Electronegativity Calculator

Calculate electronegativity differences, predict bond polarity, and determine ionic character of bonds.

Select Elements

Common Pairs:

Bond Type

Ionic

Electronegativity Difference: 2.23

1Na (pauling)
0.93
2Cl (pauling)
3.16
+/-Ionic Character
71.2%
ePartial Charge
0.531 e

Analysis:

  • More electronegative: Cl
  • Dipole direction: Na -> Cl
  • Electrons shift toward: Cl

Understanding Electronegativity

Electronegativity is a measure of an atom's ability to attract shared electrons in a chemical bond. Higher electronegativity means stronger attraction. The difference between two atoms' electronegativities determines bond polarity: <0.4 is nonpolar covalent, 0.4-1.7 is polar covalent, and >1.7 is ionic.

Electronegativity Scales

Pauling Scale

Based on bond dissociation energies. Most widely used.

Mulliken Scale

Average of ionization energy and electron affinity.

Allred-Rochow

Based on effective nuclear charge and covalent radius.

What Is Electronegativity?

Electronegativity is the tendency of an atom to attract a bonding pair of electrons toward itself in a chemical bond. It is a dimensionless quantity that varies across the periodic table in predictable patterns, making it one of the most useful properties for understanding chemical bonding and reactivity. The concept was quantified by Linus Pauling in the 1930s and has since been refined through multiple scales.

When two atoms form a bond, the more electronegative atom pulls the shared electrons closer to itself, creating a partial negative charge (δ−) on that atom and a partial positive charge (δ+) on the less electronegative atom. This charge separation is called a bond dipole and is responsible for many of the physical and chemical properties of molecules, including boiling points, solubility, and reactivity patterns.

This calculator supports three electronegativity scales: the Pauling scale (most widely used, based on bond energies), the Mulliken scale (theoretically elegant, average of ionization energy and electron affinity), and the Allred-Rochow scale (based on effective nuclear charge and covalent radius). The calculator compares two elements, predicts the bond type, calculates the ionic character and partial charges, and identifies the dipole direction.

Ionic Character from Electronegativity Difference

Ionic character (%) = (1 − e^(−0.25 × ΔEN²)) × 100

Where:

  • ΔEN= Electronegativity difference between the two bonded atoms
  • EN₁= Electronegativity of the first element
  • EN₂= Electronegativity of the second element

How to Use This Calculator

This calculator provides a comprehensive comparison of electronegativity values and bond properties. Follow these steps:

  1. Choose the electronegativity scale: Select Pauling (default, most common), Mulliken, or Allred-Rochow from the dropdown menu.
  2. Select the first element: Choose from the dropdown of 25 common elements with known electronegativity values on all three scales.
  3. Select the second element: Choose a second element for comparison. Noble gases are excluded because they do not form typical chemical bonds.
  4. Use quick-select buttons: Common element pairs (Na-Cl, H-O, C-O, H-Cl, C-H) are available for rapid comparison of representative bond types.
  5. Review results: The display shows each element's electronegativity, the difference, predicted bond type (nonpolar covalent, polar covalent, or ionic), ionic character percentage, partial charge, dipole direction, and which element is more electronegative.

The results adapt to the selected scale. Mulliken values are typically higher than Pauling values because they measure absolute electron-attracting ability rather than relative bond polarity.

Bond Polarity and Partial Charges

The partial charge on each atom in a bond can be estimated from the electronegativity difference using the Pauling equation: δ = 0.16 × ΔEN + 0.035 × ΔEN². This gives the effective charge separation in units of elementary charge (e). For example, in NaCl with ΔEN = 2.23, the partial charge is approximately 0.53 e, meaning the bond is about 53% ionic.

The dipole direction is always from the less electronegative atom (δ+) toward the more electronegative atom (δ−). In a water molecule, the dipole points from hydrogen toward oxygen because oxygen (3.44) is more electronegative than hydrogen (2.20). The overall molecular dipole moment depends on both the bond dipoles and the molecular geometry.

The calculator identifies which element is more electronegative and indicates the electron shift direction. This information is essential for predicting molecular polarity, intermolecular forces, and chemical reactivity. Molecules with large bond dipoles tend to have higher boiling points (due to stronger dipole-dipole interactions) and are often better solvents for polar and ionic compounds.

Real-World Applications

Electronegativity differences are the starting point for understanding all chemical bonding. The type of bond (ionic, polar covalent, or nonpolar covalent) determines the compound's physical properties, including melting point, boiling point, solubility, and electrical conductivity. Ionic compounds (large ΔEN) have high melting points and conduct electricity when dissolved, while nonpolar covalent compounds (small ΔEN) have low melting points and are poor conductors.

In pharmaceutical chemistry, the distribution of partial charges on drug molecules determines how they interact with biological receptors. Electronegative atoms create hydrogen bond acceptor sites, while electropositive hydrogen atoms bonded to N or O serve as hydrogen bond donors. The three-point attachment model of drug-receptor interactions relies heavily on electronegativity-driven charge distributions.

Corrosion science uses electronegativity to predict galvanic coupling between metals. When two metals with different electronegativities are in electrical contact in an electrolyte, the less electronegative (more active) metal corrodes preferentially. This principle underlies sacrificial anode protection for ships, pipelines, and underground storage tanks.

In geochemistry, electronegativity determines the bonding character of minerals and influences how elements partition between magma phases during crystallization. The Goldschmidt classification of elements (lithophile, siderophile, chalcophile, atmophile) is fundamentally based on electronegativity and related properties.

Worked Examples

NaCl: Classic Ionic Bond

Problem:

Compare Na and Cl on the Pauling scale and analyze the bond.

Solution Steps:

  1. 1Na Pauling EN = 0.93, Cl Pauling EN = 3.16
  2. 2ΔEN = |3.16 − 0.93| = 2.23
  3. 3Bond type: Ionic (ΔEN > 1.7)
  4. 4Ionic character: (1 − exp(−0.25 × 2.23²)) × 100 ≈ 71.2%
  5. 5Partial charge: 0.16 × 2.23 + 0.035 × 2.23² ≈ 0.53 e
  6. 6Dipole: Na(δ+) → Cl(δ−)

Result:

NaCl is an ionic bond with 71.2% ionic character and a partial charge of 0.53 e. Na donates electron density to Cl.

H₂O: Polar Covalent Bond

Problem:

Compare H and O on the Pauling scale.

Solution Steps:

  1. 1H Pauling EN = 2.20, O Pauling EN = 3.44
  2. 2ΔEN = |3.44 − 2.20| = 1.24
  3. 3Bond type: Polar covalent (0.4 < ΔEN < 1.7)
  4. 4Ionic character: (1 − exp(−0.25 × 1.24²)) × 100 ≈ 32.6%
  5. 5Dipole: H(δ+) → O(δ−)

Result:

H-O is a polar covalent bond with 32.6% ionic character. Oxygen attracts the shared electrons, creating the molecular dipole responsible for water's unique properties.

CH₄: Nonpolar Covalent Bond

Problem:

Compare C and H on the Pauling scale.

Solution Steps:

  1. 1C Pauling EN = 2.55, H Pauling EN = 2.20
  2. 2ΔEN = |2.55 − 2.20| = 0.35
  3. 3Bond type: Nonpolar covalent (ΔEN < 0.4)
  4. 4Electrons are shared nearly equally

Result:

C-H is a nonpolar covalent bond with ΔEN = 0.35. This explains why methane and other hydrocarbons are nonpolar, hydrophobic, and have low boiling points.

Tips & Best Practices

  • Use Pauling as the default scale unless you have a specific reason to use Mulliken or Allred-Rochow.
  • ΔEN < 0.4 = nonpolar covalent, 0.4–1.7 = polar covalent, > 1.7 = ionic (Pauling scale).
  • Partial charges from ΔEN help predict hydrogen bonding, solubility, and intermolecular forces.
  • The dipole always points from the less electronegative atom (δ+) to the more electronegative atom (δ−).
  • Mulliken EN = (IE + EA) / 2; it is theoretically cleaner but less commonly tabulated.
  • Electronegativity increases across a period and decreases down a group, following effective nuclear charge.

Frequently Asked Questions

The Pauling scale is the most widely used and is the standard in general and organic chemistry. The Mulliken scale is preferred in computational chemistry because it uses directly measurable atomic properties (ionization energy and electron affinity). The Allred-Rochow scale is useful when only atomic radii and nuclear charges are available. All three scales predict the same qualitative trends, so the choice often depends on the context and available data.
Noble gases have complete valence shells (ns²np⁶), making them extremely stable and chemically inert under normal conditions. They do not form covalent or ionic bonds, so the concept of attracting shared electrons is not applicable. While some heavy noble gases (Xe, Kr) can form compounds under extreme conditions, standard electronegativity scales exclude them.
Hybridization changes the effective electronegativity of an atom because different hybrid orbitals have different s-character. An sp-hybridized carbon (50% s-character) is more electronegative than an sp³ carbon (25% s-character) because s orbitals are closer to the nucleus. This is why terminal alkynes (sp C-H) are more acidic than alkanes (sp³ C-H) — the sp carbon holds the bonding electrons more tightly.
Electronegativity helps explain acid strength trends. For binary acids (H-A), acid strength increases with the electronegativity of A across a period (HF > H₂O > NH₃) but also depends on bond strength, which decreases down a group (HI > HBr > HCl > HF). For oxyacids (HO-X), acid strength increases with the electronegativity and oxidation state of the central atom X.
Metallic character is inversely related to electronegativity. Metals have low electronegativity (they lose electrons easily), while nonmetals have high electronegativity (they attract electrons). The diagonal line on the periodic table separating metals from nonmetals roughly follows the EN ≈ 2.0 contour. Elements with EN below 2.0 are generally metallic, while those above 2.0 are generally nonmetallic.

Sources & References

Last updated: 2026-06-06

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Editorial Note

MyCalcBuddy Editorial Team

This page is maintained as an educational calculator reference.

Source

Formula Source: Chemistry: The Central Science

by Brown, LeMay, Bursten

UpdatedLast reviewed: May 2026
CheckedFormula checks are based on standard references and internal QA review.