_n, EnE_n — the complete set of orthonormal eigenfunctions and eigenvalues of H^\hat H.
  • the sum runs over all stationary states (a discrete sum here; more generally an integral over a continuum too).

Reading: this is the fully general solution to the TDSE whenever H^\hat H is time-independent — you only ever need to solve the time-independent eigenvalue problem once, and then time evolution is just attaching phase factors e−iEnt/ℏe^{-iE_nt/\hbar} to each piece and re-summing. This is the essential content of Superposition of States: physically distinct stationary states can be combined, and the combination evolves by each component spinning at its own rate.

Derivation AFrom the TDSE to stationary states — separation of variables

Goal. Show that H^ψ=Eψ\hat H\psi = E\psi together with Ψ=ψ(r)e−iEt/ℏ\Psi = \psi(\mathbf r)e^{-iEt/\hbar} solves the full TDSE whenever H^\hat H carries no explicit time dependence, and that this is the only type of solution with time-independent probability density.

Step 1 — Assume a separable form. Since H^\hat H acts only on spatial coordinates and contains no tt, try

Ψ(r,t)=ψ(r) f(t).\Psi(\mathbf r,t) = \psi(\mathbf r)\, f(t).

Substituting into the TDSE,

iℏ ψ(r) dfdt=f(t) H^ψ(r).i\hbar\, \psi(\mathbf r)\, \frac{df}{dt} = f(t)\, \hat H \psi(\mathbf r).

Step 2 — Divide by ψ(r)f(t)\psi(\mathbf r) f(t). This isolates space on one side and time on the other:

iℏ 1f(t)dfdt=H^ψ(r)ψ(r).i\hbar\, \frac{1}{f(t)}\frac{df}{dt} = \frac{\hat H \psi(\mathbf r)}{\psi(\mathbf r)}.

The left side depends only on tt; the right side depends only on r\mathbf r. The only way a function of tt alone can equal a function of r\mathbf r alone, for all tt and all r\mathbf r, is if both sides equal the same constant. Call that constant EE (it has units of energy, since H^\hat H has units of energy).

Step 3 — Solve the temporal equation. From

iℏ 1fdfdt=E,i\hbar\, \frac{1}{f}\frac{df}{dt} = E,

rearrange to

dff=−iEℏ dt,\frac{df}{f} = -\frac{iE}{\hbar}\, dt,

and integrate:

f(t)=f(0) e−iEt/ℏ.f(t) = f(0)\, e^{-iEt/\hbar}.

Absorbing f(0)f(0) into the normalization of ψ\psi, this gives the universal phase factor e−iEt/ℏe^{-iEt/\hbar}.

Step 4 — Solve the spatial equation. The right-hand side of Step 2 set equal to EE gives

H^ψ(r)=E ψ(r),\hat H \psi(\mathbf r) = E\, \psi(\mathbf r),

which is exactly the time-independent Schrödinger equation — an eigenvalue problem for H^\hat H with eigenvalue EE.

Step 5 — Check uniqueness of "stationary" behavior. Compute ∣Ψ∣2=ψ∗(r)f∗(t)f(t)ψ(r)|\Psi|^2 = \psi^*(\mathbf r)f^*(t) f(t)\psi(\mathbf r). Since f∗(t)f(t)=e+iEt/ℏe−iEt/ℏ=1f^*(t)f(t) = e^{+iEt/\hbar}e^{-iEt/\hbar} = 1 for real EE (guaranteed because H^\hat H is Hermitian), ∣Ψ∣2=∣ψ(r)∣2|\Psi|^2 = |\psi(\mathbf r)|^2 is manifestly time-independent. Any solution of this separable form therefore has frozen probability density — hence the name "stationary state." A general (non-separable) solution is a sum of such terms with different EnE_n, and only then does ∣Ψ∣2|\Psi|^2 acquire genuine time dependence, through cross terms between different nn.

Go deeper · Derivation B · 1 minTwo-level superposition and the quantum beat frequency
Derivation BTwo-level superposition and the quantum beat frequency

Goal. Starting from a superposition of exactly two stationary states, derive the oscillation frequency of the probability density and connect it to spectroscopic transition frequencies.

Step 1 — Write the superposition. Let H^ψ1=E1ψ1\hat H\psi_1 = E_1\psi_1 and H^ψ2=E2ψ2\hat H\psi_2 = E_2\psi_2, with ψ1,ψ2\psi_1,\psi_2 orthonormal. Take the general two-term solution of the TDSE:

Ψ(x,t)=c1ψ1(x) e−iE1t/ℏ+c2ψ2(x) e−iE2t/ℏ,\Psi(x,t) = c_1 \psi_1(x)\, e^{-iE_1 t/\hbar} + c_2 \psi_2(x)\, e^{-iE_2 t/\hbar},

with real, positive c1,c2c_1, c_2 chosen (for concreteness) with c12+c22=1c_1^2 + c_2^2 = 1 so Ψ\Psi is normalized (using orthonormality of ψ1,ψ2\psi_1,\psi_2).

Step 2 — Expand ∣Ψ∣2|\Psi|^2.

∣Ψ(x,t)∣2=c12∣ψ1∣2+c22∣ψ2∣2+c1c2[ψ1∗ψ2 e−i(E2−E1)t/ℏ+ψ2∗ψ1 e+i(E2−E1)t/ℏ].|\Psi(x,t)|^2 = c_1^2 |\psi_1|^2 + c_2^2 |\psi_2|^2 + c_1 c_2 \left[\psi_1^*\psi_2\, e^{-i(E_2-E_1)t/\hbar} + \psi_2^*\psi_1\, e^{+i(E_2-E_1)t/\hbar}\right].

The first two terms are time-independent "background" densities. The bracket is the interesting part.

Step 3 — Combine the cross terms. Since ψ1,ψ2\psi_1,\psi_2 can be chosen real (true for bound states with no magnetic field), write ψ1∗ψ2=ψ2∗ψ1=ψ1(x)ψ2(x)\psi_1^*\psi_2 = \psi_2^*\psi_1 = \psi_1(x)\psi_2(x), a real function of xx. Using eiθ+e−iθ=2cos⁡θe^{i\theta}+e^{-i\theta} = 2\cos\theta,

∣Ψ(x,t)∣2=c12ψ12(x)+c22ψ22(x)+2c1c2 ψ1(x)ψ2(x) cos⁡ ⁣((E2−E1)tℏ).|\Psi(x,t)|^2 = c_1^2\psi_1^2(x) + c_2^2\psi_2^2(x) + 2c_1c_2\,\psi_1(x)\psi_2(x)\, \cos\!\left(\frac{(E_2-E_1)t}{\hbar}\right).

Step 4 — Identify the beat (angular) frequency. Define

ω21≡E2−E1ℏ.\omega_{21} \equiv \frac{E_2 - E_1}{\hbar}.

The probability density therefore oscillates sinusoidally in time at angular frequency ω21\omega_{21}, superimposed on a static background — precisely a "quantum beat."

Step 5 — Connect to Bohr's frequency condition. Since ω21=2πν21\omega_{21} = 2\pi\nu_{21}, this gives

ν21=E2−E1h,\nu_{21} = \frac{E_2 - E_1}{h},

which is exactly the Bohr frequency condition for absorption/emission spectroscopy. The TDSE thus derives, rather than merely postulates, the rule that spectroscopic lines appear at frequencies matching energy-level differences: it is a direct, inescapable consequence of linear superposition and phase evolution under H^\hat H.

Worked examples

Example 1 — Foundational: a superposition in the infinite square well. Take a particle of mass m=9.109×10−31 kgm = 9.109\times10^{-31}\,\text{kg} (an electron) confined to an infinite square well of width L=0.500 nmL = 0.500\,\text{nm} — a crude but standard model for a delocalized π\pi-electron. The normalized eigenstates and energies are

ψn(x)=2Lsin⁡ ⁣(nπxL),En=n2h28mL2.\psi_n(x) = \sqrt{\frac{2}{L}}\sin\!\left(\frac{n\pi x}{L}\right), \qquad E_n = \frac{n^2 h^2}{8mL^2}.

At t=0t=0 the electron is prepared in the asymmetric (non-special, deliberately unequal-weight) superposition

Ψ(x,0)=0.30 ψ1(x)+0.70 ψ2(x),\Psi(x,0) = \sqrt{0.30}\,\psi_1(x) + \sqrt{0.70}\,\psi_2(x),

so c1=0.30=0.5477c_1 = \sqrt{0.30} = 0.5477, c2=0.70=0.8367c_2=\sqrt{0.70}=0.8367 (chosen unequal on purpose, and already normalized since 0.30+0.70=10.30+0.70=1). Step 1: energies. With h=6.626×10−34 J sh = 6.626\times10^{-34}\,\text{J s}, m=9.109×10−31 kgm=9.109\times10^{-31}\,\text{kg}, L=5.00×10−10 mL=5.00\times10^{-10}\,\text{m}:

E1=(1)2(6.626×10−34)28(9.109×10−31)(5.00×10−10)2=2.409×10−19 J.E_1 = \frac{(1)^2(6.626\times10^{-34})^2}{8(9.109\times10^{-31})(5.00\times10^{-10})^2} = 2.409\times10^{-19}\,\text{J}.
E2=4E1=9.636×10−19 J.E_2 = 4E_1 = 9.636\times10^{-19}\,\text{J}.

Step 2: beat frequency.

ν21=E2−E1h=7.227×10−19 J6.626×10−34 J s=1.091×1015 Hz.\nu_{21} = \frac{E_2-E_1}{h} = \frac{7.227\times10^{-19}\,\text{J}}{6.626\times10^{-34}\,\text{J s}} = 1.091\times10^{15}\,\text{Hz}.

This lies in the near-ultraviolet (corresponding wavelength λ=c/ν21=275 nm\lambda = c/\nu_{21} = 275\,\text{nm}), showing that the electron's charge density genuinely sloshes back and forth at a UV-range frequency — the same frequency a photon would need to drive this transition. Step 3: the time-dependent density. Using the beat-formula derived above with c1c2=0.5477×0.8367=0.4583c_1c_2 = 0.5477\times0.8367 = 0.4583,

∣Ψ(x,t)∣2=0.30 ψ12(x)+0.70 ψ22(x)+0.9166 ψ1(x)ψ2(x)cos⁡(ω21t),|\Psi(x,t)|^2 = 0.30\,\psi_1^2(x) + 0.70\,\psi_2^2(x) + 0.9166\,\psi_1(x)\psi_2(x)\cos(\omega_{21}t),

with ω21=2πν21=6.856×1015 rad/s\omega_{21} = 2\pi\nu_{21} = 6.856\times10^{15}\,\text{rad/s}. At x=L/4x = L/4 (an asymmetric, non-central point), ψ1(L/4)=2/Lsin⁡(π/4)=2/L(0.7071)\psi_1(L/4) = \sqrt{2/L}\sin(\pi/4) = \sqrt{2/L}(0.7071) and ψ2(L/4)=2/Lsin⁡(π/2)=2/L(1)\psi_2(L/4)=\sqrt{2/L}\sin(\pi/2)=\sqrt{2/L}(1), so with 2/L=4.00×109 m−12/L = 4.00\times10^9\,\mathrm{m^{-1}}, ψ1(L/4)=4.472×104 m−1/2\psi_1(L/4)=4.472\times10^4\,\mathrm{m^{-1/2}} and ψ2(L/4)=6.325×104 m−1/2\psi_2(L/4)=6.325\times10^4\,\mathrm{m^{-1/2}}; the probability density genuinely oscillates in time between roughly 1.07×109 m−11.07\times10^9\,\mathrm{m^{-1}} and 3.87×109 m−13.87\times10^9\,\mathrm{m^{-1}} over one beat period T=1/ν21=0.917 fsT = 1/\nu_{21} = 0.917\,\text{fs}. Limiting-case check: if instead c2→0c_2 \to 0 (pure ψ1\psi_1), the cross term vanishes and ∣Ψ∣2=ψ12(x)|\Psi|^2 = \psi_1^2(x) is exactly static — recovering the stationary-state result derived above, as it must.

Example 2 — Applied: Rabi-type oscillation of a two-level chromophore in a resonant field. A two-level model of a chromophore (ground state gg, excited state ee) with transition energy ΔE=Ee−Eg=2.50 eV\Delta E = E_e - E_g = 2.50\,\text{eV} is driven by a resonant oscillating field so that its Hamiltonian in the {g,e}\{g,e\} basis (rotating-wave approximation) is

H^=(EgℏΩR/2ℏΩR/2Ee),\hat H = \begin{pmatrix} E_g & \hbar\Omega_R/2 \\ \hbar\Omega_R/2 & E_e \end{pmatrix},

with Rabi frequency ΩR=3.00×1013 rad/s\Omega_R = 3.00\times10^{13}\,\text{rad/s} (a realistic strong-field value), and the molecule starts entirely in the ground state, Ψ(0)=∣g⟩\Psi(0) = |g\rangle. Step 1: solve the 2×2 TDSE. Writing Ψ(t)=cg(t)e−iEgt/ℏ∣g⟩+ce(t)e−iEet/ℏ∣e⟩\Psi(t) = c_g(t)e^{-iE_gt/\hbar}|g\rangle + c_e(t)e^{-iE_et/\hbar}|e\rangle, substitution into iℏΨ˙=H^Ψi\hbar\dot\Psi = \hat H\Psi gives the standard coupled equations

ic˙g=ΩR2ce,ic˙e=ΩR2cg,i\dot c_g = \frac{\Omega_R}{2}c_e, \qquad i\dot c_e = \frac{\Omega_R}{2}c_g,

whose solution with cg(0)=1, ce(0)=0c_g(0)=1,\ c_e(0)=0 is

cg(t)=cos⁡ ⁣(ΩRt2),ce(t)=−isin⁡ ⁣(ΩRt2).c_g(t) = \cos\!\left(\frac{\Omega_R t}{2}\right), \qquad c_e(t) = -i\sin\!\left(\frac{\Omega_R t}{2}\right).

Step 2: excited-state population.

Pe(t)=∣ce(t)∣2=sin⁡2 ⁣(ΩRt2).P_e(t) = |c_e(t)|^2 = \sin^2\!\left(\frac{\Omega_R t}{2}\right).

Step 3: numeric evaluation at t=80.0 fs=8.00×10−14 st = 80.0\,\text{fs} = 8.00\times10^{-14}\,\text{s} (an off-round time, not a special multiple of the period).

ΩRt2=(3.00×1013)(8.00×10−14)2=1.200 rad.\frac{\Omega_R t}{2} = \frac{(3.00\times10^{13})(8.00\times10^{-14})}{2} = 1.200\ \text{rad}.
Pe=sin⁡2(1.200 rad)=(0.9320)2=0.8686.P_e = \sin^2(1.200\ \text{rad}) = (0.9320)^2 = 0.8686.

So after 80 fs, 86.9% of the population has been transferred to the excited state — this is the microscopic mechanism behind Rabi flopping used in coherent control and in modeling how a laser pulse of a specific duration can be tuned to leave a molecule almost entirely excited ("a π\pi-pulse") or in an exact 50/50 superposition ("a π/2\pi/2-pulse"). Step 4: the full period. Complete population transfer back to the ground state occurs when ΩRt/2=π\Omega_R t/2 = \pi, i.e. t=2π/ΩR=2.094×10−13 s=209.4 fst = 2\pi/\Omega_R = 2.094\times10^{-13}\,\text{s} = 209.4\,\text{fs} — the Rabi period, a directly measurable observable in pump–probe and Ramsey-fringe spectroscopy. Limiting-case check: as ΩR→0\Omega_R \to 0 (field switched off), Pe(t)→0P_e(t) \to 0 for all tt — the molecule simply sits in its stationary ground state forever, exactly reproducing the stationary-state result of the first derivation.

Example 3 — Exam/competition level: expectation value dynamics and Ehrenfest's theorem for a harmonic oscillator wavepacket. A diatomic molecule modeled as a harmonic oscillator (reduced mass μ\mu, force constant kfk_f, angular frequency ω0=kf/μ\omega_0=\sqrt{k_f/\mu}) is prepared, at t=0t=0, in a coherent superposition of its ground state ∣0⟩|0\rangle (energy 12ℏω0\tfrac12\hbar\omega_0) and first excited state ∣1⟩|1\rangle (energy 32ℏω0\tfrac32\hbar\omega_0), with unequal amplitudes c0=0.65=0.8062c_0 = \sqrt{0.65}=0.8062 and c1=0.35=0.5916c_1=\sqrt{0.35}=0.5916 (real, normalized: 0.65+0.35=10.65+0.35=1). Step 1: use the general result derived above. The energy gap is E1−E0=ℏω0E_1-E_0 = \hbar\omega_0, so the beat frequency is exactly ω0\omega_0 itself — a special feature of the harmonic oscillator's evenly spaced ladder. Step 2: expectation value of position. Using the standard raising/lowering-operator matrix elements ⟨0∣x^∣1⟩=⟨1∣x^∣0⟩=ℏ/2μω0\langle 0|\hat x|1\rangle = \langle1|\hat x|0\rangle = \sqrt{\hbar/2\mu\omega_0} and ⟨0∣x^∣0⟩=⟨1∣x^∣1⟩=0\langle0|\hat x|0\rangle=\langle1|\hat x|1\rangle=0, the same cross-term algebra as in the second derivation gives

⟨x^⟩(t)=2c0c1ℏ2μω0 cos⁡(ω0t).\langle \hat x \rangle(t) = 2c_0c_1\sqrt{\frac{\hbar}{2\mu\omega_0}}\, \cos(\omega_0 t).

With c0c1=0.8062×0.5916=0.4770c_0c_1 = 0.8062\times0.5916 = 0.4770, the prefactor is 2(0.4770)=0.95402(0.4770) = 0.9540 times the zero-point length scale. Step 3: plug in numbers for HCl-like parameters. Take μ=1.628×10−27 kg\mu = 1.628\times10^{-27}\,\text{kg} (the H–Cl reduced mass) and kf=480.0 N/mk_f = 480.0\,\text{N/m} (a representative diatomic force constant, deliberately not a round number), so

ω0=480.01.628×10−27=5.427×1014 rad/s.\omega_0 = \sqrt{\frac{480.0}{1.628\times10^{-27}}} = 5.427\times10^{14}\,\text{rad/s}.
ℏ2μω0=1.0546×10−342(1.628×10−27)(5.427×1014)=5.965×10−23 m=7.723×10−12 m.\sqrt{\frac{\hbar}{2\mu\omega_0}} = \sqrt{\frac{1.0546\times10^{-34}}{2(1.628\times10^{-27})(5.427\times10^{14})}} = \sqrt{5.965\times10^{-23}}\,\text{m} = 7.723\times10^{-12}\,\text{m}.

So

⟨x^⟩(t)=(0.9540)(7.723×10−12 m)cos⁡(ω0t)=7.368×10−12 m×cos⁡(ω0t).\langle \hat x\rangle(t) = (0.9540)(7.723\times10^{-12}\,\text{m})\cos(\omega_0 t) = 7.368\times10^{-12}\,\text{m}\times\cos(\omega_0 t).

The bond length genuinely oscillates with amplitude 7.37 pm at angular frequency 5.427×1014 rad/s5.427\times10^{14}\,\text{rad/s} (period T=2π/ω0=11.58 fsT=2\pi/\omega_0 = 11.58\,\text{fs}) — the quantum-mechanical wavepacket literally swings back and forth like a classical vibrating bond, exactly as expected from Ehrenfest's theorem, which states

d⟨x^⟩dt=⟨p^⟩μ,d⟨p^⟩dt=−⟨∂V∂x⟩,\frac{d\langle \hat x\rangle}{dt} = \frac{\langle \hat p\rangle}{\mu}, \qquad \frac{d\langle \hat p\rangle}{dt} = -\left\langle \frac{\partial V}{\partial x}\right\rangle,

i.e., quantum expectation values obey Newton's laws for the harmonic potential exactly (a special feature of quadratic potentials — for an anharmonic potential this equivalence would only be approximate). Limiting-case check: as c1→0c_1\to 0 (pure ground state), the prefactor 2c0c1→02c_0c_1\to 0 and ⟨x^⟩(t)→0\langle\hat x\rangle(t)\to 0 for all tt — the bond length sits motionless at its equilibrium value, exactly the stationary-state behavior established in the first derivation.

Limiting cases, scope & common traps

Regime / limitBehavior of the TDSEPhysical meaning
H^\hat H time-independent, single eigenstateΨ=ψne−iEnt/ℏ\Psi = \psi_n e^{-iE_nt/\hbar}; ∣Ψ∣2|\Psi|^2 frozenStationary state — orbitals, vibrational/rotational levels
H^\hat H time-independent, superposition of 2+ eigenstates∣Ψ∣2|\Psi|^2 oscillates at (Ej−Ek)/ℏ(E_j-E_k)/\hbarQuantum beats; origin of spectral transition frequencies
H^\hat H explicitly time-dependent (laser field, moving nuclei)No simple separable solution; requires perturbation theory or numerical propagationPhotoexcitation, Rabi flopping, pump–probe dynamics
ℏ→0\hbar \to 0Wavepackets stay sharply localized, ⟨x^⟩,⟨p^⟩\langle \hat x\rangle,\langle\hat p\rangle obey classical Hamilton's equationsClassical mechanics recovered (correspondence principle / Ehrenfest)
Very short times, t→0t\to0Ψ(t)≈Ψ(0)−iℏH^Ψ(0) t\Psi(t)\approx \Psi(0) - \frac{i}{\hbar}\hat H\Psi(0)\,tFirst-order (linear) approach; basis of time-dependent perturbation theory
Hermitian H^\hat H, any tt∫∣Ψ∣2dτ\int|\Psi|^2 d\tau exactly conservedTotal probability = 1 always; no "leakage" of probability

The chemist behind it

Origins · 1 minErwin Schrödinger and how this was discovered
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Erwin Schrödinger
1887–1961 · Vienna and Zurich, mid-1920s wave mechanics

Erwin Schrödinger trained as a theoretical physicist in Vienna, working initially on statistical mechanics, color theory, and general relativity before turning, in his late thirties, to atomic structure. In late 1925 and early 1926, spurred by Louis de Broglie's matter-wave hypothesis and by a colloquium remark from Peter Debye that "a wave needs a wave equation," Schrödinger — reportedly during a working retreat in Arosa, Switzerland — derived the equation that now bears his name, first in its time-independent eigenvalue form for the hydrogen atom, then in the fully time-dependent version treated here. His approach built on Hamilton–Jacobi theory in classical mechanics, exploiting a deep analogy between geometrical optics and mechanics that had been suggested decades earlier by William Rowan Hamilton. Schrödinger published a rapid sequence of four papers in 1926 that essentially created wave mechanics as a rival, and ultimately equivalent, formulation to Heisenberg's matrix mechanics. He shared the 1933 Nobel Prize in Physics with Paul Dirac. Later in his career Schrödinger turned to biology, and his 1944 lectures (published as What is Life?) on the "aperiodic crystal" encoding genetic information directly inspired Watson and Crick's search for the structure of DNA — an unusually direct line from the mathematics of wave mechanics to the birth of molecular biology.

History
- 1924 — Louis de Broglie proposes that matter has an associated wavelength λ=h/p\lambda = h/p.
- late 1925 — Schrödinger begins developing a wave equation for de Broglie's matter waves during a working stay in Arosa.
- 1926 — Schrödinger publishes the time-dependent and time-independent wave equations; solves the hydrogen atom.
- 1926 — Max Born proposes the probabilistic interpretation of ∣Ψ∣2|\Psi|^2, completing the physical meaning of the equation.
- 1928 — Paul Dirac formulates a relativistic wave equation, extending the Schrödinger framework to include electron spin and antimatter.
Is the time-dependent Schrödinger equation the same as the time-independent one?

No — they serve different purposes. The time-dependent equation, iℏ ∂Ψ/∂t=H^Ψi\hbar\,\partial\Psi/\partial t = \hat H\Psi, is the fully general law of motion for any quantum state, valid whether or not H^\hat H depends on time. The time-independent equation, H^ψ=Eψ\hat H\psi = E\psi, is an eigenvalue equation that arises only as a special case — when H^\hat H has no explicit time dependence and you look for solutions with a fixed spatial shape (stationary states). Every stationary-state orbital, vibrational level, or rotational level you compute from the time-independent equation is then dressed with a phase factor e−iEt/ℏe^{-iEt/\hbar} to get the full time-dependent wavefunction. You need the time-dependent equation for spectroscopy, laser driving, and any genuinely dynamic process; the time-independent equation suffices for computing energy levels and static orbital shapes.

Why is there an ii (imaginary unit) in the Schrödinger equation at all?

The imaginary unit is required for the equation to support traveling, oscillating wave solutions consistent with the de Broglie relations while remaining only first-order in time. A real first-order-in-time equation of the form ∂Ψ/∂t=(operator)Ψ\partial\Psi/\partial t = (\text{operator})\Psi would produce exponential growth or decay, not oscillation. Multiplying by ii converts what would be a real exponential into a complex oscillation e−iωte^{-i\omega t}, exactly matching the phase behavior of a de Broglie wave. Physically, the complex nature of Ψ\Psi is also what allows probability current (particle flow) to be nonzero for stationary states with angular momentum, and it is why Ψ\Psi itself is never a directly observable quantity — only ∣Ψ∣2|\Psi|^2 and expectation values, which are always real, are measurable.

Does the TDSE apply to multi-electron molecules, or only single particles?

The same equation applies, but Ψ\Psi becomes a function of all particle coordinates simultaneously, and H^\hat H includes kinetic energy terms for every particle plus all pairwise Coulomb interactions (electron–electron, electron–nucleus, nucleus–nucleus). For an NN-electron molecule, Ψ(r1,r2,…,rN,t)\Psi(\mathbf r_1,\mathbf r_2,\dots,\mathbf r_N,t) lives in a 3N3N-dimensional configuration space (plus spin), and solving the TDSE exactly becomes computationally intractable beyond a few electrons. This is precisely why approximate methods — Hartree–Fock, density functional theory, and their time-dependent extensions (TDDFT) — exist: they are practical strategies for approximating solutions to the same, exact many-body TDSE that this article treats in its single-particle form.

How does the TDSE relate to the uncertainty principle?

They are logically independent statements that happen to work together consistently. The TDSE governs how a wavefunction changes in time given a Hamiltonian; the uncertainty principle is a structural fact about any wavefunction at a single instant, arising from the non-commutation of operators like position and momentum. What the TDSE does guarantee is that if H^\hat H does not commute with an operator A^\hat A, then ⟨A^⟩\langle \hat A\rangle generally changes in time (via the Ehrenfest-theorem relation d⟨A^⟩/dt=iℏ⟨[H^,A^]⟩d\langle\hat A\rangle/dt = \tfrac{i}{\hbar}\langle[\hat H,\hat A]\rangle), while if [H^,A^]=0[\hat H,\hat A]=0, then ⟨A^⟩\langle\hat A\rangle is a constant of the motion. So the TDSE tells you which uncertainties and expectation values evolve, while the uncertainty principle constrains how precisely any pair of them can be simultaneously known at all.

What does it mean physically that stationary states have "frozen" probability density but nonzero energy?

It means the particle is not "at rest" in any classical sense — it has a definite, generally nonzero kinetic energy contribution — but the statistical pattern of where you would find it upon measurement never changes shape over time. Think of a standing wave on a guitar string: the string's displacement pattern (the shape of the vibration envelope) is fixed in space, yet every point on the string is still moving up and down with real kinetic energy. Similarly, a hydrogen 2p electron has genuine angular momentum and kinetic energy, and even circulating probability current for states with ml≠0m_l\neq0, but the overall electron density cloud ∣ψ∣2|\psi|^2 never changes its lobed shape in time — that invariance is exactly what justifies drawing a fixed orbital picture in chemistry textbooks.

Can the TDSE describe a chemical reaction, like bond breaking?

In principle yes, though in practice full quantum treatment is reserved for light particles (electrons, and sometimes protons in tunneling contexts) because nuclei are usually treated classically or semiclassically via the Born–Oppenheimer approximation. Formally, one can write the TDSE for the complete nuclear-plus-electronic wavefunction and watch a bond-breaking wavepacket evolve on a potential energy surface, spreading, bifurcating at a transition state, and eventually localizing into product wells — this is the basis of the field of quantum reaction dynamics and wavepacket propagation methods used to simulate photodissociation and proton/hydrogen-atom transfer reactions where tunneling and zero-point effects genuinely matter and classical trajectories would give the wrong answer.

Why do we say the TDSE is "linear," and why does that matter for chemistry?

Linearity means that if Ψ1(t)\Psi_1(t) and Ψ2(t)\Psi_2(t) are both solutions of the TDSE for the same H^\hat H, then any combination c1Ψ1(t)+c2Ψ2(t)c_1\Psi_1(t) + c_2\Psi_2(t) is also a solution. This is what guarantees that superpositions of quantum states remain valid, physically meaningful states as they evolve — nothing about the differential equation itself ever forces a system to "choose" one eigenstate over another. Linearity underlies every interference phenomenon in chemistry: the constructive and destructive interference patterns in electron diffraction, the coherent beating behind two-dimensional electronic spectroscopy, and the very existence of chemical bonding descriptions (like molecular orbitals as linear combinations of atomic orbitals) that rely on superposition being a mathematically consistent operation.

Before this

Where this leads