MO Polarity and Electronegativity
Hydrogen fluoride is a small molecule with a huge dipole moment. It packs 1.83 D into a bond just 92 pm long. Nothing about the classical picture of a shared electron pair explains this. Why do electrons in that bond spend far more time near fluorine? The explanation lives entirely in the mathematics of the molecular orbital itself. Specifically, the bonding MO is not an equal mixture of the two atomic orbitals that built it. This article makes that asymmetry precise. It shows exactly how unequal atomic-orbital (AO) coefficients in a linear combination of atomic orbitals (LCAO) encode bond polarity. It shows how those coefficients are forced to be unequal whenever the contributing atoms differ in electronegativity. And it shows how to extract quantitative charge distributions, dipole moments, and bond-ionic-character estimates. These come directly from a Hückel-style or ab initio MO calculation. The big picture is simple to state but rich in consequence. Whenever two atoms with different orbital energies combine, the resulting bonding MO leans toward the lower-energy AO. The antibonding MO leans toward the higher-energy AO instead. This single asymmetry principle explains several things. It explains why the C–O bond in carbon monoxide is polarized toward oxygen. This holds even though the molecule's dipole moment famously points the "wrong" way overall. It explains why HF is essentially covalent in orbital character yet highly ionic in charge distribution. And it explains why electronegativity itself — a concept chemists use daily without always tracing its quantum-mechanical roots — is nothing more than a bookkeeping device. It tracks the orbital-energy differences that force this leaning to occur. This matters practically far beyond diatomics. Every polar covalent bond in organic and inorganic chemistry can be described this way. This includes C–Cl, N–H, Si–O, the carbonyl π system, and the P–O bonds of phosphate esters. Exactly the same coefficient asymmetry applies to all of them. The size of that asymmetry is what a chemist is really estimating. This happens whenever one reaches for a table of Pauling electronegativities. The same machinery underlies reactivity. An electrophilic carbon in a carbonyl is electrophilic for a specific reason: the LUMO (the π MO) has a large coefficient there. This fact is inseparable from another one. The ground-state bonding MO has a large coefficient on oxygen instead. Understanding polarity at the coefficient level is therefore a direct bridge. It leads to <a class="wiki-link" href="/wiki/chem-qchem-frontier-orbitals-homo-lumo" data-track="wiki_article.body.wiki_link">Frontier Orbitals: HOMO and LUMO</a> reasoning. There, the size and location* of frontier coefficients dictate where nucleophiles and electrophiles attack. By the end of this article you will be able to do several things. You will write down the secular equations for a heteronuclear two-orbital problem. You will solve for unequal coefficients. You will connect the resulting polarization parameter directly to a Mulliken/Pauling electronegativity difference. You will compute charge separation and a predicted dipole moment from LCAO coefficients. And you will diagnose, from a coefficient table alone, whether a bond is best described as covalent, polar covalent, or essentially ionic.
- A heteronuclear bonding MO has whenever (unequal AO energies).
- The bonding MO leans toward the more electronegative atom (lower/more stable AO energy); the antibonding MO leans toward the less electronegative atom.
- The polarization is governed by the ratio of the electronegativity gap to the resonance integral : large gap/small overlap → nearly ionic; small gap/large overlap → nearly covalent.
- Mulliken population analysis converts squared coefficients into effective atomic charges, which can be compared directly to experimental dipole moments.
- CO is the classic warning case: the orbital polarization (C positive, O negative in the bonding σ/π framework) is opposite in sign to the small net dipole that experiment reports, because lone-pair and core contributions partially cancel the bonding polarization.
- Key idea: bond polarity is not a separate ionic add-on to a covalent bond — it is the covalent bond, with its degree of AO-coefficient asymmetry set by how far apart the two atomic orbital energies sit relative to their mutual coupling strength.
Where this lives today
Every modern quantum chemistry package — Gaussian, ORCA, Psi4, NWChem — prints a Mulliken (or the more robust Löwdin, Hirshfeld, or NBO/NPA) population analysis by default after any single-point calculation, and the numbers it reports are conceptually identical to the , bookkeeping worked through in this article, just computed from a full basis set rather than a two-orbital toy model. Medicinal chemists reading a docking or DFT study routinely use these partial charges, derived from exactly this coefficient asymmetry, as inputs to molecular-mechanics force fields (AMBER, CHARMM, OPLS) that predict how a drug candidate's electrostatic surface will complement a binding pocket — the entire electrostatic term in a force field is, at bottom, a coarse-grained descendant of unequal LCAO coefficients. In materials science, the same polarization parameter generalizes to extended solids as the "bond ionicity" used in semiconductor physics (the Phillips–Van Vechten ionicity scale for compound semiconductors like GaAs or ZnSe), where the degree of covalent-versus-ionic bonding character, traceable to conduction/valence band orbital energy offsets, directly controls band gap size and exciton binding energy — critical parameters for LED and photovoltaic design. In catalysis, the polarization of metal–ligand σ and π bonds (again governed by the same -gap-versus--coupling competition, now between a transition-metal d orbital and a ligand orbital) determines whether a bound CO or NO ligand is activated toward nucleophilic or electrophilic attack, directly informing hydroformylation, Fischer–Tropsch, and related industrial catalytic cycle mechanisms. And in NMR and infrared spectroscopy, bond polarity computed this way correlates tightly with chemical shift and stretching-frequency shifts, giving spectroscopists a quantitative rationale for empirical trends they use daily (a highly polarized C=O stretches at different frequency and shifts different nuclei than a nearly nonpolar C=C, precisely because the underlying MO coefficients differ).
Ask the tutor: How would the bonding-MO polarization parameter λ change if I compared the C=O σ bond to the C=O π bond within the same molecule?
The physical picture
Return to the simplest possible heteronuclear system: two atomic orbitals, on atom A and on atom B, each an eigenfunction (approximately) of its own atom's effective Hamiltonian with orbital energies and . In a homonuclear diatomic such as H or N, by symmetry, and the variational solution is forced by that symmetry to give equal-magnitude coefficients: , giving a perfectly nonpolar bonding MO. The instant — the moment we go from H to HF, from CC to CO, from a symmetric π bond to a carbonyl π bond — the symmetry argument collapses and the variational principle must instead choose how much weight to put on each AO. It always chooses in the same direction: more weight on whichever orbital has the lower (more stable, more negative) energy. Physically, is close to (though not identical to) the negative of an atom's valence-state ionization energy for that orbital — it measures how tightly that atom holds an electron in that orbital when isolated. An atom that holds its own electrons tightly (F, O, N, Cl) has a deep, very negative ; an atom that holds them loosely (H, Si, Na) has a shallower, less negative . This is precisely the intuition behind electronegativity, and indeed one of the cleanest modern definitions of electronegativity (Mulliken's) is built directly from these same atomic energies:
which is, up to a sign and scale convention, an average of how much an atom "wants" the bonding electron pair — exactly the quantity that encodes orbital-by-orbital. When the two orbitals are mixed by a resonance (coupling) integral , the bonding combination is pulled toward the deeper well. Imagine two unequal buckets connected by a small pipe: water (electron density) redistributes so that the lower bucket ends up fuller. The bonding MO is the "low" combination and inherits more of atom A's character if A is more electronegative; the antibonding MO is the "high" combination and is thrown up onto the less electronegative atom B. This is shown schematically below, with H–F as the running numerical example throughout this article.
Squaring the coefficients gives the fractional electron population each atom contributes to a given MO. For the bonding σ of HF, and (before overlap normalization details, illustrative values used throughout), meaning roughly 90% of the bonding electron density (once the two bonding electrons are counted) sits formally nearer fluorine. That lopsidedness, propagated through every bond and lone pair, is the quantum-mechanical origin of the molecule's dipole moment, and it is exactly what a Mulliken population analysis converts into a formal atomic charge. A second figure makes the connection to the periodic table explicit: electronegativity differences across a row translate directly into how far apart the two starting AO energy levels sit, which is the single input (together with ) that determines the polarization.
The pattern to internalize: moving right across a period, the effective 2p orbital energy drops (becomes more negative) because increasing nuclear charge is not fully screened by added electrons in the same shell. A bond between two row-2 atoms with a large orbital-energy gap (C–F) is far more polarized than one with a small gap (C–N), and this is exactly the trend Pauling electronegativities were built to summarize — MO theory simply supplies the mechanism.
The core ideas
The starting point is the same two-orbital LCAO problem used for homonuclear diatomics, but now with . Write the trial MO as
where:
- — normalized atomic orbitals on atoms A and B,
- — variational LCAO coefficients to be determined.
Reading: this is the same ansatz used for H-type problems, but the variational solution no longer forces because nothing in the Hamiltonian is symmetric between A and B. Applying the variational method (minimizing the energy with respect to ) yields the secular equations
where:
- , — Coulomb (site) integrals, the AO energies,
- — the resonance (coupling) integral, negative and roughly proportional to overlap,
- — the overlap integral (often set to zero in the simplest Hückel-style treatment; kept symbolic here for generality),
- — the MO energy eigenvalue.
Reading: this is literally the same secular determinant as the homonuclear case, with the single crucial change that the two diagonal entries are no longer equal. That inequality is the entire seed of polarity. Setting for clarity (the Hückel/simple-LCAO convention), the secular determinant
expands to a quadratic in whose roots are
where:
- — bonding MO energy (lower, more negative, since convention or taking the root that lies below both 's),
- — antibonding MO energy (higher, less stable),
- the term under the square root shows how both the electronegativity gap and the coupling jointly set the splitting.
Reading: when this collapses to the familiar homonuclear result . The new feature is that the gap enters under a square root together with — the two effects (electronegativity mismatch and orbital overlap/coupling strength) compete to determine both the energy splitting and, as shown next, the coefficient asymmetry. The coefficients themselves, normalized, work out to
where:
- this ratio is a single real number since and everything is real; a ratio far from signals strong polarization, a ratio near signals near-covalent, symmetric sharing.
Reading: in the homonuclear limit this ratio becomes exactly (equal sharing); as , the ratio runs to or — the bonding MO becomes pure (or pure ), i.e. the fully ionic limit where one atom simply keeps both electrons. It is useful to define a single dimensionless polarization parameter
in terms of which the normalized bonding-MO coefficients take the compact closed form
where:
- taking B as the more electronegative atom (so , hence and with the sign convention handled so that means B is favored — conventions vary by textbook, but the physical content is fixed): , i.e. more bonding density on the more electronegative atom.
Reading: (equal 's, i.e. no electronegativity difference) reproduces , perfectly covalent. As (huge electronegativity gap or vanishing coupling), and : the fully ionic limit, one electron pair completely localized on the electronegative atom, exactly the classical ionic-bond picture. This formula is the precise mathematical bridge between the MO and ionic pictures of a chemical bond, and it is the quantitative version of Pauling's qualitative resonance argument (a polar bond is "part covalent, part ionic," and literally dials the mixture).
Goal. Starting from the 2×2 secular problem with unequal Coulomb integrals, derive the closed-form expressions for and in terms of , and verify the covalent and ionic limits.
Step 1 — Set up dimensionless variables. Define (average AO energy) and (the electronegativity-driven splitting). Shift the energy scale so ; then and . The secular determinant becomes
which expands to , giving measured from .
Step 2 — Introduce λ. Factor out (assume , the normal bonding case): write , so . The bonding root (lower energy, taking by the usual sign convention so that the physically bonding combination corresponds to , i.e., the algebraically smaller root) is
Step 3 — Solve for the coefficient ratio. From the first secular equation, , so
Using and being careful with signs (, so ), this simplifies to
Take the convention that gives when B is more electronegative ( meaning A's level lies above B's), which is the physically sensible branch: .
Step 4 — Normalize. Impose (orthonormal AOs, ). Writing , normalization gives , so and . Substituting and simplifying the algebra (multiply and divide by to rationalize) yields exactly
which is the stated result.
Step 5 — Check the two limits. As (no electronegativity gap): , the covalent limit, matching the homonuclear-diatomic result exactly. As (huge gap or vanishing coupling): , so and — full ionic localization on the electronegative atom, matching the classical Lewis-ionic picture where B simply keeps the electron pair. Both limits behave exactly as chemical intuition demands, and the formula interpolates smoothly and monotonically between them for any intermediate electronegativity difference.
Go deeper · Derivation B · 2 minFrom LCAO coefficients to Mulliken charge and a predicted dipole moment
Goal. Given normalized bonding-MO coefficients for a two-electron σ bond, compute the Mulliken atomic populations, the resulting partial charges, and compare the predicted point-charge dipole moment to experiment for HF, illustrating how far "orbital covalency" and "charge-based ionicity" can diverge in magnitude even though they share the same physical origin.
Step 1 — Write the doubly-occupied bonding MO. For HF's σ bond, take illustrative simple-Hückel-style parameters , (F 2p), and for the H1s–F2p interaction. Then and
(the sign here simply reflects the labeling convention; what matters physically is , and F, being lower in energy, dominates the bonding MO).
Step 2 — Get the coefficients. Using the closed-form result from the previous derivation with :
(Here F is playing the role of "B," the more electronegative, lower-energy atom, so it receives the larger coefficient, as required.)
Step 3 — Populate with the bonding electron pair. The bonding σ MO holds 2 electrons. Mulliken's prescription (with for simplicity — the same idea extends to nonzero overlap with an extra symmetric overlap-population term) assigns each atom a gross population
Check: electrons, exactly the pair placed in the bond — a necessary bookkeeping consistency check.
Step 4 — Convert to formal charge. Each atom brought one electron of its own to the bond (H contributes 1 electron from 1s; F contributes 1 electron from an unpaired 2p). The charge transferred is the difference between what an atom "owns" now and what it contributed:
This says the bonding-electron redistribution alone, ignoring any contribution from fluorine's three lone pairs (which are essentially pure, non-polarizing F 2p orbitals contributing no further charge transfer beyond what's already localized on F), predicts F to carry roughly and H to carry .
Step 5 — Compare to the measured dipole moment. A point charge of separated by the experimental H–F bond length predicts a dipole moment
Step 6 — Confront experiment and diagnose the gap. The experimental dipole moment of HF is , noticeably smaller than the the bare bonding-charge picture predicts. The physical reason is that the fluorine lone pairs are not perfectly nonpolarizing spectators: back-polarization of the F lone-pair density and the finite spatial extent of the electron cloud (this simple point-charge model ignores the actual charge distribution's shape, using only net atomic populations) both act to reduce the effective dipole below the naive point-charge estimate. Nonetheless, both numbers agree on the qualitative and even semiquantitative story — a substantially polarized bond with F significantly negative — confirming that the coefficient asymmetry derived from the secular equations is the right underlying mechanism, even though matching absolute magnitudes precisely requires a full ab initio calculation rather than a two-parameter Hückel model.
Worked examples
Example 1 — Foundational: the HF σ bond, redone with a different (harder) parameter set to confirm the machinery, not just to repeat memorized numbers. Take (hydrogen 1s ionization energy) and, this time, a slightly different but equally defensible tabulated value for the fluorine 2p orbital energy, , with resonance integral (these numbers are deliberately different from the previous derivation's, to show the method is robust to the exact parameter choice, not tuned to one "right" answer). Step 1: . Step 2: ; take , with F (lower ) as the favored atom. Step 3: . Step 4: ; . Step 5 (Mulliken populations of the bonding pair): , ; sum ✓. Step 6 (charges): ; . Step 7 (predicted dipole with the experimental bond length 91.7 pm): . The conclusion is qualitatively identical to the first derivation's — F strongly negative, H strongly positive, orbital-derived charge somewhat larger than the experimental dipole implies — even though every input number was changed, confirming the method (not a specific fitted parameter set) is what carries the physics. Limiting check: if hydrogen's electronegativity were artificially raised to equal fluorine's (, so ), the formula collapses to and — a perfectly nonpolar bond, exactly as required for two identical atoms.
Example 2 — Applied: comparing C–F vs. C–Cl bond polarity in a haloalkane, using the same λ framework to explain a classic organic-chemistry puzzle. Chemists sometimes find it counterintuitive that C–F is the most polar carbon–halogen σ bond by electronegativity difference, yet C–Cl bonds are frequently more reactive toward nucleophilic substitution. The coefficient framework resolves this cleanly by separating two different quantities: the ground-state bonding-MO polarization (which sets the permanent dipole and charge distribution) and the σ* antibonding-MO character (which sets reactivity in / processes, foreshadowing frontier-orbital reasoning). Using illustrative valence-state orbital energies , , (chlorine's 3p energy sits close to carbon's, a real and important feature of period-3 vs. period-2 electronegativity trends), with resonance integrals and (smaller, because Cl 3p/C 2p overlap is poorer than F 2p/C 2p overlap): For C–F: ; , so .
For C–Cl: (nearly zero!); , so .
The C–F bonding MO is dramatically polarized toward F ( vs. ), while the C–Cl bonding MO is nearly covalent and almost balanced ( vs. ) — a direct MO-level confirmation of the well-known fact that carbon and chlorine have almost identical Pauling electronegativities (2.55 vs. 3.16, a modest gap, and crucially the effective valence-state gap used in orbital energies is even smaller than the raw Pauling numbers suggest for period differences). The reactivity puzzle resolves once the antibonding (σ) coefficients are considered, which by the same secular-equation algebra lean the opposite way — toward carbon, more strongly so for the weaker-coupled, more diffuse system. Because is smaller in magnitude than (poorer 2p–3p overlap), the C–Cl σ is lower-lying and more accessible for nucleophilic attack at carbon, even though the ground-state bond is less charge-polarized than C–F. This is exactly the reasoning that becomes systematic in Frontier Orbitals: HOMO and LUMO treatments of substitution reactivity: ground-state polarity (bonding MO) and kinetic reactivity (antibonding/LUMO accessibility) are related but distinct quantities, both traceable to the same secular-equation algebra.
Limiting check: setting in either bond (no coupling at all) would send regardless of , forcing on the lower-energy atom — the fully ionic limit, correctly independent of how large the electronegativity gap is once coupling vanishes entirely (a useful sanity check that isolated ions, not bonds, are the limit).
Example 3 — Exam/competition level: back out an "experimental" λ and an effective electronegativity difference from a stated MO coefficient, then predict a companion molecule's polarity. A computational chemistry output reports that the bonding σ MO of a diatomic AB (isoelectronic in valence structure to HF, with the same resonance integral magnitude ) has normalized coefficients and (readers can verify ✓, confirming proper normalization).
Task: determine , the implied , and hence estimate which atom is more electronegative and by roughly how much, expressed as an effective orbital electronegativity gap in eV. Step 1: from , use (taking A as the less-favored, higher-energy atom by inspection since ):
Step 2: solve for . Square both sides: , so , giving , so
Step 3: recover from , using :
Step 4: interpretation. Atom B, which carries the larger coefficient (, i.e., 83% of the bonding electron density), is the more electronegative atom by an effective orbital-energy gap of about — almost identical in magnitude to the HF gap used in the first worked example (5.0 eV), which correctly flags this hypothetical AB system as "HF-like" in its degree of polarization, consistent with the problem's stated isoelectronic setup. Step 5 — companion-molecule prediction: if a chemist is then told that a second diatomic, AB (same B, different A with a smaller electronegativity, so a larger , say , same ), the same formula predicts , , , so and — i.e., replacing A with a less electronegative atom A (bigger gap) pushes the bonding MO even further onto B, from 83% to 90% B-character, exactly the monotonic trend the closed-form guarantees.
Limiting check on the whole problem: if the reported coefficients had instead been (equal), the same algebra would return and exactly — correctly signaling a homonuclear-like, perfectly covalent bond with no electronegativity difference, as it must.
Limiting cases, scope & common traps
| Regime | Condition | Coefficient behavior | Physical description |
|---|---|---|---|
| Perfectly covalent | () | Homonuclear-like sharing (H, N, C–C) | |
| Weakly polar | 's differ by a small amount from | Typical C–H, C–N bonds | |
| Strongly polar covalent | 's roughly 0.8/0.2 or more skewed | H–F, C–O, C–F | |
| Near-ionic | on electronegative atom, on the other | Na–Cl-like, alkali halides treated at the valence-orbital level | |
| Strong coupling limit | regardless of | Multiple/aromatic bonding can "wash out" modest electronegativity gaps | |
| Vanishing coupling | for any nonzero | Non-bonded ions, long-range electrostatics only |
The chemist behind it
Robert S. Mulliken (1896–1986) is the figure most responsible for turning "which atom is more electronegative" from a qualitative chemical instinct into a quantity computable directly from molecular orbital coefficients. Trained originally in chemical engineering and then in physical chemistry at the University of Chicago, Mulliken spent the 1920s and 1930s doing exactly the kind of careful spectroscopic bookkeeping — assigning electronic states of diatomic molecules from their observed spectra — that forced him to take molecular orbital theory seriously as more than a mathematical convenience. He was one of the earliest and most persistent champions of the MO approach at a time when valence-bond/resonance theory (championed by Pauling) dominated American chemical thinking, and much of his career was spent demonstrating, molecule by molecule, that MO theory could match or exceed VB theory's explanatory power while being far more systematically extendable to polyatomic systems. Mulliken's 1955 population analysis — the very procedure used in this article's second worked derivation to turn squared LCAO coefficients into atomic charges — became the standard, if imperfect, bridge between the abstract MO coefficients coming out of a calculation and the everyday chemist's language of partial charges and bond polarity. He also proposed the electronegativity scale bearing his name, defined from atomic ionization energies and electron affinities rather than from bond-energy differences (Pauling's original method), giving electronegativity itself a cleaner atomic-orbital-energy foundation — precisely the quantities that drive the polarization discussed throughout this article. He shared the 1966 Nobel Prize in Chemistry, awarded solely to him, "for his fundamental work concerning chemical bonds and the electronic structure of molecules by the molecular orbital method."
Origins · 1 minRobert S. Mulliken and how this was discovered
Is bond polarity the same thing as ionic character?
They are closely related but not synonymous. Bond polarity, in the MO sense used here, refers to the unequal AO coefficients in the bonding MO — a continuous, purely covalent-orbital-based description of the bond. "Ionic character" is a percentage estimate (Pauling's original formula uses the observed dipole moment versus the fully ionic value) meant to summarize how close the actual charge distribution is to two discrete point charges. The polarization parameter derived in this article connects the two smoothly: at the bond is fully covalent with 0% ionic character; as the bonding MO becomes fully localized (100% ionic character in the coefficient sense). Real bonds sit at intermediate λ, and quoting a single "percent ionic" number is really quoting a snapshot of where a bond sits on this same continuum.
Why does the antibonding MO lean toward the less electronegative atom?
The secular equations for the antibonding root are algebraically the mirror image of the bonding-root equations: whichever atom is under-represented in the bonding combination must be over-represented in the antibonding combination, because the two MOs are required to be orthogonal and together must fully span the two-dimensional AO space. Physically, the antibonding combination has a node between the nuclei and is destabilized most strongly relative to whichever atom's orbital it resembles least — since it resembles the low-electronegativity atom's orbital most closely (having "given up" mostly on the electronegative atom's low-lying orbital), it sits close in energy to the higher, less stable . This is exactly why, in HF, the σ* orbital is overwhelmingly H 1s in character and lies at quite high energy, well above either starting AO.
How does this connect to the Pauling electronegativity scale I already know from general chemistry?
Pauling originally defined electronegativity differences from a bond-energy excess: a polar A–B bond is stronger than the geometric mean of A–A and B–B bond energies, and he attributed that "extra" stabilization to ionic-resonance stabilization, scaling the square root of that excess energy to define . The MO polarization parameter derived here is a different but consistent route to the same physical content: the same underlying orbital-energy gap that makes a bond polar in Pauling's bond-energy sense is exactly the quantity that skews the LCAO coefficients in the MO picture, and the extra bond stabilization Pauling measured is, in this language, precisely the extra bonding-MO stabilization that grows with .
Does a larger electronegativity difference always mean a more polar bond, with no exceptions?
For a fixed coupling strength , yes — polarity increases monotonically with according to the closed-form . But real bonds do not hold fixed while varying : changing the atoms usually changes the orbital overlap too. This is why bond polarity does not track electronegativity difference in perfect lockstep across the periodic table — a C–F σ bond and, say, a heavier E–F σ bond with the same electronegativity gap can differ in polarization if their orbital overlaps (hence ) differ, for instance due to poorer size-matching between orbitals from different principal quantum numbers.
Why is HF described as covalent in orbital character but the classic textbook example of a highly polar bond?
Both statements are true and not in tension. "Covalent in orbital character" simply means the bond is well described by a two-center bonding MO built from H 1s and F 2p (rather than by transferring an electron completely and invoking pure Coulomb attraction between H and F) — the wavefunction still has nonzero amplitude on both atoms, and is not negligible. "Highly polar" refers to how unequal that shared amplitude is: the worked examples above show roughly 80% of the bonding density sitting on F. A bond can be simultaneously covalent (nonzero , a genuine bonding MO exists) and strongly polar (large , very unequal coefficients) — these are two different axes, not opposite ends of one scale.
How would I estimate λ or bond polarity for a bond not covered in a textbook table?
In practice, you rarely solve the 2×2 secular equations by hand for unfamiliar bonds; instead you run a Hartree–Fock or DFT calculation and read off Mulliken, Löwdin, or NBO charges directly, which already incorporate the full multi-electron, multi-basis-function version of this same coefficient asymmetry. For a quick hand estimate without software, use tabulated valence-state ionization energies as proxies for (available in many inorganic chemistry references) and estimate from an empirical formula proportional to overlap and geometric mean of the two atoms' orbital energies (the Wolfsberg–Helmholz approximation used in extended Hückel theory), then apply the formula exactly as done in the worked examples here.
Does this framework apply to π bonds and multiple bonds the same way it applies to σ bonds?
Yes, with the caveat that σ and π systems generally have different resonance integrals (σ overlap is typically larger than π overlap between the same pair of p orbitals), so the same two atoms can show different λ, and hence different polarization, for their σ and π bonding MOs. This is exactly why the carbonyl π* orbital (heavily weighted on carbon) and π orbital (heavily weighted on oxygen) show such a dramatic asymmetry that becomes central to understanding carbonyl electrophilicity in Frontier Orbitals: HOMO and LUMO treatments — the π system of C=O polarizes by essentially the same secular-equation mechanism as the σ system of H–F, just with different numerical parameters.