radioaktivitást
Radioaktivitást is the spontaneous breakdown of unstable atomic nuclei, releasing energy and particles. This process results in the transformation of one element into another. The phenomenon was discovered by Henri Becquerel in 1896 and further studied by Marie and Pierre Curie. Radioactive decay occurs at a characteristic rate for each isotope, known as its half-life, which is the time it takes for half of the radioactive atoms in a sample to decay.
There are three main types of radioactive emissions: alpha particles, beta particles, and gamma rays. Alpha
Radioactivity has numerous applications, including in medicine for diagnostic imaging and cancer treatment, in industry for