How do we know what the inside of an atom looks like if we can never see it? The history of atomic physics is a journey of moving from theoretical guesses to experimental certainties. By observing how particles scatter and how light behaves, scientists have transitioned from seeing the atom as a simple "pudding" to understanding it as a complex system of a dense nucleus and discrete energy levels.
The Evolution of Atomic Models
In the late 19th century, after the discovery of the electron, J.J. Thomson proposed the Plum Pudding Model. In this model, the atom was envisioned as a uniform sphere of positive charge, with negatively charged electrons embedded throughout it like raisins in a pudding.
This view was fundamentally challenged in 1911 by Ernest Rutherford through the Geiger-Marsden scattering experiment. Rutherford fired high-energy alpha particles ()—which are doubly positively charged particles emitted by radioactive materials—at an extremely thin sheet of gold leaf.
If the Plum Pudding model were correct, these alpha particles should have passed through the "spread out" positive charge with minimal deflection. However, Rutherford observed that while most particles passed through, some were deflected at massive angles, and a few even bounced straight back.
Rutherford concluded that the atom's positive charge and most of its mass are not spread out, but are concentrated in a tiny, central nucleus.
Subatomic Particles and Isotopes
The modern atom is composed of three primary subatomic particles: protons, neutrons, and electrons.
- Protons: Positively charged particles () located in the nucleus. The number of protons is the proton number (), also known as the atomic number, which defines the identity of the element.
- Neutrons: Neutral particles ($0e$) also located in the nucleus. They add mass to the atom without changing its electrical charge.
- Electrons: Negatively charged particles that orbit the nucleus. In a neutral atom, the number of electrons is exactly equal to the number of protons.
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