A century before Thomson's model, John Dalton proposed his atomic theory in the early 1800s, which was groundbreaking at the time. Dalton's theory laid the groundwork for our understanding of chemical reactions and matter. The primary postulates of Dalton's theory can be distilled into four main points:
- All matter is composed of extremely small particles called atoms.
- Atoms of the same element are identical in size, mass, and other properties, but differ from those of other elements.
- Atoms cannot be subdivided, created, or destroyed.
- Atoms of different elements combine in simple whole-number ratios to form chemical compounds.
Dalton's atomic theory treated atoms as solid, indivisible particles, akin to tiny billiard balls. The assumption that atoms were unbreakable and without internal structure is what would have influenced Rutherford's expectations during his alpha particle scattering experiment. The observation of alpha particles being deflected would have shocked Rutherford if he had solely adhered to Dalton's model, as it suggested a structure within the atom and the presence of substantial forces at play.