Definition

An atomic mass (often written as m_a) is the mass of a single atom of a particular chemical element. It equals the combined masses of the atom’s constituent subatomic particles: the protons, the neutrons in the nucleus, and the electrons that surround it.

Units and numerical value

While atomic mass can be expressed in everyday units such as grams, individual atoms are extremely light, so chemists and physicists normally use the unified atomic mass unit (symbol: u). By definition, 1 u equals one twelfth of the mass of a carbon-12 atom. In SI terms this is approximately 1.66053906660(50) × 10^-27 kg.

Relation to nucleons and the mass number

Because the protons and neutrons (collectively called nucleons) have masses close to 1 u each and the electrons are much lighter, a simple estimate of an atom’s atomic mass in u is the sum of its proton and neutron counts. That count is the atom’s mass number (symbol: A), which is the total number of protons plus neutrons in the nucleus. The mass number is an integer and has no units; the true atomic mass usually differs slightly from A because of nuclear binding energy and the small contribution of electron masses.

Isotopes and average atomic mass

Many elements exist naturally as mixtures of atoms with different neutron counts; each variant is an isotope. For example, the element chlorine is commonly found as two isotopes, chlorine‑35 and chlorine‑37. Both isotopes have 17 protons, but chlorine‑35 has 18 neutrons while chlorine‑37 has 20. Each isotope has its own specific atomic mass (often called the isotopic mass), roughly equal to its mass number in whole‑number u values.

  • The term mass number refers to the integer count of protons plus neutrons and should not be confused with atomic mass.
  • Relative isotopic mass is a dimensionless quantity different from isotopic mass expressed in u.
  • Relative atomic mass (also called atomic weight) is an average, weighted by natural isotopic abundances, and is not identical to the atomic mass of any single atom.