Solving the Schrödinger Equation for Hydrogen Atom

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quantum-mechanics hydrogen atomic-physics

Core Idea

The time-independent Schrödinger equation for hydrogen separates in spherical coordinates into radial and angular parts. Solutions are labeled by quantum numbers n (principal), ℓ (orbital angular momentum), and m_ℓ (magnetic). Energy depends only on n: E_n = −13.6 eV / n². Degeneracy increases as n² because different (ℓ, m_ℓ) combinations give the same energy.

How It's Best Learned

Understand the separation of variables and radial equation with effective potential. Recognize the role of boundary conditions in quantizing energy. Compare predictions (energy levels, wavefunctions) with experimental hydrogen spectrum and atomic properties.

Common Misconceptions

The wavefunction ψ(r,θ,φ) is not an orbit—it is a probability amplitude whose square gives probability density. Quantum numbers must satisfy 0 ≤ ℓ ≤ n−1 and −ℓ ≤ m_ℓ ≤ ℓ.

Explainer

You have learned the Schrödinger equation and quantum numbers, and you know that solving it means finding the eigenvalues and eigenfunctions of the Hamiltonian operator. The hydrogen atom is the most important exactly-solvable problem in quantum mechanics — the Coulomb potential V = −ke²/r has just enough symmetry to allow a complete analytic solution that illuminates the whole structure of atomic physics.

The strategy is separation of variables. The wavefunction ψ(r,θ,φ) is written as a product R(r)Y(θ,φ), where R is a purely radial function and Y is purely angular. Substituting into the Schrödinger equation in spherical coordinates, you find that the angular part Y(θ,φ) satisfies an equation whose solutions are the spherical harmonics Y_ℓ^m(θ,φ), characterized by two quantum numbers: ℓ (orbital angular momentum, non-negative integer) and m_ℓ (magnetic quantum number, integer with |m_ℓ| ≤ ℓ). The spherical harmonics are eigenfunctions of both the total angular momentum L² and its z-component L_z — they describe the shape and orientation of the wavefunction in angle space. The radial equation, meanwhile, contains an effective potential that adds a centrifugal barrier ℏ²ℓ(ℓ+1)/(2mr²) to the Coulomb attraction, depending on ℓ.

Solving the radial equation with the requirement that the wavefunction remain normalizable (decaying to zero as r → ∞) quantizes the energy. The allowed energies are E_n = −13.6 eV/n², where n = 1, 2, 3, ... is the principal quantum number. The n = 1 ground state has the electron closest to the nucleus on average and the largest binding energy. The -13.6 eV value matches the experimentally measured ionization energy of hydrogen to high precision — this exact agreement was one of quantum mechanics' earliest triumphs. Importantly, the energy depends only on n, not on ℓ or m_ℓ: for each n, the allowed values of ℓ run from 0 to n−1, and for each ℓ, m_ℓ runs from −ℓ to +ℓ, giving n² distinct (ℓ, m_ℓ) states all at the same energy. This degeneracy is larger than what the spherical symmetry alone would require — it is a hidden symmetry of the 1/r potential specific to the Coulomb problem.

The resulting wavefunctions ψ_nlm(r,θ,φ) = R_nl(r)Y_ℓ^m(θ,φ) are called atomic orbitals. The label n = 1, ℓ = 0 gives the 1s orbital (spherically symmetric); n = 2, ℓ = 1 gives the three 2p orbitals (dumbbell-shaped, oriented along x, y, z for m_ℓ = ±1, 0). The radial function R_nl tells you where the electron is likely to be found at various distances from the nucleus, and |ψ|² gives the full three-dimensional probability density. These orbitals are the building blocks for multi-electron atoms (via the Pauli principle and orbital filling), molecular bonding, and all of chemistry. The pattern of energy levels directly predicts the hydrogen emission spectrum — each spectral line corresponds to a transition between levels, setting up the photon absorption and emission physics you will study next.

Practice Questions 5 questions

Prerequisite Chain

Counting to 10Counting to 20Understanding ZeroThe Number ZeroCounting to FiveOne-to-One CorrespondenceCombining Small Groups Within 5Addition Within 10Addition Within 20Two-Digit Addition Without RegroupingTwo-Digit Addition with RegroupingAddition Within 100Repeated Addition as MultiplicationMultiplication Facts Within 100Division as Equal SharingDivision as Grouping (Measurement Division)Division: Grouping (Repeated Subtraction) ModelDivision: Fair Sharing ModelDivision as Equal SharingDivision as GroupingBasic Division FactsDivision Facts Within 100Two-Digit by One-Digit DivisionDivision with RemaindersRemainders and Quotients in DivisionDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueReading and Writing DecimalsComparing and Ordering DecimalsAdding and Subtracting DecimalsMultiplying DecimalsDividing DecimalsDividing FractionsMixed Number ArithmeticOrder of OperationsInteger Order of OperationsVariable ExpressionsCombining Like TermsOne-Step EquationsTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesAngle Pairs: Complementary, Supplementary, and VerticalParallel Lines and TransversalsCorresponding AnglesAlternate Interior AnglesTriangle Angle Sum TheoremExterior Angle TheoremTriangle Inequality TheoremSimilar Triangles: AA SimilaritySimilar Triangles: SSS and SAS SimilarityProportions in Similar TrianglesRight Triangle Trigonometry IntroductionTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIterated Integrals and Fubini's TheoremDouble Integrals in Cartesian CoordinatesDouble Integrals over Rectangular RegionsDouble Integrals in Polar CoordinatesDouble Integrals: Definition and SetupIterated Integrals and Fubini's TheoremDouble Integrals over Rectangular RegionsDouble Integrals over General RegionsApplications of Double Integrals: Area, Mass, and MomentsTriple Integrals in Cartesian CoordinatesTriple Integrals in Cylindrical and Spherical CoordinatesChange of Variables and the Jacobian DeterminantApplications of Triple Integrals: Volume and MassVector Fields and Their RepresentationsLine Integrals of Vector FieldsGreen's TheoremSurface Integrals and Flux of Vector FieldsSurface Integrals and Flux of Vector FieldsDivergence Theorem: Flux and OutflowDivergence TheoremElectric FluxGauss's LawConductors in Electrostatic EquilibriumCapacitance and CapacitorsDielectricsDielectric Constant and Relative PermittivityElectric Field Inside Dielectric MaterialsDielectric Materials and PolarizationDielectric Susceptibility and PermittivityEnergy Density in Electric FieldsElectric Current and Current DensityElectrical Resistance and ResistivityOhm's Law and Circuit ElementsElectromotive Force (EMF) and BatteriesKirchhoff's Circuit Laws: Voltage and CurrentDC Circuit Network Analysis MethodsTransient Response in RC CircuitsRC CircuitsLC and RLC CircuitsAC Circuits: FundamentalsImpedance and ReactanceAC Power and ResonanceElectromagnetic WavesThe Electromagnetic SpectrumBlackbody Radiation and Planck's LawPhotoelectric EffectThe Photon: Light as QuantaCompton ScatteringWave-Particle Dualityde Broglie WavelengthHeisenberg Uncertainty PrincipleWavefunction and the Born RuleThe Schrödinger EquationState Vectors and WavefunctionsQuantum SuperpositionQuantum EntanglementBell Theorem and Bell InequalitiesPostulates of Quantum MechanicsQuantum Mechanical Treatment of HydrogenSolving the Schrödinger Equation for Hydrogen Atom

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