Atomic Radius
The atomic radius is defined as a measure of the size of an atom, usually represented in picometers (pm) or angstroms (Å). Estimating the atomic radius, however, poses complications due to the lack of a solid boundary around electrons. Two common methods for measuring atomic size are
- Covalent radius: derived from the distance between two atoms bonded together, with each radius being half the bond distance.
- Metallic radius: obtained from the distance between metallic core atoms in a metallic crystal structure, again halved.
Trends in atomic radius can be observed across periods and down groups in the periodic table.
1. Across a Period: The atomic radius generally decreases because, as you move from left to right across a period, electrons are added to the same energy level while the nuclear charge (number of protons) increases. This increased nuclear charge pulls the electrons closer to the nucleus, resulting in a smaller atomic radius.
2. Down a Group: The atomic radius increases as you go down a group due to the addition of principal energy levels (n), which means valence electrons are further from the nucleus and the inner electrons shield the outer electrons from the nuclear charge.
Key observations and examples are illustrated by comparing atomic radii between groups and periods, such as lithium and sodium, or chlorine and bromine. Understanding atomic radius is foundational to grasping other related properties like ionic radius, ionization enthalpy, and electronegativity, and is crucial for interpreting chemical behavior.