The decay of thorium by alpha decay the resultant nuclide is the element radium. The specific nuclide of radium cannot be determined unless we know which specific nuclide of thorium underwent alpha decay.
parent nuclide daughter nuclide + energy
parent nuclide daughter nuclide + energy
Isotopes of uranium, thorium, radium, radon, potassium, tritium, etc.
The decay product of uranium 238 by alpha disintegration (not beta or gamma) is thorium 234.
It is thorium 234.
The formula that best explains how naturally occurring elements like uranium, thorium, and potassium heat the Earth's interior is radioactive decay. These elements undergo radioactive decay, releasing heat energy as a byproduct. This heat contributes to the geothermal gradient and the overall temperature within the Earth's layers.
Common compounds of thorium: thorium dioxide, thorium trifluoride, thorium tetrafluoride, thorium tetrachloride, thorium triiodide, thorium diiodide, thorium tetraiodide, thorium nitrate, thorium oxalate, thorium carbide, thorium sulfides, thorium nitride, thorium oxinate, etc.
In beta decay of thorium-234, a neutron in the nucleus of thorium-234 is transformed into a proton, releasing an electron (beta particle) and an antineutrino. This process converts the thorium-234 nucleus into protactinium-234.
The product of this reaction is Th(NO3)2.
Francium is a naturally occurring radioactive element that is produced as a decay product of uranium and thorium. It is found in tiny amounts in uranium and thorium ores. Francium was first discovered in 1939 by Marguerite Perey in France.
232U alpha decays to 228Th. Thorium-228 is the daughter product of the alpha decay of uranium-232.
The element with a mass number of 216 is thorium (Th), which has an atomic number of 90. Thorium is a radioactive element that can be found in nature and is used in nuclear reactors and as a fertile material for producing nuclear fuel.