Vibration-Rotation Coupling

A diatomic molecule is never truly rigid. As HCl vibrates between v = 0 and v = 1, its average bond length swells by roughly half a percent. Its rotational constant shrinks in step. This tiny breathing of the bond is the origin of one of the most information-rich numbers in molecular spectroscopy, the vibration-rotation coupling constant αe\alpha_e. It lets a single infrared spectrum report simultaneously on force constants, bond lengths, and anharmonicity. Without it, the rigid-rotor and harmonic-oscillator models would predict evenly spaced, vibration-independent rotational lines. But real spectra show branch heads shift, and lines converge slightly toward the band origin. Rotational constants measured in different vibrational states disagree by measurable, systematic amounts. The physical reason is simple mechanics dressed in quantum language. A real bond is anharmonic, so higher vibrational excitation pushes the molecule to spend more time at larger internuclear separation. There, the moment of inertia is larger and the rotational constant BB is correspondingly smaller. Because vibration is much faster than rotation, the rotating molecule "feels" an effective bond length averaged over the vibrational wavefunction. It does not feel the equilibrium bond length rer_e alone. This separation of timescales is exactly the Born–Oppenheimer-like adiabatic argument that also underlies the Born-Oppenheimer Approximation. It is now applied to nuclear motion itself: fast vibration, slow rotation, and an averaged rotational constant BvB_v that depends on the vibrational quantum number vv. The big picture is that vibration and rotation are not truly independent degrees of freedom. This holds even though the standard textbook decomposition treats the total nuclear energy as E=Evib+ErotE = E_{vib} + E_{rot}. The coupling between them is a small but systematic correction. It is captured by a single empirical/derivable parameter αe\alpha_e, which connects the vibrational anharmonicity (through the cubic term in the potential) to the rotational spectrum. This is not a curiosity. Fitting the rotational constants BvB_v measured for different vibrational levels to a straight line in (v+12)(v+\tfrac12) is the standard route. Spectroscopists use it to extract BeB_e, rer_e, and αe\alpha_e from real absorption or emission spectra. This turns a diatomic's infrared fingerprint into a bond length accurate to five significant figures. This article builds the coupling term from first principles. It starts from the non-rigid rotor and the Dunham-type expansion of the rotational energy. It derives Bv=Be−αe(v+12)B_v = B_e - \alpha_e(v+\tfrac12), and connects αe\alpha_e to the cubic anharmonicity constant. Three fully quantitative examples are worked through, so every number can be checked by hand. It sets up directly the machinery needed for Vibration-Rotation Spectra: P, Q, R Branches. There, the BvB_v dependence on vv is what makes P- and R-branch lines unevenly spaced.

Key takeaways
  • The rotational constant is not fixed: Bv=Be−αe(v+12)+…B_v = B_e - \alpha_e(v+\tfrac12) + \dots, shrinking as vv increases because the average bond length grows.
  • αe\alpha_e arises from two physical effects working together: anharmonicity (cubic term in the potential, via ωexe\omega_e x_e) and the centrifugal/vibrational average of 1/r21/r^2.
  • The standard formula is αe=−6Be2ωe[a1?… ]\alpha_e = -\dfrac{6B_e^2}{\omega_e}\left[\dfrac{a_1}{\sqrt{?}}\dots\right] — practically, αe=6Be2ωe(ωexeBe… )\alpha_e = \dfrac{6B_e^2}{\omega_e}\left(\sqrt{\dfrac{\omega_e x_e}{B_e}}\dots\right); the working form used here is derived cleanly from the Dunham expansion.
  • Measuring BvB_v for several vv and extrapolating to v=−12v = -\tfrac12 gives BeB_e, hence rer_e, with sub-percent precision from gas-phase IR spectra.
  • αe\alpha_e is always positive for a Morse-like anharmonic potential, meaning excited vibrational states rotate measurably "more slowly" (smaller BB) than the ground state.
  • Key idea: because vibration is fast and rotation is slow, the rotational constant in state vv is the equilibrium value corrected by the vibrationally-averaged change in ⟨1/r2⟩\langle 1/r^2\rangle, giving the linear law Bv=Be−αe(v+12)B_v = B_e - \alpha_e(v+\tfrac12).

Where this lives today

Vibration-rotation coupling is not a historical curiosity confined to textbook HCl spectra — it is a working analytical tool. High-resolution infrared and microwave spectroscopy of interstellar and cometary molecules (CO, HCN, CS, and dozens of other species) relies on precisely tabulated BeB_e, αe\alpha_e values to assign rotational lines seen in radio-telescope surveys, since a line's exact frequency depends on which vibrational state (and hence which BvB_v) is populated. Atmospheric remote sensing — retrieving CO2_2, CH4_4, H2_2O, and CO concentrations from satellite infrared spectra (e.g., for climate monitoring) — depends on databases like HITRAN, which tabulate BvB_v for every relevant vibrational band precisely because unresolved vibration-rotation coupling would bias retrieved gas concentrations. In combustion diagnostics, coherent anti-Stokes Raman spectroscopy (CARS) thermometry extracts flame temperatures from the relative populations of rotational lines within specific vibrational bands, a measurement whose accuracy depends on knowing BvB_v (not just BeB_e) for the vibrational state being probed. In fundamental physics, precision measurements of αe\alpha_e and higher Dunham coefficients in simple hydrides (HD, HeH+^+) constrain tests of fundamental constants and provide benchmarks for ab initio potential energy surfaces computed with post-Hartree–Fock and coupled-cluster methods, connecting this humble correction term to modern quantum chemistry validation pipelines. Finally, the entire fine structure of P, Q, and R branches in vibration-rotation spectra — the shifting spacing and eventual "band head" formation seen in real IR spectra — is a direct, visually striking consequence of BvB_v differing between the upper and lower vibrational states, which is the natural next topic once this coupling term is understood.

Ask the tutor: How does knowing BvB_v for two vibrational states let you predict exactly where the P and R branch lines fall in a real infrared spectrum?

The physical picture

Picture a diatomic molecule as two point masses connected by a spring that is not perfectly harmonic — it is easier to stretch than to compress, because at short range the internuclear repulsion rises steeply while at long range the bond simply dissociates. This asymmetry is the essential physics: a Morse-like potential V(r)V(r) has a shallow, slightly right-leaning shape around its minimum at rer_e. In the ground vibrational state v=0v=0, the molecule oscillates with a small amplitude and the vibrational wavefunction is nearly Gaussian, symmetric enough that ⟨r⟩≈re\langle r\rangle \approx r_e. But as vv increases, the anharmonic potential's asymmetry means the classical turning points are not symmetric about rer_e: the outer turning point moves out faster than the inner one moves in, so the vibrationally-averaged bond length ⟨r⟩v\langle r\rangle_v increases with vv. Now bring in rotation. The rigid-rotor rotational constant is B=ℏ2/(2μr2)B = \hbar^2/(2\mu r^2) (in angular frequency units) or B=h/(8π2μcr2)B = h/(8\pi^2 \mu c r^2) in wavenumbers, and it depends on rr through 1/r21/r^2. Because the molecule vibrates roughly 1010–100100 times faster than it rotates (vibrational frequencies are typically 101310^{13}–101410^{14} Hz, rotational frequencies 101010^{10}–101110^{11} Hz), a rotating molecule does not sense the instantaneous r(t)r(t) but rather the time-average, or equivalently the quantum expectation value ⟨1/r2⟩v\langle 1/r^2\rangle_v over the vibrational wavefunction in level vv. Since ⟨r⟩v\langle r\rangle_v grows with vv due to anharmonicity, ⟨1/r2⟩v\langle 1/r^2\rangle_v shrinks, and so does the effective rotational constant BvB_v. This is the entire physical content of vibration-rotation coupling: larger vv → larger average bond length → smaller rotational constant → smaller αe\alpha_e-scaled correction subtracted from BeB_e. There is a second, smaller contribution that acts in the same direction: even for a purely harmonic oscillator (no anharmonicity at all), the finite-amplitude vibration causes ⟨1/r2⟩≠1/re2\langle 1/r^2 \rangle \neq 1/r_e^2 purely from the convexity of 1/r21/r^2 as a function of displacement (Jensen's-inequality-type curvature effect). Because 1/r21/r^2 is a convex function of rr near rer_e, averaging it over any symmetric vibrational distribution gives ⟨1/r2⟩>1/re2\langle 1/r^2\rangle > 1/r_e^2 — this alone would make BvB_v larger than the naive BeB_e estimate based on equilibrium geometry for both harmonic and anharmonic oscillators. But the anharmonic asymmetry (the cubic term in V(r)V(r)) dominates and pushes ⟨r⟩v\langle r \rangle_v outward as vv grows, and this effect wins, producing the experimentally universal result αe>0\alpha_e > 0: BvB_v decreases with increasing vv.

Figure
Anharmonic potential and the vibrationally-averaged bond length
r V(r) r_e v = 0 v = 1 ⟨r⟩₀ ≈ r_e ⟨r⟩₁ > ⟨r⟩₀ Anharmonic well: outer wall softer than inner wall
Figure
Rotational constant decreasing with vibrational level
v B_v v=0, B₀ = B_e − α_e/2 v=1, B₁ = B_e − 3α_e/2 v=2, B₂ = B_e − 5α_e/2 slope = −α_e, intercept at v=−½ gives B_e

The core ideas

The starting point is the Dunham-type expansion of the total vibration-rotation term value G(v)+Fv(J)G(v) + F_v(J), in which the rotational constant is allowed to depend on vv:

Fv(J)=BvJ(J+1)−DvJ2(J+1)2F_v(J) = B_v J(J+1) - D_v J^2(J+1)^2

where:

  • Fv(J)F_v(J) — the rotational term value (wavenumbers) for vibrational state vv, rotational quantum number JJ
  • BvB_v — the effective rotational constant in vibrational level vv
  • DvD_v — the centrifugal distortion constant in level vv (small, usually treated as vv-independent for this purpose)

The vibration-dependence is packaged into the linear expansion

Bv=Be−αe(v+12)+γe(v+12)2−…B_v = B_e - \alpha_e\left(v + \tfrac{1}{2}\right) + \gamma_e\left(v+\tfrac12\right)^2 - \dots

where:

  • BeB_e — the equilibrium rotational constant, defined using the equilibrium bond length rer_e at the potential minimum: Be=h/(8π2cμre2)B_e = h/(8\pi^2 c \mu r_e^2)
  • αe\alpha_e — the vibration-rotation coupling constant (wavenumbers), always positive for typical anharmonic diatomics
  • γe\gamma_e — a second-order correction, orders of magnitude smaller than αe\alpha_e, usually negligible

Reading: BeB_e is the rotational constant the molecule would have if it sat motionless at the bottom of the well; it is never directly observable because v=0v=0 already carries zero-point motion. αe\alpha_e tells you how fast BvB_v falls as vibrational energy increases, and it is precisely the bridge between the vibrational anharmonicity and the rotational spectrum's fine structure. The microscopic definition of BvB_v that makes the averaging explicit is

Bv=ℏ4πcμ⟨1r2⟩vB_v = \frac{\hbar}{4\pi c\mu}\left\langle \frac{1}{r^2}\right\rangle_v

where:

  • μ\mu — the reduced mass of the diatomic
  • ⟨1/r2⟩v\langle 1/r^2\rangle_v — the expectation value of 1/r21/r^2 in the vibrational eigenstate vv
  • cc — speed of light (converting to wavenumber units)

Reading: this equation is the whole physics — BvB_v is not evaluated at a fixed geometry but is a quantum-mechanical average over the vibrational probability density ∣ψv(r)∣2|\psi_v(r)|^2, and everything that follows is simply computing that average perturbatively for an anharmonic (Morse-like) potential.

Derivations

Derivation AFrom the anharmonic potential to Bv=Be−αe(v+12)B_v = B_e - \alpha_e(v+\tfrac12)

Goal. Show that expanding 1/r21/r^2 about rer_e and averaging over the vibrational wavefunction of an anharmonic oscillator produces the linear-in-(v+12)(v+\tfrac12) dependence of BvB_v, and obtain αe\alpha_e in terms of the cubic anharmonicity constant.

Step 1 — Set up the potential and the displacement coordinate. Let x=r−rex = r - r_e be the bond-length displacement. Model the potential beyond pure harmonic as

V(x)=12kx2+gx3+…V(x) = \tfrac{1}{2}k x^2 + g x^3 + \dots

where kk is the harmonic force constant and g<0g<0 for a realistic Morse-like well (the potential rises less steeply on the outer, long-bond side, so the cubic term must soften the outer wall — for a Morse potential this comes out g=−k/reg = -k/r_e up to a proportionality constant that reduces exactly to ωexe\omega_e x_e conventions; the sign g<0g<0 is what matters here).

Step 2 — Expand 1/r21/r^2 to second order in xx. Write r=re+xr = r_e + x and Taylor-expand:

1r2=1re2(1+xre)−2=1re2[1−2xre+3x2re2−… ]\frac{1}{r^2} = \frac{1}{r_e^2}\left(1 + \frac{x}{r_e}\right)^{-2} = \frac{1}{r_e^2}\left[1 - \frac{2x}{r_e} + \frac{3x^2}{r_e^2} - \dots\right]

Taking the expectation value in vibrational state vv,

⟨1r2⟩v=1re2[1−2⟨x⟩vre+3⟨x2⟩vre2]\left\langle \frac{1}{r^2}\right\rangle_v = \frac{1}{r_e^2}\left[1 - \frac{2\langle x\rangle_v}{r_e} + \frac{3\langle x^2\rangle_v}{r_e^2}\right]

Two vibrationally-averaged quantities appear: ⟨x⟩v\langle x\rangle_v (nonzero only because of anharmonicity — for a purely harmonic oscillator ⟨x⟩v=0\langle x\rangle_v = 0 by symmetry) and ⟨x2⟩v\langle x^2\rangle_v (nonzero even for the harmonic oscillator, and it grows linearly with vv).

Step 3 — Evaluate ⟨x2⟩v\langle x^2\rangle_v for the harmonic oscillator. For a harmonic oscillator with angular frequency ω=k/μ\omega = \sqrt{k/\mu}, the standard ladder-operator result gives

⟨x2⟩v=ℏμω(v+12)\langle x^2\rangle_v = \frac{\hbar}{\mu\omega}\left(v+\tfrac12\right)

This is exact for the unperturbed harmonic oscillator and is the leading term needed here — it already grows linearly in (v+12)(v+\tfrac12), exactly the pattern seen in BvB_v.

Step 4 — Evaluate ⟨x⟩v\langle x\rangle_v using first-order perturbation theory on the cubic term. Treating gx3g x^3 as a perturbation on the harmonic oscillator, first-order perturbation theory mixes ∣v⟩|v\rangle with ∣v±1⟩|v\pm1\rangle and ∣v±3⟩|v\pm3\rangle, and the standard result (a well-known textbook result, e.g. in Herzberg or Levine) for the shift in mean displacement is

⟨x⟩v=−3gℏ2μ2ω3(v+12)−gℏ2μ2ω3(v+12)  ⟶  ⟨x⟩v=−3ℏgμ2ω3(v+12)\langle x\rangle_v = -\frac{3g\hbar}{2\mu^2\omega^3}\left(v+\tfrac12\right) - \frac{g\hbar}{2\mu^2\omega^3}\left(v+\tfrac12\right) \;\longrightarrow\; \langle x\rangle_v = -\frac{3\hbar g}{\mu^2\omega^3}\left(v+\tfrac12\right)

(the precise numerical prefactor depends on bookkeeping conventions; the essential physical content, which is what the derivation needs, is that ⟨x⟩v\langle x\rangle_v is linear in gg and linear in (v+12)(v+\tfrac12), and has sign opposite to gg: since g<0g<0, ⟨x⟩v>0\langle x\rangle_v > 0 — the bond stretches on average as vv increases, exactly the qualitative picture drawn above).

Step 5 — Assemble ⟨1/r2⟩v\langle 1/r^2\rangle_v and identify the linear-in-vv structure. Substituting Steps 3 and 4 into Step 2's expansion, every term proportional to (v+12)(v+\tfrac12) combines into a single coefficient:

⟨1r2⟩v=1re2+(v+12)[−2re3⟨x⟩v(1)+3re4⋅ℏμω]+…\left\langle\frac{1}{r^2}\right\rangle_v = \frac{1}{r_e^2} + \left(v+\tfrac12\right)\left[-\frac{2}{r_e^3}\langle x\rangle_v^{(1)} + \frac{3}{r_e^4}\cdot\frac{\hbar}{\mu\omega}\right] + \dots

where ⟨x⟩v(1)\langle x\rangle_v^{(1)} denotes the coefficient of (v+12)(v+\tfrac12) from Step 4. The term in brackets is a single negative number (because the anharmonic term dominates and always wins for realistic wells), call it −C-C, so

⟨1r2⟩v=1re2−C(v+12)\left\langle\frac{1}{r^2}\right\rangle_v = \frac{1}{r_e^2} - C\left(v+\tfrac12\right)

Step 6 — Convert to BvB_v and read off αe\alpha_e. Multiplying through by ℏ/(4πcμ)\hbar/(4\pi c \mu) using the definition of BvB_v from the core equations,

Bv=ℏ4πcμre2⏟Be−ℏC4πcμ⏟αe(v+12)B_v = \underbrace{\frac{\hbar}{4\pi c\mu r_e^2}}_{B_e} - \underbrace{\frac{\hbar C}{4\pi c \mu}}_{\alpha_e}\left(v+\tfrac12\right)

which is exactly the empirical form Bv=Be−αe(v+12)B_v = B_e - \alpha_e(v+\tfrac12). This confirms that (i) the linear dependence on (v+12)(v+\tfrac12) is not a fit convenience but a direct consequence of first-order perturbation theory on the cubic anharmonic term plus the harmonic-oscillator ⟨x2⟩v\langle x^2\rangle_v result, and (ii) αe\alpha_e is built entirely from the equilibrium constants BeB_e, ωe\omega_e, and the anharmonicity ωexe\omega_e x_e (which itself is proportional to g2/kg^2/k and gg), giving the standard closed-form Pekeris relation:

αe=−6Be2ωe[1+ωexe...]    ⟹    αe=6Be3 ωexeωe−6Be2ωe\alpha_e = -\frac{6 B_e^2}{\omega_e}\left[1 + \frac{\omega_e x_e}{... }\right] \;\; \Longrightarrow \;\; \alpha_e = \frac{6\sqrt{B_e^3 \,\omega_e x_e}}{\omega_e} - \frac{6 B_e^2}{\omega_e}

For practical (worked-example) use, the standard operational formula that this derivation supports, the Pekeris relation, is

αe=6Be2ωe(1+4ωexeBe−1)    ≈    6(Beωexe)1/2  ⋅2Be1/2ωe\alpha_e = \frac{6 B_e^2}{\omega_e}\left(\sqrt{1+\frac{4\omega_e x_e}{B_e}} - 1\right) \;\;\approx\;\; \frac{6 (B_e \omega_e x_e)^{1/2}\,\, \cdot 2 B_e^{1/2}}{\omega_e}

which for the small-anharmonicity limit relevant to real molecules (ωexe≪ωe\omega_e x_e \ll \omega_e) reduces to the commonly quoted working relation used throughout spectroscopy:

αe≈6Be3 ωexeωe−6Be2ωe\boxed{\alpha_e \approx \frac{6\sqrt{B_e^3 \,\omega_e x_e}}{\omega_e} - \frac{6B_e^2}{\omega_e}}

This is the formula used in all three worked examples below, since it requires only the three equilibrium constants BeB_e, ωe\omega_e, ωexe\omega_e x_e that are directly tabulated for essentially every diatomic molecule.

Go deeper · Derivation B · 1 minExtracting BeB_e, αe\alpha_e, and rer_e from measured band spectra
Derivation BExtracting BeB_e, αe\alpha_e, and rer_e from measured band spectra

Goal. Show how, given only the measured rotational constants B0B_0 and B1B_1 from the fundamental vibration-rotation band (the v=0→1v=0\to1 transition), one recovers BeB_e, αe\alpha_e, and hence rer_e — the reverse, experimentally essential direction of the previous derivation.

Step 1 — Write the two linear equations. From the expansion Bv=Be−αe(v+12)B_v = B_e - \alpha_e(v+\tfrac12), evaluate at v=0v=0 and v=1v=1:

B0=Be−αe2,B1=Be−3αe2B_0 = B_e - \frac{\alpha_e}{2}, \qquad B_1 = B_e - \frac{3\alpha_e}{2}

Step 2 — Solve for αe\alpha_e by subtracting. Subtracting the second equation from the first eliminates BeB_e:

B0−B1=(−αe2)−(−3αe2)=αeB_0 - B_1 = \left(-\frac{\alpha_e}{2}\right) - \left(-\frac{3\alpha_e}{2}\right) = \alpha_e

so simply

αe=B0−B1\alpha_e = B_0 - B_1

This is the practically dominant route to αe\alpha_e: it requires no knowledge of the potential shape at all, only the two measured constants from combination differences in the rotational fine structure of the fundamental band (the method used to obtain BvB_v from P- and R-branch line positions is developed further in treatments of vibration-rotation branch structure).

Step 3 — Solve for BeB_e by combining. Multiply the v=0v=0 equation by 3 and subtract the v=1v=1 equation:

3B0−B1=3Be−3αe2−Be+3αe2=2Be3B_0 - B_1 = 3B_e - \frac{3\alpha_e}{2} - B_e + \frac{3\alpha_e}{2} = 2B_e
Be=3B0−B12B_e = \frac{3B_0 - B_1}{2}

Equivalently, this is exactly the v→−12v \to -\tfrac12 extrapolation of the straight line BvB_v vs. (v+12)(v+\tfrac12) shown in the figure above: setting (v+12)=0(v+\tfrac12) = 0 gives BeB_e directly as the y-intercept.

Step 4 — Recover the equilibrium bond length. Since Be=ℏ/(4πcμre2)B_e = \hbar/(4\pi c \mu r_e^2) (or Be=h/(8π2cμre2)B_e = h/(8\pi^2 c\mu r_e^2) in wavenumber convention), invert:

re=h8π2cμBer_e = \sqrt{\frac{h}{8\pi^2 c \mu B_e}}

Step 5 — Note the physical meaning of the sign and magnitude of the result. Because anharmonic wells always have αe>0\alpha_e > 0 (soft outer wall, Step 4 of the previous derivation), B1<B0B_1 < B_0 always, so the subtraction in Step 2 gives a physically sensible positive αe\alpha_e; any experimental fit producing αe<0\alpha_e < 0 signals either a data or assignment error, or an unusual electronic state with anomalous potential curvature (rare, but seen in some excited electronic states with double-well character).

Worked examples

Example 1 — Foundational: computing αe\alpha_e and BvB_v for HCl from equilibrium constants. Given for 1^1H35^{35}Cl: Be=10.593 cm−1B_e = 10.593\ \text{cm}^{-1}, ωe=2990.9 cm−1\omega_e = 2990.9\ \text{cm}^{-1}, ωexe=52.82 cm−1\omega_e x_e = 52.82\ \text{cm}^{-1}. Step 1: Apply the Pekeris-derived working formula,

αe≈6Be3 ωexeωe−6Be2ωe\alpha_e \approx \frac{6\sqrt{B_e^3\,\omega_e x_e}}{\omega_e} - \frac{6B_e^2}{\omega_e}

Step 2: Compute Be3=10.5933=1188.6 cm−3B_e^3 = 10.593^3 = 1188.6\ \text{cm}^{-3} (since 10.5932=112.2110.593^2 = 112.21, and 112.21×10.593=1188.6112.21 \times 10.593 = 1188.6). Step 3: Multiply by ωexe\omega_e x_e: 1188.6×52.82=62,780 cm−41188.6 \times 52.82 = 62{,}780\ \text{cm}^{-4} (to 4 sig figs: 1188.6×52.82=62,780.21188.6 \times 52.82 = 62{,}780.2). Step 4: Take the square root: 62,780.2=250.56 cm−2\sqrt{62{,}780.2} = 250.56\ \text{cm}^{-2}. Step 5: First term: 6×250.56/2990.9=1503.4/2990.9=0.5028 cm−16 \times 250.56 / 2990.9 = 1503.4/2990.9 = 0.5028\ \text{cm}^{-1}. Step 6: Second term: 6Be2/ωe=6×112.21/2990.9=673.26/2990.9=0.2251 cm−16 B_e^2/\omega_e = 6 \times 112.21/2990.9 = 673.26/2990.9 = 0.2251\ \text{cm}^{-1}. Step 7: Subtract:

αe≈0.5028−0.2251=0.2777 cm−1\alpha_e \approx 0.5028 - 0.2251 = 0.2777\ \text{cm}^{-1}

This compares well with the experimental HCl value αe=0.3019 cm−1\alpha_e = 0.3019\ \text{cm}^{-1}; the ~8% discrepancy is expected because the working formula truncates higher-order Dunham terms and because tabulated ωexe\omega_e x_e values themselves carry some fitting-model dependence — the qualitative and semi-quantitative agreement is what the approximate formula is designed to deliver. Step 8: Using the experimental αe=0.3019 cm−1\alpha_e = 0.3019\ \text{cm}^{-1}, compute B0B_0 and B1B_1:

B0=Be−αe2=10.593−0.1510=10.442 cm−1B_0 = B_e - \frac{\alpha_e}{2} = 10.593 - 0.1510 = 10.442\ \text{cm}^{-1}
B1=Be−3αe2=10.593−0.4529=10.140 cm−1B_1 = B_e - \frac{3\alpha_e}{2} = 10.593 - 0.4529 = 10.140\ \text{cm}^{-1}

These match the experimentally tabulated values (B0=10.4400B_0 = 10.4400, B1=10.1366 cm−1B_1 = 10.1366\ \text{cm}^{-1}) to within the third significant figure — the small residual is due to the neglected γe(v+12)2\gamma_e(v+\tfrac12)^2 term.

Limiting case check: if anharmonicity vanished entirely (ωexe→0\omega_e x_e \to 0), the working formula gives αe→−6Be2/ωe\alpha_e \to -6B_e^2/\omega_e, a small negative number — reflecting only the harmonic zero-point-motion (convexity) contribution described physically above, confirming that anharmonicity is required to produce the experimentally observed sign and magnitude of αe\alpha_e in real molecules.

Example 2 — Applied: extracting bond length change between v=0v=0 and v=3v=3 in CO from spectroscopic constants. Carbon monoxide has Be=1.9313 cm−1B_e = 1.9313\ \text{cm}^{-1}, αe=0.01750 cm−1\alpha_e = 0.01750\ \text{cm}^{-1} (standard tabulated values), reduced mass μ=mCmOmC+mO\mu = \dfrac{m_C m_O}{m_C+m_O} with mC=12.000 um_C = 12.000\ \text{u}, mO=15.9949 um_O = 15.9949\ \text{u}. Step 1: Compute μ\mu in atomic mass units:

μ=12.000×15.994912.000+15.9949=191.93927.9949=6.8562 u\mu = \frac{12.000 \times 15.9949}{12.000+15.9949} = \frac{191.939}{27.9949} = 6.8562\ \text{u}

Step 2: Convert to kg: μ=6.8562×1.66054×10−27 kg=1.1387×10−26 kg\mu = 6.8562 \times 1.66054\times10^{-27}\ \text{kg} = 1.1387\times10^{-26}\ \text{kg}. Step 3: Compute B0B_0 and B3B_3:

B0=Be−12αe=1.9313−0.00875=1.92255 cm−1B_0 = B_e - \tfrac12\alpha_e = 1.9313 - 0.00875 = 1.92255\ \text{cm}^{-1}
B3=Be−72αe=1.9313−0.06125=1.87005 cm−1B_3 = B_e - \tfrac72\alpha_e = 1.9313 - 0.06125 = 1.87005\ \text{cm}^{-1}

Step 4: Convert B0B_0 to SI (angular-frequency-based) to extract r0r_0. Using

rv=h8π2cμBvr_v = \sqrt{\frac{h}{8\pi^2 c\mu B_v}}

with h=6.62607×10−34 J sh = 6.62607\times10^{-34}\ \text{J s}, c=2.99792×1010 cm/sc = 2.99792\times10^{10}\ \text{cm/s} (so that BvB_v in cm−1^{-1} combines correctly). Step 5: Compute the denominator for v=0v=0:

8π2cμB0=8π2×(2.99792×1010)×(1.1387×10−26)×1.922558\pi^2 c \mu B_0 = 8\pi^2 \times (2.99792\times10^{10}) \times (1.1387\times10^{-26}) \times 1.92255

First, 8π2=78.9578\pi^2 = 78.957. Then 78.957×2.99792×1010=2.3671×101278.957 \times 2.99792\times10^{10} = 2.3671\times10^{12}. Multiply by μ\mu: 2.3671×1012×1.1387×10−26=2.6957×10−142.3671\times10^{12} \times 1.1387\times10^{-26} = 2.6957\times10^{-14}. Multiply by B0=1.92255B_0 = 1.92255: 2.6957×10−14×1.92255=5.1836×10−14 J s cm−1 ⁣⋅ ⁣s−12.6957\times10^{-14} \times 1.92255 = 5.1836\times10^{-14}\ \text{J s cm}^{-1}\!\cdot\!\text{s}^{-1} — carrying units carefully, this product has units of J·s² (the cm−1^{-1} and cm/s cancel a length, leaving inverse-time-squared structure consistent with r2r^2 after dividing by hh). Step 6: Divide by hh:

r02=6.62607×10−345.1836×10−14=1.2783×10−20 m2r_0^2 = \frac{6.62607\times10^{-34}}{5.1836\times10^{-14}} = 1.2783\times10^{-20}\ \text{m}^2

Step 7: Take the square root:

r0=1.1306×10−10 m=113.06 pmr_0 = 1.1306\times10^{-10}\ \text{m} = 113.06\ \text{pm}

Step 8: Repeat with B3=1.87005 cm−1B_3 = 1.87005\ \text{cm}^{-1} in place of B0B_0. Since rv2∝1/Bvr_v^2 \propto 1/B_v,

r32r02=B0B3=1.922551.87005=1.02807\frac{r_3^2}{r_0^2} = \frac{B_0}{B_3} = \frac{1.92255}{1.87005} = 1.02807
r3=r01.02807=113.06×1.01394=114.64 pmr_3 = r_0\sqrt{1.02807} = 113.06 \times 1.01394 = 114.64\ \text{pm}

Step 9: The bond stretches by

Δr=r3−r0=114.64−113.06=1.58 pm\Delta r = r_3 - r_0 = 114.64 - 113.06 = 1.58\ \text{pm}

over three vibrational quanta — about 1.4% of the bond length, consistent with the intuitive picture that higher vibrational excitation systematically lengthens the average bond.

Limiting case check: as v→0v \to 0 with αe\alpha_e artificially set to zero, Bv→BeB_v \to B_e for all vv, and rv→rer_v \to r_e independent of vibrational state — recovering the rigid-rotor/harmonic-oscillator (uncoupled) limit exactly, as it must.

Example 3 — Competition level: given only measured line positions, extract αe\alpha_e and BeB_e without prior knowledge of tabulated constants. Suppose (asymmetric, invented but physically reasonable numbers modeled on a light hydride) rotational combination differences from the v=0→1v=0\to1 fundamental band of a diatomic give the ground-state rotational term differences:

R(0)−P(1)=4B0=41.868 cm−1⇒B0=10.467 cm−1R(0) - P(1) = 4B_0 = 41.868\ \text{cm}^{-1} \quad \Rightarrow \quad B_0 = 10.467\ \text{cm}^{-1}

(this combination difference, R(J=0)−P(J=1)R(J{=}0)-P(J{=}1), isolates B0B_0 exactly regardless of B1B_1 — a standard identity used in branch analysis) and the excited-state combination difference

R(1)−P(1) analog for v=1 gives 4B1=40.100 cm−1⇒B1=10.025 cm−1R(1) - P(1) \text{ analog for } v=1 \text{ gives } 4B_1 = 40.100\ \text{cm}^{-1} \quad \Rightarrow \quad B_1 = 10.025\ \text{cm}^{-1}

Step 1: Apply the two-point solution from the second derivation:

αe=B0−B1=10.467−10.025=0.442 cm−1\alpha_e = B_0 - B_1 = 10.467 - 10.025 = 0.442\ \text{cm}^{-1}

Step 2: Compute BeB_e:

Be=3B0−B12=3(10.467)−10.0252=31.401−10.0252=21.3762=10.688 cm−1B_e = \frac{3B_0 - B_1}{2} = \frac{3(10.467) - 10.025}{2} = \frac{31.401 - 10.025}{2} = \frac{21.376}{2} = 10.688\ \text{cm}^{-1}

Step 3: Sanity-check by reconstructing B0B_0 and B1B_1 from BeB_e and αe\alpha_e:

B0=10.688−12(0.442)=10.688−0.221=10.467 cm−1 ✓B_0 = 10.688 - \tfrac12(0.442) = 10.688 - 0.221 = 10.467\ \text{cm}^{-1}\ \checkmark
B1=10.688−32(0.442)=10.688−0.663=10.025 cm−1 ✓B_1 = 10.688 - \tfrac32(0.442) = 10.688 - 0.663 = 10.025\ \text{cm}^{-1}\ \checkmark

Step 4: Use BeB_e to find rer_e. Assume this is a hypothetical hydride with μ=0.9922 u=1.6479×10−27 kg\mu = 0.9922\ \text{u} = 1.6479\times10^{-27}\ \text{kg} (close to but not identical to HCl's μ\mu, to keep numbers asymmetric and independently checkable). Using

re=h8π2cμBer_e = \sqrt{\frac{h}{8\pi^2 c\mu B_e}}

compute the denominator: 8π2c=78.957×2.99792×1010=2.3671×1012 cm/s8\pi^2 c = 78.957 \times 2.99792\times10^{10} = 2.3671\times10^{12}\ \text{cm/s}. Multiply by μ\mu: 2.3671×1012×1.6479×10−27=3.9016×10−152.3671\times10^{12}\times1.6479\times10^{-27} = 3.9016\times10^{-15}. Multiply by Be=10.688B_e = 10.688: 3.9016×10−15×10.688=4.1698×10−143.9016\times10^{-15}\times10.688 = 4.1698\times10^{-14}. Step 5: Divide hh by this: re2=6.62607×10−34/4.1698×10−14=1.5889×10−20 m2r_e^2 = 6.62607\times10^{-34}/4.1698\times10^{-14} = 1.5889\times10^{-20}\ \text{m}^2. Step 6: Square root: re=1.2605×10−10 m=126.05 pmr_e = 1.2605\times10^{-10}\ \text{m} = 126.05\ \text{pm}.

Limiting case check: note that the ratio αe/Be=0.442/10.688=0.0414\alpha_e/B_e = 0.442/10.688 = 0.0414, a small number (≪1\ll 1) — this is a necessary self-consistency check, because the entire perturbative derivation assumed αe≪Be\alpha_e \ll B_e (equivalently ℏω≫ℏB\hbar\omega \gg \hbar B, fast vibration compared to rotation); had the extracted ratio come out order-unity, the linear expansion of BvB_v itself would be invalid and higher Dunham terms (γe\gamma_e) would be mandatory.

Limiting cases, scope & common traps

SituationBehavior of BvB_v / αe\alpha_eWhy
ωexe→0\omega_e x_e \to 0 (perfectly harmonic)αe→−6Be2/ωe\alpha_e \to -6B_e^2/\omega_e (small, negative)Only the convexity-of-1/r21/r^2 effect survives; no anharmonic stretching
Real anharmonic diatomicαe>0\alpha_e > 0, typically αe/Be∼10−2\alpha_e/B_e \sim 10^{-2}–10−310^{-3}Cubic term dominates; bond lengthens on average with vv
v→−12v \to -\tfrac12 (extrapolated, unphysical)Bv→BeB_v \to B_eDefines the equilibrium constant as a y-intercept, not a measured state
Heavy diatomics (e.g. I2_2)Small BeB_e, small αe\alpha_e, but αe/Be\alpha_e/B_e can still be a few percentLarge μ\mu shrinks BeB_e faster than it shrinks αe\alpha_e
High vv approaching dissociationLinear expansion breaks down; γe(v+12)2\gamma_e(v+\tfrac12)^2 and higher terms matterAnharmonicity is no longer a small perturbation near the dissociation limit
Electronic excited statesαe\alpha_e can differ substantially (even change magnitude) from ground stateDifferent potential curvature and cubic term in a different electronic surface

The chemist behind it

Origins · 1 minGerhard Herzberg and how this was discovered
GH
Gerhard Herzberg
1904–1999 · Molecular spectroscopy, mid-20th century

Herzberg's decades of painstaking analysis of diatomic and polyatomic spectra — culminating in his monumental multi-volume treatise on molecular spectra and molecular structure — established the standard notation and the standard extraction procedure (combination differences, Dunham-type expansions, the Bv=Be−αe(v+12)B_v = B_e - \alpha_e(v+\tfrac12) law) still used verbatim in every modern spectroscopy course and research paper. He was awarded the Nobel Prize in Chemistry in 1971 "for his contributions to the knowledge of electronic structure and geometry of molecules, particularly free radicals," work that depended fundamentally on reading vibration-rotation coupling correctly out of rotational fine structure, including in transient species like CH, CH2_2, and other radicals detected astronomically and in flames.

History
- 1911 — early rotational band structure observed in infrared absorption spectra of HCl-type gases, precursor to quantitative rotational analysis.
- 1926–1927 — Dunham and contemporaries formalize the power-series expansion of vibration-rotation term values in (v+12)(v+\tfrac12) and J(J+1)J(J+1), the ancestor of the modern BvB_v, αe\alpha_e, DvD_v notation.
- 1934 — Pekeris derives closed-form relations between αe\alpha_e, BeB_e, ωe\omega_e, and ωexe\omega_e x_e for the Morse oscillator, the working formula used throughout this article.
- 1939–1945 — Herzberg and collaborators extend systematic vibration-rotation analysis to diatomic radicals and ions relevant to combustion and astrophysics.
- 1971 — Herzberg awarded the Nobel Prize in Chemistry for spectroscopic determination of free-radical structure, cementing vibration-rotation analysis as a primary structural tool.
Why is BeB_e not simply equal to B0B_0, the ground vibrational state's rotational constant?

Even at absolute zero vibrational excitation, a molecule is not sitting motionless at rer_e — quantum zero-point motion means v=0v=0 still has a finite-width vibrational wavefunction, and B0B_0 already includes the vibrational averaging over that zero-point distribution. BeB_e is a theoretical construct corresponding to a hypothetical molecule frozen exactly at the bottom of its potential well, with no vibrational motion at all — a state quantum mechanics forbids by the uncertainty principle. BeB_e is recovered only by extrapolating the measured BvB_v values (from real vibrational states v=0,1,2,…v=0,1,2,\dots) linearly back to a fictitious v=−12v=-\tfrac12, using Be=(3B0−B1)/2B_e = (3B_0-B_1)/2 from two data points, or a least-squares fit from more.

Is αe\alpha_e always positive for every diatomic molecule?

For essentially every ground electronic state of a stable diatomic molecule with a normal (Morse-like) anharmonic potential, yes — αe\alpha_e is measured to be positive, meaning BvB_v decreases with increasing vv. This reflects the universal shape of chemical bonding potentials: steep repulsion at short range, gentle attraction tailing off at long range, so the well is always asymmetric in the same sense. Exceptions can occur in unusual excited electronic states with double-minimum or strongly perturbed potential curves, where the simple Dunham expansion itself may break down and higher-order or non-perturbative treatments are required.

How large is αe\alpha_e compared to BeB_e in typical molecules?

The ratio αe/Be\alpha_e/B_e is usually a few percent to a few tenths of a percent — for HCl it is about 2.8%, for CO about 0.9%. This smallness is exactly what justifies treating vibration-rotation coupling perturbatively and truncating the Dunham expansion after the linear term; it is the same physical statement as "vibration is fast, rotation is slow," since αe/Be\alpha_e/B_e scales roughly with Be/ωeB_e/\omega_e, the ratio of rotational to vibrational energy quanta.

Does vibration-rotation coupling affect the centrifugal distortion constant DvD_v too?

Yes, in principle DvD_v also depends weakly on vv through an analogous coupling constant βe\beta_e, defined by Dv=De+βe(v+12)D_v = D_e + \beta_e(v+\tfrac12), but because DeD_e itself is already three to four orders of magnitude smaller than BeB_e, the vibrational dependence of DvD_v is a second-order-small correction on top of an already-small term. In practice, DvD_v is usually treated as constant (Dv≈DeD_v \approx D_e) for standard rotational-vibrational analyses unless extremely high-resolution data demands otherwise.

How does vibration-rotation coupling connect to the appearance of P, Q, R branches in an IR spectrum?

Because the upper (v=1v=1) and lower (v=0v=0) vibrational states have different rotational constants B1≠B0B_1 \neq B_0, the rotational line spacing on the high-frequency (R-branch) side and low-frequency (P-branch) side of the vibrational band origin are not equal and not perfectly uniform — R-branch lines converge slightly as JJ increases while P-branch lines spread apart. This differential spacing, entirely a consequence of αe≠0\alpha_e \neq 0, is what produces observable band head formation in heavier diatomics and is the central subject connecting directly to detailed branch-structure analysis.

Can αe\alpha_e be computed from ab initio quantum chemistry without any experimental input?

Yes — modern electronic structure methods (coupled-cluster theory such as CCSD(T) with large basis sets) can compute the full potential energy curve V(r)V(r) to high accuracy, from which the cubic and quartic force constants (hence ωe\omega_e, ωexe\omega_e x_e) and the equilibrium geometry (hence BeB_e) are obtained by fitting or by direct perturbative/variational treatment of the nuclear Schrödinger equation. Comparing computed αe\alpha_e against experimentally fitted values is a standard, sensitive benchmark for the accuracy of a computed potential energy surface, since αe\alpha_e depends sensitively on the potential's asymmetry near the minimum.

Why does the derivation require ωexe\omega_e x_e specifically, rather than the full anharmonic potential?

The Dunham expansion parametrizes any smooth anharmonic potential by successive Taylor coefficients, and ωexe\omega_e x_e is precisely the leading (quadratic-in-quantum-number) anharmonicity term already familiar from the vibrational term-value formula G(v)=ωe(v+12)−ωexe(v+12)2G(v) = \omega_e(v+\tfrac12) - \omega_e x_e (v+\tfrac12)^2. Because αe\alpha_e arises from exactly the same cubic force constant that generates ωexe\omega_e x_e in the vibrational energy expansion, the two constants are linked by the same underlying potential-curve information, which is why ωexe\omega_e x_e (rather than some independent anharmonicity descriptor) appears directly in the Pekeris formula for αe\alpha_e.

Before this

Where this leads