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Isoelectronic Species: Same Electrons, Different Sizes

Atomic StructureIntermediate7 min read
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  1. Definition
  2. How to spot isoelectronic species
  3. The big idea: more protons, smaller species
  4. Worked example: ranking by size
  5. Ionisation energy in an isoelectronic series
  6. Isoelectronic molecules
  7. Why the concept is useful
  8. Isoelectronic ions in crystals and minerals
  9. Why the concept is worth mastering
  10. Practice questions
  11. Key takeaways

The oxide ion, the fluoride ion, a neon atom and the sodium ion look nothing alike chemically. One is a strongly basic anion, one is a noble gas, one is a spectator ion in table salt. Yet they have one thing in common: exactly 10 electrons, arranged in exactly the same way, 1s² 2s² 2p⁶. Species like this are called isoelectronic, and comparing them is one of the cleanest ways to see how nuclear charge controls the size and behaviour of atoms and ions.

Definition

Isoelectronic species have the same number of electrons and the same electron configuration.

The word comes from the Greek iso, “equal”. The species can be atoms, ions or even molecules.

How to spot isoelectronic species

  1. For each species, find the number of electrons: atomic number − charge (for an ion with charge +2, subtract 2; for charge −2, add 2).
  2. Species with the same electron count (and configuration) are isoelectronic.

Example: the 10-electron series

Species Protons (Z) Charge Electrons
N³⁻ 7 −3 10
O²⁻ 8 −2 10
F⁻ 9 −1 10
Ne 10 0 10
Na⁺ 11 +1 10
Mg²⁺ 12 +2 10
Al³⁺ 13 +3 10

All have the configuration 1s² 2s² 2p⁶, the same as neon. See electron configurations of ions.

Example: the 18-electron series

P³⁻, S²⁻, Cl⁻, Ar, K⁺, Ca²⁺, Sc³⁺ all have 18 electrons, configuration [Ne] 3s² 3p⁶, the same as argon.

The big idea: more protons, smaller species

Within an isoelectronic series, the electrons are identical in number and arrangement, so shielding is essentially the same. What changes is the number of protons in the nucleus. More protons mean a stronger pull on the same electron cloud, so the species gets smaller.

Species Protons Approximate radius (pm)
N³⁻ 7 146
O²⁻ 8 140
F⁻ 9 133
Na⁺ 11 102
Mg²⁺ 12 72
Al³⁺ 13 54

(Ionic radii vary with the method and the coordination environment, so values from different sources differ slightly, but the order never changes.)

From N³⁻ to Al³⁺, the radius nearly triples, even though every species has exactly 10 electrons. This is one of the most striking demonstrations that nuclear charge controls size. For the underlying idea, see effective nuclear charge.

Why anions are large and cations small

  • An anion has more electrons than protons. The electrons repel each other and are held relatively weakly, so the cloud spreads out.
  • A cation has fewer electrons than protons. The excess positive charge pulls the electrons in tightly.

So in any isoelectronic series, the most negative ion is largest and the most positive ion is smallest.

Worked example: ranking by size

Arrange in order of increasing radius: Cl⁻, K⁺, S²⁻, Ca²⁺, Ar.

  1. Check electrons: all have 18. They’re isoelectronic.
  2. Count protons: S (16), Cl (17), Ar (18), K (19), Ca (20).
  3. More protons → smaller.

Increasing radius: Ca²⁺ < K⁺ < Ar < Cl⁻ < S²⁻

(Comparing a noble gas radius with ionic radii is slightly tricky, because noble gas radii are usually measured differently, but its position in the sequence follows the same logic.)

Ionisation energy in an isoelectronic series

The energy needed to remove an electron also rises steeply with nuclear charge, because the electrons are held more tightly:

  • Removing an electron from F⁻ is relatively easy (it’s the reverse of fluorine’s electron affinity, about 328 kJ/mol).
  • Removing an electron from Ne takes about 2,081 kJ/mol.
  • Removing an electron from Na⁺ (sodium’s second ionisation energy) takes about 4,562 kJ/mol.
  • Removing one from Mg²⁺ (magnesium’s third ionisation energy) takes about 7,733 kJ/mol.

Same configuration, very different energies, all because of the increasing number of protons. See ionization energy trend and electron affinity.

Isoelectronic molecules

The idea extends to molecules and polyatomic ions with the same total number of electrons (and similar structures):

Species Total electrons Notes
N₂ 14 triple bond, very stable
CO 14 triple bond; isoelectronic with N₂
CN⁻ 14 triple bond; binds strongly to metals
NO⁺ 14 triple bond
CO₂ 22 linear
N₂O 22 linear; isoelectronic with CO₂
NO₂⁺ 22 linear
CH₄ 10 tetrahedral
NH₄⁺ 10 tetrahedral; isoelectronic with CH₄

Isoelectronic molecules often have similar shapes and bonding. CO₂, N₂O and NO₂⁺ are all linear; CH₄ and NH₄⁺ are both tetrahedral. See VSEPR and molecular geometry.

But similar structure doesn’t mean identical chemistry. N₂ is almost inert, while CO is poisonous, because CO binds tightly to the iron in haemoglobin, and CN⁻ is highly toxic because it binds to iron in an essential respiratory enzyme. The difference lies in how the electrons are distributed between atoms of different electronegativity.

Why the concept is useful

  • Predicting sizes of ions, important in understanding crystal structures and lattice energies.
  • Explaining ionisation energies and why certain ions form.
  • Predicting molecular shapes from a known isoelectronic partner.
  • Spectroscopy: isoelectronic atoms and ions have similar spectral patterns, shifted to higher energies as nuclear charge increases. Astronomers use this to identify highly charged ions in hot stellar atmospheres.

Isoelectronic ions in crystals and minerals

Size differences in isoelectronic series have real consequences in the solid state. In ionic crystals, the ratio of cation size to anion size helps decide how many anions pack around each cation. The tiny Al³⁺ ion fits into small gaps between oxide ions in aluminium oxide (corundum, the mineral of rubies and sapphires), while the larger Na⁺ ion is surrounded by six chloride ions in rock salt. Geologists use similar size arguments to explain why certain ions substitute for each other in minerals: ions of similar size and charge can swap places in a crystal lattice, even if they belong to different elements.

Why the concept is worth mastering

Isoelectronic comparisons are a favourite of examiners because they isolate a single variable. Normally, when you compare two atoms, both the nuclear charge and the electron arrangement change, which makes explanations messy. In an isoelectronic series, the electron arrangement is held constant, so any difference in size or ionisation energy must come from the nucleus. It’s the chemical equivalent of a fair test. See fair tests.

Practice questions

  1. Which of these are isoelectronic with argon: K⁺, Na⁺, S²⁻, Ca²⁺, O²⁻?
  2. Arrange in order of decreasing size: Mg²⁺, F⁻, Na⁺, O²⁻.
  3. Name a molecule or ion isoelectronic with CO₂.
  4. Which is harder to remove an electron from, K⁺ or Cl⁻? Explain.

Answers:

  1. K⁺, S²⁻ and Ca²⁺ (18 electrons each). Na⁺ and O²⁻ have 10.
  2. All have 10 electrons: O²⁻ > F⁻ > Na⁺ > Mg²⁺ (8, 9, 11, 12 protons).
  3. N₂O or NO₂⁺ (22 electrons each).
  4. K⁺: it has 19 protons holding 18 electrons, while Cl⁻ has only 17 protons for the same 18 electrons, so K⁺’s electrons are held far more tightly.

Key takeaways

  • Isoelectronic species have the same number of electrons and the same configuration.
  • Electrons = atomic number − charge; use this to spot isoelectronic sets.
  • In an isoelectronic series, more protons means a smaller radius and a higher ionisation energy.
  • Anions are larger than the isoelectronic noble gas; cations are smaller.
  • Isoelectronic molecules (N₂, CO, CN⁻; CO₂, N₂O) often share shapes and bonding patterns but differ in reactivity.

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