M. Curie and P. Curie with Becquerel, were awarded the Nobel Prize in Physics for their discovery of Radioactivity, in 1903.
Radioactivity is the phenomenon of spontaneous disintegration, attended by emission of electromagnetic radiations, of heavy atomic nuclei like Uranium, Radium, etc. at a constant rate unaffected by any physical or chemical changes or influences such as temperature, pressure, etc. to which the atom may be subjected. It is a nuclear property of the active element and in all radioactive processes. There are three features of radioactivity from the perspective of classical physics:R = - dN / dt
The minus sign is used to make R a positive quantity since dN / dt is a negative quantity. The SI unit of activity is named after Becquerel:1 becquerel = 1 B q = 1 decay/s
The other unit of activity is Curie(Ci), which is defined as 1 g of radium Ra 88 226 .1 curie = 1 Ci = 3.70 10 10 decay/s = 37 GB q
The most important single source is the radioactive gas radon, a decay product of radium traces back to the decay of uranium. Uranium is found in many common rocks such as granite. Hence radon, colorless or odorless, is present nearly everywhere, usually in small amounts to endanger health. As a cause of lung cancer, radon is second only to cigarette smoking. Other natural sources of radiation dosage include cosmic rays from space and radionuclides present in rocks, soil, and building materials. Food, water, and the human body itself contain small amounts of radionuclides of such elements as potassium and carbon. The activities of radioactive samples show that it falls off exponentially with time. When the period starts, the activity drops to half of what it was at the start of the period. Every radionuclide has a characteristic half-life. Some half-lives are only millions of seconds and some are billions of years. One of the major problems faced by nuclear power plants is the safe disposal of radioactive waste since some nuclides have long half-lives. The time variation of activity follows the formulaR = R 0 e - λ t
Whereλ is a decay constant having a different value for each radionuclide.1/2R 0 = R 0 e -λT 1/2
e - T 1/2 = 2
Taking logs on both sides, λ T 1/2 = ln2T 1/2 = ln2/ = 0.693/ λ
The larger the decay constant, the greater the chance a given nucleus will decay in a certain period of time. If we assume a constant probability per unit of time for the decay of each nucleus of a given nuclide. With the probability per unit time, dt is the probability that any nucleus will undergo decay in a time interval dt. If a sample contains N undecayed nuclei, the number dN that decays in a time dt is the product of the number of nuclei N and the probability dt that each will decay in dt.dN = -N λ dt
Where the minus sign indicates that N decreases as time increases.R = - dN/dt
R = N 0 e - λ t
R = λ N