Periodic trends: ionization energy, electron affinity, atomic radius, and electronegativity
Anchor (Master): Pyykkö — Phys. Chem. Chem. Phys. 13, 161 (2011); Allen — J. Am. Chem. Soc. 111, 9003 (1989)
Intuition Beginner
Atoms differ in how tightly they hold their outermost electrons. Moving from left to right across a row of the periodic table, the nuclear charge increases but the shielding from inner electrons stays roughly constant. The net pull on the valence electrons grows, and they are drawn closer to the nucleus. This single idea — that effective nuclear charge increases across a period — explains almost every periodic trend.
Ionization energy is the energy required to remove the outermost electron from a gaseous atom. Atoms with a large effective nuclear charge hold their electrons tightly, so they have high ionization energies. Atoms with a small effective nuclear charge lose electrons easily, so they have low ionization energies. Across a period, ionization energy rises. Down a group, it falls because the valence electrons sit in shells farther from the nucleus, where the nuclear pull is weaker.
Atomic radius is the distance from the nucleus to the outermost electrons. As effective nuclear charge increases across a period, the electron cloud is pulled inward and the atom shrinks. Down a group, each new period adds a shell, so the atom grows larger. Cations (positive ions) are smaller than their parent atoms because removing electrons reduces electron-electron repulsion and the remaining electrons are pulled closer. Anions (negative ions) are larger because added electrons increase repulsion and the cloud expands.
Visual Beginner
Summary of the four major periodic trends:
| Trend | Across a period (L to R) | Down a group |
|---|---|---|
| Ionization energy | Increases | Decreases |
| Electron affinity | Generally becomes more negative | Generally becomes less negative |
| Atomic radius | Decreases | Increases |
| Electronegativity | Increases | Decreases |
Electronegativity is a measure of how strongly an atom attracts electrons in a chemical bond. Fluorine is the most electronegative element (3.98 on the Pauling scale). Francium and cesium are the least electronegative. The trend follows ionization energy closely because both depend on effective nuclear charge.
Worked example Beginner
Rank the following atoms by first ionization energy from lowest to highest: Na, Mg, Al, Si.
Step 1. Identify the period. All four are in period 3, so shielding from inner shells is identical.
Step 2. Apply the across-period trend. Ionization energy generally increases from Na to Si as increases from 11 to 14 and the valence electrons feel a stronger nuclear pull.
Step 3. Check for anomalies. Al () has configuration . Its outermost electron is a electron, which is higher in energy than the electrons of Mg (). So Al has a lower first ionization energy than Mg despite having one more proton.
The ranking: Na (496 kJ/mol) < Al (578 kJ/mol) < Mg (738 kJ/mol) < Si (786 kJ/mol).
The dip at Al is one of the characteristic anomalies caused by subshell boundaries. A similar dip occurs between P and S, where S has a paired electron that is easier to remove than one of P's three unpaired electrons.
Check your understanding Beginner
Formal definition Intermediate+
Effective nuclear charge
The effective nuclear charge is the net positive charge experienced by an electron in an atom, after accounting for shielding by other electrons:
where is the atomic number and is the shielding constant. Slater's rules (1930) provide a systematic procedure for estimating :
- Write the electron configuration in the order
- Electrons in groups to the right of the electron of interest contribute nothing to .
- Electrons in the same group as the electron of interest contribute each (except , where the contribution is ).
- For or electrons: electrons in the shell contribute each; electrons in and lower shells contribute each.
- For or electrons: all electrons in lower groups contribute each.
Slater's rules are approximate. More accurate values come from Hartree-Fock calculations, but the rules capture the essential physics with minimal computation.
Ionization energy
The first ionization energy is the minimum energy required to remove the most loosely bound electron from a gaseous atom:
The second ionization energy removes a second electron: . Successive ionization energies always increase because each removal leaves fewer electrons to shield and a more positive ion to escape. A large jump in successive ionization energies occurs when electrons are removed from a new (more tightly bound) shell.
In the Hartree-Fock framework, Koopmans' theorem provides the connection: , where is the orbital energy of the electron removed. This approximation neglects orbital relaxation and electron correlation but gives the correct qualitative ordering.
Electron affinity
The electron affinity is the energy change when a gaseous atom gains an electron:
By convention, if the process releases energy, is reported as a negative number (following the IUPAC sign convention). A more negative electron affinity means the atom more readily accepts an electron. Chlorine has the most negative electron affinity ( kJ/mol) among the main-group elements. Noble gases have positive electron affinities — adding an electron to a closed shell is energetically unfavorable.
Electron affinity does not follow a smooth periodic trend. The general trend is toward more negative values across a period, but anomalies are frequent. The Group 2 elements (Be, Mg, Ca) have less negative electron affinities than the Group 1 elements in the same period because the added electron would enter a higher-energy orbital rather than a half-filled orbital. Nitrogen has a less negative electron affinity than carbon because the added electron must pair with an existing electron in N's half-filled subshell.
Atomic and ionic radius
The atomic radius is not a directly measurable quantity because electron densities decay exponentially and have no sharp boundary. Several operational definitions exist:
- Covalent radius: half the distance between two identical bonded atoms.
- Metallic radius: half the distance between adjacent atoms in a metallic crystal.
- Van der Waals radius: half the closest distance between non-bonded atoms in adjacent molecules.
Despite the ambiguity, all definitions give the same qualitative trends. The atomic radius decreases across a period (increasing draws electrons inward) and increases down a group (additional electron shells).
For ions, isoelectronic series provide clean comparisons. The species , , , , , all have 10 electrons. Their radii decrease as increases because the same number of electrons is attracted by an increasingly positive nucleus: (140 pm) (133 pm) (102 pm) (72 pm) (54 pm).
Electronegativity
Electronegativity quantifies an atom's tendency to attract electrons in a chemical bond. Three major scales exist:
Pauling scale (1932). Based on bond dissociation energies. If the bond energy of A–B exceeds the geometric mean of A–A and B–B bond energies, the excess is attributed to ionic character:
where is the dissociation energy of the A–B bond in eV. The scale is relative, anchored by .
Mulliken scale (1934). Defined as the average of the first ionization energy and the negative of the electron affinity:
The Mulliken scale has a clear physical interpretation: an atom is electronegative if it is both hard to ionize (high ) and eager to gain an electron (large ). Conversion to the Pauling scale is approximately when and are in eV.
Allen scale (1989). Based on the average one-electron energy of the valence-shell electrons:
where and are the numbers of and valence electrons and , are their spectroscopic energies (from Hartree-Fock calculations). The Allen scale is the most directly connected to atomic spectroscopy and avoids the thermodynamic empiricism of the Pauling scale.
Anomalies and fine structure in periodic trends
Half-filled subshell stability. The first ionization energy of nitrogen (1402 kJ/mol) is higher than that of oxygen (1314 kJ/mol), even though oxygen is one column to the right. Nitrogen's configuration has one electron in each orbital — a half-filled subshell with maximum exchange energy. Removing an electron from oxygen means removing a paired electron, which experiences additional electron-electron repulsion. This anomaly repeats for P/S and As/Se in later periods.
d-Block contraction. The atomic radii of Ga, Ge, As, Se, Br are smaller than expected from simple extrapolation because the intervening transition series does not shield the and electrons very effectively. The poor shielding by electrons means for the period-4 -block elements is larger than a naive model predicts. This is why Ga is approximately the same size as Al despite being one period lower.
Lanthanide contraction. The 14 electrons added across the lanthanide series (Ce–Lu) shield very poorly. By the time the and elements are reached, has increased substantially, pulling the outer electrons inward. The result is that period-6 transition metals (Hf, Ta, W, Re, Os, Ir, Pt, Au) have nearly the same atomic radii as their period-5 congeners (Zr, Nb, Mo, Tc, Ru, Rh, Pd, Ag). This has profound chemical consequences: Zr and Hf are so similar in size and chemistry that separating them industrially is difficult, and Pt and Pd have overlapping catalytic properties.
Diagonal relationships. Elements diagonally adjacent in the periodic table (Li/Mg, Be/Al, B/Si) show unexpected similarities in their chemical properties. The diagonal relationship arises because the increase in across a period roughly compensates for the decrease down a group, producing similar charge densities. Lithium and magnesium both form covalent organometallic compounds (Grignard-like behavior), unlike the other Group 1 elements.
Key theorem with proof Intermediate+
Theorem (Ionic radius in an isoelectronic series). Consider a series of ions , all with electrons. The ionic radius is a decreasing function of the nuclear charge : if , then .
Proof. For an -electron ion with nuclear charge , the electronic Hamiltonian (in atomic units) is
By the Feynman-Hellmann theorem, the derivative of the energy with respect to is
Increasing lowers the energy. The virial theorem for Coulomb systems gives , so approximately, and the characteristic orbital radius scales as . For a fixed electron count , increasing increases for every electron, contracting the charge distribution and reducing . This is rigorous for hydrogen-like ions () and remains qualitatively valid for many-electron systems.
Corollary. In the isoelectronic series , , Ne, , , (all 10 electrons), the ionic radius decreases monotonically with increasing .
Exercises Intermediate+
Quantitative periodic-trend models Master
The qualitative trends described above follow from three quantitative inputs: (1) the effective nuclear charge , (2) the principal quantum number of the valence shell, and (3) the subshell type .
Ionization energy scaling. For hydrogen-like ions, . For many-electron atoms, Koopmans' theorem gives , where is the Hartree-Fock energy of the highest occupied orbital. A useful semi-empirical approximation for main-group elements is
where is an effective principal quantum number that accounts for penetration: for , for , for , but for (Slater's values). This formula predicts the correct ordering across periods and groups but fails quantitatively by 10–30% because it neglects electron correlation and the detailed orbital structure.
Atomic radius scaling. For hydrogen-like systems, . For many-electron atoms, the covalent radius scales approximately as
with corrections for subshell type. The electrons penetrate closer to the nucleus than electrons of the same , so -block elements are somewhat smaller than this formula predicts. The -block and -block elements have inner or electrons that shield poorly, making the outer electrons experience a larger than expected — this is the mechanism behind the -block and lanthanide contractions.
Mulliken electronegativity as a bridge. The Mulliken scale connects electronegativity to two directly measurable atomic properties. It reveals that electronegativity is not an independent quantity but a composite: it measures the average tendency of an atom to either retain its own electrons (high ) or acquire additional ones (large ). The Periodic-table trend in follows the trends in both and , which in turn follow from and .
Relativistic contributions to periodic trends Master
For heavy elements, relativistic effects modify the periodic trends in ways that the non-relativistic framework cannot capture. The three principal relativistic corrections — mass-velocity, Darwin, and spin-orbit — affect periodic trends through two mechanisms:
Orbital contraction of and orbitals. The relativistic mass increase for electrons moving near the speed of light in the deep potential well of a heavy nucleus contracts and orbitals. This contraction increases for the outer electrons, raising their ionization energy and electronegativity above the non-relativistic prediction. Gold's ionization energy (890 kJ/mol) is about 200 kJ/mol higher than the non-relativistic estimate, and its Pauling electronegativity (2.54) is unusually high for a Group 11 element (compare Cu at 1.90, Ag at 1.93).
Orbital expansion of and orbitals. The contracted and orbitals shield the and orbitals more effectively, causing them to expand and rise in energy. This indirect destabilization lowers the ionization energy of and electrons and makes them more available for bonding in some cases (e.g., the variable oxidation states of the late transition metals).
Pyykko's 2011 review [Pyykko 2011] provides a comprehensive table of relativistic effects on atomic properties across the periodic table. The key insight: for , relativistic corrections to atomic radii exceed 5%, and for , they dominate the chemical behavior. The non-relativistic periodic table is a good approximation for the first five periods but fails qualitatively for the sixth and seventh.
The inert-pair effect is the most chemically visible consequence. In Tl (), Pb (), and Bi (), the pair is stabilized relativistically, making the lower oxidation state (Tl, Pb, Bi) more stable than the group oxidation state (Tl, Pb, Bi). This is a direct relativistic modification of the ionization-energy trend.
Connections Master
Atomic structure and electron configurations
14.01.01established the electron configurations and that are the mechanistic origin of every periodic trend discussed here. Slater's rules, first introduced in that unit, are the quantitative tool used throughout this unit.Lewis structures and VSEPR
14.02.01uses electronegativity to determine bond polarity, assign partial charges (, ), and predict the most plausible Lewis structure when multiple resonance forms exist. The electronegativity values computed here are inputs to bond-polarity analysis.Hydrogen atom quantum chemistry
14.04.01provides the hydrogen-like orbital energies and radial functions that underpin the and scaling laws used in the quantitative trend models.The Dirac equation
12.11.01is the fundamental equation from which the scalar relativistic corrections and spin-orbit coupling that modify periodic trends in heavy elements derive. The -dependent orbital splitting and the scaling of relativistic corrections originate in the Dirac solution.Inorganic chemistry: periodic trends quantified
16.01.01extends the qualitative trends of this unit to quantitative applications in transition-metal chemistry, including crystal-field stabilization energies, oxidation-state stability diagrams, and Hard-Soft Acid-Base theory.
Historical notes Master
The recognition that elements exhibit recurring properties dates to Mendeleev's 1869 periodic table and earlier work by Dobereiner (triads, 1817) and Newlands (law of octaves, 1865). Mendeleev's table organized elements by atomic weight and predicted the properties of undiscovered elements (Ga, Ge, Sc) with remarkable accuracy. The concept of atomic number () was introduced by Moseley in 1913 using X-ray spectra, correcting several ordering anomalies in Mendeleev's table.
Effective nuclear charge. The concept of shielding was developed by J. C. Slater in 1930 [Slater 1930], who proposed the rules still used in general chemistry. More sophisticated treatments by Clementi and Raimondi (1963) computed from Hartree-Fock wave functions, producing the accurate values used in modern computational chemistry.
Electronegativity scales. Linus Pauling introduced the first electronegativity scale in 1932 as part of The Nature of the Chemical Bond. Robert Mulliken proposed his scale in 1934 [Mulliken 1934], grounding electronegativity in measurable atomic properties. Leland Allen's spectroscopic scale (1989) [Allen 1989] connected electronegativity to orbital energies, providing the most physically transparent definition. All three scales agree qualitatively on the periodic trend but differ in absolute values by scaling factors.
The lanthanide contraction was first recognized by Goldschmidt in 1926 from ionic-radius measurements on rare-earth compounds. Its chemical implications — the near-identity of Zr/Hf, Nb/Ta, and Mo/W chemistries — were elaborated by numerous inorganic chemists through the mid-20th century. The relativistic interpretation of the contraction (that poor shielding by electrons is augmented by relativistic contraction) was developed by Pyykko and Desclaux in the 1970s.
Bibliography Master
- Pauling, L., The Nature of the Chemical Bond, 3e (Cornell, 1960), Ch. 3.
- Mulliken, R. S., "A New Electroaffinity Scale; Together with Data on Valence States and on Valence Ionization Energies and Electron Affinities", J. Chem. Phys. 2 (1934), 782--793.
- Slater, J. C., "Atomic Shielding Constants", Phys. Rev. 36 (1930), 57--64.
- Allen, L. C., "Electronegativity Values for the Electronegativity Scale", J. Am. Chem. Soc. 111 (1989), 9003--9014.
- Clementi, E. & Raimondi, D. L., "Atomic Screening Constants from SCF Functions", J. Chem. Phys. 38 (1963), 2686--2689.
- Pyykko, P., "Relativistic Effects in Chemistry: More Common than You Thought", Annu. Rev. Phys. Chem. 63 (2012), 45--64.
- Pyykko, P., "A Suggested Periodic Table up to Z = 172, Based on Dirac-Fock Calculations", Phys. Chem. Chem. Phys. 13 (2011), 161--168.
- Huheey, J. E., Keiter, E. A. & Keiter, R. L., Inorganic Chemistry, 3e (HarperCollins, 1993), Ch. 2.
- Zumdahl, S. S. & DeCoste, D. J., Chemical Principles, 8e (Cengage, 2017), Ch. 7.
- Atkins, P. & Jones, L., Chemical Principles, 2e (Freeman, 2010), Ch. 1.
- Goldschmidt, V. M., "Geochemische Verteilungsgesetze der Elemente VII: Die Gesetze der Krystallochemie", Skrifter Norske Videnskaps-Akad. Oslo, I. Mat.-Naturv. Kl. (1926).