ViewWiki
ExploreMatter

The world, a little closer

Atoms.

Everything is built from atoms, and one number decides which kind. Add protons one at a time and watch hydrogen become carbon, oxygen, and neon.

Explore the scene Interactive article

01 / The experiment

One proton at a time.

Add protons and watch the element change. Then switch shells to a cloud.

Interactive scene

Preparing your experiment…

The explanation below is available while the scene loads.

Neutral atoms, so electrons always equal protons. Neutron counts follow the most common isotope.Shells and orbits are a simplified model. Sizes and distances are not to scale.

02 / Three particles

Two in the middle, one around the outside.

Same parts in every atom. Different counts.

In the nucleus01
+

Proton

Protons give the nucleus its positive charge. Count them and you have the atomic number: the identity of the element.

Charge
Positive (+1)
Mass
1
Job
Its count decides the element
In the nucleus02
0

Neutron

Neutrons weigh about the same as protons but carry no charge. They hold the nucleus together and set which isotope an atom is.

Charge
None (0)
Mass
1
Job
Adds mass, makes isotopes
In shells around it03

Electron

Electrons are tiny and fast, arranged in shells. The outer shell decides how, and whether, an atom bonds with others.

Charge
Negative (−1)
Mass
1⁄1836
Job
Does the chemistry
The big idea

The number of protons decides which element an atom is. Electrons in the outer shell decide how it behaves.

6 p⁺ = C

Smaller than small

Every solid, liquid and gas is made of atoms, and atoms are astonishingly small. A single drop of water holds more of them than there are stars in the observable universe. Yet each one has the same simple architecture: a dense centre, the nucleus, wrapped in a much larger space where the electrons live.

Three kinds of particle

The nucleus contains protons, which carry a positive charge, and neutrons, which carry none. Almost all of the atom’s mass sits there. Around it move the electrons, negatively charged and nearly two thousand times lighter than a proton. In a neutral atom the number of electrons equals the number of protons, so the charges cancel.

The number of protons is the whole story of which element an atom is. Six protons is carbon, always. Add one and it is nitrogen; take one away and it is boron. Nothing else about the atom changes what it is called. That number is the element’s atomic number.

Shells, and why they matter

Electrons are not scattered at random. They occupy layers called shells, and each shell holds a limited number: two in the first, eight in the second, eight in the third for the elements shown here. Electrons fill the inner shells first.

Try it: choose He, then Ne. Both have a completely full outer shell. Now choose Na, which has exactly one electron beyond a full shell.

Chemistry is mostly the story of that outer shell. Atoms with a full one, like helium and neon, barely react with anything. Atoms with one electron too many, like sodium, or one too few, like chlorine, react eagerly to get to a full shell. That is why the elements in one column of the periodic table behave alike: they have the same number of outer electrons.

Clouds, not orbits

The rings in the scene are a picture, not a photograph. Electrons do not travel on tidy circular tracks. Each one is spread out in a region of space where it is likely to be found, and the shells are really nested regions of that kind. Switch Shells to Cloud to see the same atom drawn that way: a fuzzy layered haze whose brightness shows where the electrons spend their time.

Both pictures are useful. The shell picture counts electrons and predicts chemistry. The cloud picture is closer to how atoms actually behave.

Same element, different weight

Two atoms with the same number of protons can have different numbers of neutrons. They are the same element, with the same chemistry, but different masses. These variants are called isotopes. Most carbon has six neutrons; a small fraction has eight, and that heavier carbon slowly decays, which is what lets scientists date ancient wood and bone.