it must eject the extra nucleons and should be conveted into a stable isotope.
The radioactive isotope is disintegrated in time and emit radiations.
radioactive decay
daughter isotope
When an isotope is stable, it does not undergo radioactive decay. Stable isotopes have a balanced number of protons and neutrons in the nucleus, which prevents them from spontaneously changing into another element over time.
The process where an unstable parent isotope becomes a stable daughter isotope is called radioactive decay. During this process, the parent isotope undergoes a series of transformations, such as alpha or beta decay, emitting particles or energy until it reaches a stable state as a daughter isotope.
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.
Radioactive elements break down in to stable isotopes through nuclear decay. The list of isotopes from a nuclear isotope to a stable isotope is called its decay chain.
The stable isotope produced by radioactive decay is called a daughter isotope.
The radioactive isotope is disintegrated in time and emit radiations.
The radioactive isotope is disintegrated in time and emit radiations.
radioactive decay
daughter isotope
When an isotope is stable, it does not undergo radioactive decay. Stable isotopes have a balanced number of protons and neutrons in the nucleus, which prevents them from spontaneously changing into another element over time.
The process where an unstable parent isotope becomes a stable daughter isotope is called radioactive decay. During this process, the parent isotope undergoes a series of transformations, such as alpha or beta decay, emitting particles or energy until it reaches a stable state as a daughter isotope.
No, it has only one stable isotope.
A stable isotope is an isotope that does not undergo radioactive decay, meaning its nucleus is stable and does not change over time. These isotopes have a constant number of protons and neutrons, making them suitable for use in scientific studies like tracing biological processes or determining the age of rocks. Examples include carbon-12, oxygen-16, and nitrogen-14.
A radioactive element (atom) can decay up to a stable isotope.