Atomic models changed because observations did not fit older explanations. Dalton’s solid-particle model was useful for chemical combination but could not represent internal structure. Evidence for electrons led to a divisible atom. Rutherford-style scattering evidence supported a tiny dense positive nucleus. Later evidence for protons and neutrons refined the nuclear model.
Some nuclei are unstable. In natural radioactive decay, a nucleus changes and releases radiation, producing a different nuclear arrangement that may be more stable. The exact decay time of one nucleus is unpredictable; large samples show statistically predictable behaviour. This lesson does not require quantum orbitals or senior nuclear mathematics.