Anharmonicity and the Morse Potential

A real chemical bond can break; a harmonic spring cannot. That single fact — that dissociation exists — forces every quantum treatment of vibration to go beyond the parabola of the Vibrational Transitions and the Harmonic Oscillator model. Near the bottom of a potential well the harmonic approximation is excellent. This is why it works so well for fundamental bands. But as a diatomic molecule climbs its vibrational ladder, the levels bunch closer together. Overtones fall at less than exact integer multiples of the fundamental. Eventually the molecule flies apart. None of this is visible in a quadratic potential, where the levels are perfectly evenly spaced forever. The Morse potential is the standard chemist's fix. It is an analytic, exactly solvable curve. It curves over correctly at large bond extension. It has a finite number of bound states. It reproduces the two most robust experimental numbers for any diatomic. These are the harmonic frequency ωe\omega_e and the anharmonicity constant ωexe\omega_e x_e. It matters because essentially every quantitative feature of vibrational spectroscopy depends on anharmonicity. This holds true for measurements chemists actually make, not the idealized harmonic oscillator. This includes dissociation energies from Birge–Sponer plots, and overtone intensities in IR and Raman spectra. It also includes hot-band structure in high-temperature gases. Finally, it includes the vibrational envelopes underlying Electronic Transitions and Franck-Condon analysis. The big picture is that anharmonicity is not a small correction to be apologized for. It is the physical content of bond-breaking encoded in spectroscopy. A Taylor expansion of any realistic potential energy curve beyond quadratic order automatically produces cubic and quartic terms. Perturbation theory on those terms produces exactly the same energy-level formula. This is the same formula that the exactly-solvable Morse oscillator gives at leading order. This convergence between "expand the true potential" and "solve a specific analytic model" is important. It is what makes the Morse potential such a trusted workhorse. It is simple enough to solve in closed form. Yet it is rich enough to capture the essential physics of level convergence and dissociation. This article builds the Morse potential from physical requirements. It derives its exact bound-state energies. It connects them to the spectroscopist's anharmonicity constant ωexe\omega_e x_e. It shows how overtones, hot bands, and the Birge–Sponer extrapolation to dissociation energy all fall out of one formula. Three worked examples pin every number to a check. These are a textbook diatomic, an applied IR/Raman case, and a competition-level extrapolation problem.

Key takeaways
  • The harmonic oscillator gives evenly spaced levels forever; real bonds dissociate, so the potential must flatten at large rr and support only finitely many bound states.
  • The Morse potential V(r)=De[1−e−a(r−re)]2V(r) = D_e\left[1 - e^{-a(r-r_e)}\right]^2 is exactly solvable and gives converging vibrational levels.
  • The exact result G(v)=ωe(v+12)−ωexe(v+12)2G(v) = \omega_e(v+\tfrac12) - \omega_e x_e (v+\tfrac12)^2 shows levels crowding together as vv increases.
  • Overtones (Δv=2,3,…\Delta v = 2,3,\dots) appear at less than integer multiples of the fundamental because of ωexe\omega_e x_e; hot bands arise from thermally populated v=1v=1 starting states.
  • A Birge–Sponer plot of ΔGv+1/2\Delta G_{v+1/2} vs. v+1v+1 extrapolates linearly to zero to estimate the dissociation energy D0D_0.
  • Key idea: anharmonicity converts an infinite ladder of equal steps into a finite, converging ladder whose curvature directly encodes the bond's dissociation energy.

Where this lives today

Modern Fourier-transform infrared and Raman spectrometers routinely resolve overtone and combination bands to fractions of a wavenumber, and anharmonicity constants extracted from these spectra feed directly into force-field and potential-energy-surface refinement for computational chemistry — a calculated harmonic frequency from density functional theory is systematically scaled or explicitly anharmonically corrected (VPT2, vibrational perturbation theory to second order) precisely because raw harmonic DFT frequencies overestimate observed fundamentals by an amount closely related to ωexe\omega_e x_e. Atmospheric and combustion chemistry rely on Morse-type anharmonic data for CO2_2, CO, H2_2O, and OH radical bands to model infrared absorption accurately across the wide temperature ranges found in flames, engines, and planetary atmospheres, where hot bands are not a curiosity but a dominant spectral feature. In astrochemistry, the anharmonicity constants of simple diatomics and small hydrides measured in cold interstellar clouds versus hot circumstellar envelopes are used as thermometers, since hot-band intensities directly encode the local vibrational temperature. Pharmaceutical and materials laboratories use overtone spectroscopy (near-infrared, where overtones and combination bands of C–H, O–H, and N–H stretches dominate) for rapid, nondestructive quantitative analysis, and the quantitative shift of these overtones below exact harmonic multiples is a direct, routinely-exploited consequence of the anharmonicity discussed here. Finally, the same convergence-toward-dissociation picture underlies the vibrational envelopes seen in Electronic Transitions and Franck-Condon spectra, where anharmonic vibrational wavefunctions in both electronic states control which vibronic transitions carry intensity, and it underlies the fine rotational structure analyzed in Vibration-Rotation Spectra: P, Q, R Branches, where vibration–rotation coupling constants are themselves consequences of the anharmonic, non-rigid nature of the real potential curve.

Ask the tutor: How would the Birge–Sponer extrapolation change if a third-order anharmonicity constant ω_e y_e were included in the level formula?

The physical picture — thorough prose

Picture the potential energy of a diatomic molecule as a function of internuclear distance rr. Near the equilibrium separation rer_e, any smooth potential looks locally like a parabola — this is simply the statement that the first derivative vanishes at a minimum and the leading nonzero term in a Taylor series is quadratic. This is exactly the justification for the harmonic oscillator model used for small-amplitude vibrations. But a parabola rises without bound as r→∞r\to\infty, which is unphysical: real bonds have a finite dissociation energy DeD_e, beyond which the atoms simply separate and the potential becomes flat. The true potential curve is therefore asymmetric. It rises steeply on the compression side (nuclei and electron clouds pushing into each other cost much more energy than the same displacement in the stretching direction), and it rises only gently, then plateaus, on the stretching side. This asymmetry has three consequences that dominate real vibrational spectra. First, the vibrational levels are not evenly spaced — they crowd together as vv increases, converging on the dissociation limit. Second, the average bond length increases with vibrational quantum number (because the potential is "softer" on the outside), which shows up as a temperature-dependent effective bond length in rotational spectra. Third, the wavefunctions become skewed toward large rr for higher vv, changing intensity patterns for hot bands and overtones. The Morse function is the simplest analytic curve that captures all of this while remaining exactly solvable by the same operator methods used for the harmonic oscillator. It is built from three physically motivated ingredients: a finite well depth DeD_e, a curvature parameter aa that controls how sharply the well is shaped (and is fixed by matching the second derivative at the minimum to the harmonic force constant kk), and the correct qualitative shape — steep on the inner wall, flat on the outer wall, exactly one minimum.

Figure
The Morse potential compared to the harmonic parabola: the true well flattens toward dissociation while the parabola rises forever
r (bond length) V(r) Morse V(r) harmonic V(r) r_e D_e v=4 v=3 v=2 v=1 v=0

Notice how the green level spacings shrink as vv increases — that convergence is the direct visual signature of anharmonicity, and it is completely absent in the dashed harmonic parabola, whose levels (not drawn, but implied) would stay evenly spaced all the way up.

Figure
Level convergence toward D_e and the Birge–Sponer extrapolation
v + 1 ΔG_(v+1/2) extrapolated to 0 1 2 3 8 area under bars = D_0 (Birge–Sponer sum)

The core ideas — the governing equations/relationships

The Morse potential itself is defined as

V(r)=De[1−e−a(r−re)]2V(r) = D_e\left[1 - e^{-a(r - r_e)}\right]^2

where:

  • DeD_e is the well depth measured from the potential minimum (not from v=0v=0),
  • rer_e is the equilibrium bond length,
  • aa is a range parameter (units of inverse length) controlling the width of the well,
  • rr is the internuclear separation.

Reading: at r=rer = r_e, V=0V=0 (the minimum); as r→∞r\to\infty, V→DeV\to D_e (dissociation limit, flat); as r→0r\to 0, V→De(1−eare)2V\to D_e(1-e^{ar_e})^2, a large finite number — the Morse potential is actually too soft at very short range compared to real repulsive walls, but this defect rarely matters for the low-lying levels chemists probe. The curvature parameter is fixed by matching the harmonic force constant:

a=ωe2π2cμDehequivalentlyk=2Dea2a = \omega_e\sqrt{\frac{2\pi^2 c \mu}{D_e h}} \quad\text{equivalently}\quad k = 2D_e a^2

where:

  • kk is the harmonic force constant obtained from d2Vdr2∣re\left.\dfrac{d^2V}{dr^2}\right|_{r_e},
  • μ\mu is the reduced mass of the diatomic,
  • ωe\omega_e is the harmonic vibrational wavenumber (cm−1^{-1}) that would be observed if the well were purely quadratic.

Reading: aa is not an independent free parameter once DeD_e and ωe\omega_e (equivalently kk) are known — the shape of the well near the bottom is tied to the same force constant that governs the harmonic oscillator, while DeD_e controls how far out the well extends before flattening. The exact bound-state vibrational term values (in wavenumbers) are

G(v)=ωe(v+12)−ωexe(v+12)2G(v) = \omega_e\left(v + \tfrac12\right) - \omega_e x_e\left(v + \tfrac12\right)^2

where:

  • v=0,1,2,…v = 0, 1, 2, \dots is the vibrational quantum number, restricted to a finite set of values,
  • ωe\omega_e is the harmonic wavenumber (the spacing the levels would have at the very bottom of the well),
  • ωexe\omega_e x_e is the anharmonicity constant (also in cm−1^{-1}), always positive for a Morse-like well, and related to ωe\omega_e and DeD_e by
ωexe=ωe24De\omega_e x_e = \frac{\omega_e^2}{4D_e}

Reading: the correction term is quadratic in (v+12)(v+\tfrac12), so successive level spacings decrease linearly with vv — this single fact is what makes the Birge–Sponer plot a straight line. The spacing between adjacent levels — the quantity directly measured in a spectrum as a "hot band" or overtone spacing — is

ΔGv+1/2≡G(v+1)−G(v)=ωe−2ωexe(v+1)\Delta G_{v+1/2} \equiv G(v+1) - G(v) = \omega_e - 2\omega_e x_e (v+1)

where:

  • ΔGv+1/2\Delta G_{v+1/2} is the energy gap between levels vv and v+1v+1, indexed at the half-integer midpoint by convention,
  • the right-hand side is linear in (v+1)(v+1), decreasing steadily as vv increases.

Reading: plotting ΔGv+1/2\Delta G_{v+1/2} against (v+1)(v+1) gives a straight line of slope −2ωexe-2\omega_e x_e and intercept ωe\omega_e — exactly the Birge–Sponer extrapolation used to estimate dissociation energies from a handful of measured overtone spacings.

Two derivations

Derivation AExact bound-state energies of the Morse oscillator

Goal: solve the vibrational Schrödinger equation for V(r)=De(1−e−ax)2V(r) = D_e(1-e^{-a x})^2, with x≡r−rex \equiv r - r_e, and show that the eigenvalues are exactly G(v)=ωe(v+12)−ωexe(v+12)2G(v) = \omega_e(v+\tfrac12) - \omega_e x_e (v+\tfrac12)^2, with only finitely many bound vv.

Step 1 — Set up the radial Schrödinger equation. For a diatomic vibrating along x=r−rex = r-r_e with reduced mass μ\mu, the nuclear Schrödinger equation is

−ℏ22μd2ψdx2+De(1−e−ax)2ψ=E ψ-\frac{\hbar^2}{2\mu}\frac{d^2\psi}{dx^2} + D_e\left(1-e^{-ax}\right)^2 \psi = E\,\psi

This is a genuine special-function eigenvalue problem, not perturbation theory — it can be solved exactly because the Morse potential, after the substitution below, maps onto the same differential equation that generates the associated Laguerre polynomials (structurally related to the radial hydrogen atom problem).

Step 2 — Change variables to expose the Laguerre structure. Introduce the dimensionless variable y=e−axy = e^{-ax} (so y→0y\to 0 as x→∞x\to\infty, dissociation, and y→∞y\to\infty as x→−∞x\to -\infty, deep compression) and the parameter

λ=2μDeaℏ\lambda = \frac{\sqrt{2\mu D_e}}{a\hbar}

Substituting transforms the Schrödinger equation into a form whose polynomial solutions exist only when a combinatorial quantity

n=λ−v−12,v=0,1,2,…n = \lambda - v - \tfrac12, \qquad v = 0,1,2,\dots

remains non-negative — this is exactly analogous to the quantization condition n=0,1,2,…n=0,1,2,\dots that emerges for the Coulomb problem, and it is what forces vv to be bounded above (there are only finitely many non-negative integers less than λ−12\lambda - \tfrac12).

Step 3 — Extract the eigenvalues. Carrying through the algebra (the standard result, verifiable by direct substitution of the ladder of Laguerre-type solutions back into the differential equation) gives eigenenergies

Ev=ℏωe(v+12)−(ℏωe)24De(v+12)2,ωe=a2DeμE_v = \hbar\omega_e\left(v+\tfrac12\right) - \frac{(\hbar\omega_e)^2}{4D_e}\left(v+\tfrac12\right)^2, \qquad \omega_e = a\sqrt{\frac{2D_e}{\mu}}

Converting to wavenumbers by dividing by hchc throughout, and defining ωexe≡(ℏωe)24Dehc⋅hc=ωe24De\omega_e x_e \equiv \dfrac{(\hbar\omega_e)^2}{4D_e hc} \cdot hc= \dfrac{\omega_e^2}{4D_e} (all quantities now in cm−1^{-1} once DeD_e is also expressed in cm−1^{-1}), reproduces exactly

G(v)=ωe(v+12)−ωexe(v+12)2G(v) = \omega_e\left(v+\tfrac12\right) - \omega_e x_e\left(v+\tfrac12\right)^2

Step 4 — Confirm the finite bound-state count. Because n=λ−v−12≥0n = \lambda - v - \tfrac12 \ge 0 is required for a normalizable (polynomial, not exponentially blowing-up) solution, the maximum vibrational quantum number is

vmax⁡=λ−12=ωe2 ωexe−12v_{\max} = \lambda - \tfrac12 = \frac{\omega_e}{2\,\omega_e x_e} - \tfrac12

Beyond vmax⁡v_{\max} there are no more bound states — the molecule has dissociated. This finite ceiling is the exact-solution counterpart of "the levels converge," and it is completely absent from the harmonic oscillator, which has no such bound.

Go deeper · Derivation B · 2 minAnharmonicity from perturbation theory on a cubic/quartic-corrected harmonic potential
Derivation BAnharmonicity from perturbation theory on a cubic/quartic-corrected harmonic potential

Goal: show that expanding any realistic potential to quartic order and applying second-order perturbation theory reproduces the same −ωexe(v+12)2-\omega_e x_e (v+\tfrac12)^2 structure — confirming that the Morse result is not an artifact of one specific functional form but the generic leading-order behavior of any anharmonic well.

Step 1 — Taylor-expand the true potential about rer_e. Any smooth V(r)V(r) with a minimum at rer_e can be written, with x=r−rex = r-r_e,

V(x)=12kx2+gx3+hx4+⋯V(x) = \tfrac12 k x^2 + g x^3 + h x^4 + \cdots

where the quadratic term defines the harmonic force constant kk (and hence ωe\omega_e, the zeroth-order frequency), while gg (cubic) and hh (quartic) are small anharmonic corrections — small in the sense that they are treated perturbatively relative to the harmonic term.

Step 2 — Treat gx3+hx4g x^3 + h x^4 as a perturbation on the harmonic-oscillator eigenstates. Using the harmonic oscillator raising/lowering operator representation of xx in terms of a^†,a^\hat a^\dagger, \hat a, one computes first-order corrections from the quartic term (diagonal, nonzero at first order) and second-order corrections from the cubic term (off-diagonal, contributes only at second order, since ⟨v∣x3∣v⟩=0\langle v|x^3|v\rangle = 0 by parity). Both contributions scale as (v+12)2(v+\tfrac12)^2 plus a vv-independent constant — this is the key structural fact, and it follows purely from the matrix elements of x3x^3 and x4x^4 between adjacent harmonic oscillator states (which connect vv to v±1,v±3v\pm1, v\pm3 for the cubic term and to v,v±2,v±4v, v\pm2, v\pm4 for the quartic term).

Step 3 — Collect terms into the standard spectroscopic form. After the algebra (a standard but lengthy exercise in Rayleigh–Schrödinger perturbation theory on the displaced harmonic oscillator), the corrected term values take the universal form

G(v)=ωe(v+12)−ωexe(v+12)2+ωeye(v+12)3+⋯G(v) = \omega_e\left(v+\tfrac12\right) - \omega_e x_e \left(v+\tfrac12\right)^2 + \omega_e y_e\left(v+\tfrac12\right)^3 + \cdots

with ωexe\omega_e x_e expressed in terms of gg, hh, kk, and μ\mu — the precise combination is not needed for chemistry students to reproduce, but its existence and sign are the point: for a well that is steep on the inside and shallow on the outside (the physically correct shape, exactly as the Morse curve has), ωexe\omega_e x_e comes out positive, meaning the levels converge, matching the exact Morse result derived above.

Step 4 — Match to the Morse potential as a special case. If one starts specifically from the Morse function itself, Taylor-expanding De(1−e−ax)2D_e(1-e^{-ax})^2 gives g=−Dea3g = -D_e a^3 and h=712Dea4h = \tfrac{7}{12}D_e a^4 (verifiable by direct series expansion of (1−e−ax)2(1-e^{-ax})^2), and substituting these into the general perturbative formula for ωexe\omega_e x_e reproduces exactly ωexe=ωe2/(4De)\omega_e x_e = \omega_e^2/(4D_e) — the same number obtained from the exact solution. This agreement between "exact solution of one specific model potential" and "perturbation theory on the generic Taylor expansion of any potential" is precisely why spectroscopists trust ωexe\omega_e x_e as a physically meaningful, model-independent anharmonicity constant, not an artifact of choosing the Morse functional form.

Worked examples

Example 1 — Foundational: level spacings and dissociation for a textbook diatomic. Consider a diatomic (asymmetric numbers, not 1^1H35^{35}Cl exactly, to keep the arithmetic transparent but realistic) with

ωe=2143.7 cm−1,ωexe=13.29 cm−1\omega_e = 2143.7\ \text{cm}^{-1}, \qquad \omega_e x_e = 13.29\ \text{cm}^{-1}

(these are, in fact, close to real CO values, chosen because CO is a workhorse in vibrational spectroscopy). Step 1: Zero-point energy.

G(0)=ωe(0.5)−ωexe(0.5)2=1071.85−3.3225=1068.53 cm−1G(0) = \omega_e(0.5) - \omega_e x_e (0.5)^2 = 1071.85 - 3.3225 = 1068.53\ \text{cm}^{-1}

Step 2: Fundamental transition v=0→1v=0\to1.

ΔG1/2=ωe−2ωexe(1)=2143.7−26.58=2117.12 cm−1\Delta G_{1/2} = \omega_e - 2\omega_e x_e(1) = 2143.7 - 26.58 = 2117.12\ \text{cm}^{-1}

This is the observed IR fundamental — already 26.6 cm−1^{-1} below the harmonic value ωe\omega_e, a directly measurable anharmonic shift. Step 3: First overtone v=0→2v=0\to2.

G(2)−G(0)=[ωe(2.5)−ωexe(2.5)2]−[ωe(0.5)−ωexe(0.5)2]G(2) - G(0) = \left[\omega_e(2.5) - \omega_e x_e(2.5)^2\right] - \left[\omega_e(0.5)-\omega_e x_e(0.5)^2\right]
=ωe(2.0)−ωexe(6.0)=4287.4−79.74=4207.66 cm−1= \omega_e(2.0) - \omega_e x_e(6.0) = 4287.4 - 79.74 = 4207.66\ \text{cm}^{-1}

Compare to twice the fundamental: 2×2117.12=4234.24 cm−12\times 2117.12 = 4234.24\ \text{cm}^{-1}. The overtone falls 26.6 cm−1^{-1} below twice the fundamental — the signature "less than double" pattern of real overtones, not an artifact of rounding. Step 4: Limiting case check. As ωexe→0\omega_e x_e \to 0 (approaching the pure harmonic limit), ΔG1/2→ωe\Delta G_{1/2}\to \omega_e and the overtone →2ωe\to 2\omega_e exactly — recovering the evenly-spaced harmonic ladder, confirming the formula collapses correctly onto the known limiting behavior. Step 5: Maximum vibrational quantum number and dissociation energy estimate.

vmax⁡=ωe2ωexe−12=2143.726.58−0.5=80.65−0.5=80.15  ⟹  vmax⁡=80v_{\max} = \frac{\omega_e}{2\omega_e x_e} - \frac12 = \frac{2143.7}{26.58} - 0.5 = 80.65 - 0.5 = 80.15 \implies v_{\max}=80
De=ωe24 ωexe=(2143.7)24(13.29)=4,595,44653.16=86,457 cm−1D_e = \frac{\omega_e^2}{4\,\omega_e x_e} = \frac{(2143.7)^2}{4(13.29)} = \frac{4{,}595{,}446}{53.16} = 86{,}457\ \text{cm}^{-1}

Converting to more familiar units (11 cm−1^{-1} = 0.011960.01196 kJ/mol):

De≈86,457×0.01196=1034 kJ/molD_e \approx 86{,}457 \times 0.01196 = 1034\ \text{kJ/mol}

This overshoots the true D0D_0 of CO (about 10721072 kJ/mol from DeD_e, actually — the Morse model is not perfect but lands in the right ballpark), which is the expected behavior: the Morse potential's outer wall is somewhat too soft/hard compared to the true curve at very large vv, so DeD_e from the simple formula is an approximation, refined in practice by higher-order terms (ωeye\omega_e y_e, etc.) and by the Birge–Sponer sum described next.

Example 2 — Applied: distinguishing hot bands from overtones in a heated IR cell. A vibrational spectroscopy experiment heats a sample of HCl-like gas (using the same illustrative constants as Example 1's molecule for continuity, applied here to a different diatomic scenario with ωe=2990.9 cm−1\omega_e = 2990.9\ \text{cm}^{-1}, ωexe=52.8 cm−1\omega_e x_e = 52.8\ \text{cm}^{-1}, values close to real HCl) to a temperature high enough to populate v=1v=1 appreciably. Two new lines appear near the fundamental: a hot band (v=1→2v=1\to2) and the first overtone (v=0→2v=0\to2). The task is to predict both positions and show they are not degenerate. Step 1: Fundamental v=0→1v=0\to1.

ΔG1/2=ωe−2ωexe(1)=2990.9−105.6=2885.3 cm−1\Delta G_{1/2} = \omega_e - 2\omega_e x_e(1) = 2990.9 - 105.6 = 2885.3\ \text{cm}^{-1}

Step 2: Hot band v=1→2v=1\to2.

ΔG3/2=ωe−2ωexe(2)=2990.9−211.2=2779.7 cm−1\Delta G_{3/2} = \omega_e - 2\omega_e x_e(2) = 2990.9 - 211.2 = 2779.7\ \text{cm}^{-1}

This line sits 2885.3−2779.7=105.6 cm−12885.3-2779.7=105.6\ \text{cm}^{-1} below the fundamental — always shifted to lower wavenumber (red of the fundamental) because deeper anharmonic levels have smaller spacings, and the hot band starts from an already-excited, more weakly bound level. Step 3: First overtone v=0→2v=0\to2.

G(2)−G(0)=ωe(2)−ωexe(6)=5981.8−316.8=5665.0 cm−1G(2)-G(0) = \omega_e(2) - \omega_e x_e(6) = 5981.8 - 316.8 = 5665.0\ \text{cm}^{-1}

which is close to, but measurably different from, twice the fundamental (2×2885.3=5770.6 cm−12\times 2885.3 = 5770.6\ \text{cm}^{-1}), a gap of 105.6 cm−1105.6\ \text{cm}^{-1} — again exactly 2ωexe2\omega_e x_e, consistent with the general spacing formula. Step 4: Relative intensity reasoning (qualitative but essential for interpretation). At room temperature the Boltzmann population of v=1v=1 relative to v=0v=0 is governed by

N1N0=exp⁡(−hc ΔG1/2kBT)\frac{N_1}{N_0} = \exp\left(-\frac{hc\,\Delta G_{1/2}}{k_BT}\right)

Using ΔG1/2=2885.3 cm−1\Delta G_{1/2}=2885.3\ \text{cm}^{-1} and T=298T=298 K, with hc/kB=1.4388hc/k_B = 1.4388 cm·K,

N1N0=exp⁡(−1.4388×2885.3298)=exp⁡(−13.93)≈8.9×10−7\frac{N_1}{N_0} = \exp\left(-\frac{1.4388 \times 2885.3}{298}\right) = \exp(-13.93) \approx 8.9\times 10^{-7}

This vanishingly small population explains why hot bands are normally negligible at room temperature and only become visible upon heating (or in vibrationally hot flames/plasmas) — a point that connects directly to why hot-band analysis is an experimental technique for high-temperature or laser-pumped samples, not routine cold-gas IR. Step 5: Limiting-case check. If T→0T\to 0, N1/N0→0N_1/N_0\to 0 exactly, the hot band vanishes entirely, and only the fundamental and (weak) overtone survive — consistent with the physical picture that hot bands require thermal population of excited vibrational states.

Example 3 — Competition-level: Birge–Sponer extrapolation from four measured overtone spacings. A student measures four successive vibrational spacings for a diatomic (constructed with deliberately non-round, unequal numbers to test the method honestly) in an emission spectrum:

ΔG1/2=1556.3 cm−1,ΔG3/2=1508.7 cm−1,ΔG5/2=1461.1 cm−1,ΔG7/2=1413.5 cm−1\Delta G_{1/2} = 1556.3\ \text{cm}^{-1}, \quad \Delta G_{3/2} = 1508.7\ \text{cm}^{-1}, \quad \Delta G_{5/2}=1461.1\ \text{cm}^{-1}, \quad \Delta G_{7/2}=1413.5\ \text{cm}^{-1}

Task: extract ωe\omega_e, ωexe\omega_e x_e, and estimate D0D_0 by Birge–Sponer summation, without assuming these are round textbook constants. Step 1: Confirm linearity and extract the slope. The formula predicts ΔGv+1/2=ωe−2ωexe(v+1)\Delta G_{v+1/2} = \omega_e - 2\omega_e x_e(v+1), linear in (v+1)(v+1). Taking successive differences:

ΔG3/2−ΔG1/2=1508.7−1556.3=−47.6 cm−1\Delta G_{3/2}-\Delta G_{1/2} = 1508.7 - 1556.3 = -47.6\ \text{cm}^{-1}
ΔG5/2−ΔG3/2=1461.1−1508.7=−47.6 cm−1\Delta G_{5/2}-\Delta G_{3/2} = 1461.1-1508.7 = -47.6\ \text{cm}^{-1}
ΔG7/2−ΔG5/2=1413.5−1461.1=−47.6 cm−1\Delta G_{7/2}-\Delta G_{5/2} = 1413.5-1461.1 = -47.6\ \text{cm}^{-1}

The constant difference of −47.6-47.6 cm−1^{-1} per step confirms the linear Morse prediction and directly gives

−2ωexe=−47.6  ⟹  ωexe=23.8 cm−1-2\omega_e x_e = -47.6 \implies \omega_e x_e = 23.8\ \text{cm}^{-1}

Step 2: Extract ωe\omega_e from the intercept. Using ΔG1/2=ωe−2ωexe(1)\Delta G_{1/2} = \omega_e - 2\omega_e x_e(1):

ωe=ΔG1/2+2ωexe=1556.3+47.6=1603.9 cm−1\omega_e = \Delta G_{1/2} + 2\omega_e x_e = 1556.3 + 47.6 = 1603.9\ \text{cm}^{-1}

Step 3: Find where the extrapolated line hits zero — this locates vmax⁡v_{\max}.

0=ωe−2ωexe(vmax⁡+1)  ⟹  vmax⁡+1=ωe2ωexe=1603.947.6=33.700 = \omega_e - 2\omega_e x_e(v_{\max}+1) \implies v_{\max}+1 = \frac{\omega_e}{2\omega_e x_e} = \frac{1603.9}{47.6} = 33.70

so vmax⁡≈32.70v_{\max} \approx 32.70 (the last bound level is near v=32v=32). Step 4: Birge–Sponer sum for D0D_0. The dissociation energy measured from v=0v=0 (i.e., D0D_0, not DeD_e) is the sum of all level spacings from v=0v=0 up to vmax⁡v_{\max}, which — because the spacings form an arithmetic sequence — is well approximated by the area of the triangle in the Birge–Sponer plot:

D0≈∑v=0vmax⁡ΔGv+1/2≈12 ωe (vmax⁡+1)=12(1603.9)(33.70)D_0 \approx \sum_{v=0}^{v_{\max}} \Delta G_{v+1/2} \approx \frac12 \,\omega_e\,(v_{\max}+1) = \frac12 (1603.9)(33.70)
D0≈12(54,051.4)=27,025.7 cm−1D_0 \approx \frac12 (54{,}051.4) = 27{,}025.7\ \text{cm}^{-1}

Converting to kJ/mol:

D0≈27,025.7×0.01196≈323.3 kJ/molD_0 \approx 27{,}025.7 \times 0.01196 \approx 323.3\ \text{kJ/mol}

Step 5: Cross-check using the closed-form Morse relation and compare. Independently, De=ωe2/(4ωexe)=(1603.9)2/(4×23.8)=2,572,495/95.2=27,022.6 cm−1D_e = \omega_e^2/(4\omega_e x_e) = (1603.9)^2/(4\times23.8) = 2{,}572{,}495/95.2 = 27{,}022.6\ \text{cm}^{-1}, in close agreement (within rounding) with the triangular Birge–Sponer sum — the tiny discrepancy of about 33 cm−1^{-1} arises because the triangle approximation slightly overcounts compared to the exact discrete sum, and this is the well-known systematic tendency of Birge–Sponer plots to overestimate D0D_0 if extrapolated using only low-vv data, since real potentials deviate from the pure Morse shape near dissociation. Step 6: Limiting-case sanity check. If the four measured spacings had instead been equal rather than linearly decreasing, the extracted ωexe\omega_e x_e would be exactly zero, vmax⁡→∞v_{\max}\to\infty, and the Birge–Sponer sum would diverge — correctly signaling that a genuinely harmonic (never-dissociating) oscillator has no finite dissociation energy, an internally consistent limiting behavior of the method.

Limiting cases, scope & common traps

Regime / questionBehaviorWhy
v→0v \to 0 (ground state, small amplitude)Morse and harmonic oscillator nearly coincideOnly the quadratic term in the Taylor expansion matters near the bottom of the well
ωexe→0\omega_e x_e \to 0Morse formula →\to harmonic ladder, G(v)=ωe(v+12)G(v)=\omega_e(v+\tfrac12)Corresponds to De→∞D_e\to\infty: an infinitely deep, never-dissociating well
v→vmax⁡v \to v_{\max}Level spacing ΔGv+1/2→0\Delta G_{v+1/2}\to 0Levels pile up at the dissociation limit; the "last" bound state merges into the continuum
High TT, thermally populated v=1,2,…v=1,2,\dotsHot bands appear, red-shifted from the fundamental by 2ωexe,4ωexe,…2\omega_e x_e, 4\omega_e x_e,\dotsExcited-state spacings are smaller than the v=0→1v=0\to1 spacing
Overtones Δv=2,3,…\Delta v=2,3,\dotsFall below exact integer multiples of the fundamentalQuadratic term in G(v)G(v) subtracts more from higher (v+12)2(v+\tfrac12)^2
Very high vv, near dissociationMorse potential systematically deviates from the true curveThe true outer wall does not follow (1−e−ax)2(1-e^{-ax})^2 exactly; Birge–Sponer overestimates D0D_0
Short internuclear distance (compressed bond)Morse potential is too soft (finite value instead of true steep repulsive wall)The exponential form does not reproduce the correct hard-core repulsion at very small rr

The chemist behind it

Origins · 1 minPhilip M. Morse and how this was discovered
PM
Philip M. Morse
1903–1985 · American theoretical physicist, MIT

Philip McCord Morse trained under Arnold Sommerfeld's tradition of rigorous quantum mechanics in the late 1920s, at the moment when Schrödinger's equation was being applied to increasingly realistic chemical problems. Working at Princeton and then Massachusetts Institute of Technology, Morse recognized that the exponential form De(1−e−ax)2D_e(1-e^{-ax})^2 was both a physically sensible shape for a bond potential — steep on compression, flat toward dissociation — and, remarkably, exactly solvable using the same special-function machinery (associated Laguerre-type equations) that had made the hydrogen atom tractable. His 1929 paper, "Diatomic Molecules According to the Wave Mechanics II: Vibrational Levels," gave spectroscopists a closed-form energy expression they could fit directly to observed band spacings, turning an intractable general anharmonic problem into an algebraic exercise. Morse went on to a broad career in acoustics, operations research, and mathematical physics — he later co-founded the field of operations research in the United States and wrote enduringly influential textbooks on theoretical physics and acoustics — but it is this one potential, bearing his name, that remains a fixture of every physical chemistry curriculum, quoted wherever a diatomic vibrational spectrum needs a model beyond the harmonic oscillator.

History
- 1900 — Planck's quantum hypothesis opens the door to quantized vibrational energy.
- 1925–1926 — Heisenberg and Schrödinger formulate matrix and wave mechanics, enabling exact treatments of model potentials.
- 1929 — Philip Morse publishes the exactly-solvable exponential potential bearing his name, giving closed-form vibrational term values for diatomics.
- 1930s — Birge and Sponer develop the graphical extrapolation method using measured level spacings to estimate dissociation energies.
- Mid-20th century onward — Dunham expansion and higher-order spectroscopic constants (ωeye\omega_e y_e, etc.) refine the Morse picture for precision spectroscopy.
Why does the harmonic oscillator fail to describe real vibrational spectra at high v?

The harmonic oscillator's potential is a parabola that rises without bound, so it predicts perfectly evenly spaced energy levels forever, with no possibility of dissociation. Real bonds break: the true potential curve flattens at large separation, converging to a finite dissociation energy. This means real vibrational levels must crowd together and eventually stop altogether at a finite quantum number. The harmonic oscillator, being exactly quadratic, has no mechanism to produce this convergence — it is an excellent approximation only for the lowest few vibrational states near the bottom of the well, where the true potential is locally well-approximated by a parabola, but it systematically fails for overtones, hot bands, and anything near dissociation.

Is the Morse potential the "correct" potential for real molecules?

No — it is a useful, exactly solvable analytic approximation, not an exact physical law. It correctly captures the qualitative shape (steep inner wall, flat outer wall, finite well depth) and gives a good two-parameter fit to low-lying vibrational levels, but real potentials deviate from the precise exponential form, especially very close to dissociation and at very short bond lengths (the Morse inner wall is actually too soft compared to real repulsive interactions). More accurate work uses higher-order Dunham expansions with additional constants (ωeye\omega_e y_e, ωeze\omega_e z_e, …) or numerically constructed RKR (Rydberg-Klein-Rees) potentials fitted directly to observed spectroscopic term values.

What is the physical meaning of the anharmonicity constant ω_e x_e?

It measures how quickly vibrational level spacings shrink as the quantum number v increases, and equivalently how curved (non-parabolic) the true potential is away from its minimum. A larger ω_e x_e relative to ω_e means a shallower, more rapidly converging well — fewer bound vibrational states and a lower dissociation energy, since De=ωe2/(4ωexe)D_e = \omega_e^2/(4\omega_e x_e). Conversely, a vanishingly small ω_e x_e describes an almost perfectly harmonic, very deep well that would require enormous energy to dissociate. In practice, ωexe\omega_e x_e is typically one to a few percent of ωe\omega_e for strong covalent bonds like CO or N₂, and larger for weakly bound or highly polarizable diatomics.

How do hot bands differ from overtones, and how can a spectroscopist tell them apart?

An overtone is a transition from v=0v=0 directly to v=2,3,…v=2,3,\dots (formally forbidden in the pure harmonic approximation but weakly allowed once anharmonicity mixes in higher-order dipole moment terms), appearing near, but below, an integer multiple of the fundamental. A hot band is a transition between two excited states, most commonly v=1→2v=1\to2, which requires thermal population of v=1v=1 to begin with. Hot bands are distinguished experimentally by their strong temperature dependence — they grow dramatically upon heating the sample and nearly vanish at low temperature — whereas overtone intensities depend mainly on anharmonic corrections to the dipole moment function and are comparatively temperature-independent (governed instead by the fixed v=0v=0 population).

Why does the Birge–Sponer method tend to overestimate the true dissociation energy?

The Birge–Sponer extrapolation assumes the linear relationship ΔGv+1/2=ωe−2ωexe(v+1)\Delta G_{v+1/2} = \omega_e - 2\omega_e x_e(v+1) holds all the way from low vv up to the dissociation limit, using only a handful of measured low-vv spacings to fix the slope and intercept. In reality, cubic and higher anharmonicity terms (ωeye\omega_e y_e, etc.) become significant near dissociation, so the actual level spacings curve downward faster than the simple straight-line extrapolation predicts. Because the triangular Birge–Sponer sum extends the straight line further than the true curve allows, it overcounts the total binding energy, systematically overestimating D0D_0 — a well-documented, textbook-level caveat whenever this method is applied using only a few low-lying data points.

Does the Morse potential apply to polyatomic molecules?

Directly, no — the Morse potential as derived here is a one-dimensional model for a single bond stretch in a diatomic, parameterized by a single reduced mass and a single coordinate. For polyatomics, each normal mode can be treated approximately with its own effective Morse-like anharmonic correction along that normal coordinate, but true polyatomic anharmonicity also includes mode-mode coupling terms (Fermi resonances, Darling-Dennison resonances) that have no single-diatomic analog. Nonetheless, the qualitative lessons — level convergence, overtone shortfalls, hot bands — carry over directly to individual stretching and bending modes of polyatomic molecules, and Morse-type functions are still commonly used as convenient building blocks in constructing full multidimensional potential energy surfaces.

How does anharmonicity connect to the Franck-Condon principle in electronic spectroscopy?

In electronic transitions, the molecule typically jumps between two different electronic potential energy curves, each of which is itself anharmonic and best modeled with its own Morse-like (or more accurate) shape. The vibrational wavefunctions used to compute Franck-Condon overlap integrals are the anharmonic Morse eigenfunctions, not simple harmonic oscillator functions, especially for transitions reaching high vibrational levels of an excited electronic state near its own dissociation limit. This is essential for understanding vibrational progressions in electronic absorption and emission spectra, where the anharmonic convergence of levels in the excited state directly shapes which vibronic peaks appear and how the intensity envelope tails off toward the dissociation continuum.

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