8.1.3: Ionization energy roughly increases towards the upper left of the periodic table but is also influenced by orbital energy and pairing energy effects
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As with electronegativity, the ioniation elenergy of the main group elements (Figure \(\PageIndex{1}\)) decreases down a group and increases from left to right across the periodic table.
Figure \(\PageIndex{1}\). Ionization energies of the elements in kJ/mol. Taken from https://chem.libretexts.org/Courses/Mount_Royal_University/Chem_1201/Unit_2._Periodic_Properties_of_the_Elements/2.09%3A_Ionization_Energy.
As may be seen in Figure \(\PageIndex{1}\) ionization energy does not increase steadily from left to right across a group. Instead there are two discontinuities. These discontinuities are summarized in Figure \(\PageIndex{2}\).
Figure \(\PageIndex{2}\). Discontinuities in the expected decrease in first ionization energy (IE1) trends among the main group elements and their explanation in terms of changing valence subshells and their occupancy. The periodic table of ionization energies in this figure is adapted from from https://chem.libretexts.org/Courses/Mount_Royal_University/Chem_1201/Unit_2._Periodic_Properties_of_the_Elements/2.09%3A_Ionization_Energy. Otherwise this work by Stephen Contakes is licensed under a Creative Commons Attribution 4.0 International License.
Briefly, the two discontinuities are as follows:
- There is a decrease or meager increase in ionization energy that occurs on going from the alkaline earth metals to the boron group, which is caused by the change in the highest occupied orbital from a lower energy ns to a higher energy np subshell.
- There is a decrease or anomalously modest increase in ionization energy on going from the pnictides to the chalcoenides caused by the presence of Coulombic repulsion in the chalcogenide np4 configuration that is not present in the pnictide np3 configuration.
These discontinuities illustrate how orbital energy and electron configuration effects should be considered when considering the reactivity of the elements.
Contributors and Attributions
Stephen Contakes, Westmont College