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Alpha decay or α-decay is a type of radioactive decay in which an atomic nucleus emits an alpha particle ... For example, uranium-238 decays to form thorium-234.
Examples of this sort of nuclear transmutation by alpha decay are the decay of uranium to thorium, and that of radium to radon. Alpha particles are commonly emitted by all of the larger radioactive nuclei such as uranium, thorium, actinium, and radium, as well as the transuranic elements. Unlike other types of decay, alpha decay as a process ...
Any decay daughters that are the result of an alpha decay will also result in helium atoms being created. Some radionuclides may have several different paths of decay. For example, 35.94(6) % [27] of bismuth-212 decays, through alpha-emission, to thallium-208 while 64.06(6) % [27] of bismuth-212 decays, through beta-emission, to polonium-212.
For example, the third atom of nihonium-278 synthesised underwent six alpha decays down to mendelevium-254, [2] followed by an electron capture (a form of beta decay) to fermium-254, [2] and then a seventh alpha to californium-250, [2] upon which it would have followed the 4n + 2 chain (radium series) as given in this article.
Beta decay: beta particle is emitted from an atomic nucleus Compton scattering: scattering of a photon by a charged particle Neutrino-less double beta decay: If neutrinos are Majorana fermions (that is, their own antiparticle), Neutrino-less double beta decay is possible. Several experiments are searching for this. Pair production and annihilation
The decay scheme of a radioactive substance is a graphical presentation of all the transitions occurring in a decay, and of their relationships. Examples are shown below. It is useful to think of the decay scheme as placed in a coordinate system, where the vertical axis is energy, increasing from bottom to top, and the horizontal axis is the proton number, increasing from left to right.
One type of natural transmutation observable in the present occurs when certain radioactive elements present in nature spontaneously decay by a process that causes transmutation, such as alpha or beta decay. An example is the natural decay of potassium-40 to argon-40, which forms most of the argon in the air.
Per unit of energy, alpha particles are at least 20 times more effective at cell-damage than gamma rays and X-rays. See relative biological effectiveness for a discussion of this. Examples of highly poisonous alpha-emitters are all isotopes of radium, radon, and polonium, due to the amount of decay that occur in these short half-life materials.