Audited 31 Jul 2026·Last updated 28 Oct 2026·5 citations·Tier 1·0 uses

Electronegativity Calculator

Find the electronegativity difference between two bonded atoms from their values on one scale, such as Pauling's, to judge how unevenly the bond is shared.

Electronegativity Calculator

Electronegativity difference
1.24
The absolute gap between the two electronegativity values, a pure number on whichever scale you used; larger means a more polar bond.
Model scope
Difference of two user-supplied values on the same scale; it does not supply a periodic table, mix Pauling/Mulliken/Allen scales, or convert the difference into a universal ionic/covalent bond classification.

Background.

Two atoms sharing a pair of electrons rarely share it equally. The atom with the stronger pull, the higher electronegativity, draws the bonding electrons toward itself and takes on a slight negative charge, leaving its partner slightly positive. That lopsidedness is why water molecules cling to one another, why table salt dissolves in water and why oil does not. The difference in electronegativity between the two atoms, Δχ = |χA − χB|, is the first number chemists reach for to judge how lopsided a bond is.

Electronegativity cannot be measured directly. Linus Pauling built the first scale in 1932 from bond energies: a bond between two different atoms is usually stronger than the average of the matching like-atom bonds, and he traced the extra energy to the uneven sharing. On the revised Pauling scale used in most textbooks, fluorine sits at the top with 3.98 and caesium near the bottom at 0.79, with oxygen at 3.44, carbon at 2.55 and hydrogen at 2.20. Mulliken's scale and Allen's scale rest on other atomic energies and give different numbers, so both values entered here must come from the same table.

A bigger difference means a more polar bond. Chlorine bonded to chlorine shares evenly, and the 0.35 between carbon and hydrogen is small enough that hydrocarbons are barely polar. Oxygen and hydrogen, 1.24 apart, make the strongly polar O–H bond; sodium and chlorine, 2.23 apart, make a bond usually called ionic. Where polar covalent ends and ionic begins is a convention that textbooks set in different places, so the page reports the difference and leaves the label to you.

Polarity is not the same thing as reactivity, and the carbon–halogen bonds of organic chemistry show the difference. Carbon–fluorine, 1.43 apart, is the most polar of them and also the hardest to break; carbon–iodine, only 0.11 apart, is almost nonpolar, yet alkyl iodides are the ones that react fastest when the halogen is displaced, because the long, weak C–I bond and the stable iodide ion matter more than the charge separation. The difference tells you where electron density sits in a bond; what happens next depends on bond strength, molecular shape and the reaction itself.

What is electronegativity calculator?

Electronegativity is the power of an atom in a molecule to attract the shared electrons of a bond toward itself, a concept introduced by Linus Pauling. It is a relative scale rather than a measured physical quantity, and on the Pauling scale it is treated as a pure number. The electronegativity difference is the absolute gap between the values of two bonded atoms on the same scale. It describes the polarity of one bond, not of a whole molecule. On the revised Pauling scale values run from about 0.79 for caesium to 3.98 for fluorine. The reactive metals sit at the low end, the halogens, oxygen and nitrogen at the high end, and carbon, hydrogen, phosphorus and sulfur cluster in the middle, between 2.19 and 2.58, which is why bonds among those four are only weakly polar. A tabulated value is an average over many compounds, and an atom's real pull shifts with its bonding: carbon with sp hybridisation, as in acetylene, holds electrons more tightly than the sp³ carbon of ethane, and a metal in a high oxidation state pulls harder than the same metal in a low one. Gold is a reminder that the trends have exceptions; at 2.54 it is almost as electronegative as carbon, and with caesium, 1.75 apart, it forms caesium auride, a salt containing the Au⁻ ion.

How to use this calculator.

  1. Look up both atoms on one electronegativity scale; the Pauling scale is the one most textbooks and periodic tables print, usually to two decimals (nitrogen 3.04, sulfur 2.58, chlorine 3.16). Some older books round to one decimal, which is fine as long as both values come from the same book.
  2. Enter the two values in either order. The difference is taken as a positive number, so swapping them changes nothing.
  3. Do not mix scales. Mulliken values quoted in electronvolts are on a different footing from Pauling values and must be converted before they can be compared.
  4. Note which atom had the higher value before reading the result. That atom carries the partial negative charge, and the difference alone does not record it.
  5. For a molecule, take each kind of bond in turn and then look at the shape. In chloromethane, C–H gives 0.35 and C–Cl 0.61, and because the bonds point in different directions around a tetrahedral carbon they do not cancel, so the molecule is polar. In tetrachloromethane four identical C–Cl bonds do cancel, and the molecule is not.
  6. Two atoms of the same element, as in Cl–Cl or a carbon–carbon bond, give a difference of 0: the electrons are shared evenly, and that is the reference point every other result is measured from.

The formula.

Δχ = |χ_A - χ_B|

Δχ = |χA − χB|, the absolute value of the difference between the two electronegativities. There are no constants, because all the physics sits inside the tabulated values. In Pauling's construction the difference is actually the primary quantity: the square of Δχ, in electronvolts, matches the extra energy of an A–B bond over the average of the A–A and B–B bond energies, and individual atomic values follow once the scale is anchored to a reference element. That is why a difference read from one scale should not be compared with thresholds taken from another. The result depends only on the gap, so carbon at 2.55 paired with hydrogen at 2.20 gives the same 0.35 as any other pair 0.35 apart. Hydrogen chloride shows the construction working. Approximate bond energies are 436 kJ/mol for H–H, 242 for Cl–Cl and 431 for H–Cl. The average of the first two is 339, so H–Cl is about 92 kJ/mol stronger than the average; that is about 0.954 eV, whose square root is 0.98, close to the tabulated gap of 3.16 − 2.20 = 0.96. The match is close rather than exact because the scale is a best fit across many bonds, not a value read from any one of them, and that is also why Pauling values carry the formal unit eV^½ but are used as plain numbers. The model's weakness is that it assigns one fixed value per element, so it cannot register the hybridisation and oxidation-state effects that change an atom's pull from one compound to the next.

A worked example.

Example

Take the O–H bond, using Pauling values: oxygen has an electronegativity of 3.44 and hydrogen 2.20. The difference is 3.44 − 2.20 = 1.24. Entered the other way round, 2.20 − 3.44 = −1.24, and taking the absolute value gives the same 1.24. A gap of 1.24 makes the O–H bond strongly polar. Oxygen, with the higher value, carries the partial negative charge and hydrogen the partial positive one, which is what lets water molecules hydrogen-bond to each other. For comparison, the C–H bond gives 2.55 − 2.20 = 0.35, barely polar at all, while Na–Cl gives 3.16 − 0.93 = 2.23, at the ionic end of the range. Read back through Pauling's construction, a gap of 1.24 corresponds to 1.24² = 1.5376 eV, about 148 kJ/mol of extra bond energy beyond the average of the H–H and O–O bonds: the energetic signature of the uneven sharing.

electronegativity A3.44
electronegativity B2.2

Frequently asked questions.

Which atom ends up with the partial negative charge?
The one with the higher electronegativity. In an O–H bond that is oxygen, at 3.44 against hydrogen's 2.20. The difference reported here is always positive, so it tells you how uneven the bond is but not which way the electrons lean; check which value was larger.
At what difference does a bond count as ionic?
There is no single agreed cut-off; textbooks draw the line in different places, most often at 1.7 or 2.0. Hydrogen fluoride shows why a fixed number misleads: its difference of 3.98 − 2.20 = 1.78 is larger than some textbook thresholds for ionic bonding, yet HF is a covalent molecule. Treat bonding type as a spectrum.
Why is carbon dioxide nonpolar when its C=O bonds have a difference of 0.89?
Each C=O bond is polar, with oxygen at 3.44 and carbon at 2.55, but CO₂ is a straight line with the two bonds pointing in opposite directions. Their pulls cancel, so the molecule has no overall dipole. Molecular polarity depends on shape as well as on bond differences. Water is the contrast: its two O–H bonds, 1.24 apart each, meet at an angle of about 104.5°, so their pulls add rather than cancel and the molecule is strongly polar.
Can I use a Mulliken value for one atom and a Pauling value for the other?
No. Mulliken's electronegativity averages an atom's ionization energy and electron affinity and is often quoted in electronvolts, while Allen's uses the average energy of valence electrons. Each scale has its own spread of numbers, so a difference across two scales means nothing chemically.
Can the difference be turned into a percentage of ionic character?
Pauling proposed an empirical estimate, ionic character ≈ 1 − e^(−Δχ²/4). For O–H, with Δχ = 1.24, it gives about 32%; for Na–Cl, with 2.23, about 71%; and for caesium fluoride, 3.19 apart and about as wide a gap as everyday compounds reach, about 92%. It is a rough guide from the 1930s rather than a measurement, and this page does not calculate it.
Why does electronegativity rise across a period and fall down a group?
Across a period, protons are added to the nucleus while the new electrons go into the same shell, so bonding electrons feel a steadily stronger pull: on the Pauling scale lithium is 0.98 and fluorine 3.98. Down a group, the outer electrons sit in shells further out, screened by more inner electrons. The halogens show it plainly, from fluorine at 3.98 through chlorine at 3.16 and bromine at 2.96 to iodine at 2.66, so the gap to hydrogen shrinks from 1.78 in HF to 0.46 in HI.
My textbook gives oxygen 3.5 and hydrogen 2.1. Which values should I use?
Those are Pauling's original rounded figures. The two-decimal values most tables now print, such as oxygen 3.44 and hydrogen 2.20, come from a 1961 revision by A. L. Allred that drew on more bond-energy data. Either set works as long as both atoms come from it, but the answers differ: O–H gives 1.4 with the older values and 1.24 with the revised ones, so use whichever table your course or exam expects.
How is electronegativity used to assign oxidation numbers?
Oxidation numbers are counted as if every bond were fully ionic, with both shared electrons credited to the more electronegative atom, however small the gap. In methane, carbon at 2.55 outranks hydrogen at 2.20, so carbon is credited with all eight bonding electrons and gets −4, leaving +1 on each hydrogen. In CO₂ oxygen outranks carbon, which becomes +4. A bond between two atoms of the same element is split evenly and changes nothing.
Can hydrogen be the negative end of a bond?
Yes, whenever its partner is less electronegative than 2.20. In C–H the carbon (2.55) is the negative end, but in Si–H silicon sits at 1.90 and boron in B–H at 2.04, so the hydrogen carries the partial negative charge. In sodium hydride, 1.27 apart, hydrogen is present as the hydride ion H⁻, which is why such compounds react with water to release hydrogen gas.
Why can N–H bonds hydrogen-bond when Cl–H, with a larger difference, barely does?
N–H is 0.84 apart and Cl–H 0.96, yet ammonia hydrogen-bonds strongly and hydrogen chloride only weakly. Strong hydrogen bonds need a small, electronegative atom with a lone pair that can come close to the hydrogen, which is why the classic donors and acceptors are nitrogen, oxygen and fluorine. Chlorine's larger size spreads its charge out, so the difference alone does not predict hydrogen bonding.

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Method
Δχ = |χ_A - χ_B|
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