What Is First and Second Ionization Energy?

First ionization energy is the energy needed to remove the outermost electron from a neutral atom in the gas phase. Second ionization energy is the energy needed to remove the next electron, this time from the 1+ ion that remains. The second ionization energy is always larger than the first because you’re pulling a negative electron away from an ion that now carries a positive charge.

How First Ionization Energy Works

Picture a neutral atom with equal numbers of protons and electrons. The first ionization energy measures how much energy it takes to strip away the least tightly held electron. For hydrogen, the simplest case, the process looks like this:

H(g) → H⁺(g) + e⁻

The neutral gaseous atom absorbs energy, loses one electron, and becomes a positively charged ion. Every element has a measurable first ionization energy, reported in kilojoules per mole (kJ/mol) or electron volts (eV). A higher number means the atom holds its outermost electron more tightly.

How Second Ionization Energy Works

Once that first electron is gone, the atom is no longer neutral. It’s a 1+ ion. The second ionization energy is the energy required to remove the next outermost electron from that ion. Using sodium as an example:

Na⁺(g) → Na²⁺(g) + e⁻

The key difference is that you’re now pulling a negatively charged electron away from something that already has a net positive charge. That extra positive charge creates a stronger electrostatic pull on every remaining electron, so removing the second one always costs more energy than removing the first. This pattern continues for every successive electron: the third ionization energy is higher than the second, the fourth higher than the third, and so on.

Three Factors That Control Ionization Energy

Distance from the nucleus. The farther an electron sits from the nucleus, the weaker the attraction holding it in place. Larger atoms have lower ionization energies because their outermost electrons are simply farther away from the positive charge at the center.

Nuclear charge. More protons in the nucleus means a stronger pull on every electron. When you compare atoms of similar size, the one with more protons will have a higher ionization energy. This is also why ionization energy jumps after each removal: with one fewer electron, the remaining electrons feel the nuclear charge more strongly.

Shielding. Inner electrons sit between the nucleus and the outer electrons, partially blocking the full positive charge. This is called the shielding effect. The more layers of inner electrons an atom has, the less pull the nucleus exerts on the outermost electron, and the less energy it takes to remove it.

Trends Across the Periodic Table

First ionization energy follows two reliable patterns on the periodic table. Moving left to right across a period (row), ionization energy generally increases. Each step to the right adds a proton to the nucleus without adding a new electron shell, so the effective nuclear charge grows and electrons are held more tightly. Noble gases, sitting at the far right with completely filled outer shells, have some of the highest first ionization energies of any elements in their row.

Moving top to bottom down a group (column), ionization energy decreases. Each row adds a new electron shell, pushing the outermost electrons farther from the nucleus and increasing shielding from inner electrons. Both effects make the outermost electron easier to remove.

Two Notable Exceptions

The left-to-right trend breaks in two predictable spots. First, boron has a lower ionization energy than beryllium, even though boron is one step to the right. The reason: boron’s outermost electron sits in a p orbital, which is higher in energy and more effectively shielded from the nucleus than beryllium’s outermost electron in an s orbital. That p electron is simply easier to pull away.

Second, oxygen has a lower ionization energy than nitrogen, despite being further right. Nitrogen has a half-filled set of p orbitals, with one electron in each. Oxygen has one extra electron that is forced to share an orbital with another electron. The repulsion between those two electrons in the same orbital makes one of them easier to remove. These two exceptions repeat in every period of the table for the same structural reasons.

The Big Jump Between Valence and Core Electrons

Successive ionization energies don’t just increase gradually. They increase steadily while you’re removing electrons from the outermost shell, then spike dramatically when you start pulling electrons from the next shell inward (the core electrons). This jump is enormous because core electrons are much closer to the nucleus, feel far less shielding, and are held far more tightly.

Sodium is a perfect example. It has one valence electron, so its first ionization energy is relatively modest. But removing the second electron means breaking into a fully filled inner shell, and the second ionization energy is roughly ten times larger. For aluminum, which has three valence electrons, the big spike happens at the fourth ionization energy. For silicon, it happens at the fifth.

This pattern is actually useful: by looking at where the largest jump falls in a series of successive ionization energies, you can determine how many valence electrons an element has. The jump always appears right after the last valence electron is removed. It also explains why elements typically only participate in chemical reactions using their valence electrons. Removing core electrons costs so much energy that it essentially never happens in ordinary chemistry.

Why the Difference Matters in Chemistry

The gap between first and second ionization energy helps explain why certain elements form the ions they do. Sodium readily loses one electron to form Na⁺ because its first ionization energy is low and its second is prohibitively high. Magnesium can lose two electrons to form Mg²⁺ because both its first and second ionization energies are manageable, but the third would require breaking into a core shell. These energy thresholds determine the charge an element typically carries in ionic compounds, which in turn shapes the formulas and properties of salts, minerals, and countless other substances.