Radioactivity
Overview
Radioactivity refers to the sudden ejection of particles from an unstable atomic nucleus. This instability arises from an imbalance in the forces holding protons and neutrons together at the center of an atom, leading to excess energy. By ejecting particles with this energy—a process called radioactive decay—the atomic nucleus becomes stabilized. These energetic particles comprise ionizing radiation, which, like gamma rays, X-rays, and high-energy UV light, can break chemical bonds and damage DNA.
The phenomenon was accidentally discovered by Henri Becquerel in 1896, when he noticed that uranium salts emitted radiation. Two years later, Marie and Pierre Curie coined the term "radioactivity" when studying similar radiation-emitting ores. After Ernest Rutherford and Frederick Soddy observed that radioactive thorium changed into radium, they theorized that radioactivity could transform one element into another. By 1903, Rutherford distinguished the three most common types of radioactive decay—alpha, beta, and gamma—and found that radioactive samples decay in a predictable, exponential way based on a value specific to the sample that he called half-life.
Subsequent research revealed the composition of these decay particles, alongside the existence of isotopes, protons, and neutrons. Collectively, these discoveries established the physics behind radiometric dating, nuclear power, and medical diagnostics and treatment, and more.
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