An isotope of an element has a specific number of neutrons. (Calculated as the mass number minus the atomic number) Most elements have more than one isotope, for example Cl with 17 protons has three naturally occurring isotopes in nature, chlorine-35, with 18 neutrons and chlorine 37 with 20 neutrons along with a trace of chlorine-36 with 19 neutrons.
The radioactive isotope is disintegrated in time and emit radiations.
The process in which one isotope changes to another isotope is called radioactive decay. During this process, the unstable nucleus of an isotope emits radiation in the form of alpha particles, beta particles, or gamma rays to transform into a more stable isotope. The rate at which radioactive decay occurs is measured by the isotope's half-life.
The parent isotope is the original radioactive isotope that undergoes decay to form the daughter isotope. The daughter isotope is the stable isotope that is formed as a result of the radioactive decay of the parent isotope.
it must eject the extra nucleons and should be conveted into a stable isotope.
When an isotope is unstable, it is said to be radioactive.
The number of neutrons and protons together constitutes the mass number of a single isotope of an element.
If you take one day equal to 24 hours, then 1 day constitutes 2 Half lives. Mass of isotope left after 12 hours=10/2=5g Mass of isotope left after 2 half lives or 1 day=5/2=2.5g.
The stable isotope formed by the breakdown of a radioactive isotope is called a daughter isotope. This process is known as radioactive decay, where a radioactive isotope transforms into a stable daughter isotope through the emission of particles or energy.
isotope
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It is called an isotope.
The most common isotope of silicon is the isotope 28Si: 92,23 %.
The radioactive isotope is disintegrated in time and emit radiations.
The radioactive isotope is disintegrated in time and emit radiations.
The process in which one isotope changes to another isotope is called radioactive decay. During this process, the unstable nucleus of an isotope emits radiation in the form of alpha particles, beta particles, or gamma rays to transform into a more stable isotope. The rate at which radioactive decay occurs is measured by the isotope's half-life.
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The parent isotope is the original radioactive isotope that undergoes decay to form the daughter isotope. The daughter isotope is the stable isotope that is formed as a result of the radioactive decay of the parent isotope.