There are quite a few - for the answer to this please look in the link I will place below.
Iron-57 is a stable isotope of iron, meaning it does not undergo radioactive decay. It has 26 protons and 31 neutrons, giving it a mass number of 57. Iron-57 is commonly used in Mössbauer spectroscopy to study the properties of iron-containing compounds.
Carbon 12 and Carbon 13 are stable. All other isotopes of carbon are unstable and radioactive
30 neutrons in the most stable isotope of iron (Fe-56).
it must eject the extra nucleons and should be conveted into a stable isotope.
The stable isotope produced by radioactive decay is called a daughter isotope.
26 protons, 26 electrons in iron. Fe-56, the most stable isotope of iron, has 30 neutrons
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.
The most prevalent isotope in an iron sample is iron-56 (Fe-56). It accounts for about 91.7% of naturally occurring iron isotopes. Fe-56 is stable and is commonly found in various iron-containing materials. Other isotopes, such as Fe-54, Fe-57, and Fe-58, are present in much smaller amounts.
The radioactive isotope is disintegrated in time and emit radiations.
The radioactive isotope is disintegrated in time and emit radiations.
daughter isotope
False. When an unstable isotope decays, the resulting daughter isotope may or may not be stable. Some daughter isotopes are stable, while others may still be radioactive and undergo further decay.