Atomic structure: protons, neutrons and electrons
TutorAura guide · Updated
An atom has a tiny, dense nucleus containing protons and neutrons, surrounded by electrons in shells. Atoms have no overall charge because they have equal numbers of protons and electrons. Atoms are tiny: their radius is about 0.1 nm ( m), and the nucleus is less than a ten-thousandth of that.
Key takeaways
- Protons: charge +1, mass 1. Neutrons: charge 0, mass 1. Electrons: charge −1, tiny mass.
- Atomic number = protons. Mass number = protons + neutrons.
- Isotopes: same protons, different neutrons.
- Electron shells fill 2, 8, 8 for the first 20 elements.
The three particles
| Particle | Relative charge | Relative mass | Where |
|---|---|---|---|
| Proton | +1 | 1 | Nucleus |
| Neutron | 0 | 1 | Nucleus |
| Electron | −1 | Very small (about 1/2000) | Shells around the nucleus |
Atomic number and mass number
- Atomic number = number of protons (which also equals electrons in an atom).
- Mass number = protons + neutrons.
- Neutrons = mass number − atomic number.
Example: sodium has atomic number 11 and mass number 23, so it has 11 protons, 11 electrons and neutrons.
Isotopes
Isotopes are atoms of the same element with different numbers of neutrons. Carbon-12 has 6 neutrons and carbon-14 has 8; both have 6 protons. Isotopes have the same chemical properties but different masses, and some (like carbon-14) are radioactive. Radioactive decay is measured by half-life.
Electron shells
Electrons fill shells from the inside: up to 2 in the first shell, then 8 in the second and 8 in the third (for the first 20 elements). Sodium (11 electrons) is 2, 8, 1. The number of outer electrons gives the element's group in the periodic table, and the number of shells gives its period. Explore it with our interactive periodic table.
How the model developed
- Dalton (early 1800s): atoms as solid spheres.
- Thomson (1897): discovered the electron; the "plum pudding" model of a ball of positive charge with electrons in it.
- Rutherford (1911): the alpha-scattering experiment showed most of the atom is empty space with a small, dense, positive nucleus.
- Bohr (1913): electrons orbit at fixed distances (shells).
- Chadwick (1932): discovered the neutron.
Each model changed because new evidence didn't fit the old one.
Common mistakes
- Using the mass number as the number of neutrons.
- Saying ions change the number of protons (ions gain or lose electrons).
- Mixing up groups (columns) and periods (rows).
Calculate relative formula masses with our Mr calculator.
Ions
Atoms become ions by gaining or losing electrons, never protons. A sodium atom (2, 8, 1) loses one electron to become Na⁺ (2, 8), with a full outer shell. A chlorine atom (2, 8, 7) gains one electron to become Cl⁻ (2, 8, 8). Metals tend to form positive ions; non-metals form negative ions.
Practice questions
- Chlorine-35 has atomic number 17. How many protons, neutrons and electrons does it have?
- Write the electron arrangement of magnesium (atomic number 12).
- How do chlorine-35 and chlorine-37 differ?
- How many electrons does a magnesium ion, Mg²⁺, have?
Answers: 1. 17 protons, 18 neutrons, 17 electrons. 2. 2, 8, 2. 3. Chlorine-37 has two more neutrons. 4. 10.
Relative atomic mass
Most elements are a mixture of isotopes, so the relative atomic mass on the periodic table is a weighted average. Chlorine is about 75% chlorine-35 and 25% chlorine-37:
That's why chlorine's relative atomic mass isn't a whole number. Use values to work out formula masses with our Mr calculator.
Frequently asked questions
What are the three subatomic particles?
Protons (+1 charge, in the nucleus), neutrons (no charge, in the nucleus) and electrons (−1 charge, in shells).
How do you find the number of neutrons?
Subtract the atomic number from the mass number.
What is an isotope?
An atom of the same element (same number of protons) with a different number of neutrons.
Sources
Keep reading
Interactive periodic table of elements
All 118 elements with atomic masses, electron configurations, groups and properties.
Relative formula mass (Mr) calculator
Mr for any formula, including brackets and water of crystallisation, with a breakdown table.
Half-life and radioactive decay explained
Half-life calculations and graphs, alpha, beta and gamma, nuclear equations and safety.
Ionic vs covalent bonding (and metallic bonding)
How each type of bond forms, dot-and-cross examples, and how structure explains properties.